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<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Mar. Sci.</journal-id>
<journal-title>Frontiers in Marine Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Mar. Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-7745</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.3389/fmars.2016.00260</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Marine Science</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Light Intensity Modulates the Response of Two Antarctic Diatom Species to Ocean Acidification</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name><surname>Heiden</surname> <given-names>Jasmin P.</given-names></name>
<xref ref-type="aff" rid="aff1"><sup>1</sup></xref>
<xref ref-type="aff" rid="aff2"><sup>2</sup></xref>
<xref ref-type="author-notes" rid="fn001"><sup>&#x0002A;</sup></xref>
<uri xlink:href="http://loop.frontiersin.org/people/379908/overview"/>
</contrib>
<contrib contrib-type="author">
<name><surname>Bischof</surname> <given-names>Kai</given-names></name>
<xref ref-type="aff" rid="aff2"><sup>2</sup></xref>
</contrib>
<contrib contrib-type="author">
<name><surname>Trimborn</surname> <given-names>Scarlett</given-names></name>
<xref ref-type="aff" rid="aff1"><sup>1</sup></xref>
<xref ref-type="aff" rid="aff2"><sup>2</sup></xref>
<uri xlink:href="http://loop.frontiersin.org/people/137802/overview"/>
</contrib>
</contrib-group>
<aff id="aff1"><sup>1</sup><institution>EcoTrace, Biogeosciences Department, Alfred Wegener Institute for Polar and Marine Research</institution> <country>Bremerhaven, Germany</country></aff>
<aff id="aff2"><sup>2</sup><institution>Faculty 02: Biology/Chemistry, Marine Botany, University of Bremen</institution> <country>Bremen, Germany</country></aff>
<author-notes>
<fn fn-type="edited-by"><p>Edited by: Susana Agusti, King Abdullah University of Science and Technology, Saudi Arabia</p></fn>
<fn fn-type="edited-by"><p>Reviewed by: Pedro Echeveste, Pontifical Catholic University of Chile, Chile; Peng Jin, King Abdullah University of Science and Technology, Saudi Arabia</p></fn>
<fn fn-type="corresp" id="fn001"><p>&#x0002A;Correspondence: Jasmin P. Heiden <email>jasmin.heiden&#x00040;awi.de</email></p></fn>
<fn fn-type="other" id="fn002"><p>This article was submitted to Global Change and the Future Ocean, a section of the journal Frontiers in Marine Science</p></fn></author-notes>
<pub-date pub-type="epub">
<day>15</day>
<month>12</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="collection">
<year>2016</year>
</pub-date>
<volume>3</volume>
<elocation-id>260</elocation-id>
<history>
<date date-type="received">
<day>24</day>
<month>09</month>
<year>2016</year>
</date>
<date date-type="accepted">
<day>25</day>
<month>11</month>
<year>2016</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#x000A9; 2016 Heiden, Bischof and Trimborn.</copyright-statement>
<copyright-year>2016</copyright-year>
<copyright-holder>Heiden, Bischof and Trimborn</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/"><p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p></license>
</permissions>
<abstract><p>It is largely unknown how rising atmospheric CO<sub>2</sub> concentrations and changes in the upper mixed layer depth, with its subsequent effects on light availability will affect phytoplankton physiology in the Southern Ocean. Linking seasonal variations in the availability of CO<sub>2</sub> and light to abundances and physiological traits of key phytoplankton species could aid to understand their abilities to acclimate to predicted future climatic conditions. To investigate the combined effects of CO<sub>2</sub> and light on two ecologically relevant Antarctic diatoms (<italic>Fragilariopsis curta</italic> and <italic>Odontella weisflogii</italic>) a matrix of three light intensities (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and three pCO<sub>2</sub> levels (low &#x0003D; 180, ambient &#x0003D; 380, high &#x0003D; 1000 &#x003BC;atm) was applied assessing their effects on growth, particulate organic carbon (POC) fixation and photophysiology. Under ambient pCO<sub>2</sub>, POC production rates were highest already at low light in <italic>Fragilariopsis</italic>, indicating saturation of photosynthesis, while in <italic>Odontella</italic> highest rates were only reached at medium irradiances. In both species ocean acidification did not stimulate, but rather inhibited, growth and POC production under low and medium light. This effect was, however, amended under high growth irradiances. Low pCO<sub>2</sub> levels inhibited growth and POC production in both species at low and medium light, and further decreased absolute electron transport rates under high light. Our results suggest that Southern Ocean diatoms were sensitive to changes in pCO<sub>2</sub>, showing species-specific responses, which were further modulated by light intensity. The two diatom species represent distinct ecotypes and revealed discrete physiological traits that matched their seasonal occurrence with the related physical conditions in Antarctic coastal waters.</p></abstract>
<kwd-group>
<kwd>Southern Ocean</kwd>
<kwd>photophysiology</kwd>
<kwd>growth</kwd>
<kwd>carbon fixation</kwd>
<kwd>season</kwd>
<kwd>phytoplankton</kwd>
<kwd>CO<sub>2</sub></kwd>
<kwd>climate change</kwd>
</kwd-group>
<counts>
<fig-count count="4"/>
<table-count count="4"/>
<equation-count count="5"/>
<ref-count count="88"/>
<page-count count="17"/>
<word-count count="12608"/>
</counts>
</article-meta>
</front>
<body>
<sec sec-type="intro" id="s1">
<title>Introduction</title>
<p>Concentrations of atmospheric carbon dioxide (CO<sub>2</sub>) are predicted to rise from 400 &#x003BC;atm today to over 750 &#x003BC;atm by the end of this century affecting carbonate chemistry in ocean surface waters by increasing dissolved inorganic carbon availability and decreasing pH (IPCC, <xref ref-type="bibr" rid="B35">2014</xref>). This will potentially affect the physiology and ecology of primary producers (Tortell et al., <xref ref-type="bibr" rid="B79">2008</xref>; Trimborn et al., <xref ref-type="bibr" rid="B80">2013</xref>, <xref ref-type="bibr" rid="B81">2014</xref>). Elevated concentrations of CO<sub>2</sub> in surface waters can be beneficial to phytoplankton, because at present-day the amount of aqueous CO<sub>2</sub> accounts for &#x0007E;1% within the total inorganic carbon pool (Zeebe and Wolf-Gladrow, <xref ref-type="bibr" rid="B88">2001</xref>). As the enzyme Ribulose-1,5- bisphosphate carboxylase&#x02013;oxygenase (RubisCO) requires CO<sub>2</sub> as substrate for the production of particulate organic carbon (POC) during photosynthesis, most phytoplankton, including several Southern Ocean (SO) species, operate so-called carbon concentrating mechanisms (CCMs) (Reinfelder, <xref ref-type="bibr" rid="B66">2011</xref>; Trimborn et al., <xref ref-type="bibr" rid="B80">2013</xref>). CCMs are energetically costly as they include active transport of CO<sub>2</sub> and bicarbonate (<inline-formula><mml:math id="M1"><mml:mrow><mml:msubsup><mml:mtext>HCO</mml:mtext><mml:mn>3</mml:mn><mml:mo>&#x02212;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>) across cell membranes, operation of the enzyme carbonic anhydrase (CA, interconverting CO<sub>2</sub> and <inline-formula><mml:math id="M2"><mml:mrow><mml:msubsup><mml:mtext>HCO</mml:mtext><mml:mn>3</mml:mn><mml:mo>&#x02212;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>) and prevention of diffusive CO<sub>2</sub> efflux (Raven and Johnston, <xref ref-type="bibr" rid="B64">1991</xref>; Hopkinson et al., <xref ref-type="bibr" rid="B31">2011</xref>). Increasing pCO<sub>2</sub> in surface waters will lead to an increase in the fraction of aqueous CO<sub>2</sub> available to phytoplankton, allowing cells to potentially down-regulate their CCMs, which can save up to &#x0007E;20% of CCM-related energy expenditures (Hopkinson et al., <xref ref-type="bibr" rid="B31">2011</xref>; Reinfelder, <xref ref-type="bibr" rid="B66">2011</xref>). Down-regulation of CCMs is expected to promote growth through energy savings especially under limiting conditions such as light- or iron-limitation (Hopkinson et al., <xref ref-type="bibr" rid="B31">2011</xref>). Increased CO<sub>2</sub> concentrations have been shown to influence Southern Ocean phytoplankton growth and community composition (Tortell et al., <xref ref-type="bibr" rid="B79">2008</xref>; Feng et al., <xref ref-type="bibr" rid="B19">2010</xref>; Hoppe et al., <xref ref-type="bibr" rid="B32">2013</xref>). Laboratory studies on Antarctic phytoplankton species, however, did not find stimulating effects by elevated pCO<sub>2</sub> on growth (Boelen et al., <xref ref-type="bibr" rid="B7">2011</xref>; Hoppe et al., <xref ref-type="bibr" rid="B33">2015</xref>).</p>
<p>Alongside elevated atmospheric CO<sub>2</sub> concentrations, sea surface temperatures are on the rise, thus influencing water column stratification. The expected outcome is a shallower upper-mixed layer (UML), in which phytoplankton cells become exposed to higher mean light intensities (Boyd et al., <xref ref-type="bibr" rid="B9">2015b</xref>). As major parts of the Southern Ocean are generally assumed to be light limited, these changes could be beneficial for phytoplankton species (Mitchell and Brody, <xref ref-type="bibr" rid="B49">1991</xref>; Mitchell and Holm-Hansen, <xref ref-type="bibr" rid="B50">1991</xref>; Nelson and Smith, <xref ref-type="bibr" rid="B54">1991</xref>). Yet, increased westerly winds (predicted trends for the Southern Annular Mode) could lead to opposite effects, causing a deepening of the UML (Hauck et al., <xref ref-type="bibr" rid="B27">2015</xref>) thereby decreasing light availability to phytoplankton and thus creating an unfavorable environment.</p>
<p>The amount of available light is substantial for phytoplankton growth and photosynthesis. Light limiting conditions can be stressful for phytoplankton species as light-harvesting has to become more efficient in order to sustain electron transport between photosystems (MacIntyre et al., <xref ref-type="bibr" rid="B45">2002</xref>; Dubinsky and Stambler, <xref ref-type="bibr" rid="B16">2009</xref>) and thereby generation of energy equivalents necessary for carbon fixation in the Calvin-Benson-Cycle (Falkowski and Raven, <xref ref-type="bibr" rid="B18">2007</xref>). If the generation of energy equivalents and carbon fixation through photosynthesis gets restricted by a deficit in excitation energy capture, the energy demands within the phytoplankton cell cannot be met, leading to reduced metabolic rates (Shi et al., <xref ref-type="bibr" rid="B73">2015</xref>).</p>
<p>Oversaturating light intensities on the other hand can lead to photoinactivation of photosystem II (PSII) reaction centers and, when not fully counteracted by repair mechanisms, can cause photoinhibition and cell damage (Murata et al., <xref ref-type="bibr" rid="B53">2007</xref>; Raven, <xref ref-type="bibr" rid="B62">2011</xref>). Therefore, most phytoplankton species possess various dissipation pathways such as non-photochemical quenching (NPQ). The NPQ involves pigment de-epoxidation that can be induced within seconds upon changes in light intensity (Krause and Weis, <xref ref-type="bibr" rid="B39">1991</xref>; M&#x000FC;ller et al., <xref ref-type="bibr" rid="B52">2001</xref>). Antarctic diatoms rely on the xanthophyll cycle for photoprotection (Kropuenske et al., <xref ref-type="bibr" rid="B41">2009</xref>; Arrigo et al., <xref ref-type="bibr" rid="B3">2010</xref>; Mills et al., <xref ref-type="bibr" rid="B48">2010</xref>) involving the pigment diadinoxanthin (DD), which can be de-epoxidised to diatoxanthin (DT), thereby dissipating excess energy captured by light-harvesting pigments (reviewed in Goss and Lepetit, <xref ref-type="bibr" rid="B25">2014</xref>). The adjustment of the functional absorption cross section of PSII (&#x003C3;<sub>PSII</sub>) rather than the number of photosynthetic units per cell is considered to act as an important photoacclimation strategy particularly in polar diatoms (Kropuenske et al., <xref ref-type="bibr" rid="B41">2009</xref>, <xref ref-type="bibr" rid="B40">2010</xref>; Strzepek et al., <xref ref-type="bibr" rid="B75">2012</xref>). Photoacclimation strategies of polar phytoplankton could be related to species-specific occurrences during the season, as changes in vertical mixing with its effects on light availability influence the seasonal succession of phytoplankton species (Mitchell and Holm-Hansen, <xref ref-type="bibr" rid="B50">1991</xref>; Garibotti et al., <xref ref-type="bibr" rid="B21">2005</xref>).</p>
<p>Next to light availability, also the partial pressure of CO<sub>2</sub> (pCO<sub>2</sub>) of Antarctic coastal waters substantially varies over the season with reported values from 190 to 560 &#x003BC;atm (Kapsenberg et al., <xref ref-type="bibr" rid="B37">2015</xref>). During winter time, sea ice prevents gas exchange between ocean surface waters and the atmosphere, causing the pCO<sub>2</sub> to exceed atmospheric levels after sea-ice retreat in spring (Sweeney, <xref ref-type="bibr" rid="B78">2003</xref>; Arrigo et al., <xref ref-type="bibr" rid="B4">2008</xref>). While in spring the UML is deep and phytoplankton needs to cope with light-limiting conditions, during summer the increasing surface warming creates a stable and shallow upper water body with high irradiances (Mitchell and Holm-Hansen, <xref ref-type="bibr" rid="B50">1991</xref>; Nelson and Smith, <xref ref-type="bibr" rid="B54">1991</xref>). Solar irradiances increase during the season promoting phytoplankton blooms. Through high rates of photosynthetic carbon fixation, especially towards the end of the bloom, pCO<sub>2</sub> can be drawn down to or even below pre-industrial values in Antarctic surface waters (Sweeney, <xref ref-type="bibr" rid="B78">2003</xref>; Arrigo et al., <xref ref-type="bibr" rid="B4">2008</xref>; Kapsenberg et al., <xref ref-type="bibr" rid="B37">2015</xref>). Thus light and pCO<sub>2</sub> are important factors influencing phytoplankton in Antarctic coastal waters, which unlike the open waters of the Southern Ocean display high iron concentrations and thus exhibit regular and extensive bloom events over the season (Holm-Hansen et al., <xref ref-type="bibr" rid="B29">1989</xref>; Martin et al., <xref ref-type="bibr" rid="B46">1990</xref>; Pr&#x000E9;zelin et al., <xref ref-type="bibr" rid="B60">2000</xref>; Garibotti et al., <xref ref-type="bibr" rid="B22">2003</xref>; de Jong et al., <xref ref-type="bibr" rid="B14">2012</xref>). The frequent occurrence of pronounced blooms in coastal waters and their immense productivity make them very important for the global carbon cycle and thus important to study (Comiso et al., <xref ref-type="bibr" rid="B13">1993</xref>; Arrigo et al., <xref ref-type="bibr" rid="B4">2008</xref>).</p>
<p>At present it is largely unknown what the combined effects of pCO<sub>2</sub> and light on Southern Ocean phytoplankton physiology are. For various temperate phytoplankton species, elevated CO<sub>2</sub> concentrations in combination with low light were found to stimulate growth and carbon fixation, while the combination with high light showed reduced primary production and increased light stress in a natural phytoplankton community from the South China Sea (Gao et al., <xref ref-type="bibr" rid="B20">2012</xref>). Whether similar responses can be expected for Southern Ocean phytoplankton species remains yet unclear. Studies on the combined effects of light and pCO<sub>2</sub> on Antarctic phytoplankton are sparse and results are diverging. The diatom <italic>Proboscia alata</italic> showed elevated particulate organic carbon content with increasing pCO<sub>2</sub> when combined with a high constant irradiance, whereas the opposite was true for low light conditions (Hoogstraten et al., <xref ref-type="bibr" rid="B30">2012</xref>). For the Antarctic diatom <italic>Chaetoceros brevis</italic>, growth remained unaffected by pCO<sub>2</sub> irrespective of the dynamic light regime applied (Boelen et al., <xref ref-type="bibr" rid="B7">2011</xref>). Yet, in the diatom <italic>C. debilis</italic>, under dynamic light, elevated pCO<sub>2</sub> decreased primary production (Hoppe et al., <xref ref-type="bibr" rid="B33">2015</xref>). Experiments on multiple stressors including not only pCO<sub>2</sub> and light, but also temperature, nutrients and iron, found that light increased growth, when nutrients were not limiting, while pCO<sub>2</sub> did not have any effect (Xu et al., <xref ref-type="bibr" rid="B86">2014</xref>; Boyd et al., <xref ref-type="bibr" rid="B8">2015a</xref>). There are great differences in the definition of high and potentially stressful irradiances that are used in studies investigating effects of constant irradiances in temperate and Antarctic phytoplankton species (125 to 380 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>; Kropuenske et al., <xref ref-type="bibr" rid="B40">2010</xref>; Mills et al., <xref ref-type="bibr" rid="B48">2010</xref>; Norici et al., <xref ref-type="bibr" rid="B55">2011</xref>; Hoogstraten et al., <xref ref-type="bibr" rid="B30">2012</xref>). However, applied irradiances often are below the extremes that phytoplankton cells can encounter in shallow mixed coastal waters with reported values of integrated daily mean irradiances ranging between 77 and 740 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup> under constant light in a 16:8 light:dark cycle (Lancelot et al., <xref ref-type="bibr" rid="B42">1993</xref>; Moline and Pr&#x000E9;zelin, <xref ref-type="bibr" rid="B51">1996</xref>; Venables et al., <xref ref-type="bibr" rid="B83">2013</xref>). Studies on fluctuating light regimes applied higher irradiances which reach levels between 250 and 1200 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>. Yet, exposure to these high irradiances occured for short and repeated periods (Kropuenske et al., <xref ref-type="bibr" rid="B41">2009</xref>; Mills et al., <xref ref-type="bibr" rid="B48">2010</xref>; Boelen et al., <xref ref-type="bibr" rid="B7">2011</xref>; Xu et al., <xref ref-type="bibr" rid="B86">2014</xref>; Boyd et al., <xref ref-type="bibr" rid="B8">2015a</xref>; Hoppe et al., <xref ref-type="bibr" rid="B33">2015</xref>). In a future ocean, the mixed layer depth of Antarctic coastal waters may decrease potentially implying higher integrated daily irradiances including longer periods of light exposure that phytoplankton encounter (Boyd et al., <xref ref-type="bibr" rid="B9">2015b</xref>). Therefore, it is important to study also the effects of exposure to very high and persisting light conditions on phytoplankton physiology.</p>
<p>This study aims to investigate the interactive effects of pCO<sub>2</sub> and light availability on two Antarctic bloom-forming species typically occurring within spring (<italic>Fragilariopsis curta</italic>) and summer (<italic>Odontella weisflogii</italic>) in iron replete Antarctic coastal waters (Martin et al., <xref ref-type="bibr" rid="B46">1990</xref>; Garibotti et al., <xref ref-type="bibr" rid="B21">2005</xref>; Annett et al., <xref ref-type="bibr" rid="B2">2010</xref>; de Jong et al., <xref ref-type="bibr" rid="B14">2012</xref>). To better understand their physiological responses under different light and CO<sub>2</sub> scenarios a matrix of three pCO<sub>2</sub> conditions (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) was applied in order to span the range of late-bloom to future ocean acidification (OA) conditions. These were combined with light conditions chosen to represent low, medium and high irradiances (LL &#x0003D; 20, ML &#x0003D; 200 and HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>, respectively). The physiological responses of both species were studied on growth, carbon fixation, pigment content and photophysiology. We aimed to investigate whether increased pCO<sub>2</sub> levels, at limiting light conditions, may promote growth and productivity due to lowered energy expenditures for CCM operation. Also we tested whether high pCO<sub>2</sub> in conjunction with high light availability may synergistically trigger light stress. This study further tried to link the seasonal occurrence of the two phytoplankton species with respect to their physiological characteristics.</p>
</sec>
<sec sec-type="materials and methods" id="s2">
<title>Materials and methods</title>
<sec>
<title>Culture conditions</title>
<p>Semi-continuous cultures of the two diatom species <italic>Fragilariopsis curta</italic> (isolated from the Weddell Sea by Thomas Mock during ANT XVI/3 in 1999) and <italic>Odontella weisflogii</italic> (isolated in the Atlantic sector of the Southern Ocean by Bank Beszteri during ANT-XXIX/5, 2013) were grown at 4&#x000B0;C in sterile-filtered (0.2 &#x003BC;m) unbuffered natural Antarctic seawater (30.2) enriched with silicate, trace metals and vitamins according to F/2 medium (Guillard and Ryther, <xref ref-type="bibr" rid="B26">1962</xref>). Nitrate and phosphate were added in concentrations reflecting the Redfield N:P ratio of 16:1, 100 and 6.25 &#x003BC;mol L<sup>&#x02212;1</sup> respectively (Redfield, <xref ref-type="bibr" rid="B65">1958</xref>).</p>
<p>Based on photosynthesis-irradiance-curves (PE-curves) with both species acclimated to ambient pCO<sub>2</sub> and 150 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup> light treatments were chosen. Both species were grown in triplicates under low, medium and high light (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) conditions at a 16:8 h light:dark light cycle using light-emitting diodes (LED) lamps (SolarStinger LED SunStrip Marine Daylight, Econlux). The three light treatments were further continuously bubbled through a frit with humidified air of the three CO<sub>2</sub> partial pressures (pCO<sub>2</sub>) of 180, 380, and 1000 &#x003BC;atm (low, ambient and high pCO<sub>2</sub>). A gas flow controller (CGM 2000, MCZ Umwelttechnik) was used to generate the CO<sub>2</sub> gas mixtures from CO<sub>2</sub>-free air (&#x0003C;1 ppmv CO<sub>2</sub>, Nitrox CO2 RP280, Domnick Hunter ltd.) and pure CO<sub>2</sub> (Air Liquide Deutschland ltd., Germany). Triplicates of both species were exposed to all light and pCO<sub>2</sub> treatment combinations. All replicates of one experimental treatments were run in parallel.</p>
<p>For each light treatment chlorophyll <italic>a</italic> (Chl <italic>a</italic>) fluorescence was calibrated against cell number and pH, allowing us to monitor the status of the culture using fluorescence alone. Cultures were grown in 1 L glass bottles (custom made), kept in exponential phase and harvested at cell densities of 224,000 &#x000B1; 97,000 and 732 &#x000B1; 170 cells per mL for the small <italic>Fragilariopsis</italic> (&#x0007E;5 &#x003BC;m) and the much larger <italic>Odontella</italic> (&#x0003E;50 &#x003BC;m) respectively to prevent drift of carbonate chemistry.</p>
<p>Only during the pre-acclimation phase to all experimental conditions of at least 10 days, cultures were diluted two to three times using pre-equilibrated medium. During the main experiment, cells grew for 3.8 &#x000B1; 1.7 days until all parameters were sampled.</p>
</sec>
<sec>
<title>Carbonate chemistry</title>
<p>The pH was measured every other day and at the final sampling day using a pH-ion meter (pH-Meter 827, Metrohm), calibrated (3 point calibration) with National Institute of Standards and Technology-certified buffer systems. The pH remained constant at 8.39 &#x000B1; 0.03, 8.02 &#x000B1; 0.03, and 7.76 &#x000B1; 0.02 for the low, ambient and high pCO<sub>2</sub> treatments respectively (Table <xref ref-type="table" rid="T1">1</xref>). Total Alkalinity (TA) was measured by duplicate potentiometric titrations (TW alpha plus, SI Analytics, Brewer et al., <xref ref-type="bibr" rid="B10">1986</xref>) of filtrated samples (Whatman GF/F glass fiber filters, &#x0007E; 0.6 mm), having been stored at 4&#x000B0;C in 150 mL borosilicate bottles until analysis. Certified reference material (CRMs provided by Prof. A. Dickson, Scripps, USA; batch no. 111; reproducibility &#x000B1;13 &#x003BC;mol kg<sup>&#x02212;1</sup>) was used to correct TA for systematic errors. Dissolved inorganic carbon (DIC) samples were sterile-filtered (0.2 &#x003BC;m) and stored at 4&#x000B0;C in 5 mL gas-tight borosilicate bottles without headspace until analysis. DIC was measured colourimetrically in duplicates with a QuAAtro autoanalyzer (Seal Analytical, Stoll et al., <xref ref-type="bibr" rid="B74">2001</xref>). The analyzer was calibrated with NaHCO<sub>3</sub> solutions (salinity of 35, achieved by NaCl addition) with concentrations ranging between 1800 and 2300 mmol DIC kg<sup>&#x02212;1</sup>. Certified reference materials (reproducibility &#x000B1; 8 &#x003BC;mol kg<sup>&#x02212;1</sup>) were used to correct for errors in instrument performance such as baseline drifts. The carbonate system was calculated based on TA, pH, silicate, phosphate, temperature and salinity using the CO2Sys program (results shown in Table <xref ref-type="table" rid="T1">1</xref>, Pierrot et al., <xref ref-type="bibr" rid="B59">2006</xref>) choosing the equilibrium constant of Mehrbach et al. (<xref ref-type="bibr" rid="B47">1973</xref>) refitted by Dickson and Millero (<xref ref-type="bibr" rid="B15">1987</xref>).</p>
<table-wrap position="float" id="T1">
<label>Table 1</label>
<caption><p><bold>Dissolved inorganic carbon concentrations (DIC) and partial pressure of CO<sub>2</sub> (pCO<sub>2</sub>) were calculated from total alkalinity (TA), pH, silicate, phosphate, temperature, and salinity using the CO2Sys program (Pierrot et al., <xref ref-type="bibr" rid="B59">2006</xref>)</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th valign="top" align="left"><bold>Target P<sub><italic>CO</italic>2</sub> (&#x003BC;atm)</bold></th>
<th valign="top" align="center"><bold>P<sub><italic>CO</italic>2</sub> (&#x003BC;atm)</bold></th>
<th valign="top" align="center"><bold>DIC (&#x003BC;mol kg<sup>&#x02212;1</sup>)</bold></th>
<th valign="top" align="center"><bold>TA (&#x003BC;mol kg<sup>&#x02212;1</sup>)</bold></th>
<th valign="top" align="center"><bold>pH (NBS)</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Low, 180</td>
<td valign="top" align="center">192 &#x000B1; 18</td>
<td valign="top" align="center">1966 &#x000B1; 58</td>
<td valign="top" align="center">2001 &#x000B1; 45</td>
<td valign="top" align="center">8.39 &#x000B1; 0.03</td>
</tr>
<tr>
<td valign="top" align="left">Ambient, 380</td>
<td valign="top" align="center">384 &#x000B1; 27</td>
<td valign="top" align="center">2082 &#x000B1; 28</td>
<td valign="top" align="center">2154 &#x000B1; 17</td>
<td valign="top" align="center">8.02 &#x000B1; 0.03</td>
</tr>
<tr>
<td valign="top" align="left">High, 1000</td>
<td valign="top" align="center">1003 &#x000B1; 58</td>
<td valign="top" align="center">2137 &#x000B1; 37</td>
<td valign="top" align="center">2017 &#x000B1; 37</td>
<td valign="top" align="center">7.76 &#x000B1; 0.02</td>
</tr>
</tbody>
</table>
</table-wrap></sec>
<sec>
<title>Growth</title>
<p>Samples for cell counts of every treatment were fixed with acid Lugol&#x00027;s solution (10% final concentration) and stored at 3&#x000B0;C in the dark until analysis. Cells were counted on an inverted light microscope (Axio Observer.D1; Zeiss) after sedimentation for 24 h in 10 mL Uterm&#x000F6;hl chambers (Hydro-Bios). Growth rates were determined from samples taken right after at the beginning of the experiment (N<sub>0</sub>) and at the day of sampling (N<sub>fin</sub>) and for each sample &#x0003E;400 cells were counted. Cell specific growth rate (&#x003BC;, day<sup>&#x02212;1</sup>) was calculated as</p>
<disp-formula id="E1"><label>(1)</label><mml:math id="M3"><mml:mtable class="eqnarray" columnalign="right center left"><mml:mtr><mml:mtd><mml:mi>&#x003BC;</mml:mi><mml:mo>=</mml:mo><mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mrow><mml:mtext>ln&#x000A0;</mml:mtext><mml:msub><mml:mrow><mml:mtext>N</mml:mtext></mml:mrow><mml:mrow><mml:mtext>fin</mml:mtext></mml:mrow></mml:msub><mml:mo>-</mml:mo><mml:mtext>ln&#x000A0;</mml:mtext><mml:msub><mml:mrow><mml:mtext>N</mml:mtext></mml:mrow><mml:mrow><mml:mn>0</mml:mn></mml:mrow></mml:msub></mml:mrow><mml:mo stretchy="false">)</mml:mo></mml:mrow><mml:mo>/</mml:mo><mml:mi>&#x00394;</mml:mi><mml:mtext>t</mml:mtext></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
<p>where &#x00394;t is the incubation duration in days.</p>
</sec>
<sec>
<title>Particulate organic carbon and particulate organic nitrogen</title>
<p>Particulate organic carbon (POC) and nitrogen (PON) were determined from gently filtered (&#x0003C;20 mmHg) subsamples of each treatment using pre-combusted GF/F filters (15h, 200&#x000B0;C; Whatman). Samples were stored at &#x02212;20&#x000B0;C and defrosted prior to analysis (&#x0003E;12 h, 60&#x000B0;C), acidified with 0.1 mol HCl L<sup>&#x02212;1</sup> and dried over night at 60&#x000B0;C. Samples were analyzed using an elemental analyzer (EURO EA Elemental Analyzer, Euro Vector). Contents of POC and PON were corrected using blank measurements and normalized to filtered volume and cell densities to yield cell quotas. Production rates of POC and PON, were calculated by multiplication of the cellular quota with the specific growth rate of the respective treatment.</p>
</sec>
<sec>
<title>Pigments</title>
<p>Pigment concentrations of chlorophyll <italic>a</italic>, chlorophyll c2, fucoxanthin, diadino- and diatoxanthin were determined using High-Performance-Liquid-Chromatography (HPLC). Samples were gently filtered onto GF/F (Whatman) filters, immediately frozen and stored at &#x02212;80&#x000B0;C for later analysis. Pigments were extracted in 90:10 acetone:water for 24 h at 4&#x000B0;C in the dark and filtered (4 mm nylon syringe filters, 0.45 &#x003BC;m pore size, NalgeneC; Labware) prior to analysis. Analyses were performed on a LaChromElite&#x000AE; system consisting of a chilled autosampler L-2200, a DAD detector L-2450 (VWR-Hitachi International GmbH) and a Spherisorb ODS-2 column (25 cm &#x000D7; 4.6 mm, 5 &#x003BC;m particle size; Waters). The system used a LiChrospher&#x000AE; 100 RP-18 guard cartridge for pigment separation applying a gradient following Wright et al. (<xref ref-type="bibr" rid="B84">1991</xref>) detecting peaks at 440 nm which were identified and quantified via co-chromatography of pigment standards obtained from DHI Lab Products (ORT, Denmark) using the software EZChrom Elite ver. 3.1.3.</p>
<p>From concentrations of diadinoxanthin (DD) and its de-epoxidised equivalent diatoxanthin (DT) the de-epoxidation state (DES) was calculated according to</p>
<disp-formula id="E2"><label>(2)</label><mml:math id="M4"><mml:mtable class="eqnarray" columnalign="right center left"><mml:mtr><mml:mtd><mml:mtext>DES</mml:mtext><mml:mo>=</mml:mo><mml:mrow><mml:mo stretchy="false">[</mml:mo><mml:mrow><mml:msup><mml:mrow><mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mrow><mml:mtext>DT</mml:mtext><mml:mo>/</mml:mo><mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mrow><mml:mtext>DD</mml:mtext><mml:mo>&#x0002B;</mml:mo><mml:mtext>DT</mml:mtext></mml:mrow><mml:mo stretchy="false">)</mml:mo></mml:mrow></mml:mrow><mml:mo stretchy="false">)</mml:mo></mml:mrow></mml:mrow><mml:mrow><mml:mo>&#x0002A;</mml:mo></mml:mrow></mml:msup><mml:mn>100</mml:mn></mml:mrow><mml:mo stretchy="false">]</mml:mo></mml:mrow><mml:mo>.</mml:mo></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
</sec>
<sec>
<title>Chlorophyll <italic>a</italic> fluorescence</title>
<p>Photophysiological parameters were measured using a Fast Repetition Rate fluorometer (FRRf, FastOcean PTX; Chelsea Technologies) in combination with a FastAct Laboratory system (Chelsea Technologies). Measurements were conducted at growth temperature (4&#x000B0;C). Samples were dark-acclimated for 10 min prior to measurement. The duration of the dark acclimation phase was chosen after pre-testing different time intervals (5, 10, 20, 30 min) to ensure that all photosystem II (PS II) reaction centers were fully oxidized and non-photochemical quenching was relaxed. Excitation wavelength of the fluorometer&#x00027;s LED was 450 nm with an automated adjustment of the light intensity (between 0.66 and 1.2 &#x000D7; 10<sup>22</sup> photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>). The single turnover mode was used with 100 flashlets saturation phase on a 2 &#x003BC;s pitch and 40 flashlets relaxation phase on a 40 &#x003BC;s pitch in order to cumulatively saturate PS II. Estimation of minimum (F<sub>0</sub>) and maximum chlorophyll <italic>a</italic> (Chl <italic>a</italic>) fluorescence (F<sub>m</sub>) was based on iterative algorithms for induction (Kolber et al., <xref ref-type="bibr" rid="B38">1998</xref>) and relaxation phase (Oxborough et al., <xref ref-type="bibr" rid="B56">2012</xref>). Minimum and maximum Chl <italic>a</italic> fluorescence were used to calculate the apparent maximum quantum yield of photochemistry in PS II (F<sub>v</sub>/F<sub>m</sub>) according to the following equation:</p>
<disp-formula id="E3"><label>(3)</label><mml:math id="M5"><mml:mtable class="eqnarray" columnalign="right center left"><mml:mtr><mml:mtd><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>v</mml:mtext></mml:mrow></mml:msub><mml:mo>/</mml:mo><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>m</mml:mtext></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mrow><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>m</mml:mtext></mml:mrow></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mn>0</mml:mn></mml:mrow></mml:msub></mml:mrow><mml:mo stretchy="false">)</mml:mo></mml:mrow><mml:mo>/</mml:mo><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>m</mml:mtext></mml:mrow></mml:msub></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
<p>Additional Chl <italic>a</italic> fluorescence measurements of every treatment were performed in response to increasing incident irradiances (E) generating photosynthesis-irradiance-curves (PE-curves; irradiances ranged between 0 and 1800 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) using 15 steps with an acclimation duration of 5 min per light step and six subsequent Chl <italic>a</italic> fluorescence measurements. From these fluorescence measurements, the light-adapted minimum (F&#x02032;) and maximum (<inline-formula><mml:math id="M6"><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>m</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>) fluorescence of the single turnover acquisition was estimated. The effective PSII quantum yield under ambient light (<inline-formula><mml:math id="M7"><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>q</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>/<inline-formula><mml:math id="M8"><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>m</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>) was derived according to the equation (<inline-formula><mml:math id="M9"><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>m</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>/F&#x02032;)/<inline-formula><mml:math id="M10"><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>m</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> (Genty et al., <xref ref-type="bibr" rid="B23">1989</xref>). Absolute electron transport rates (absETR, e<sup>&#x02212;</sup> PSII<sup>&#x02212;1</sup> s<sup>&#x02212;1</sup>) at the different light steps of the PE-curve were calculated as (Suggett et al., <xref ref-type="bibr" rid="B76">2004</xref>, <xref ref-type="bibr" rid="B77">2009</xref>; Huot and Babin, <xref ref-type="bibr" rid="B34">2010</xref>):</p>
<disp-formula id="E4"><label>(4)</label><mml:math id="M11"><mml:mtable class="eqnarray" columnalign="right center left"><mml:mtr><mml:mtd><mml:mtext>absETR</mml:mtext><mml:mo>=</mml:mo><mml:msub><mml:mrow><mml:mi>&#x003C3;</mml:mi></mml:mrow><mml:mrow><mml:mtext>PSII</mml:mtext></mml:mrow></mml:msub><mml:mtext>&#x000A0;x&#x000A0;</mml:mtext><mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>q</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow><mml:mo>/</mml:mo><mml:mrow><mml:msubsup><mml:mtext>F</mml:mtext><mml:mtext>m</mml:mtext><mml:mo>&#x02032;</mml:mo></mml:msubsup></mml:mrow><mml:mo stretchy="false">)</mml:mo></mml:mrow><mml:mo>/</mml:mo><mml:mrow><mml:mo stretchy="false">(</mml:mo><mml:mrow><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>v</mml:mtext></mml:mrow></mml:msub><mml:mo>/</mml:mo><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>m</mml:mtext></mml:mrow></mml:msub></mml:mrow><mml:mo stretchy="false">)</mml:mo></mml:mrow><mml:mtext>&#x000A0;x&#x000A0;E</mml:mtext></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
<p>where &#x003C3;<sub>PSII</sub> is the functional absorption cross section of PSII photochemistry (in nm<sup>2</sup> quanta<sup>&#x02212;1</sup>) and E denotes the instantaneous irradiance (&#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>). Light-use characteristics were analyzed by fitting irradiance-dependent ETRs according to Ralph and Gademann (<xref ref-type="bibr" rid="B61">2005</xref>), including maximum absolute ETR (ETR<sub>m</sub>), minimum saturating irradiance (I<sub>K</sub>) and maximum light utilization efficiency (&#x003B1;). The PE-Curve was followed by another 10 min of dark acclimation with single turnover flashlets in order to assess PSII recovery (yield recovery). Yield recovery was calculated from the F<sub>v</sub>/F<sub>m</sub> measured before and after the PE-curve and given as % of the initial F<sub>v</sub>/F<sub>m</sub> (before the PE-curve). Non-photochemical quenching (NPQ, Equation 5) was calculated following the Stern-Volmer equation.</p>
<disp-formula id="E5"><label>(5)</label><mml:math id="M12"><mml:mtable class="eqnarray" columnalign="right center left"><mml:mtr><mml:mtd><mml:mtext>NPQ</mml:mtext><mml:mo>=</mml:mo><mml:msub><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>m</mml:mtext></mml:mrow></mml:msub><mml:mo>/</mml:mo><mml:msubsup><mml:mrow><mml:mtext>F</mml:mtext></mml:mrow><mml:mrow><mml:mtext>m</mml:mtext></mml:mrow><mml:mrow><mml:mi>&#x02032;</mml:mi></mml:mrow></mml:msubsup><mml:mo>-</mml:mo><mml:mn>1</mml:mn></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
<p>From the single turnover measurement of dark-adapted cells, also the time constant for electron transport at the acceptor side of PSII (&#x003C4;<sub>Qa</sub>, &#x003BC;s), the connectivity factor of adjacent PSII light-harvesting pigment matrices (p, dimensionless) and the concentration of functional PSII reaction centers ([RCII], nmol m<sup>&#x02212;3</sup>), were derived according to Oxborough et al. (<xref ref-type="bibr" rid="B56">2012</xref>), using FastPro8 software (Version 1.0.50, Kevin Oxborough, CTG Ltd.).</p>
</sec>
<sec>
<title>Statistics</title>
<p>All data are given as replicate means (<italic>n</italic> &#x0003D; 3) &#x000B1; SE. To test for significant differences between treatments, two-way analyses of variance (ANOVA) with additional normality (Shapiro-Wilk) and <italic>post hoc</italic> (Holm&#x02013;Sidak method) tests were performed (&#x003B1; &#x0003D; 0.05). In addition to this, to test for direct effects between two particular treatments standard <italic>t</italic>-tests were used. All statistical analyses were carried out with SigmaPlot 12.3 (SysStat Software Inc.). Different letters in figures and tables indicate statistical differences between treatments based on <italic>post-hoc</italic> tests.</p>
</sec></sec>
<sec sec-type="results" id="s3">
<title>Results</title>
<sec>
<title>Growth rates</title>
<p>Despite the large difference in cell size both investigated species showed comparable growth rates (Figures <xref ref-type="fig" rid="F1">1A,B</xref>). Several studies, investigating polar diatom species, of very different cell sizes, reported growth rates that are comparable to those found in this study (Gilstad and Sakshaug, <xref ref-type="bibr" rid="B24">1990</xref>; Kropuenske et al., <xref ref-type="bibr" rid="B41">2009</xref>; Arrigo et al., <xref ref-type="bibr" rid="B3">2010</xref>; Boelen et al., <xref ref-type="bibr" rid="B7">2011</xref>; Petrou et al., <xref ref-type="bibr" rid="B58">2014</xref>). Hence, within polar diatoms growth rates generally seem not to be greatly affected by cell size, but much more by abiotic factors such as temperature and light availability. Growth rates of <italic>Fragilariopsis curta</italic> (<italic>Fragilariopsis</italic>) generally increased from low (LL) to medium light (ML) conditions and slightly decreased toward high light (HL, Figure <xref ref-type="fig" rid="F1">1A</xref>). At ambient pCO<sub>2</sub> (380 &#x003BC;atm), <italic>Fragilariopsis</italic> increased growth by 20% from LL to ML, whereas it decreased growth by 58% between ML and HL conditions. Under high pCO<sub>2</sub> (1000 &#x003BC;atm), no significant light effects were detectable in growth. At low pCO<sub>2</sub> (180 &#x003BC;atm), however, a strong increase in growth (86%) occurred between LL and ML, with no detectable changes from ML to HL. There were no overall trends with increasing pCO<sub>2</sub> discernible within all light treatments. At LL, growth of <italic>Fragilariopsis</italic> was suppressed in low pCO<sub>2</sub> treatments compared to the other two pCO<sub>2</sub> treatments, whereas at ML both low and high pCO<sub>2</sub> treatments grew less than the ambient treatment, yet only the former was statistically significant. The reverse pattern occurred at HL, exhibiting decreased growth at ambient pCO<sub>2</sub>, 22% compared to low and 39% toward high pCO<sub>2</sub> treatments.</p>
<fig id="F1" position="float">
<label>Figure 1</label>
<caption><p><bold>Growth rates (&#x003BC;, d<sup>&#x02212;1</sup>), particulate organic carbon production (POC, pg d<sup>&#x02212;1</sup>) and cellular carbon to nitrogen ratio (C:N, mol mol<sup>&#x02212;1</sup>) of (A,C,E)</bold> <italic>Fragilariopsis</italic> and <bold>(B,D,F)</bold> <italic>Odontella</italic> acclimated to different light (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions. Values represent mean &#x000B1; SE (<italic>n</italic> &#x0003D; 3). <italic>Odontella</italic> did not grow at low light in combination with low pCO<sub>2</sub> as indicated by <sup>&#x0002A;</sup>. Statistical differences between two treatments (<italic>p</italic> &#x0003D; 0.05) derived from <italic>post-hoc</italic> tests are indicated by different letters.</p></caption>
<graphic xlink:href="fmars-03-00260-g0001.tif"/>
</fig>
<p>In <italic>Odontella weisflogii</italic>, (<italic>Odontella</italic>), in the ambient and high pCO<sub>2</sub> treatments growth increased from LL to ML by 58% and 79%, respectively, yet both pCO<sub>2</sub> treatments showed no changes between ML and HL (Figure <xref ref-type="fig" rid="F1">1B</xref>). Within the low pCO<sub>2</sub> treatments, no light effects on growth were found from ML to HL, yet at LL despite several attempts <italic>Odontella</italic> could not grow. At LL and ML, growth of <italic>Odontella</italic> decreased from ambient to high pCO<sub>2</sub>. No differences between pCO<sub>2</sub> treatments were detectable at HL. At ML and HL, low pCO<sub>2</sub> acclimated cells grew slower than the ones acclimated to ambient pCO<sub>2</sub> while they reached similar growth rates as cells grown at high pCO<sub>2</sub>.</p>
</sec>
<sec>
<title>Elemental composition</title>
<p>The production rate of particulate organic carbon (POC) revealed species-specific trends (Figures <xref ref-type="fig" rid="F1">1C,D</xref>). In <italic>Fragilariopsis</italic>, at ambient pCO<sub>2</sub> POC production significantly decreased (84%) from LL to HL. Under high pCO<sub>2</sub>, POC production decreased by 51% from LL to ML and showed no further changes from ML to HL. Under low pCO<sub>2</sub>, POC production increased about 86% from LL to ML and decreased about 67% from ML to HL. At LL, POC production rates increased about 91% from low to ambient pCO<sub>2</sub> and decreased by 39% in response to high pCO<sub>2</sub>. At ML, POC production decreased about 53% from low to high pCO<sub>2</sub>, whereas at HL no differences between pCO<sub>2</sub> treatments were found.</p>
<p>In <italic>Odontella</italic>, POC production rates increased from LL to ML by 86 and 93% at ambient and high pCO<sub>2</sub>, respectively. At ambient pCO<sub>2</sub>, POC production rates decreased from ML to HL. Within high and low pCO<sub>2</sub> treatments, no changes were detected between ML and HL. At LL and ML, the ambient pCO<sub>2</sub> treatments had higher POC production rates than high pCO<sub>2</sub> treatments. Low pCO<sub>2</sub> treatments revealed lower POC production rates at ML, when compared to the two other pCO<sub>2</sub> treatments. No differences between pCO<sub>2</sub> treatments were observed at HL.</p>
<p>In <italic>Fragilariopsis</italic>, the ratio of cellular carbon to nitrogen (C:N, mol mol<sup>&#x02212;1</sup>) showed effects of both light and pCO<sub>2</sub>. Under all three pCO<sub>2</sub> treatments C:N ratios decreased from LL to ML, but increased from ML to HL under high pCO<sub>2</sub> (Figure <xref ref-type="fig" rid="F1">1E</xref>). Under LL, effects of pCO<sub>2</sub> became evident as C:N ratios were reduced under high compared to low and ambient pCO<sub>2</sub>, whereas the opposite was true under HL with increased C:N ratios under high pCO<sub>2</sub>. <italic>Odontella</italic>, however, showed no effects of light on the C:N ratio (Figure <xref ref-type="fig" rid="F1">1F</xref>). Only under ML, the ratio of C:N increased from low to ambient pCO<sub>2</sub> with no further increase toward high pCO<sub>2</sub>.</p>
</sec>
<sec>
<title>Chl a fluorescence-based physiology</title>
<p>Photosynthesis-irradiance curves (PE-curves; Figure <xref ref-type="fig" rid="F2">2</xref>) displayed a strong light effect as maximum electron transport rates (ETRm), light saturation point (I<sub>K</sub>) and light use efficiency (&#x003B1;, Table <xref ref-type="table" rid="T2">2</xref>) increased with increasing irradiance in both <italic>Fragilariopsis</italic> and <italic>Odontella</italic>, but there were no differences in I<sub>k</sub> and &#x003B1; between LL and ML in both species. The pCO<sub>2</sub> did not affect absolute ETRs (absETR) within LL treatments in both species (Figures <xref ref-type="fig" rid="F2">2A,B</xref>). Under ML, ETRm and &#x003B1; increased from low to ambient pCO<sub>2</sub> in both species, but remained unaltered between ambient and high pCO<sub>2</sub>. Only at HL, an effect of pCO<sub>2</sub> on absETR (Figures <xref ref-type="fig" rid="F2">2E,F</xref>) and I<sub>K</sub> (Table <xref ref-type="table" rid="T2">2</xref>) was evident in <italic>Fragilariopsis</italic> and <italic>Odontella</italic>, with decreased ETRm and I<sub>K</sub> values in the low compared to ambient and high pCO<sub>2</sub> treatments, respectively.</p>
<fig id="F2" position="float">
<label>Figure 2</label>
<caption><p><bold>Absolute electron transport rates (absETR, e<sup>&#x02212;</sup> PSII<sup>&#x02212;1</sup> s<sup>&#x02212;1</sup>) of <italic>Fragilariopsis</italic> and <italic>Odontella</italic> acclimated to different light</bold> (LL &#x0003D; 20 in <bold>A,B</bold>; ML &#x0003D; 200 in <bold>C,D</bold>; HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup> in <bold>E,F</bold>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions. Values represent mean &#x000B1; SE (<italic>n</italic> &#x0003D; 3). Lines represent the fit following Ralph and Gademann (<xref ref-type="bibr" rid="B61">2005</xref>).</p></caption>
<graphic xlink:href="fmars-03-00260-g0002.tif"/>
</fig>
<table-wrap position="float" id="T2">
<label>Table 2</label>
<caption><p><bold>Photosynthetic parameters from photosynthesis-irradiance curve fits based on Ralph and Gademann (<xref ref-type="bibr" rid="B61">2005</xref>) maximum electron transport rate (ETRm, e<sup>&#x02212;</sup> PSII<sup>&#x02212;1</sup> s<sup>&#x02212;1</sup>), light saturation point (I<sub><italic>K</italic></sub>, &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and light use efficiency (&#x003B1;, rel. unit) were determined for <italic>Fragilariopsis</italic> and <italic>Odontella</italic> acclimated to different light (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th valign="top" align="left"><bold>pCO<sub>2</sub></bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>ETRm</bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>I</bold><sub><bold><italic><bold>K</bold></italic></bold></sub></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>&#x003B1;</bold></th>
</tr>
<tr>
<th valign="top" align="left"><bold>Light intensity</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left" colspan="10" style="background-color:#bbbdc0"><italic><bold>FRAGILARIOPSIS</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">110 &#x000B1; 9<sup>a</sup></td>
<td valign="top" align="center">118 &#x000B1; 6<sup>a</sup></td>
<td valign="top" align="center">123 &#x000B1; 8<sup>a</sup></td>
<td valign="top" align="center">43 &#x000B1; 5<sup>a</sup></td>
<td valign="top" align="center">47 &#x000B1; 4<sup>a</sup></td>
<td valign="top" align="center">54 &#x000B1; 3<sup>a</sup></td>
<td valign="top" align="center">2.63 &#x000B1; 0.09<sup>a</sup></td>
<td valign="top" align="center">2.50 &#x000B1; 0.07<sup>b</sup></td>
<td valign="top" align="center">2.31 &#x000B1; 0.18<sup>b</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">224 &#x000B1; 15<sup>b</sup></td>
<td valign="top" align="center">275 &#x000B1; 7<sup>c</sup></td>
<td valign="top" align="center">288 &#x000B1; 4<sup>c</sup></td>
<td valign="top" align="center">137 &#x000B1; 26<sup>b</sup></td>
<td valign="top" align="center">115 &#x000B1; 3<sup>b</sup></td>
<td valign="top" align="center">156 &#x000B1; 13<sup>b</sup></td>
<td valign="top" align="center">1.74 &#x000B1; 0.19<sup>ac</sup></td>
<td valign="top" align="center">2.39 &#x000B1; 0.01<sup>c</sup></td>
<td valign="top" align="center">1.89 &#x000B1; 0.18<sup>b</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">267 &#x000B1; 17<sup>c</sup></td>
<td valign="top" align="center">652 &#x000B1; 122<sup>d</sup></td>
<td valign="top" align="center">435 &#x000B1; 26<sup>e</sup></td>
<td valign="top" align="center">145 &#x000B1; 15<sup>b</sup></td>
<td valign="top" align="center">409 &#x000B1; 87<sup>c</sup></td>
<td valign="top" align="center">241 &#x000B1; 27<sup>b</sup></td>
<td valign="top" align="center">1.86 &#x000B1; 0.07<sup>abc</sup></td>
<td valign="top" align="center">1.63 &#x000B1; 0.10<sup>b</sup></td>
<td valign="top" align="center">1.84 &#x000B1; 0.12<sup>b</sup></td>
</tr>
<tr>
<td valign="top" align="left" colspan="10" style="background-color:#bbbdc0"><italic><bold>ODONTELLA</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">117 &#x000B1; 5<sup>a</sup></td>
<td valign="top" align="center">123 &#x000B1; 8<sup>ac</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">47 &#x000B1; 3<sup>b</sup></td>
<td valign="top" align="center">54 &#x000B1; 3<sup>b</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">2.50 &#x000B1; 0.07<sup>b</sup></td>
<td valign="top" align="center">2.31 &#x000B1; 0.18<sup>d</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">268 &#x000B1; 17<sup>b</sup></td>
<td valign="top" align="center">186 &#x000B1; 14<sup>c</sup></td>
<td valign="top" align="center">216 &#x000B1; 15<sup>c</sup></td>
<td valign="top" align="center">170 &#x000B1; 10<sup>a</sup></td>
<td valign="top" align="center">94 &#x000B1; 9<sup>c</sup></td>
<td valign="top" align="center">106 &#x000B1; 7<sup>d</sup></td>
<td valign="top" align="center">1.58 &#x000B1; 0.04<sup>a</sup></td>
<td valign="top" align="center">2.00 &#x000B1; 0.08<sup>c</sup></td>
<td valign="top" align="center">2.03 &#x000B1; 0.04<sup>d</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">267 &#x000B1; 21<sup>b</sup></td>
<td valign="top" align="center">676 &#x000B1; 140<sup>d</sup></td>
<td valign="top" align="center">665 &#x000B1; 93<sup>d</sup></td>
<td valign="top" align="center">191 &#x000B1; 15<sup>a</sup></td>
<td valign="top" align="center">490 &#x000B1; 91<sup>c</sup></td>
<td valign="top" align="center">635 &#x000B1; 69<sup>d</sup></td>
<td valign="top" align="center">1.40 &#x000B1; 0.04<sup>ac</sup></td>
<td valign="top" align="center">1.37 &#x000B1; 0.07<sup>c</sup></td>
<td valign="top" align="center">1.04 &#x000B1; 0.06<sup>e</sup></td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<p><italic>Values represent mean &#x000B1; SE (n &#x0003D; 3). Odontella did not grow at low light in combination with low pCO<sub>2</sub> as indicated by /. Statistical differences between two treatments (p &#x0003D; 0.05) derived from post-hoc tests are indicated by different letters</italic>.</p>
</table-wrap-foot>
</table-wrap>
<p>The maximum quantum yield (F<sub>v</sub>/F<sub>m</sub>) is an indicator for overall fitness and revealed species-specific patterns under the different experimental treatments (Figures <xref ref-type="fig" rid="F3">3A,B</xref>). In <italic>Fragilariopsis</italic>, F<sub>v</sub>/F<sub>m</sub> decreased from LL to ML and remained unchanged between ML and HL in the ambient pCO<sub>2</sub> treatments. At LL, the low pCO<sub>2</sub> treatments exhibited the lowest yield. Besides this, no pCO<sub>2</sub> effects were found. In <italic>Odontella</italic>, F<sub>v</sub>/F<sub>m</sub> did not change between LL and ML in the ambient pCO<sub>2</sub> treatments, whereas it decreased from LL to ML in the high pCO<sub>2</sub> treatments. Between ML and HL, F<sub>v</sub>/F<sub>m</sub> decreased in all pCO<sub>2</sub> treatments.</p>
<fig id="F3" position="float">
<label>Figure 3</label>
<caption><p><bold>Maximum photosynthetic yield (F<sub>v</sub>/F<sub>m</sub>, rel. unit), yield recovery after short term light stress (% of initial) of (A,C)</bold> <italic>Fragilariopsis</italic> and <bold>(B,D)</bold> <italic>Odontella</italic> acclimated to different light (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions. Values represent mean &#x000B1; SE (<italic>n</italic> &#x0003D; 3). <italic>Odontella</italic> did not grow at low light in combination with low pCO<sub>2</sub> as indicated by <sup>&#x0002A;</sup>. Statistical differences between two treatments (<italic>p</italic> &#x0003D; 0.05) derived from <italic>post-hoc</italic> tests are indicated by different letters.</p></caption>
<graphic xlink:href="fmars-03-00260-g0003.tif"/>
</fig>
<p>To test whether both species experienced short-term light stress or any damage in PSII, potentially induced during the PE-curve, a second dark acclimation phase right after the PE-curve was carried out followed by another F<sub>v</sub>/F<sub>m</sub> measurement, named yield recovery (given as % of initial F<sub>v</sub>/F<sub>m</sub>, Figures <xref ref-type="fig" rid="F3">3C,D</xref>). The two species showed diverging patterns of yield recovery. In <italic>Fragilariopsis</italic>, the recovery potential increased with increasing light intensity. In <italic>Odontella</italic>, a reversed bell shape was observed with a decrease in recovery from LL to ML and an increase from ML to HL. Yield recovery was not affected by pCO<sub>2</sub> under all light conditions in <italic>Odontella</italic>, whereas in <italic>Fragilariopsis</italic> the recovery increased from low to high pCO<sub>2</sub> conditions at LL and ML, but remained unaffected by pCO<sub>2</sub> at HL.</p>
</sec>
<sec>
<title>Light harvesting pigment content</title>
<p>Cellular pigment content generally decreased with increasing light intensity (Table <xref ref-type="table" rid="T3">3</xref>). In both species and for all light-harvesting pigments (Chl <italic>a</italic>, Chl c2, fucoxanthin, &#x003B2;-carotene, Table <xref ref-type="table" rid="T3">3</xref>), a significant decrease between LL and ML was observed in all pCO<sub>2</sub> treatments and only minor or no decreases were observed between ML and HL conditions. Besides the light effect, <italic>Fragilariopsis</italic> showed a pCO<sub>2</sub> effect on all light-harvesting pigments (Chl <italic>a</italic>, Chl c2, fucoxanthin and &#x003B2;-carotene, Table <xref ref-type="table" rid="T3">3</xref>). To prevent repetition only the CO<sub>2</sub>-dependent change in Chl <italic>a</italic> will be described exemplarily for all light-harvesting pigments. At LL, cellular Chl <italic>a</italic> concentrations increased from low to ambient pCO<sub>2</sub> and decreased toward high pCO<sub>2</sub>. At ML and HL, no pCO<sub>2</sub> effects were detected. In contrast to <italic>Fragilariopsis</italic>, in <italic>Odontella</italic> cellular Chl <italic>a</italic> concentrations remained unaltered in response to changes in pCO<sub>2</sub>(Table <xref ref-type="table" rid="T3">3</xref>).</p>
<table-wrap position="float" id="T3">
<label>Table 3</label>
<caption><p><bold>Cellular chlorophyll <italic>a</italic> (Chl <italic>a</italic>), chlorophyll c2 (Chl c2), fucoxanthin, &#x003B2;-carotene, diadinoxanthin (DD) and diatoxanthin (DT) were determined for <italic>Fragilariopsis</italic> (fg cell<sup>&#x02212;1</sup>) and <italic>Odontella</italic> (pg cell<sup>&#x02212;1</sup>) acclimated to different light (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions. De-epoxidation state (DES) was calculated as [(DT/(DD&#x0002B;DT))<sup>&#x0002A;</sup>100]</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th valign="top" align="left"><bold>pCO<sub>2</sub></bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>Chlorophyll</bold> <italic><bold>a</bold></italic></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>Chlorophyll c2</bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>Fucoxanthin</bold></th>
</tr>
<tr>
<th valign="top" align="left"><bold>Light intensity</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left" colspan="10" style="background-color:#bbbdc0"><italic><bold>FRAGILARIOPSIS</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">107 &#x000B1; 4<sup>a</sup></td>
<td valign="top" align="center">387 &#x000B1; 72<sup>b</sup></td>
<td valign="top" align="center">214 &#x000B1; 28<sup>c</sup></td>
<td valign="top" align="center">9.0 &#x000B1; 6.3<sup>a</sup></td>
<td valign="top" align="center">45.8 &#x000B1; 4.4<sup>b</sup></td>
<td valign="top" align="center">17.7 &#x000B1; 0.5<sup>a</sup></td>
<td valign="top" align="center">82.2 &#x000B1; 4.5<sup>a</sup></td>
<td valign="top" align="center">350.4 &#x000B1; 68.4<sup>d</sup></td>
<td valign="top" align="center">185.1 &#x000B1; 28.5<sup>d</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">33 &#x000B1; 1<sup>d</sup></td>
<td valign="top" align="center">8 &#x000B1; 3<sup>e</sup></td>
<td valign="top" align="center">15 &#x000B1; 3<sup>e</sup></td>
<td valign="top" align="center">4.2 &#x000B1; 0.2<sup>c</sup></td>
<td valign="top" align="center">0.6 &#x000B1; 0.3<sup>d</sup></td>
<td valign="top" align="center">1.3 &#x000B1; 0.4<sup>d</sup></td>
<td valign="top" align="center">20.2 &#x000B1; 0.8<sup>b</sup></td>
<td valign="top" align="center">5.8 &#x000B1; 2.5<sup>e</sup></td>
<td valign="top" align="center">12.2 &#x000B1; 2.2<sup>e</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">25 &#x000B1; 1<sup>d</sup></td>
<td valign="top" align="center">12 &#x000B1; 1<sup>e</sup></td>
<td valign="top" align="center">13 &#x000B1; 3<sup>e</sup></td>
<td valign="top" align="center">2.2 &#x000B1; 0.1<sub>d</sub></td>
<td valign="top" align="center">1.1 &#x000B1; 0.2<sup>d</sup></td>
<td valign="top" align="center">1.1 &#x000B1; 0.4<sup>d</sup></td>
<td valign="top" align="center">14.7 &#x000B1; 0.8<sup>c</sup></td>
<td valign="top" align="center">8.6 &#x000B1; 0.3<sup>e</sup></td>
<td valign="top" align="center">9.9 &#x000B1; 2.8<sup>de</sup></td>
</tr>
<tr>
<td valign="top" align="left" colspan="10" style="background-color:#bbbdc0"><italic><bold>ODONTELLA</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">30 &#x000B1; 7<sup>a</sup></td>
<td valign="top" align="center">61 &#x000B1; 5<sup>a</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">3.9 &#x000B1; 0.9<sup>a</sup></td>
<td valign="top" align="center">6.9 &#x000B1; 0.8<sup>a</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">16.1 &#x000B1; 4.3<sup>a</sup></td>
<td valign="top" align="center">28.1 &#x000B1; 2.6<sup>a</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">15 &#x000B1; 2<sup>b</sup></td>
<td valign="top" align="center">17 &#x000B1; 3<italic>a</italic><sup>b</sup></td>
<td valign="top" align="center">23 &#x000B1; 2<sup>b</sup></td>
<td valign="top" align="center">1.5 &#x000B1; 0.2<sup>b</sup></td>
<td valign="top" align="center">2.1 &#x000B1; 0.2<sup>abc</sup></td>
<td valign="top" align="center">2.6 &#x000B1; 0.2<sup>c</sup></td>
<td valign="top" align="center">9.7 &#x000B1; 1.0<sup>b</sup></td>
<td valign="top" align="center">13.7 &#x000B1; 1.3<sup>abc</sup></td>
<td valign="top" align="center">16.0 &#x000B1; 1.2<sup>c</sup></td>
</tr>
<tr style="border-bottom: thin solid #000000;">
<td valign="top" align="left">500</td>
<td valign="top" align="center">15 &#x000B1; 2<sup>b</sup></td>
<td valign="top" align="center">14 &#x000B1; 1<sup>b</sup></td>
<td valign="top" align="center">5 &#x000B1; 2<sup>b</sup></td>
<td valign="top" align="center">1.5 &#x000B1; 0.1<sup>b</sup></td>
<td valign="top" align="center">1.7 &#x000B1; 0.2<sup>b</sup></td>
<td valign="top" align="center">1.6 &#x000B1; 0.2<sup>b</sup></td>
<td valign="top" align="center">8.5 &#x000B1; 1.3<sup>b</sup></td>
<td valign="top" align="center">9.4 &#x000B1; 0.3<sup>b</sup></td>
<td valign="top" align="center">8.6 &#x000B1; 0.7<sup>b</sup></td>
</tr> <tr>
<td/>
<td valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>DES</bold></td>
<td valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>DD&#x0002B;DT pool</bold></td>
<td valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>&#x003B2;-carotene</bold></td>
</tr>
<tr style="border-bottom: thin solid #000000;">
<td/>
<td valign="top" align="center"><bold>Low</bold></td>
<td valign="top" align="center"><bold>Ambient</bold></td>
<td valign="top" align="center"><bold>High</bold></td>
<td valign="top" align="center"><bold>Low</bold></td>
<td valign="top" align="center"><bold>Ambient</bold></td>
<td valign="top" align="center"><bold>High</bold></td>
<td valign="top" align="center"><bold>Low</bold></td>
<td valign="top" align="center"><bold>Ambient</bold></td>
<td valign="top" align="center"><bold>High</bold></td>
</tr> <tr>
<td valign="top" align="left" colspan="10" style="background-color:#bbbdc0"><italic><bold>FRAGILARIOPSIS</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">4.5 &#x000B1; 3.2<sup>a</sup></td>
<td valign="top" align="center">0.0 &#x000B1; 0.0</td>
<td valign="top" align="center">0.0 &#x000B1; 0.0</td>
<td valign="top" align="center">6.7 &#x000B1; 0.2<sup>a</sup></td>
<td valign="top" align="center">9.4 &#x000B1; 1.2<sup>b</sup></td>
<td valign="top" align="center">5.3 &#x000B1; 0.6<sup>c</sup></td>
<td valign="top" align="center">1.88 &#x000B1; 0.10<sup>a</sup></td>
<td valign="top" align="center">3.30 &#x000B1; 0.48<sup>b</sup></td>
<td valign="top" align="center">2.32 &#x000B1; 0.16<sup>a</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">26.8 &#x000B1; 1.0<sup>b</sup></td>
<td valign="top" align="center">37.5 &#x000B1; 8.8<sup>c</sup></td>
<td valign="top" align="center">34.2 &#x000B1; 8.2<sup>c</sup></td>
<td valign="top" align="center">9.5 &#x000B1; 0.4<sup>b</sup></td>
<td valign="top" align="center">2.4 &#x000B1; 0.6<sup>d</sup></td>
<td valign="top" align="center">4.3 &#x000B1; 1.1<sup>cd</sup></td>
<td valign="top" align="center">0.95 &#x000B1; 0.03<sup>d</sup></td>
<td valign="top" align="center">0.17 &#x000B1; 0.15<sup>e</sup></td>
<td valign="top" align="center">0.31 &#x000B1; 0.18<sup>e</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">14.5 &#x000B1; 0.1<sup>d</sup></td>
<td valign="top" align="center">21.4 &#x000B1; 2.9<sup>eb</sup></td>
<td valign="top" align="center">13.3 &#x000B1; 5.9<sup>ed</sup></td>
<td valign="top" align="center">10.4 &#x000B1; 0.6<sup>b</sup></td>
<td valign="top" align="center">3.5 &#x000B1; 0.3<sup>cd</sup></td>
<td valign="top" align="center">3.1 &#x000B1; 1.1<sup>cd</sup></td>
<td valign="top" align="center">0.75 &#x000B1; 0.05<sup>f</sup></td>
<td valign="top" align="center">0.17 &#x000B1; 0.14<sup>e</sup></td>
<td valign="top" align="center">0.10 &#x000B1; 0.08<sup>e</sup></td>
</tr>
<tr>
<td valign="top" align="left" colspan="10" style="background-color:#bbbdc0"><italic><bold>ODONTELLA</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">3.1 &#x000B1; 2.2<sup>a</sup></td>
<td valign="top" align="center">8.9 &#x000B1; 3.7<sup>ac</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">1.3 &#x000B1; 0.6<sup>a</sup></td>
<td valign="top" align="center">1.6 &#x000B1; 0.1<sup>a</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">0.51 &#x000B1; 0.18<sup>a</sup></td>
<td valign="top" align="center">0.83 &#x000B1; 0.04<sup>a</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">26.7 &#x000B1; 1.6<sup>b</sup></td>
<td valign="top" align="center">11.5 &#x000B1; 0.9<sup>c</sup></td>
<td valign="top" align="center">11.0 &#x000B1; 0.5<sup>c</sup></td>
<td valign="top" align="center">3.1 &#x000B1; 0.2<sup>b</sup></td>
<td valign="top" align="center">5.3 &#x000B1; 0.5<sup>cd</sup></td>
<td valign="top" align="center">6.9 &#x000B1; 0.5<sup>b</sup></td>
<td valign="top" align="center">0.43 &#x000B1; 0.06<sup>b</sup></td>
<td valign="top" align="center">0.84 &#x000B1; 0.09<sup>a</sup></td>
<td valign="top" align="center">0.94 &#x000B1; 0.08<sup>a</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">38.8 &#x000B1; 1.5<sup>d</sup></td>
<td valign="top" align="center">28.6 &#x000B1; 1.2<sup>be</sup></td>
<td valign="top" align="center">32.7 &#x000B1; 1.4<sup>e</sup></td>
<td valign="top" align="center">3.7 &#x000B1; 0.7<sup>bc</sup></td>
<td valign="top" align="center">2.9 &#x000B1; 0.2<sup>d</sup></td>
<td valign="top" align="center">3.4 &#x000B1; 0.2<sup>b</sup></td>
<td valign="top" align="center">0.50 &#x000B1; 0.06<sup>b</sup></td>
<td valign="top" align="center">0.52 &#x000B1; 0.07<sup>b</sup></td>
<td valign="top" align="center">0.59 &#x000B1; 0.03<sup>b</sup></td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<p><italic>Values represent mean &#x000B1; SE (n &#x0003D; 3). Odontella did not grow at low light in combination with low pCO<sub>2</sub> as indicated by /. Statistical differences between two treatments (p &#x0003D; 0.05) derived from post-hoc tests are indicated by different letters</italic>.</p>
</table-wrap-foot>
</table-wrap></sec>
<sec>
<title>Adjustments of photosystem II</title>
<p>The functional absorption cross section of PSII (&#x003C3;<sub>PSII</sub>, Table <xref ref-type="table" rid="T4">4</xref>), is a measure of the size of the functional &#x0201C;target area&#x0201D; of light-harvesting antenna. In <italic>Fragilariopsis</italic>, &#x003C3;<sub>PSII</sub> decreased with increasing light intensity, whereas there was no change detectable in <italic>Odontella</italic>. However, effects of pCO<sub>2</sub> on &#x003C3;<sub>PSII</sub> were found in both species. Under low compared to ambient and high pCO<sub>2</sub>, &#x003C3;<sub>PSII</sub> was significantly lower at ML and HL in both diatoms.</p>
<table-wrap position="float" id="T4">
<label>Table 4</label>
<caption><p><bold>Functional absorption cross section (&#x003C3;<sub>PSII</sub>, nm<sup>&#x02212;2</sup> quanta<sup>&#x02212;1</sup>), the connectivity factor (p, dimensionless) of adjacent PSII light-harvesting pigment matrices, time constant for electron transport at the acceptor side of PSII (&#x003C4;<sub>Qa</sub>, &#x003BC;s) and the concentration of functional PSII reaction centers ([RCII], nmol m<sup>&#x02212;3</sup>) were determined for <italic>Fragilariopsis</italic> and <italic>Odontella</italic> acclimated to different light (LL &#x0003D; 20, ML &#x0003D; 200, HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions</bold>.</p></caption>
<table frame="hsides" rules="groups">
<thead><tr>
<th/>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>&#x003C3;<sub>PSII</sub></bold></th>
<th valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><italic><bold>p</bold></italic></th>
</tr>
<tr>
<th/>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
<th valign="top" align="center"><bold>Low</bold></th>
<th valign="top" align="center"><bold>Ambient</bold></th>
<th valign="top" align="center"><bold>High</bold></th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left" colspan="7" style="background-color:#bbbdc0"><italic><bold>FRAGILARIOPSIS</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">7.66 &#x000B1; 0.83<sup>a</sup></td>
<td valign="top" align="center">7.25 &#x000B1; 0.38<sup>a</sup></td>
<td valign="top" align="center">6.98 &#x000B1; 0.18<sup>a</sup></td>
<td valign="top" align="center">0.2 &#x000B1; 0.01<sup>a</sup></td>
<td valign="top" align="center">0.29 &#x000B1; 0.01<sup>b</sup></td>
<td valign="top" align="center">0.29 &#x000B1; 0.02<sup>b</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">5.07 &#x000B1; 0.01<sup>b</sup></td>
<td valign="top" align="center">6.62 &#x000B1; 0.05<sup>a</sup></td>
<td valign="top" align="center">6.51 &#x000B1; 0.21<sup>ac</sup></td>
<td valign="top" align="center">0.2 &#x000B1; 0.01<sup>a</sup></td>
<td valign="top" align="center">0.29 &#x000B1; 0.02<sup>b</sup></td>
<td valign="top" align="center">0.24 &#x000B1; 0.02<sup>ab</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">4.98 &#x000B1; 0.06<sup>b</sup></td>
<td valign="top" align="center">5.95 &#x000B1; 0.1<sup>c</sup></td>
<td valign="top" align="center">3.88 &#x000B1; 0.20<sup>c</sup></td>
<td valign="top" align="center">0.24 &#x000B1; 0.01<sup>ac</sup></td>
<td valign="top" align="center">0.26 &#x000B1; 0.01<sup>bc</sup></td>
<td valign="top" align="center">0.27 &#x000B1; 0.01<sup>bc</sup></td>
</tr>
<tr>
<td valign="top" align="left" colspan="7" style="background-color:#bbbdc0"><italic><bold>ODONTELLA</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">4.21 &#x000B1; 0.34<sup>a</sup></td>
<td valign="top" align="center">3.88 &#x000B1; 0.2<sup>ab</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">0.32 &#x000B1; 0.02<sup>a</sup></td>
<td valign="top" align="center">0.33 &#x000B1; 0.02<sup>a</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">3.55 &#x000B1; 0.08<sup>b</sup></td>
<td valign="top" align="center">4.03 &#x000B1; 0.12<sup>a</sup></td>
<td valign="top" align="center">3.99 &#x000B1; 0.08<sup>a</sup></td>
<td valign="top" align="center">0.37 &#x000B1; 0.01<sup>ab</sup></td>
<td valign="top" align="center">0.40 &#x000B1; 0.01<sup>b</sup></td>
<td valign="top" align="center">0.39 &#x000B1; 0.01<sup>b</sup></td>
</tr>
<tr style="border-bottom: thin solid #000000;">
<td valign="top" align="left">500</td>
<td valign="top" align="center">3.65 &#x000B1; 0.05<sup>b</sup></td>
<td valign="top" align="center">4.09 &#x000B1; 0.01<sup>a</sup></td>
<td valign="top" align="center">4.01 &#x000B1; 0.05<sup>a</sup></td>
<td valign="top" align="center">0.29 &#x000B1; 0.03<sup>ac</sup></td>
<td valign="top" align="center">0.32 &#x000B1; 0.02<sup>a</sup></td>
<td valign="top" align="center">0.23 &#x000B1; 0.02<sup>c</sup></td>
</tr> <tr>
<td/>
<td valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>&#x003C4;<sub><italic>Qa</italic></sub></bold></td>
<td valign="top" align="center" colspan="3" style="border-bottom: thin solid #000000;"><bold>[RCII]</bold></td>
</tr>
<tr style="border-bottom: thin solid #000000;">
<td/>
<td valign="top" align="center"><bold>Low</bold></td>
<td valign="top" align="center"><bold>Ambient</bold></td>
<td valign="top" align="center"><bold>High</bold></td>
<td valign="top" align="center"><bold>Low</bold></td>
<td valign="top" align="center"><bold>Ambient</bold></td>
<td valign="top" align="center"><bold>High</bold></td>
</tr> <tr>
<td valign="top" align="left" colspan="7" style="background-color:#bbbdc0"><italic><bold>FRAGILARIOPSIS</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">505 &#x000B1; 1<sup>a</sup></td>
<td valign="top" align="center">414 &#x000B1; 13<sup>b</sup></td>
<td valign="top" align="center">428 &#x000B1; 7<sup>b</sup></td>
<td valign="top" align="center">6.6 &#x000B1; 2.2<sup>as</sup></td>
<td valign="top" align="center">13.2 &#x000B1; 0.5<sup>b</sup></td>
<td valign="top" align="center">18.2 &#x000B1; 1.0<sup>c</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">499 &#x000B1; 5<sup>a</sup></td>
<td valign="top" align="center">557 &#x000B1; 14<sup>c</sup></td>
<td valign="top" align="center">616 &#x000B1; 30<sup>c</sup></td>
<td valign="top" align="center">6.3 &#x000B1; 0.3<sup>ad</sup></td>
<td valign="top" align="center">7.4 &#x000B1; 0.3<sup>a</sup></td>
<td valign="top" align="center">4.5 &#x000B1; 1.2<sup>d</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">583 &#x000B1; 19<sup>c</sup></td>
<td valign="top" align="center">600 &#x000B1; 13<sup>c</sup></td>
<td valign="top" align="center">568 &#x000B1; 11<sup>c</sup></td>
<td valign="top" align="center">5.6 &#x000B1; 0.4<sup>ad</sup></td>
<td valign="top" align="center">10.6 &#x000B1; 2.5<sup>ab</sup></td>
<td valign="top" align="center">6.7 &#x000B1; 1.2<sup>ad</sup></td>
</tr>
<tr>
<td valign="top" align="left" colspan="7" style="background-color:#bbbdc0"><italic><bold>ODONTELLA</bold></italic></td>
</tr>
<tr>
<td valign="top" align="left">20</td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">738 &#x000B1; 23<sup>ac</sup></td>
<td valign="top" align="center">626 &#x000B1; 64<sup>b</sup></td>
<td valign="top" align="center">/</td>
<td valign="top" align="center">10.5 &#x000B1; 0.3<sup>a</sup></td>
<td valign="top" align="center">9.9 &#x000B1; 1.2<sup>a</sup></td>
</tr>
<tr>
<td valign="top" align="left">200</td>
<td valign="top" align="center">660 &#x000B1; 17<sup>b</sup></td>
<td valign="top" align="center">809 &#x000B1; 29<sup>a</sup></td>
<td valign="top" align="center">746 &#x000B1; 35<sup>ac</sup></td>
<td valign="top" align="center">9.8 &#x000B1; 2.0<sup>ac</sup></td>
<td valign="top" align="center">16.0 &#x000B1; 1.1<sup>b</sup></td>
<td valign="top" align="center">17.1 &#x000B1; 1.5<sup>b</sup></td>
</tr>
<tr>
<td valign="top" align="left">500</td>
<td valign="top" align="center">651 &#x000B1; 11<sup>b</sup></td>
<td valign="top" align="center">723 &#x000B1; 11<sup>c</sup></td>
<td valign="top" align="center">885 &#x000B1; 83<sup>ac</sup></td>
<td valign="top" align="center">4.8 &#x000B1; 0.8<sup>cd</sup></td>
<td valign="top" align="center">6.6 &#x000B1; 0.7<sup>d</sup></td>
<td valign="top" align="center">3.8 &#x000B1; 0.3<sup>c</sup></td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<p><italic>Values represent mean &#x000B1; SE (n &#x0003D; 3). Odontella did not grow at low light in combination with low pCO<sub>2</sub> as indicated by /. Statistical differences between two treatments (p &#x0003D; 0.05) derived from post-hoc tests are indicated by different letters</italic>.</p>
</table-wrap-foot>
</table-wrap>
<p>Light had an influence on re-oxidation times of the primary electron acceptor Q<sub>a</sub> (&#x003C4;<sub>Qa</sub>, Table <xref ref-type="table" rid="T4">4</xref>), but with different effects for the two investigated species. In <italic>Fragilariopsis</italic>, at LL, low pCO<sub>2</sub> treatments showed the highest re-oxidation times with no differences between ambient and high pCO<sub>2</sub>, whereas at ML the re-oxidation time increased from low to high pCO<sub>2</sub>, and at HL no differences between pCO<sub>2</sub> treatments were detectable. In <italic>Odontella</italic>, at ambient pCO<sub>2</sub>, &#x003C4;<sub>Qa</sub> decreased from ML to HL. In the high pCO<sub>2</sub> treatments of <italic>Odontella</italic> &#x003C4;<sub>Qa</sub> increased with light. There was no light effect present in low pCO<sub>2</sub> treatments. When light was limiting (LL), &#x003C4;<sub>Qa</sub> was lower at high than at ambient pCO<sub>2</sub>. At ML and HL, in <italic>Odontella</italic> &#x003C4;<sub>Qa</sub> was less at low compared to ambient and high pCO<sub>2</sub>. At HL, the high pCO<sub>2</sub> treatments showed a higher &#x003C4;<sub>Qa</sub> than ambient treatments (results are insignificant due to a lack of statistical power).</p>
<p>The connectivity between PSIIs (p, Table <xref ref-type="table" rid="T4">4</xref>) was influenced by pCO<sub>2</sub> in <italic>Fragilariopsis</italic>. Low pCO<sub>2</sub> treatments showed decreased connectivity compared to ambient and high pCO<sub>2</sub> treatments at LL and ML. In <italic>Odontella</italic>, in all pCO<sub>2</sub> treatments p decreased from ML to HL. At ML, p increased from low to ambient pCO<sub>2</sub> and remained constant between ambient and high pCO<sub>2</sub>. At HL the high pCO<sub>2</sub> treatments showed the lowest p. Yet, statistical results for <italic>Odontella</italic> were not significant.</p>
<p>In <italic>Fragilariopsis</italic>, the concentration of PSII reaction centers ([RCII]) varied with light, decreasing significantly between LL and ML in the ambient and high pCO<sub>2</sub> treatments, respectively and increasing between ML and HL at ambient, but not at high pCO<sub>2</sub> (Table <xref ref-type="table" rid="T4">4</xref>). Only in the low pCO<sub>2</sub> treatments, [RCII] was not altered in response to increasing light intensities. At LL, [RCII] increased with increasing pCO<sub>2</sub> in <italic>Fragilariopsis</italic>, whereas at ML the ambient pCO<sub>2</sub> treatments showed higher concentrations than the low pCO<sub>2</sub> treatments and no difference from the high pCO<sub>2</sub> treatments. Compared to <italic>Fragilariopsis</italic>, in <italic>Odontella</italic> [RCII] exhibited a different pattern with light. Concentrations of RCII increased from LL to ML in ambient and high pCO<sub>2</sub> treatments, but decreased from ML to HL in all pCO<sub>2</sub> treatments. At LL, [RCII] did not change in response to pCO<sub>2</sub> in <italic>Odontella</italic>. At ML, [RCII] increased from low to ambient pCO<sub>2</sub>, but not from ambient to high pCO<sub>2</sub>. Only at HL, the low and high pCO<sub>2</sub> treatments displayed lower concentrations of RCII than the ambient pCO<sub>2</sub> treatments.</p>
</sec>
<sec>
<title>Cellular protective pigment content</title>
<p>The two diatom species showed different light-dependent trends in the de-epoxidation state (DES), an indicator for the dissipation of excess light energy (Table <xref ref-type="table" rid="T3">3</xref>). In <italic>Odontella</italic> DES increased with increasing light intensity in all pCO<sub>2</sub> treatments, whereas <italic>Fragilariopsis</italic> showed a bell shaped pattern. DES increased from LL to ML in <italic>Fragilariopsis</italic>, and decreased toward HL in all pCO<sub>2</sub> treatments. Besides the low pCO<sub>2</sub> treatments, no de-epoxidation was observed in <italic>Fragilariopsis</italic> at LL. Furthermore, in <italic>Fragilariopsis</italic> at ML and HL DES was lower in the low compared to ambient pCO<sub>2</sub> treatments. <italic>Odontella</italic> exhibited elevated DES only in the low pCO<sub>2</sub> treatments at ML and HL.</p>
</sec>
<sec>
<title>Non-photochemical quenching (NPQ)</title>
<p>The NPQ in <italic>Fragilariopsis</italic> showed an increase with increasing light intensity, while <italic>Odontella</italic> displayed a bell shaped pattern with highest quenching rates at ML (Figure <xref ref-type="fig" rid="F4">4</xref>). For the low pCO<sub>2</sub> treatments, NPQ reached higher values at LL in <italic>Fragilariopsis</italic> and at HL in <italic>Odontella</italic>.</p>
<fig id="F4" position="float">
<label>Figure 4</label>
<caption><p><bold>Non-photochemical quenching (NPQ, rel. unit) was determined in response to increasing irradiances in <italic>Fragilariopsis</italic> and <italic>Odontella</italic> acclimated to different light</bold> (LL &#x0003D; 20 in <bold>A,B</bold>; ML &#x0003D; 200 in <bold>C,D</bold>; HL &#x0003D; 500 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup> in <bold>E,F</bold>) and pCO<sub>2</sub> (low &#x0003D; 180, ambient &#x0003D; 380 and high &#x0003D; 1000 &#x003BC;atm) conditions. Values represent mean &#x000B1; SE (<italic>n</italic> &#x0003D; 3).</p></caption>
<graphic xlink:href="fmars-03-00260-g0004.tif"/>
</fig></sec></sec>
<sec sec-type="discussion" id="s4">
<title>Discussion</title>
<p>This study investigated the physiological responses of two Antarctic key diatom species over a range of low to high light intensities in combination with low, ambient and elevated pCO<sub>2</sub> levels. As future changes in water column stratification are considered to go in hand with ocean acidification, the potential for acclimation of Southern Ocean phytoplankton to these two factors can indicate potential future shifts in species composition. Next to climate change, light availability during summer and early spring greatly differs, with lower mean irradiances in spring (Dubinsky and Stambler, <xref ref-type="bibr" rid="B16">2009</xref>) and higher incident light during summer (Mitchell and Brody, <xref ref-type="bibr" rid="B49">1991</xref>; Mitchell and Holm-Hansen, <xref ref-type="bibr" rid="B50">1991</xref>; Nelson and Smith, <xref ref-type="bibr" rid="B54">1991</xref>). Moreover, large seasonal variation in pCO<sub>2</sub> is frequently observed. The pCO<sub>2</sub> in ocean surface waters is slightly elevated in early spring and can decrease tremendously during phytoplankton blooms (Sweeney, <xref ref-type="bibr" rid="B78">2003</xref>; Arrigo et al., <xref ref-type="bibr" rid="B4">2008</xref>). Our study was designed to link abiotic conditions to the physiological traits of phytoplankton species, in order to understand spatial and temporal distribution patterns under future light and pCO<sub>2</sub> scenarios. The two diatom species studied here were found to occur in high abundances during different times of the year. <italic>Odontella weisflogii</italic> (<italic>Odontella</italic>) forms blooms in Antarctic coastal waters in summer (Garibotti et al., <xref ref-type="bibr" rid="B21">2005</xref>; Annett et al., <xref ref-type="bibr" rid="B2">2010</xref>), whereas elevated abundances of <italic>Fragilariopsis curta</italic> (<italic>Fragilariopsis</italic>) were observed rather early in season when the sea ice retreats (Garibotti et al., <xref ref-type="bibr" rid="B21">2005</xref>; Annett et al., <xref ref-type="bibr" rid="B2">2010</xref>). In our study, the observed physiological responses of <italic>Fragilariopsis</italic> and <italic>Odontella</italic> were clearly species-specific and varied largely in response to the applied CO<sub>2</sub> and light scenarios and could further be related to their seasonal occurrence.</p>
<sec>
<title>Light optima for photosynthesis are species-specific</title>
<p>Under ambient pCO<sub>2</sub>, an increase in light intensity from low light (LL) to medium light (ML) stimulated growth by 42% in <italic>Odontella</italic>, with no further stimulation between ML and high light (HL, Figure <xref ref-type="fig" rid="F1">1B</xref>), indicating that growth was saturated at ML in this species. Other studies also reported that growth was stimulated by light when increased from lower to higher irradiances in various diatoms and prymnesiophytes (Bartual and G&#x000E1;lvez, <xref ref-type="bibr" rid="B5">2002</xref>; Arrigo et al., <xref ref-type="bibr" rid="B3">2010</xref>; Boelen et al., <xref ref-type="bibr" rid="B7">2011</xref>). Congruently, growth of <italic>Fragilariopsis</italic> was also stimulated by 20% from LL to ML, but declined by 58% from ML to HL (Figure <xref ref-type="fig" rid="F1">1A</xref>). Such a decline at high light intensities was already found in the diatom <italic>Phaeodactylum tricornutum</italic> and the prymnesiophyte <italic>Phaeocystis antarctica</italic> (Arrigo et al., <xref ref-type="bibr" rid="B3">2010</xref>; Li et al., <xref ref-type="bibr" rid="B43">2014</xref>). In <italic>Fragilariopsis</italic>, particulate organic carbon (POC) production rates and quantum yield of photosynthesis (F<sub>v</sub>/F<sub>m</sub>), a measure of a cell&#x00027;s photosynthetic performance, were highest under LL and decreased from LL to ML, indicating saturation of photosynthesis already at LL conditions and an onset of light stress under ML (Figures <xref ref-type="fig" rid="F1">1C</xref>, <xref ref-type="fig" rid="F3">3A</xref>). In contrast, POC production increased from LL to ML in <italic>Odontella</italic>. This finding suggests that even under LL conditions <italic>Fragilariopsis</italic> was able to fix POC at a maximum rate while for <italic>Odontella</italic> this was only the case at ML, thus indicating species-specific light optima for photosynthesis. Despite the decrease in POC production from LL to ML in <italic>Fragilariopsis</italic>, growth increased suggesting that cell volumes might have changed. However, cell size measurements did not show any changes in both species and in all treatments (data not shown). Considering further that cell volume of <italic>Odontella</italic> was on average 2000 times larger than of <italic>Fragilariopsis</italic> (cell volumes estimated based on Hillebrand et al. (<xref ref-type="bibr" rid="B28">1999</xref>), data not shown) this potentially implied a much higher carbon demand in the former. For both species from ML to HL, we observed a significant decline in POC production (Figures <xref ref-type="fig" rid="F1">1C,D</xref>) and in <italic>Odontella</italic> a decrease in F<sub>v</sub>/F<sub>m</sub> (Figure <xref ref-type="fig" rid="F3">3B</xref>). In contrast to this observation, ETRm increased in both species from LL to HL, indicating no light saturation (Table <xref ref-type="table" rid="T2">2</xref>). Due to this, the observed reduced POC production rates, between LL and HL in <italic>Fragilariopsis</italic> and between ML and HL in <italic>Odontella</italic>, might have resulted from a saturation of the Calvin-Benson-Cycle. The Calvin-Benson-Cycle is considered to be the rate-limiting step of photosynthesis under excessive light conditions, thus creating the demand of alternative electron pathways such as Mehler reaction, midstream oxidase pathways and cyclic electron transport around PSI to dissipate excess electrons (Behrenfeld and Milligan, <xref ref-type="bibr" rid="B6">2012</xref>). Cyclic electron transport would rise the transthylakoid pH gradient and consequently lead to a higher production of ATP at the expense of NADPH and thereby would result in lower POC fixation rates (Falk and Palmqvist, <xref ref-type="bibr" rid="B17">1992</xref>). Congruently with the changes in POC production the photosynthetic performance (F<sub>v</sub>/F<sub>m</sub>) declined from LL to ML in <italic>Fragilariopsis</italic> and from ML to HL in <italic>Odontella</italic> (Figures <xref ref-type="fig" rid="F1">1C,D</xref>, <xref ref-type="fig" rid="F3">3A,B</xref>). With increasing irradiance, F<sub>v</sub>/F<sub>m</sub> was commonly found to decrease in various temperate and Antarctic phytoplankton species (Boelen et al., <xref ref-type="bibr" rid="B7">2011</xref>; Hoogstraten et al., <xref ref-type="bibr" rid="B30">2012</xref>; Li et al., <xref ref-type="bibr" rid="B43">2014</xref>) implying a lower photosynthetic capacity through photoinhibition and eventually photodamage of PSII. The observed species-specific changes in F<sub>v</sub>/F<sub>m</sub> may have resulted from a decreased ratio of photons absorbed per electrons generated in PSII. The amount of electrons generated depends on the cell&#x00027;s ability to capture light energy via light-harvesting pigments and the amount of functional PSII reaction centers. Less active PSII can result from closure of reaction centers (Schreiber, <xref ref-type="bibr" rid="B72">2004</xref>) through photodamage (e.g., damage of D1 protein of PSII; Alderkamp et al., <xref ref-type="bibr" rid="B1">2010</xref>), which can be an initial stage of photoacclimation process yielding reduced concentrations of PSII (Sakshaug et al., <xref ref-type="bibr" rid="B71">1997</xref>).</p>
<p>For both diatoms, cellular concentrations of light-harvesting pigments (Ch <italic>a</italic>, Chl c2, fucoxanthin) significantly decreased similarly between LL and ML conditions, suggesting an acclimation to increased light by reducing light-harvesting pigment concentration for both species (Table <xref ref-type="table" rid="T3">3</xref>). Yet, between ML and HL concentrations of light-harvesting pigments remained similar in both species, indicating a lower limit of pigment content for light absorption. We, however, found that concentrations of functional reaction centers ([RCII]) and F<sub>v</sub>/F<sub>m</sub> decreased significantly between ML and HL in <italic>Odontella</italic> while the absorption cross section of PSII (&#x003C3;<sub>PSII</sub>) remained unchanged (Figure <xref ref-type="fig" rid="F3">3B</xref>, Table <xref ref-type="table" rid="T4">4</xref>). This shows that <italic>Odontella</italic> experienced stress at HL compared to ML. In comparison, F<sub>v</sub>/F<sub>m</sub>, [RCII] and &#x003C3;<sub>PSII</sub> already declined from LL to ML in <italic>Fragilariopsis</italic> (Figure <xref ref-type="fig" rid="F3">3A</xref>, Table <xref ref-type="table" rid="T4">4</xref>). This finding suggests a higher susceptibility of this species to light stress already at moderate light intensities, yet these did not affect growth rates until HL conditions were applied.</p>
<p>To counteract photodamage, phytoplankton cells possess various strategies such as non-photochemical quenching (NPQ) including the operation of the xanthophyll cycle (XC), therefore dissipation of excess light energy in <italic>Odontella</italic> and <italic>Fragilariopsis</italic> was investigated via the concentrations of cellular diadinoxanthin (DD), its de-epoxidised form diatoxanthin (DT) and the de-epoxidation state (DES). An increase in DES (Table <xref ref-type="table" rid="T3">3</xref>) with incident light is a response commonly found in phytoplankton (Casper-Lindley and Bj&#x000F6;rkman, <xref ref-type="bibr" rid="B12">1998</xref>; Arrigo et al., <xref ref-type="bibr" rid="B3">2010</xref>; Petrou et al., <xref ref-type="bibr" rid="B57">2011</xref>). NPQ increased from LL to HL in <italic>Fragilariopsis</italic> while in <italic>Odontella</italic> it increased mainly from LL to ML, but decreased from ML to HL (Figure <xref ref-type="fig" rid="F4">4</xref>). In <italic>Odontella</italic>, DES rose from LL to HL whereas there was no XC activity detectable in <italic>Fragilariopsis</italic> at LL, but there was a decrease from ML to HL (Table <xref ref-type="table" rid="T3">3</xref>). The discrepancy in the trends of NPQ and DES from ML to HL in both species could result from smaller and much larger cellular DD&#x0002B;DT pools in <italic>Odontella</italic> and <italic>Fragilariopsis</italic> (&#x02212;60 and &#x0002B;300%; Table <xref ref-type="table" rid="T3">3</xref>), respectively under these conditions changing the general capacity for energy dissipation.</p>
<p>Overall, the two diatom species showed diverging responses to increasing light at ambient pCO<sub>2</sub> during acclimation. <italic>Fragilariopsis</italic> was characterized by highest POC production rates and photosynthetic performance (F<sub>v</sub>/F<sub>m</sub>) under LL, but experienced light stress with increasing light intensity, as POC production rates decreased and NPQ increased from LL to HL. Hence, it showed good ability for energy dissipation even under HL conditions and thus seemed better able to cope with light stress. In comparison, <italic>Odontella</italic> showed an increase in POC production rates from LL to ML, indicating no saturation at LL. With increasing light intensities, <italic>Odontella</italic> was susceptible to light stress as POC production, F<sub>v</sub>/F<sub>m</sub> and NPQ declined indicating a limited potential to tolerate HL conditions.</p>
</sec>
<sec>
<title>Low pCO<sub>2</sub> inhibits growth and carbon fixation regardless of the light conditions</title>
<p>Phytoplankton blooms in Antarctic coastal waters occur annually and have been found to sometimes coincide with a severe drawdown of inorganic carbon through high photosynthetic carbon fixation rates in surface waters (Sweeney, <xref ref-type="bibr" rid="B78">2003</xref>; Arrigo et al., <xref ref-type="bibr" rid="B4">2008</xref>). In order to sustain photosynthesis under these low CO<sub>2</sub> conditions, phytoplankton cells need to up-regulate their carbon concentrating mechanisms (CCMs) leading to increased energy demands and potentially impeding carbon fixation (Raven et al., <xref ref-type="bibr" rid="B63">2014</xref>).</p>
<p>Low pCO<sub>2</sub> in combination with LL was found to have the strongest impact on growth and carbon fixation in comparison to all other treatments. Under these conditions, both factors light and CO<sub>2</sub> were limiting, causing lowest growth and POC production rates in <italic>Fragilariopsis</italic> while <italic>Odontella</italic> did not grow (Figures <xref ref-type="fig" rid="F1">1A&#x02013;D</xref>). Commonly, the CCM is up-regulated under low pCO<sub>2</sub> in order to supply CO<sub>2</sub> to RubisCO, which is highly energy demanding (Hopkinson et al., <xref ref-type="bibr" rid="B31">2011</xref>). Yet, in conjunction with LL conditions, the production of energy equivalents during photosynthesis might not be sufficient to maintain carbon fixation at a maximum, potentially causing the here observed minimal growth and POC production in <italic>Fragilariopsis</italic>. Additionally, light-harvesting pigment concentrations (Table <xref ref-type="table" rid="T3">3</xref>), [RCII] and p (Table <xref ref-type="table" rid="T4">4</xref>) were lowest under these conditions, indicating a small efficiency of individual PSII reactions centers with a low probability of excitation distribution among them. Furthermore, an excess of excitation energy was clearly visible as NPQ during PE-curves (Figure <xref ref-type="fig" rid="F4">4</xref>) was highest and yield recovery thereafter was lowest (Figure <xref ref-type="fig" rid="F3">3C</xref>). Overall, <italic>Fragilariopsis</italic> revealed great difficulties to grow under LL in conjunction with low pCO<sub>2</sub>. Nonetheless, it grew whereas <italic>Odontella</italic> could not cope with these highly stressful conditions. With increasing light availability the energetic constraints under LL were alleviated in both species, as potentially a larger share of photosynthetically generated energy (ATP and NADPH) was available to fuel their CCMs. Hence, at ML in conjunction with low pCO<sub>2</sub> <italic>Odontella</italic> was able to grow and fix POC. This stimulative light effect was also found in <italic>Fragilariopsis</italic>, strongly increasing growth and POC production from LL to ML (Figures <xref ref-type="fig" rid="F1">1A,C</xref>).</p>
<p>Within the ML treatments, pCO<sub>2</sub> was also found to stimulate growth rates of <italic>Odontella</italic> and <italic>Fragilariopsis</italic> by 8 and 42% from low to ambient pCO<sub>2</sub>, respectively (Figures <xref ref-type="fig" rid="F1">1A,B</xref>), suggesting optimal growth conditions for both species at ambient pCO<sub>2</sub>. A similar CO<sub>2</sub>-dependent increase in growth was previously reported for the two polar diatoms <italic>Rhizosolenia</italic> cf. <italic>alata</italic> and <italic>C. debilis</italic> (Riebesell et al., <xref ref-type="bibr" rid="B68">1993</xref>; Trimborn et al., <xref ref-type="bibr" rid="B80">2013</xref>). POC production was enhanced from low to ambient pCO<sub>2</sub> levels in <italic>Odontella</italic> (Figure <xref ref-type="fig" rid="F1">1D</xref>) potentially resulting from a higher diffusive CO<sub>2</sub> supply and therewith a lower energy demand. However, for <italic>Fragilariopsis</italic> we observed a CO<sub>2</sub>-dependent decline in POC production (Figure <xref ref-type="fig" rid="F1">1C</xref>). This decline was accompanied by a reduced capability for light absorption as cellular light-harvesting pigment concentrations were decreased at ambient compared to low pCO<sub>2</sub> (Chl <italic>a</italic>, Chl c2, fucoxanthin, Table <xref ref-type="table" rid="T3">3</xref>). Please note that <italic>Fragilariopsis</italic> experienced light stress already at ML when grown at ambient pCO<sub>2</sub>, hinting toward a higher susceptibility to light stress in this species. Through the down-regulation of the CCM from low to ambient pCO<sub>2</sub>, it may serve less as an energy sink and thereby increasing light stress exerted by excessive light (Gao et al., <xref ref-type="bibr" rid="B20">2012</xref>). This was, however, not reflected in any change in F<sub>v</sub>/F<sub>m</sub>. In <italic>Odontella</italic>, under ML absETRs, ETRm, I<sub>K</sub> and &#x003B1; decreased from low to ambient pCO<sub>2</sub> while POC production increased indicating that carbon uptake might not have been sufficient to saturate RubisCO and the Calvin-Benson-Cycle. The reason for this might be its higher cell volume compared to <italic>Fragilariopsis</italic> and thereby higher amount of carbon necessary to saturate the Calvin-Benson-Cycle and to sustain growth. Increased absETR under these conditions could further indicate cycling of electrons around PSI and thus generation of energy equivalents that could be funneled into carbon uptake. At HL, we observed an increase of the photosynthetic efficiency from low to ambient pCO<sub>2</sub>treatments of both species, displaying higher absETR (Figures <xref ref-type="fig" rid="F2">2E,F</xref>), ETRm, I<sub>K</sub>, &#x003B1; (Table <xref ref-type="table" rid="T2">2</xref>), &#x003C3;<sub>PSII</sub>, &#x003C4;<sub>Qa</sub> (<italic>Odontella</italic> only), p and [RCII] (<italic>Fragilariopsis</italic> only, Table <xref ref-type="table" rid="T4">4</xref>) while NPQ and DD&#x0002B;DT pools decreased in both species, indicating lowered energy dissipation with increasing pCO<sub>2</sub>. Hence, in the low pCO<sub>2</sub> treatments the HL was not utilized, but cells rather dissipated the excess light energy absorbed. As the CCM of both species was potentially down-regulated from low to ambient pCO<sub>2</sub>, the higher photosynthetic efficiencies as well as lowered energy dissipation at HL suggest that the CCM does not represent an important sink for excess energy under high light conditions (Gao et al., <xref ref-type="bibr" rid="B20">2012</xref>).</p>
<p>Overall, this study revealed that low pCO<sub>2</sub> concentrations were stressful for both Antarctic diatoms, but especially in conjunction with light limiting conditions. According to our results, the hypothesis that the regulation of the CCM aids in the dissipation of excess energy at high light intensities cannot be conclusively answered for the two species tested here.</p>
</sec>
<sec>
<title>OA effects are modulated by light availability</title>
<p>Under OA, Antarctic diatoms might benefit from diffusive CO<sub>2</sub> uptake as has been shown for temperate species (Burkhardt et al., <xref ref-type="bibr" rid="B11">2001</xref>; Rost et al., <xref ref-type="bibr" rid="B70">2003</xref>; Trimborn et al., <xref ref-type="bibr" rid="B82">2009</xref>), decreasing the demand for CCM operation. Especially under limiting light conditions, the lowered energy demand through down-regulation of the CCM was found to stimulate growth and carbon fixation in temperate phytoplankton species (Wu et al., <xref ref-type="bibr" rid="B85">2010</xref>; Li et al., <xref ref-type="bibr" rid="B43">2014</xref>). Similarly, the temperate coccolithophorid <italic>Emiliania huxleyi</italic> showed increased POC production rates under OA when irradiances are low, yet under higher light intensities this effect was amended (Rokitta and Rost, <xref ref-type="bibr" rid="B69">2012</xref>). In our investigated species, however, growth and POC production remained either unaffected or declined under OA and LL (Figures <xref ref-type="fig" rid="F1">1A&#x02013;D</xref>) contradicting the aforementioned assumption of a stimulative effect of OA, but going in line with other findings for Antarctic phytoplankton species (Hoogstraten et al., <xref ref-type="bibr" rid="B30">2012</xref>). We even observed for <italic>Fragilariopsis</italic> negative effects of OA under LL on light-harvesting pigment concentrations (Chl <italic>a</italic>, Chl c2, and fucoxanthin; Table <xref ref-type="table" rid="T3">3</xref>) potentially compensated by an increased number of active RCII (Table <xref ref-type="table" rid="T4">4</xref>). Interestingly, in <italic>Odontella</italic> light harvesting pigments (Chl c2, fucoxanthin, Table <xref ref-type="table" rid="T3">3</xref>) were increased under elevated pCO<sub>2</sub>, indicating a maximization of light absorption under LL. In agreement with this, an OA-dependent induction of chlorophyll-fucoxanthin protein genes were reported for the temperate diatom <italic>Phaeodactylum tricornutum</italic> (Li et al., <xref ref-type="bibr" rid="B44">2015</xref>). In addition to this, enhanced rates of mitochondrial respiration were previously reported under OA in combination with relatively LL levels in the temperate diatom <italic>Thalassiosira pseudonana</italic> (Yang and Gao, <xref ref-type="bibr" rid="B87">2012</xref>). Together with the species-specific photoacclimation responses under OA, one could hypothesize that the two investigated species may have experienced higher metabolic costs, potentially causing the observed decline in POC production.</p>
<p>For both species, the negative OA effects were amplified under ML conditions. Next to negative responses in growth and POC production (Figures <xref ref-type="fig" rid="F1">1A&#x02013;D</xref>), the two species displayed OA-dependent photoacclimation. While <italic>Odontella</italic> revealed lowered photochemical efficiencies (Figure <xref ref-type="fig" rid="F3">3B</xref>), <italic>Fragilariopsis</italic> had less active RCIIs with reduced connectivity between PSIIs (Table <xref ref-type="table" rid="T4">4</xref>) potentially counteracted by increased light harvesting pigmentation (Chl <italic>a</italic> and fucoxanthin, Table <xref ref-type="table" rid="T3">3</xref>). For both species, acclimation to high light conditions was indicated by a larger cellular DD&#x0002B;DT pool size (Table <xref ref-type="table" rid="T3">3</xref>). This is in line with previous suggestions that down-regulated CCMs serve less as a sink for excess light energy under OA in conjunction with saturating light intensities (Gao et al., <xref ref-type="bibr" rid="B20">2012</xref>). However, this positive effect of CCM operation under excessive irradiances was not found when comparing low and ambient pCO<sub>2</sub> treatments under HL (see discussion above). Unexpectedly, this negative OA effect was alleviated under HL conditions in our two tested species. In this case, growth rates and POC production remained unaffected (Figures <xref ref-type="fig" rid="F1">1A&#x02013;C</xref>). Only for <italic>Fragilariopsis</italic>, POC production was stimulated by OA and HL. For the latter, C:N ratios were also found to raise (Figure <xref ref-type="fig" rid="F1">1E</xref>). For the two coccolithophores <italic>Gephyrocapsa oceanica</italic> and <italic>Coccolithus pelagicus</italic> ssp. <italic>braarudii</italic>, OA also increased POC production rates, but C:N ratios were either stimulated (200 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>, Rickaby et al., <xref ref-type="bibr" rid="B67">2010</xref>) or reduced (100 &#x003BC;mol photons m<sup>&#x02212;2</sup> s<sup>&#x02212;1</sup>, Jin et al., <xref ref-type="bibr" rid="B36">2013</xref>) in <italic>G. oceanica</italic>. In our study, the CO<sub>2</sub>-dependent increase in C:N ratios under HL was mainly due to lowered cellular PON content (data not shown), the underlying reason for this, however, remains unclear.</p>
<p>From our results, we can conclude that OA in conjunction with all tested irradiances did not lead to stimulation in growth or POC production in any of the tested species. It was, however, evident that increasing light intensities during acclimation caused OA-dependent photoacclimation responses and negatively impacted POC production. Only under HL, this OA effect was alleviated in <italic>Odontella</italic>, while in <italic>Fragilariopsis</italic> POC production was even increased, potentially resulting from a shift in carbon allocation. Congruently we cannot support the finding that a down-regulation of the CCM and consequent decrease of energy dissipation therein increases light stress under OA in conjunction with HL in these Antarctic diatoms.</p>
</sec>
<sec>
<title>Ecological implications and conclusion</title>
<p>Antarctic coastal waters were found to have high iron concentrations and form highly productive and extensive blooms over the season (Holm-Hansen et al., <xref ref-type="bibr" rid="B29">1989</xref>; Martin et al., <xref ref-type="bibr" rid="B46">1990</xref>; Pr&#x000E9;zelin et al., <xref ref-type="bibr" rid="B60">2000</xref>; Garibotti et al., <xref ref-type="bibr" rid="B22">2003</xref>; de Jong et al., <xref ref-type="bibr" rid="B14">2012</xref>). Annual patterns of phytoplankton species succession and their presence in either spring or summer blooms can be related to species-specific abilities to acclimate, utilize and tolerate different light intensities. The physiological characteristics of both species we observed match well their seasonal occurrence. In line with its presence in spring (Garibotti et al., <xref ref-type="bibr" rid="B21">2005</xref>; Annett et al., <xref ref-type="bibr" rid="B2">2010</xref>), <italic>Fragilariopsis</italic> showed greater ability than <italic>Odontella</italic> to grow under LL conditions. Accordingly, it was characterized by highest POC production rates under limiting light as well as a good ability to endure high light stress when mixed to the water surface. <italic>Odontella</italic> was still light limited under LL, requiring higher irradiances coinciding with its occurrence in high abundances in summer when the upper mixed layer is shallow and stable (Mitchell and Holm-Hansen, <xref ref-type="bibr" rid="B50">1991</xref>; Nelson and Smith, <xref ref-type="bibr" rid="B54">1991</xref>). Congruently, it was able to endure longer periods of high irradiances. Yet, at the peak of a bloom when cell density is high, light is reduced and CO<sub>2</sub> gets drawn down by high photosynthetic activity, this creates very unfavorable growth conditions for <italic>Odontella</italic>.</p>
<p>Strong species-specific physiological responses were apparent in response to different future climate scenarios, mimicking either OA in conjunction with increased irradiances due to shallower UML depth or OA associated with decreased daily irradiances due to deepening of the UML through increased winds. Under ML, both species experienced light stress, which was further amplified by OA. Yet, in the HL OA-scenario <italic>Fragilariopsis</italic> was able to tolerate the HL conditions. Also under the LL OA-scenario, neither of the investigated species showed an OA-dependent stimulation in growth or POC production. Hence, OA mainly showed negative effects on growth and carbon fixation in both diatom species, implying that OA could potentially reduce the strength of the biological carbon pump under the tested light scenarios.</p>
<p>The results of this study indicate that physiological traits can help to explain the spatial distribution of diatom species in the current Southern Ocean. We further demonstrate that the here tested future climatic scenarios could negatively affect growth and carbon fixation of both diatom species with potential implications for a future SO. Furthermore, the results of this study demonstrated that the effect of OA was strongly modulated by the irradiance regime, pointing out the need to conduct multiple stressor experiments to better understand the impact of climate change on Southern Ocean key phytoplankton species.</p>
</sec></sec>
<sec id="s5">
<title>Author contributions</title>
<p>JH acquired the presented data. JH, KB, and ST were involved in the study conception and design, the analysis and interpretation of data as well as drafting and critically revising the manuscript.</p>
</sec>
<sec id="s6">
<title>Funding</title>
<p>ST and JH were funded by the Helmholtz Impulse Fond (HGF Young Investigators Group EcoTrace).</p>
<sec>
<title>Conflict of interest statement</title>
<p>The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest. The reviewer PJ and handling Editor declared their shared affiliation, and the handling Editor states that the process nevertheless met the standards of a fair and objective review</p></sec>
</sec>
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<ack><p>We would like to thank Britta Meyer-Schlosser and Tina Brenneis for laboratory assistance.</p>
</ack>
<ref-list>
<title>References</title>
<ref id="B1">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Alderkamp</surname> <given-names>A.-C.</given-names></name> <name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name> <name><surname>Visser</surname> <given-names>R. J. W.</given-names></name> <name><surname>Arrigo</surname> <given-names>K. R.</given-names></name></person-group> (<year>2010</year>). <article-title>Can photoinhibition control phytoplankton abundance in deeply mixed water columns of the Southern Ocean?</article-title> <source>Limnol. Oceanogr.</source> <volume>55</volume>, <fpage>1248</fpage>&#x02013;<lpage>1264</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2010.55.3.1248</pub-id></citation>
</ref>
<ref id="B2">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Annett</surname> <given-names>A. L.</given-names></name> <name><surname>Carson</surname> <given-names>D. S.</given-names></name> <name><surname>Crosta</surname> <given-names>X.</given-names></name> <name><surname>Clarke</surname> <given-names>A.</given-names></name> <name><surname>Ganeshram</surname> <given-names>R. S.</given-names></name></person-group> (<year>2010</year>). <article-title>Seasonal progression of diatom assemblages in surface waters of Ryder Bay, Antarctica</article-title>. <source>Polar Biol.</source> <volume>33</volume>, <fpage>13</fpage>&#x02013;<lpage>29</lpage>. <pub-id pub-id-type="doi">10.1007/s00300-009-0681-7</pub-id></citation>
</ref>
<ref id="B3">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Arrigo</surname> <given-names>K. R.</given-names></name> <name><surname>Mills</surname> <given-names>M. M.</given-names></name> <name><surname>Kropuenske</surname> <given-names>L. R.</given-names></name> <name><surname>Van Dijken</surname> <given-names>G. L.</given-names></name> <name><surname>Alderkamp</surname> <given-names>A. C.</given-names></name> <name><surname>Robinson</surname> <given-names>D. H.</given-names></name></person-group> (<year>2010</year>). <article-title>Photophysiology in two major southern ocean phytoplankton taxa: Photosynthesis and growth of Phaeocystis antarctica and Fragilariopsis cylindrus under different irradiance levels</article-title>. <source>Integr. Comp. Biol.</source> <fpage>950</fpage>&#x02013;<lpage>966</lpage>. <pub-id pub-id-type="doi">10.1093/icb/icq021</pub-id><pub-id pub-id-type="pmid">21558252</pub-id></citation>
</ref>
<ref id="B4">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Arrigo</surname> <given-names>K. R.</given-names></name> <name><surname>van Dijken</surname> <given-names>G.</given-names></name> <name><surname>Long</surname> <given-names>M.</given-names></name></person-group> (<year>2008</year>). <article-title>Coastal Southern Ocean: a strong anthropogenic CO<sub>2</sub> sink</article-title>. <source>Geophys. Res. Lett.</source> <volume>35</volume>, <fpage>1</fpage>&#x02013;<lpage>6</lpage>. <pub-id pub-id-type="doi">10.1029/2008GL035624</pub-id></citation>
</ref>
<ref id="B5">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Bartual</surname> <given-names>A.</given-names></name> <name><surname>G&#x000E1;lvez</surname> <given-names>J. A.</given-names></name></person-group> (<year>2002</year>). <article-title>Growth and biochemical composition of the diatom <italic>Phaeodactylum tricornutum</italic> at different pH and inorganic carbon levels under saturating and subsaturating light regimes</article-title>. <source>Bot. Mar.</source> <volume>45</volume>, <fpage>491</fpage>&#x02013;<lpage>501</lpage>. <pub-id pub-id-type="doi">10.1515/BOT.2002.052</pub-id></citation>
</ref>
<ref id="B6">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Behrenfeld</surname> <given-names>M. J.</given-names></name> <name><surname>Milligan</surname> <given-names>A. J.</given-names></name></person-group> (<year>2012</year>). <article-title>Photophysiological expressions of iron stress in phytoplankton</article-title>. <source>Ann. Rev. Mar. Sci.</source> <volume>5</volume>, <fpage>217</fpage>&#x02013;<lpage>246</lpage>. <pub-id pub-id-type="doi">10.1146/annurev-marine-121211-172356</pub-id><pub-id pub-id-type="pmid">22881354</pub-id></citation>
</ref>
<ref id="B7">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Boelen</surname> <given-names>P.</given-names></name> <name><surname>van de Poll</surname> <given-names>W. H.</given-names></name> <name><surname>van der Strate</surname> <given-names>H. J.</given-names></name> <name><surname>Neven</surname> <given-names>I. A.</given-names></name> <name><surname>Beardall</surname> <given-names>J.</given-names></name> <name><surname>Buma</surname> <given-names>A. G. J.</given-names></name></person-group> (<year>2011</year>). <article-title>Neither elevated nor reduced CO<sub>2</sub> affects the photophysiological performance of the marine Antarctic diatom <italic>Chaetoceros brevis</italic></article-title>. <source>J. Exp. Mar. Bio. Ecol.</source> <volume>406</volume>, <fpage>38</fpage>&#x02013;<lpage>45</lpage>. <pub-id pub-id-type="doi">10.1016/j.jembe.2011.06.012</pub-id></citation>
</ref>
<ref id="B8">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Boyd</surname> <given-names>P. W.</given-names></name> <name><surname>Dillingham</surname> <given-names>P. W.</given-names></name> <name><surname>McGraw</surname> <given-names>C. M.</given-names></name> <name><surname>Armstrong</surname> <given-names>E. A.</given-names></name> <name><surname>Cornwall</surname> <given-names>C. E.</given-names></name> <name><surname>Feng</surname> <given-names>Y. Y.</given-names></name> <etal/></person-group>. (<year>2015a</year>). <article-title>Physiological responses of a Southern Ocean diatom to complex future ocean conditions</article-title>. <source>Nat. Clim. Chang.</source> <volume>6</volume>, <fpage>207</fpage>&#x02013;<lpage>213</lpage>. <pub-id pub-id-type="doi">10.1038/nclimate2811</pub-id></citation>
</ref>
<ref id="B9">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Boyd</surname> <given-names>P. W.</given-names></name> <name><surname>Lennartz</surname> <given-names>S. T.</given-names></name> <name><surname>Glover</surname> <given-names>D. M.</given-names></name> <name><surname>Doney</surname> <given-names>S. C.</given-names></name></person-group> (<year>2015b</year>). <article-title>Biological ramifications of climate-change-mediated oceanic multi-stressors</article-title>. <source>Nat. Clim. Chang.</source> <volume>5</volume>, <fpage>71</fpage>&#x02013;<lpage>79</lpage>. <pub-id pub-id-type="doi">10.1038/nclimate2441</pub-id></citation>
</ref>
<ref id="B10">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Brewer</surname> <given-names>P. G.</given-names></name> <name><surname>Bradshaw</surname> <given-names>A. L.</given-names></name> <name><surname>Williams</surname> <given-names>R. T.</given-names></name></person-group> (<year>1986</year>). <article-title>Measurements of total carbon dioxide and alkalinity in the North Atlantic Ocean in 1981</article-title>, in <source>The Changing Carbon Cycle</source>, eds <person-group person-group-type="editor"><name><surname>Trabalka</surname> <given-names>J. R.</given-names></name> <name><surname>Reichle</surname> <given-names>D. E.</given-names></name></person-group> (<publisher-loc>New York, NY</publisher-loc>: <publisher-name>Springer</publisher-name>), <fpage>348</fpage>&#x02013;<lpage>370</lpage>.</citation>
</ref>
<ref id="B11">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Burkhardt</surname> <given-names>S.</given-names></name> <name><surname>Amoroso</surname> <given-names>G.</given-names></name> <name><surname>Riebesell</surname> <given-names>U.</given-names></name> <name><surname>Sultemeyer</surname> <given-names>D.</given-names></name></person-group> (<year>2001</year>). <article-title>CO<sub>2</sub> and HCO3- uptake in marine diatoms acclimated to different CO<sub>2</sub> concentrations</article-title>. <source>Limnol. Oceanogr.</source> <volume>46</volume>, <fpage>1378</fpage>&#x02013;<lpage>1391</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2001.46.6.1378</pub-id></citation>
</ref>
<ref id="B12">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Casper-Lindley</surname> <given-names>C.</given-names></name> <name><surname>Bj&#x000F6;rkman</surname> <given-names>O.</given-names></name></person-group> (<year>1998</year>). <article-title>Fluorescence quenching in four unicellular algae with different light-harvesting and xanthophyll-cycle pigments</article-title>. <source>Photosyn. Res.</source> <volume>56</volume>, <fpage>277</fpage>&#x02013;<lpage>289</lpage>. <pub-id pub-id-type="doi">10.1023/A:1006037516479</pub-id></citation>
</ref>
<ref id="B13">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Comiso</surname> <given-names>J. C.</given-names></name> <name><surname>McClain</surname> <given-names>C. R.</given-names></name> <name><surname>Sullivan</surname> <given-names>C. W.</given-names></name> <name><surname>Ryan</surname> <given-names>J. P.</given-names></name> <name><surname>Leonard</surname> <given-names>C. L.</given-names></name></person-group> (<year>1993</year>). <article-title>Coastal zone color scanner pigment concentration in the Southern Ocean and relationships to geophysical surface features</article-title>. <source>J. Geophys. Res.</source> <volume>98</volume>, <fpage>2419</fpage>&#x02013;<lpage>2451</lpage>. <pub-id pub-id-type="doi">10.1029/92JC02505</pub-id></citation>
</ref>
<ref id="B14">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>de Jong</surname> <given-names>J.</given-names></name> <name><surname>Schoemann</surname> <given-names>V.</given-names></name> <name><surname>Lannuzel</surname> <given-names>D.</given-names></name> <name><surname>Croot</surname> <given-names>P.</given-names></name> <name><surname>de Baar</surname> <given-names>H.</given-names></name> <name><surname>Tison</surname> <given-names>J.-L.</given-names></name></person-group> (<year>2012</year>). <article-title>Natural iron fertilization of the Atlantic sector of the Southern Ocean by continental shelf sources of the Antarctic Peninsula</article-title>. <source>J. Geophys. Res.</source> <volume>117</volume>:<fpage>G01029</fpage>. <pub-id pub-id-type="doi">10.1029/2011JG001679</pub-id></citation>
</ref>
<ref id="B15">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Dickson</surname> <given-names>A. G.</given-names></name> <name><surname>Millero</surname> <given-names>F. J.</given-names></name></person-group> (<year>1987</year>). <article-title>A comparison of the equilibrium constants for the dissociation of carbonic acid in seawater media</article-title>. <source>Deep Sea Res.</source> <volume>34</volume>, <fpage>1733</fpage>&#x02013;<lpage>1743</lpage>. <pub-id pub-id-type="doi">10.1016/0198-0149(87)90021-5</pub-id></citation>
</ref>
<ref id="B16">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Dubinsky</surname> <given-names>Z.</given-names></name> <name><surname>Stambler</surname> <given-names>N.</given-names></name></person-group> (<year>2009</year>). <article-title>Photoacclimation processes in phytoplankton: mechanisms, consequences, and applications</article-title>. <source>Aquat. Microb. Ecol.</source> <volume>56</volume>, <fpage>163</fpage>&#x02013;<lpage>176</lpage>. <pub-id pub-id-type="doi">10.3354/ame01345</pub-id></citation>
</ref>
<ref id="B17">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Falk</surname> <given-names>S.</given-names></name> <name><surname>Palmqvist</surname> <given-names>K.</given-names></name></person-group> (<year>1992</year>). <article-title>Photosynthetic light utilization efficiency, photosystem II heterogeneity, and fluorescence quenching in Chlamydomonas reinhardtii during the induction of the CO2-concentrating mechanism</article-title>. <source>Plant Physiol.</source> <volume>100</volume>, <fpage>685</fpage>&#x02013;<lpage>691</lpage>. <pub-id pub-id-type="doi">10.1104/pp.100.2.685</pub-id></citation>
</ref>
<ref id="B18">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Falkowski</surname> <given-names>P. G.</given-names></name> <name><surname>Raven</surname> <given-names>J. A.</given-names></name></person-group> (<year>2007</year>). <source>Aquatic Photosynthesis, 1st Edn.</source> <publisher-loc>Princeton, NJ</publisher-loc>: <publisher-name>Princeton University Press</publisher-name>.</citation>
</ref>
<ref id="B19">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Feng</surname> <given-names>Y.</given-names></name> <name><surname>Hare</surname> <given-names>C. E.</given-names></name> <name><surname>Rose</surname> <given-names>J. M.</given-names></name> <name><surname>Handy</surname> <given-names>S. M.</given-names></name> <name><surname>DiTullio</surname> <given-names>G. R.</given-names></name> <name><surname>Lee</surname> <given-names>P. A.</given-names></name> <etal/></person-group>. (<year>2010</year>). <article-title>Interactive effects of iron, irradiance and CO<sub>2</sub> on Ross Sea phytoplankton</article-title>. <source>Deep. Res. I</source> <volume>57</volume>, <fpage>368</fpage>&#x02013;<lpage>383</lpage>. <pub-id pub-id-type="doi">10.1016/j.dsr.2009.10.013</pub-id></citation>
</ref>
<ref id="B20">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gao</surname> <given-names>K.</given-names></name> <name><surname>Xu</surname> <given-names>J.</given-names></name> <name><surname>Gao</surname> <given-names>G.</given-names></name> <name><surname>Li</surname> <given-names>Y.</given-names></name> <name><surname>Hutchins</surname> <given-names>D. A.</given-names></name> <name><surname>Huang</surname> <given-names>B.</given-names></name> <etal/></person-group>. (<year>2012</year>). <article-title>Rising CO<sub>2</sub> and increased light exposure synergistically reduce marine primary productivity</article-title>. <source>Nat. Clim. Chang.</source> <volume>2</volume>, <fpage>519</fpage>&#x02013;<lpage>523</lpage>. <pub-id pub-id-type="doi">10.1038/nclimate1507</pub-id></citation>
</ref>
<ref id="B21">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Garibotti</surname> <given-names>I. A.</given-names></name> <name><surname>Vernet</surname> <given-names>M.</given-names></name> <name><surname>Ferrario</surname> <given-names>M. E.</given-names></name></person-group> (<year>2005</year>). <article-title>Annually recurrent phytoplanktonic assemblages during summer in the seasonal ice zone west of the Antarctic Peninsula (Southern Ocean)</article-title>. <source>Deep Sea Res. Part I Oceanogr. Res. Pap.</source> <volume>52</volume>, <fpage>1823</fpage>&#x02013;<lpage>1841</lpage>. <pub-id pub-id-type="doi">10.1016/j.dsr.2005.05.003</pub-id></citation>
</ref>
<ref id="B22">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Garibotti</surname> <given-names>I.</given-names></name> <name><surname>Vernet</surname> <given-names>M.</given-names></name> <name><surname>Kozlowski</surname> <given-names>W.</given-names></name> <name><surname>Ferrario</surname> <given-names>M.</given-names></name></person-group> (<year>2003</year>). <article-title>Composition and biomass of phytoplankton assemblages in coastal Antarctic waters: a comparison of chemotaxonomic and microscopic analyses</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>247</volume>, <fpage>27</fpage>&#x02013;<lpage>42</lpage>. <pub-id pub-id-type="doi">10.3354/meps247027</pub-id></citation>
</ref>
<ref id="B23">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Genty</surname> <given-names>B.</given-names></name> <name><surname>Briantais</surname> <given-names>J.-M.</given-names></name> <name><surname>Baker</surname> <given-names>N. R.</given-names></name></person-group> (<year>1989</year>). <article-title>The relationship between the quantum yield of photosynthetic electron transport and quenching of chlorophyll fluorescence</article-title>. <source>Biochim. Biophys. Acta</source> <volume>990</volume>, <fpage>87</fpage>&#x02013;<lpage>92</lpage>. <pub-id pub-id-type="doi">10.1016/S0304-4165(89)80016-9</pub-id></citation>
</ref>
<ref id="B24">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Gilstad</surname> <given-names>M.</given-names></name> <name><surname>Sakshaug</surname> <given-names>E.</given-names></name></person-group> (<year>1990</year>). <article-title>Growth rates of ten diatom species from the Barents Sea at different irradiances and day lengths</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>64</volume>, <fpage>169</fpage>&#x02013;<lpage>173</lpage>. <pub-id pub-id-type="doi">10.3354/meps064169</pub-id></citation>
</ref>
<ref id="B25">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Goss</surname> <given-names>R.</given-names></name> <name><surname>Lepetit</surname> <given-names>B.</given-names></name></person-group> (<year>2014</year>). <article-title>Biodiversity of NPQ</article-title>. <source>J. Plant Physiol. Physiol.</source> <volume>172</volume>, <fpage>13</fpage>&#x02013;<lpage>32</lpage>. <pub-id pub-id-type="doi">10.1016/j.jplph.2014.03.004</pub-id><pub-id pub-id-type="pmid">24854581</pub-id></citation>
</ref>
<ref id="B26">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Guillard</surname> <given-names>R. R.</given-names></name> <name><surname>Ryther</surname> <given-names>J. H.</given-names></name></person-group> (<year>1962</year>). <article-title>Studies of marine planktonic diatoms: I. Cyclotella nana Hustedt, and Detonula confervacea (Cleve) Gran</article-title>. <source>Can. J. Microbiol.</source> <volume>8</volume>, <fpage>229</fpage>&#x02013;<lpage>239</lpage>. <pub-id pub-id-type="doi">10.1139/m62-029</pub-id><pub-id pub-id-type="pmid">13902807</pub-id></citation>
</ref>
<ref id="B27">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hauck</surname> <given-names>J.</given-names></name> <name><surname>V&#x000F6;lker</surname> <given-names>C.</given-names></name> <name><surname>Wolf-gladrow</surname> <given-names>D. A.</given-names></name> <name><surname>Laufk&#x000F6;tter</surname> <given-names>C.</given-names></name> <name><surname>Vogt</surname> <given-names>M.</given-names></name> <name><surname>Aumont</surname> <given-names>O.</given-names></name> <etal/></person-group>. (<year>2015</year>). <article-title>On the Southern Ocean CO<sub>2</sub> uptake and the role of the biological carbon pump in the 21st century</article-title>. <source>Glob. Biogeochem. Cycles</source> <volume>29</volume>, <fpage>1451</fpage>&#x02013;<lpage>1470</lpage>. <pub-id pub-id-type="doi">10.1002/2015GB005140</pub-id></citation>
</ref>
<ref id="B28">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hillebrand</surname> <given-names>H.</given-names></name> <name><surname>D&#x000FC;rselen</surname> <given-names>C.-D.</given-names></name> <name><surname>Kirschtel</surname> <given-names>D.</given-names></name> <name><surname>Pollingher</surname> <given-names>U.</given-names></name> <name><surname>Zohary</surname> <given-names>T.</given-names></name></person-group> (<year>1999</year>). <article-title>Biovolume calculation for pelagic and benthic microalgae</article-title>. <source>J. Phycol.</source> <volume>35</volume>, <fpage>403</fpage>&#x02013;<lpage>424</lpage>. <pub-id pub-id-type="doi">10.1046/j.1529-8817.1999.3520403.x</pub-id></citation>
</ref>
<ref id="B29">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Holm-Hansen</surname> <given-names>O.</given-names></name> <name><surname>Mitchell</surname> <given-names>B. G.</given-names></name> <name><surname>Hewes</surname> <given-names>C. D.</given-names></name> <name><surname>Karl</surname> <given-names>D. M.</given-names></name></person-group> (<year>1989</year>). <article-title>Phytoplankton blooms in the vicinity of Palmer Station, Antarctica</article-title>. <source>Polar Biol.</source> <volume>10</volume>, <fpage>49</fpage>&#x02013;<lpage>57</lpage>. <pub-id pub-id-type="doi">10.1007/BF00238290</pub-id></citation>
</ref>
<ref id="B30">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hoogstraten</surname> <given-names>A.</given-names></name> <name><surname>Timmermans</surname> <given-names>K. R.</given-names></name> <name><surname>de Baar</surname> <given-names>H. J. W.</given-names></name></person-group> (<year>2012</year>). <article-title>Morphological and physiological effects in <italic>Proboscia Alata</italic> (Bacillariophyceae) grown under different light and CO<sub>2</sub> conditions of the modern Southern Ocean</article-title>. <source>J. Phycol.</source> <volume>48</volume>, <fpage>559</fpage>&#x02013;<lpage>568</lpage>. <pub-id pub-id-type="doi">10.1111/j.1529-8817.2012.01148.x</pub-id><pub-id pub-id-type="pmid">27011071</pub-id></citation>
</ref>
<ref id="B31">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hopkinson</surname> <given-names>B. M.</given-names></name> <name><surname>Dupont</surname> <given-names>C. L.</given-names></name> <name><surname>Allen</surname> <given-names>A. E.</given-names></name> <name><surname>Morel</surname> <given-names>F. M.</given-names></name></person-group> (<year>2011</year>). <article-title>Efficiency of the CO2-concentrating mechanism of diatoms</article-title>. <source>Proc. Natl. Acad. Sci. U.S.A.</source> <volume>108</volume>, <fpage>3830</fpage>&#x02013;<lpage>3837</lpage>. <pub-id pub-id-type="doi">10.1073/pnas.1018062108</pub-id><pub-id pub-id-type="pmid">21321195</pub-id></citation>
</ref>
<ref id="B32">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hoppe</surname> <given-names>C. J.</given-names></name> <name><surname>Hassler</surname> <given-names>C. S.</given-names></name> <name><surname>Payne</surname> <given-names>C. D.</given-names></name> <name><surname>Tortell</surname> <given-names>P. D.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name> <name><surname>Trimborn</surname> <given-names>S.</given-names></name></person-group> (<year>2013</year>). <article-title>Iron limitation modulates ocean acidification effects on southern ocean phytoplankton communities</article-title>. <source>PLoS ONE</source> <volume>8</volume>:<fpage>e79890</fpage>. <pub-id pub-id-type="doi">10.1371/journal.pone.0079890</pub-id><pub-id pub-id-type="pmid">24278207</pub-id></citation>
</ref>
<ref id="B33">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Hoppe</surname> <given-names>C. J. M.</given-names></name> <name><surname>Holtz</surname> <given-names>L.</given-names></name> <name><surname>Trimborn</surname> <given-names>S.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name></person-group> (<year>2015</year>). <article-title>Ocean acidification decreases the light-use efficiency in an Antarctic diatom under dynamic but not constant light</article-title>. <source>New Phytol.</source> <volume>207</volume>, <fpage>159</fpage>&#x02013;<lpage>171</lpage>. <pub-id pub-id-type="doi">10.1111/nph.13334</pub-id></citation>
</ref>
<ref id="B34">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Huot</surname> <given-names>Y.</given-names></name> <name><surname>Babin</surname> <given-names>M.</given-names></name></person-group> (<year>2010</year>). <article-title>Overview of fluorescence protocols: theory, basic concepts, and practice</article-title>, in <source>Chlorophyll a Fluorescence in Aquatic Sciences: Methods and Applications</source>, eds <person-group person-group-type="editor"><name><surname>Suggett</surname> <given-names>J. D.</given-names></name> <name><surname>Pr&#x000E1;&#x00161;il</surname> <given-names>O.</given-names></name> <name><surname>Borowitzka</surname> <given-names>A. M.</given-names></name></person-group> (<publisher-loc>Dordrecht</publisher-loc>: <publisher-name>Springer</publisher-name>), <fpage>31</fpage>&#x02013;<lpage>74</lpage>.</citation>
</ref>
<ref id="B35">
<citation citation-type="book"><person-group person-group-type="author"><collab>IPCC</collab></person-group> (<year>2014</year>). <article-title>Climate Change 2014: Synthesis Report</article-title>, in <source>Contribution of Workinggroups I; II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change</source>, eds <person-group person-group-type="editor"><name><surname>Pachauri</surname> <given-names>R. K.</given-names></name> <name><surname>Meyer</surname> <given-names>L.A.</given-names></name></person-group> (<publisher-loc>Geneva</publisher-loc>: <publisher-name>IPCC</publisher-name>), <fpage>151</fpage>.</citation>
</ref>
<ref id="B36">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Jin</surname> <given-names>P.</given-names></name> <name><surname>Gao</surname> <given-names>K.</given-names></name> <name><surname>Beardall</surname> <given-names>J.</given-names></name></person-group> (<year>2013</year>). <article-title>Evolutionary responses of a coccolithophorid <italic>Gephyrocapsa Oceanica</italic> to Ocean acidification</article-title>. <source>Evolution</source> <volume>67</volume>, <fpage>1869</fpage>&#x02013;<lpage>1878</lpage>. <pub-id pub-id-type="doi">10.1111/evo.12112</pub-id><pub-id pub-id-type="pmid">23815645</pub-id></citation>
</ref>
<ref id="B37">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Kapsenberg</surname> <given-names>L.</given-names></name> <name><surname>Kelley</surname> <given-names>A. L.</given-names></name> <name><surname>Shaw</surname> <given-names>E. C.</given-names></name> <name><surname>Martz</surname> <given-names>T. R.</given-names></name> <name><surname>Hofmann</surname> <given-names>G. E.</given-names></name></person-group> (<year>2015</year>). <article-title>Near-shore Antarctic pH variability has implications for the design of ocean acidification experiments</article-title>. <source>Sci. Rep.</source> <volume>5</volume>, <fpage>9638</fpage>. <pub-id pub-id-type="doi">10.1038/srep10497</pub-id><pub-id pub-id-type="pmid">26135460</pub-id></citation>
</ref>
<ref id="B38">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Kolber</surname> <given-names>Z. S.</given-names></name> <name><surname>Pr&#x000E1;&#x00161;il</surname> <given-names>O.</given-names></name> <name><surname>Falkowski</surname> <given-names>P. G.</given-names></name></person-group> (<year>1998</year>). <article-title>Measurements of variable chlorophyll fluorescence using fast repetition rate techniques: defining methodology and experimental protocols</article-title>. <source>Biochim. Biophys. Acta</source> <volume>1367</volume>, <fpage>88</fpage>&#x02013;<lpage>106</lpage>. <pub-id pub-id-type="doi">10.1016/S0005-2728(98)00135-2</pub-id><pub-id pub-id-type="pmid">9784616</pub-id></citation>
</ref>
<ref id="B39">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Krause</surname> <given-names>G. H.</given-names></name> <name><surname>Weis</surname> <given-names>E.</given-names></name></person-group> (<year>1991</year>). <article-title>Chlorophyll fluorescence and photosynthesis: the basics</article-title>. <source>Annu. Rev. Plant Physiol. Plant Mol. Biol.</source> <volume>42</volume>, <fpage>313</fpage>&#x02013;<lpage>349</lpage>. <pub-id pub-id-type="doi">10.1146/annurev.pp.42.060191.001525</pub-id></citation>
</ref>
<ref id="B40">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Kropuenske</surname> <given-names>L. R.</given-names></name> <name><surname>Mills</surname> <given-names>M. M.</given-names></name> <name><surname>van Dijken</surname> <given-names>G. L.</given-names></name> <name><surname>Alderkamp</surname> <given-names>A.-C.</given-names></name> <name><surname>Mine Berg</surname> <given-names>G.</given-names></name> <name><surname>Robinson</surname> <given-names>D. H.</given-names></name> <etal/></person-group>. (<year>2010</year>). <article-title>Strategies and rates of photoacclimation in two major Southern Ocean phytoplankton taxa: Phaeocystis antarctica (Haptophyta) and Fragilariopsis cylindrus (Bacillariophyceae)</article-title>. <source>J. Phycol.</source> <volume>46</volume>, <fpage>1138</fpage>&#x02013;<lpage>1151</lpage>. <pub-id pub-id-type="doi">10.1111/j.1529-8817.2010.00922.x</pub-id></citation>
</ref>
<ref id="B41">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Kropuenske</surname> <given-names>L. R.</given-names></name> <name><surname>Mills</surname> <given-names>M. M.</given-names></name> <name><surname>van Dijken</surname> <given-names>G. L.</given-names></name> <name><surname>Bailey</surname> <given-names>S.</given-names></name> <name><surname>Robinson</surname> <given-names>D. H.</given-names></name> <name><surname>Welschmeyer</surname> <given-names>N. A.</given-names></name> <etal/></person-group>. (<year>2009</year>). <article-title>Photophysiology in two major Southern Ocean phytoplankton taxa: Photoprotection in Phaeocystis antarctica and Fragilariopsis cylindrus</article-title>. <source>Limnol. Oceanogr.</source> <volume>54</volume>, <fpage>1176</fpage>&#x02013;<lpage>1196</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2009.54.4.1176</pub-id></citation>
</ref>
<ref id="B42">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Lancelot</surname> <given-names>C.</given-names></name> <name><surname>Mathot</surname> <given-names>S.</given-names></name> <name><surname>Veth</surname> <given-names>C.</given-names></name> <name><surname>de Baar</surname> <given-names>H.</given-names></name></person-group> (<year>1993</year>). <article-title>Factors controlling phytoplankton ice-edge blooms in the marginal ice-zone of the northwestern Weddell Sea during sea ice retreat 1988: field observations and mathematical modelling</article-title>. <source>Polar Biol.</source> <volume>13</volume>, <fpage>377</fpage>&#x02013;<lpage>387</lpage>. <pub-id pub-id-type="doi">10.1007/BF01681979</pub-id></citation>
</ref>
<ref id="B43">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Li</surname> <given-names>Y.</given-names></name> <name><surname>Xu</surname> <given-names>J.</given-names></name> <name><surname>Gao</surname> <given-names>K.</given-names></name></person-group> (<year>2014</year>). <article-title>Light-modulated responses of growth and photosynthetic performance to ocean acidification in the model diatom <italic>Phaeodactylum tricornutum</italic></article-title>. <source>PLoS ONE</source> <volume>9</volume>:<fpage>e96173</fpage>. <pub-id pub-id-type="doi">10.1371/journal.pone.0096173</pub-id><pub-id pub-id-type="pmid">24828454</pub-id></citation>
</ref>
<ref id="B44">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Li</surname> <given-names>Y.</given-names></name> <name><surname>Zhuang</surname> <given-names>S.</given-names></name> <name><surname>Wu</surname> <given-names>Y.</given-names></name> <name><surname>Ren</surname> <given-names>H.</given-names></name> <name><surname>Cheng</surname> <given-names>F.</given-names></name> <name><surname>Lin</surname> <given-names>X.</given-names></name> <etal/></person-group>. (<year>2015</year>). <article-title>Ocean acidification modulates expression of genes and physiological performance of a marine diatom</article-title>. <source>Biogeosci. Discuss.</source> <volume>12</volume>, <fpage>15809</fpage>&#x02013;<lpage>15833</lpage>. <pub-id pub-id-type="doi">10.5194/bgd-12-15809-2015</pub-id></citation>
</ref>
<ref id="B45">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>MacIntyre</surname> <given-names>H. L.</given-names></name> <name><surname>Kana</surname> <given-names>T. M.</given-names></name> <name><surname>Anning</surname> <given-names>T.</given-names></name> <name><surname>Geider</surname> <given-names>R. J.</given-names></name></person-group> (<year>2002</year>). <article-title>Photoacclimation of photosynthesis irradiance response curves and photosynthetic pigments in microalgae and cyanobacteria</article-title>. <source>J. Phycol.</source> <volume>38</volume>, <fpage>17</fpage>&#x02013;<lpage>38</lpage>. <pub-id pub-id-type="doi">10.1046/j.1529-8817.2002.00094.x</pub-id></citation>
</ref>
<ref id="B46">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Martin</surname> <given-names>J. H.</given-names></name> <name><surname>Gordon</surname> <given-names>R. M.</given-names></name> <name><surname>Fitzwater</surname> <given-names>S. E.</given-names></name></person-group> (<year>1990</year>). <article-title>Iron in Antarctic waters</article-title>. <source>Nature</source> <volume>345</volume>, <fpage>156</fpage>&#x02013;<lpage>158</lpage>. <pub-id pub-id-type="doi">10.1038/345156a0</pub-id></citation>
</ref>
<ref id="B47">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mehrbach</surname> <given-names>C.</given-names></name> <name><surname>Culberson</surname> <given-names>C. H.</given-names></name> <name><surname>Hawley</surname> <given-names>J. E.</given-names></name> <name><surname>Pytkowicz</surname> <given-names>R. M.</given-names></name></person-group> (<year>1973</year>). <article-title>Measurement of the apparent dissociation constants of carbonic acid in seawater at atmospheric pressure</article-title>. <source>Limnol. Oceanogr.</source> <volume>18</volume>, <fpage>897</fpage>&#x02013;<lpage>907</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1973.18.6.0897</pub-id></citation>
</ref>
<ref id="B48">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mills</surname> <given-names>M. M.</given-names></name> <name><surname>Kropuenske</surname> <given-names>L. R.</given-names></name> <name><surname>van Dijken</surname> <given-names>G. L.</given-names></name> <name><surname>Alderkamp</surname> <given-names>A.-C.</given-names></name> <name><surname>Berg</surname> <given-names>G. M.</given-names></name> <name><surname>Robinson</surname> <given-names>D. H.</given-names></name> <etal/></person-group>. (<year>2010</year>). <article-title>Photophysiology in two Southern Ocean phytoplankton taxa: Photosynthesis of Phaeocystis antarctica (Prymnesiophyceae) and Fragilariopsis cylindrus (Bacillariophyceae) under simulated mixed-layer irradiance</article-title>. <source>J. Phycol.</source> <volume>46</volume>, <fpage>1114</fpage>&#x02013;<lpage>1127</lpage>. <pub-id pub-id-type="doi">10.1111/j.1529-8817.2010.00923.x</pub-id></citation>
</ref>
<ref id="B49">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mitchell</surname> <given-names>B. G.</given-names></name> <name><surname>Brody</surname> <given-names>E. A.</given-names></name></person-group> (<year>1991</year>). <article-title>Light limitation of phytoplankton biomass and macronutrient utilization in the Southern Ocean</article-title>. <source>Limnol. Oceanogr.</source> <volume>36</volume>, <fpage>1662</fpage>&#x02013;<lpage>1677</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1991.36.8.1662</pub-id></citation>
</ref>
<ref id="B50">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Mitchell</surname> <given-names>B. G.</given-names></name> <name><surname>Holm-Hansen</surname> <given-names>O.</given-names></name></person-group> (<year>1991</year>). <article-title>Observations and modeling of the antarctic phytoplankton crop in relation to mixing depth</article-title>. <source>Deep Sea Res.</source> <volume>38</volume>, <fpage>981</fpage>&#x02013;<lpage>1007</lpage>. <pub-id pub-id-type="doi">10.1016/0198-0149(91)90093-U</pub-id></citation>
</ref>
<ref id="B51">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Moline</surname> <given-names>M. A.</given-names></name> <name><surname>Pr&#x000E9;zelin</surname> <given-names>B. B.</given-names></name></person-group> (<year>1996</year>). <article-title>Long-term monitoring and analyses of physical factors regulating variability in coastal Antarctic phytoplankton biomass, in situ productivity and taxonomic composition over seasonal and interannual timescales</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>145</volume>, <fpage>143</fpage>&#x02013;<lpage>160</lpage>. <pub-id pub-id-type="doi">10.3354/meps145143</pub-id></citation>
</ref>
<ref id="B52">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>M&#x000FC;ller</surname> <given-names>P.</given-names></name> <name><surname>Li</surname> <given-names>X. P.</given-names></name> <name><surname>Niyogi</surname> <given-names>K. K.</given-names></name></person-group> (<year>2001</year>). <article-title>Non-photochemical quenching. A response to excess light energy</article-title>. <source>Plant Physiol.</source> <volume>125</volume>, <fpage>1558</fpage>&#x02013;<lpage>1566</lpage>. <pub-id pub-id-type="doi">10.1104/pp.125.4.1558</pub-id><pub-id pub-id-type="pmid">11299337</pub-id></citation>
</ref>
<ref id="B53">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Murata</surname> <given-names>N.</given-names></name> <name><surname>Takahashi</surname> <given-names>S.</given-names></name> <name><surname>Nishiyama</surname> <given-names>Y.</given-names></name> <name><surname>Allakhverdiev</surname> <given-names>S. I.</given-names></name></person-group> (<year>2007</year>). <article-title>Photoinhibition of photosystem II under environmental stress</article-title>. <source>Biochim. Biophys. Acta</source> <volume>1767</volume>, <fpage>414</fpage>&#x02013;<lpage>421</lpage>. <pub-id pub-id-type="doi">10.1016/j.bbabio.2006.11.019</pub-id><pub-id pub-id-type="pmid">17207454</pub-id></citation>
</ref>
<ref id="B54">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Nelson</surname> <given-names>D. M.</given-names></name> <name><surname>Smith</surname> <given-names>W. O.</given-names></name></person-group> (<year>1991</year>). <article-title>The role of light and major nautrients</article-title>. <source>Limnol. Oceanogr.</source> <volume>36</volume>, <fpage>1650</fpage>&#x02013;<lpage>1661</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1991.36.8.1650</pub-id></citation>
</ref>
<ref id="B55">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Norici</surname> <given-names>A.</given-names></name> <name><surname>Bazzoni</surname> <given-names>A. M.</given-names></name> <name><surname>Pugnetti</surname> <given-names>A.</given-names></name> <name><surname>Raven</surname> <given-names>J. A.</given-names></name> <name><surname>Giordano</surname> <given-names>M.</given-names></name></person-group> (<year>2011</year>). <article-title>Impact of irradiance on the C allocation in the coastal marine diatom Skeletonema marinoi Sarno and Zingone</article-title>. <source>Plant Cell Environ.</source> <volume>34</volume>, <fpage>1666</fpage>&#x02013;<lpage>1677</lpage>. <pub-id pub-id-type="doi">10.1111/j.1365-3040.2011.02362.x</pub-id><pub-id pub-id-type="pmid">21707652</pub-id></citation>
</ref>
<ref id="B56">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Oxborough</surname> <given-names>K.</given-names></name> <name><surname>Moore</surname> <given-names>C. M.</given-names></name> <name><surname>Suggett</surname> <given-names>D. J.</given-names></name> <name><surname>Lawson</surname> <given-names>T.</given-names></name> <name><surname>Chan</surname> <given-names>H. G.</given-names></name> <name><surname>Geider</surname> <given-names>R. J.</given-names></name></person-group> (<year>2012</year>). <article-title>Direct estimation of functional PSII reaction center concentration and PSII electron flux on a volume basis: a new approach to the analysis of Fast Repetition Rate fluorometry (FRRf) data</article-title>. <source>Limnol. Oceanogr. Methods</source> <volume>10</volume>, <fpage>142</fpage>&#x02013;<lpage>154</lpage>. <pub-id pub-id-type="doi">10.4319/lom.2012.10.142</pub-id></citation>
</ref>
<ref id="B57">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Petrou</surname> <given-names>K.</given-names></name> <name><surname>Hill</surname> <given-names>R.</given-names></name> <name><surname>Doblin</surname> <given-names>M. A.</given-names></name> <name><surname>McMinn</surname> <given-names>A.</given-names></name> <name><surname>Johnson</surname> <given-names>R.</given-names></name> <name><surname>Wright</surname> <given-names>S. W.</given-names></name> <etal/></person-group>. (<year>2011</year>). <article-title>Photoprotection of sea-ice microalgal communities from the east antarctic pack ice</article-title>. <source>J. Phycol.</source> <volume>47</volume>, <fpage>77</fpage>&#x02013;<lpage>86</lpage>. <pub-id pub-id-type="doi">10.1111/j.1529-8817.2010.00944.x</pub-id><pub-id pub-id-type="pmid">27021712</pub-id></citation>
</ref>
<ref id="B58">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Petrou</surname> <given-names>K.</given-names></name> <name><surname>Trimborn</surname> <given-names>S.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name> <name><surname>Ralph</surname> <given-names>P. J.</given-names></name> <name><surname>Hassler</surname> <given-names>C. S.</given-names></name></person-group> (<year>2014</year>). <article-title>The impact of iron limitation on the physiology of the Antarctic diatom Chaetoceros simplex</article-title>. <source>Mar. Biol.</source> <volume>4</volume>, <fpage>925</fpage>&#x02013;<lpage>937</lpage>. <pub-id pub-id-type="doi">10.1007/s00227-014-2392-z</pub-id></citation>
</ref>
<ref id="B59">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Pierrot</surname> <given-names>D.</given-names></name> <name><surname>Lewis</surname> <given-names>E.</given-names></name> <name><surname>Wallace</surname> <given-names>D. W. R.</given-names></name></person-group> (<year>2006</year>). <source>MS Excel Program Developed for CO<sub>2</sub> System Calculations</source>. <publisher-loc>Oak Ridge</publisher-loc>: <publisher-name>Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, US Department of Energy</publisher-name>.</citation>
</ref>
<ref id="B60">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Pr&#x000E9;zelin</surname> <given-names>B. B.</given-names></name> <name><surname>Hofmann</surname> <given-names>E. E.</given-names></name> <name><surname>Mengelt</surname> <given-names>C.</given-names></name> <name><surname>Klinck</surname> <given-names>J. M.</given-names></name></person-group> (<year>2000</year>). <article-title>The linkage between Upper Circumpolar Deep Water (UCDW) and phytoplankton assemblages on the west Antarctic Peninsula continental shelf</article-title>. <source>J. Mar. Res.</source> <volume>58</volume>, <fpage>165</fpage>&#x02013;<lpage>202</lpage>. <pub-id pub-id-type="doi">10.1357/002224000321511133</pub-id></citation>
</ref>
<ref id="B61">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Ralph</surname> <given-names>P. J.</given-names></name> <name><surname>Gademann</surname> <given-names>R.</given-names></name></person-group> (<year>2005</year>). <article-title>Rapid light curves: a powerful tool to assess photosynthetic activity</article-title>. <source>Aquat. Bot.</source> <volume>82</volume>, <fpage>222</fpage>&#x02013;<lpage>237</lpage>. <pub-id pub-id-type="doi">10.1016/j.aquabot.2005.02.006</pub-id></citation>
</ref>
<ref id="B62">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Raven</surname> <given-names>J. A.</given-names></name></person-group> (<year>2011</year>). <article-title>The cost of photoinhibition</article-title>. <source>Physiol. Plant.</source> <volume>142</volume>, <fpage>87</fpage>&#x02013;<lpage>104</lpage>. <pub-id pub-id-type="doi">10.1111/j.1399-3054.2011.01465.x</pub-id><pub-id pub-id-type="pmid">21382037</pub-id></citation>
</ref>
<ref id="B63">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Raven</surname> <given-names>J. A.</given-names></name> <name><surname>Beardall</surname> <given-names>J.</given-names></name> <name><surname>Giordano</surname> <given-names>M.</given-names></name></person-group> (<year>2014</year>). <article-title>Energy costs of carbon dioxide concentrating mechanisms in aquatic organisms</article-title>. <source>Photosynth. Res.</source> <volume>121</volume>, <fpage>111</fpage>&#x02013;<lpage>124</lpage>. <pub-id pub-id-type="doi">10.1007/s11120-013-9962-7</pub-id><pub-id pub-id-type="pmid">24390639</pub-id></citation>
</ref>
<ref id="B64">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Raven</surname> <given-names>J. A.</given-names></name> <name><surname>Johnston</surname> <given-names>A. M.</given-names></name></person-group> (<year>1991</year>). <article-title>Mechanisms of inorganic-carbon acquisition in marine phytoplankton and their implications for the use of other resources</article-title>. <source>Limnol. Oceanogr.</source> <volume>36</volume>, <fpage>1701</fpage>&#x02013;<lpage>1714</lpage>. <pub-id pub-id-type="doi">10.4319/lo.1991.36.8.1701</pub-id></citation>
</ref>
<ref id="B65">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Redfield</surname> <given-names>A. C.</given-names></name></person-group> (<year>1958</year>). <article-title>The biological control of chemical factors in the environment</article-title>. <source>Am. Sci.</source> <volume>64</volume>, <fpage>205</fpage>&#x02013;<lpage>221</lpage>.</citation>
</ref>
<ref id="B66">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Reinfelder</surname> <given-names>J. R.</given-names></name></person-group> (<year>2011</year>). <article-title>Carbon concentrating mechanisms in eukaryotic marine phytoplankton</article-title>. <source>Ann. Rev. Mar. Sci.</source> <volume>3</volume>, <fpage>291</fpage>&#x02013;<lpage>315</lpage>. <pub-id pub-id-type="doi">10.1146/annurev-marine-120709-142720</pub-id><pub-id pub-id-type="pmid">21329207</pub-id></citation>
</ref>
<ref id="B67">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Rickaby</surname> <given-names>R. E. M.</given-names></name> <name><surname>Henderiks</surname> <given-names>J.</given-names></name> <name><surname>Young</surname> <given-names>J. N.</given-names></name></person-group> (<year>2010</year>). <article-title>Perturbing phytoplankton: response and isotopic fractionation with changing carbonate chemistry in two coccolithophore species</article-title>. <source>Clim. Past</source> <volume>6</volume>, <fpage>771</fpage>&#x02013;<lpage>785</lpage>. <pub-id pub-id-type="doi">10.5194/cp-6-771-2010</pub-id></citation>
</ref>
<ref id="B68">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Riebesell</surname> <given-names>U.</given-names></name> <name><surname>Wolf-Gladrow</surname> <given-names>D. A.</given-names></name> <name><surname>Smetacek</surname> <given-names>V.</given-names></name></person-group> (<year>1993</year>). <article-title>Carbon dioxide limitation of marine phytoplankton growth rates</article-title>. <source>Nature</source> <volume>361</volume>, <fpage>249</fpage>&#x02013;<lpage>251</lpage>. <pub-id pub-id-type="doi">10.1038/361249a0</pub-id></citation>
</ref>
<ref id="B69">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Rokitta</surname> <given-names>S. D.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name></person-group> (<year>2012</year>). <article-title>Effects of CO<sub>2</sub> and their modulation by light in the life-cycle stages of the coccolithophore <italic>Emiliania huxleyi</italic></article-title>. <source>Limnol. Oceanogr.</source> <volume>57</volume>, <fpage>607</fpage>&#x02013;<lpage>618</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2012.57.2.0607</pub-id></citation>
</ref>
<ref id="B70">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Rost</surname> <given-names>B.</given-names></name> <name><surname>Riebesell</surname> <given-names>U.</given-names></name> <name><surname>Burkhardt</surname> <given-names>S.</given-names></name> <name><surname>S&#x000FC;ltmeyer</surname> <given-names>D.</given-names></name></person-group> (<year>2003</year>). <article-title>Carbon acquisition of bloom-forming marine phytoplankton</article-title>. <source>Limnol. Oceanogr.</source> <volume>48</volume>, <fpage>55</fpage>&#x02013;<lpage>67</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2003.48.1.0055</pub-id></citation>
</ref>
<ref id="B71">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Sakshaug</surname> <given-names>E.</given-names></name> <name><surname>Bricaud</surname> <given-names>A.</given-names></name> <name><surname>Dandonneau</surname> <given-names>Y.</given-names></name> <name><surname>Falkowski</surname> <given-names>P. G.</given-names></name> <name><surname>Kiefer</surname> <given-names>D. A.</given-names></name> <name><surname>Legendre</surname> <given-names>L.</given-names></name> <etal/></person-group>. (<year>1997</year>). <article-title>Parameters of photosynthesis: definations, theory and interpretation of results</article-title>. <source>J. Plankton Res.</source> <volume>19</volume>, <fpage>1637</fpage>&#x02013;<lpage>1670</lpage>. <pub-id pub-id-type="doi">10.1093/plankt/19.11.1637</pub-id></citation>
</ref>
<ref id="B72">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Schreiber</surname> <given-names>U.</given-names></name></person-group> (<year>2004</year>). <article-title>Pulse-Amplitude-Modulation (PAM) fluorometry and saturation pulse method: an overview</article-title>, in <source>Chlorophyll a Fluorescence: A Signature of Photosynthesis</source>, eds <person-group person-group-type="editor"><name><surname>Papageorgiou</surname> <given-names>G. C.</given-names></name> <name><surname>Govindjee</surname></name></person-group> (<publisher-loc>Dordrecht</publisher-loc>: <publisher-name>Springer</publisher-name>), <fpage>279</fpage>&#x02013;<lpage>319</lpage>.</citation>
</ref>
<ref id="B73">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Shi</surname> <given-names>D.</given-names></name> <name><surname>Li</surname> <given-names>W.</given-names></name> <name><surname>Hopkinson</surname> <given-names>B. M.</given-names></name> <name><surname>Hong</surname> <given-names>H.</given-names></name> <name><surname>Li</surname> <given-names>D.</given-names></name> <name><surname>Kao</surname> <given-names>S.-J.</given-names></name> <etal/></person-group>. (<year>2015</year>). <article-title>Interactive effects of light, nitrogen source, and carbon dioxide on energy metabolism in the diatom <italic>Thalassiosira pseudonana</italic></article-title>. <source>Limnol. Oceanogr.</source> <volume>60</volume>, <fpage>1805</fpage>&#x02013;<lpage>1822</lpage>. <pub-id pub-id-type="doi">10.1002/lno.10134</pub-id></citation>
</ref>
<ref id="B74">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Stoll</surname> <given-names>M. H. C.</given-names></name> <name><surname>Bakker</surname> <given-names>K.</given-names></name> <name><surname>Nobbe</surname> <given-names>G. H.</given-names></name> <name><surname>Haese</surname> <given-names>R. R.</given-names></name></person-group> (<year>2001</year>). <article-title>Continous-flow analysis of dissolved inorganic carbon content in seawater</article-title>. <source>Anal. Chem.</source> <volume>73</volume>, <fpage>4111</fpage>&#x02013;<lpage>4116</lpage>. <pub-id pub-id-type="doi">10.1021/ac010303r</pub-id></citation>
</ref>
<ref id="B75">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Strzepek</surname> <given-names>R. F.</given-names></name> <name><surname>Hunter</surname> <given-names>K. A.</given-names></name> <name><surname>Frew</surname> <given-names>R. D.</given-names></name> <name><surname>Harrison</surname> <given-names>P. J.</given-names></name> <name><surname>Boyd</surname> <given-names>P. W.</given-names></name></person-group> (<year>2012</year>). <article-title>Iron-light interactions differ in Southern Ocean phytoplankton</article-title>. <source>Limnol. Oceanogr.</source> <volume>57</volume>, <fpage>1182</fpage>&#x02013;<lpage>1200</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2012.57.4.1182</pub-id></citation>
</ref>
<ref id="B76">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Suggett</surname> <given-names>D. J.</given-names></name> <name><surname>MacIntyre</surname> <given-names>H. L.</given-names></name> <name><surname>Geider</surname> <given-names>R. J.</given-names></name></person-group> (<year>2004</year>). <article-title>Evaluation of biophysical and optical determinations of light absorption by photosystem II in phytoplankton</article-title>. <source>Limnol. Oceanogr. Methods</source> <volume>2</volume>, <fpage>316</fpage>&#x02013;<lpage>332</lpage>. <pub-id pub-id-type="doi">10.4319/lom.2004.2.316</pub-id></citation>
</ref>
<ref id="B77">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Suggett</surname> <given-names>D. J.</given-names></name> <name><surname>Moore</surname> <given-names>C. M.</given-names></name> <name><surname>Hickman</surname> <given-names>A. E.</given-names></name> <name><surname>Geider</surname> <given-names>R. J.</given-names></name></person-group> (<year>2009</year>). <article-title>Interpretation of fast repetition rate (FRR) fluorescence: Signatures of phytoplankton community structure versus physiological state</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>376</volume>, <fpage>1</fpage>&#x02013;<lpage>19</lpage>. <pub-id pub-id-type="doi">10.3354/meps07830</pub-id></citation>
</ref>
<ref id="B78">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Sweeney</surname> <given-names>C.</given-names></name></person-group> (<year>2003</year>). <article-title>The annual cycle of surface CO<sub>2</sub> and O<sub>2</sub> in the Ross Sea: a model for gas exchange on the continental shelves of Antarctica</article-title>, in <source>Biogeochemistry of the Ross Sea</source>, eds <person-group person-group-type="editor"><name><surname>DiTullio</surname> <given-names>G. R.</given-names></name> <name><surname>Dunbar</surname> <given-names>R. B.</given-names></name></person-group> (<publisher-loc>Washington, DC</publisher-loc>: <publisher-name>AGU</publisher-name>), <fpage>295</fpage>&#x02013;<lpage>312</lpage>.</citation>
</ref>
<ref id="B79">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Tortell</surname> <given-names>P. D.</given-names></name> <name><surname>Payne</surname> <given-names>C.</given-names></name> <name><surname>Gueguen</surname> <given-names>C.</given-names></name> <name><surname>Strzepek</surname> <given-names>R. F.</given-names></name> <name><surname>Boyd</surname> <given-names>P. W.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name></person-group> (<year>2008</year>). <article-title>Inorganic carbon uptake by Southern Ocean phytoplankton</article-title>. <source>Limnol. Oceanogr.</source> <volume>53</volume>, <fpage>1266</fpage>&#x02013;<lpage>1278</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2008.53.4.1266</pub-id></citation>
</ref>
<ref id="B80">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Trimborn</surname> <given-names>S.</given-names></name> <name><surname>Brenneis</surname> <given-names>T.</given-names></name> <name><surname>Sweet</surname> <given-names>E.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name></person-group> (<year>2013</year>). <article-title>Sensitivity of Antarctic phytoplankton species to ocean acidification: Growth, carbon acquisition, and species interaction</article-title>. <source>Limnol. Oceanogr.</source> <volume>58</volume>, <fpage>997</fpage>&#x02013;<lpage>1007</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2013.58.3.0997</pub-id></citation>
</ref>
<ref id="B81">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Trimborn</surname> <given-names>S.</given-names></name> <name><surname>Thoms</surname> <given-names>S.</given-names></name> <name><surname>Petrou</surname> <given-names>K.</given-names></name> <name><surname>Kranz</surname> <given-names>S. A.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name></person-group> (<year>2014</year>). <article-title>Photophysiological responses of Southern Ocean phytoplankton to changes in CO<sub>2</sub> concentrations: short-term versus acclimation effects</article-title>. <source>J. Exp. Mar. Bio. Ecol.</source> <volume>451</volume>, <fpage>44</fpage>&#x02013;<lpage>54</lpage>. <pub-id pub-id-type="doi">10.1016/j.jembe.2013.11.001</pub-id></citation>
</ref>
<ref id="B82">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Trimborn</surname> <given-names>S.</given-names></name> <name><surname>Wolf-Gladrow</surname> <given-names>D.</given-names></name> <name><surname>Richter</surname> <given-names>K. U.</given-names></name> <name><surname>Rost</surname> <given-names>B.</given-names></name></person-group> (<year>2009</year>). <article-title>The effect of pCO2 on carbon acquisition and intracellular assimilation in four marine diatoms</article-title>. <source>J. Exp. Mar. Bio. Ecol.</source> <volume>376</volume>, <fpage>26</fpage>&#x02013;<lpage>36</lpage>. <pub-id pub-id-type="doi">10.1016/j.jembe.2009.05.017</pub-id></citation>
</ref>
<ref id="B83">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Venables</surname> <given-names>H. J.</given-names></name> <name><surname>Clarke</surname> <given-names>A.</given-names></name> <name><surname>Meredith</surname> <given-names>M. P.</given-names></name></person-group> (<year>2013</year>). <article-title>Wintertime controls on summer stratification and productivity at the western Antarctic Peninsula</article-title>. <source>Limnol. Oceanogr.</source> <volume>58</volume>, <fpage>1035</fpage>&#x02013;<lpage>1047</lpage>. <pub-id pub-id-type="doi">10.4319/lo.2013.58.3.1035</pub-id></citation>
</ref>
<ref id="B84">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Wright</surname> <given-names>S. W.</given-names></name> <name><surname>Jeffrey</surname> <given-names>S. W.</given-names></name> <name><surname>Mantoura</surname> <given-names>R. F. C.</given-names></name> <name><surname>Llewellyn</surname> <given-names>C. A.</given-names></name> <name><surname>Bjornland</surname> <given-names>T.</given-names></name> <name><surname>Repeta</surname> <given-names>D.</given-names></name> <etal/></person-group>. (<year>1991</year>). <article-title>Improved HPLC method for the analysis of chlorophylls and carotenoids from marine phytoplankton</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>77</volume>, <fpage>183</fpage>&#x02013;<lpage>196</lpage>. <pub-id pub-id-type="doi">10.3354/meps077183</pub-id></citation>
</ref>
<ref id="B85">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Wu</surname> <given-names>Y.</given-names></name> <name><surname>Gao</surname> <given-names>K.</given-names></name> <name><surname>Riebesell</surname> <given-names>U.</given-names></name></person-group> (<year>2010</year>). <article-title>CO2-induced seawater acidification affects physiological performance of the marine diatom <italic>Phaeodactylum tricornutum</italic></article-title>. <source>Biogeosciences</source> <volume>7</volume>, <fpage>2915</fpage>&#x02013;<lpage>2923</lpage>. <pub-id pub-id-type="doi">10.5194/bg-7-2915-2010</pub-id></citation>
</ref>
<ref id="B86">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Xu</surname> <given-names>J.</given-names></name> <name><surname>Gao</surname> <given-names>K.</given-names></name> <name><surname>Li</surname> <given-names>Y.</given-names></name> <name><surname>Hutchins</surname> <given-names>D. A.</given-names></name></person-group> (<year>2014</year>). <article-title>Physiological and biochemical responses of diatoms to projected ocean changes</article-title>. <source>Mar. Ecol. Prog. Ser.</source> <volume>515</volume>, <fpage>73</fpage>&#x02013;<lpage>81</lpage>. <pub-id pub-id-type="doi">10.3354/meps11026</pub-id></citation>
</ref>
<ref id="B87">
<citation citation-type="journal"><person-group person-group-type="author"><name><surname>Yang</surname> <given-names>G.</given-names></name> <name><surname>Gao</surname> <given-names>K.</given-names></name></person-group> (<year>2012</year>). <article-title>Physiological responses of the marine diatom Thalassiosira pseudonana to increased pCO2 and seawater acidity</article-title>. <source>Mar. Environ. Res.</source> <volume>79</volume>, <fpage>142</fpage>&#x02013;<lpage>151</lpage>. <pub-id pub-id-type="doi">10.1016/j.marenvres.2012.06.002</pub-id><pub-id pub-id-type="pmid">22770534</pub-id></citation>
</ref>
<ref id="B88">
<citation citation-type="book"><person-group person-group-type="author"><name><surname>Zeebe</surname> <given-names>R. E.</given-names></name> <name><surname>Wolf-Gladrow</surname> <given-names>D. A.</given-names></name></person-group> (<year>2001</year>). <source>CO<sub>2</sub> in Seawater: Equilibrium, Kinetics, Isotopes, 1st Edn</source>. <publisher-loc>Amsterdam; London; New York, NY</publisher-loc>: <publisher-name>Elsevier</publisher-name></citation>
</ref>
</ref-list>
</back>
</article>