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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.2022.870792</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>Microscopic Stages of North Atlantic <italic>Laminaria digitata</italic> (Phaeophyceae) Exhibit Trait-Dependent Thermal Adaptation Along Latitudes</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Schimpf</surname>
<given-names>Nele M.</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>*</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1538539"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Liesner</surname>
<given-names>Daniel</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/938312"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Franke</surname>
<given-names>Kiara</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1807377"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Roleda</surname>
<given-names>Michael Y.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/139814"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Bartsch</surname>
<given-names>Inka</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/810072"/>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research</institution>, <addr-line>Bremerhaven</addr-line>, <country>Germany</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>School of Biological and Marine Sciences, University of Plymouth</institution>, <addr-line>Plymouth</addr-line>, <country>United Kingdom</country>
</aff>
<aff id="aff3">
<sup>3</sup>
<institution>Department of Algal Development and Evolution, Max Planck Institute for Biology T&#xfc;bingen</institution>, <addr-line>T&#xfc;bingen</addr-line>, <country>Germany</country>
</aff>
<aff id="aff4">
<sup>4</sup>
<institution>Applied Ecology and Phycology, University of Rostock</institution>, <addr-line>Rostock</addr-line>, <country>Germany</country>
</aff>
<aff id="aff5">
<sup>5</sup>
<institution>Division of Biotechnology and Plant Health, Norwegian Institute of Bioeconomy Research (NIBIO)</institution>, <addr-line>&#xc5;s</addr-line>, <country>Norway</country>
</aff>
<aff id="aff6">
<sup>6</sup>
<institution>Biomarine Resource Valorisation, Division of Food Production and Society, Norwegian Institute of Bioeconomy Research (NIBIO)</institution>, <addr-line>Bod&#xf8;</addr-line>, <country>Norway</country>
</aff>
<aff id="aff7">
<sup>7</sup>
<institution>The Marine Science Institute, College of Science, University of the Philippines</institution>, <addr-line>Quezon City</addr-line>, <country>Philippines</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>Edited by: Bernardo Antonio Perez Da Gama, Fluminense Federal University, Brazil</p>
</fn>
<fn fn-type="edited-by">
<p>Reviewed by: Trine Bekkby, Norwegian Institute for Water Research (NIVA), Norway; Lydia Ladah, Center for Scientific Research and Higher Education in Ensenada (CICESE), Mexico</p>
</fn>
<fn fn-type="corresp" id="fn001">
<p>*Correspondence: Nele M. Schimpf, <email xlink:href="mailto:nele.schimpf@gmx.net">nele.schimpf@gmx.net</email>
</p>
</fn>
<fn fn-type="other" id="fn002">
<p>This article was submitted to Marine Ecosystem Ecology, a section of the journal Frontiers in Marine Science</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>17</day>
<month>06</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="collection">
<year>2022</year>
</pub-date>
<volume>9</volume>
<elocation-id>870792</elocation-id>
<history>
<date date-type="received">
<day>07</day>
<month>02</month>
<year>2022</year>
</date>
<date date-type="accepted">
<day>09</day>
<month>05</month>
<year>2022</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2022 Schimpf, Liesner, Franke, Roleda and Bartsch</copyright-statement>
<copyright-year>2022</copyright-year>
<copyright-holder>Schimpf, Liesner, Franke, Roleda and Bartsch</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) and the copyright owner(s) 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>Kelp forests in the North Atlantic are at risk of decline at their warm temperature distribution margins due to anthropogenic temperature rise and more frequent marine heat waves. To investigate the thermal adaptation of the cold-temperate kelp <italic>Laminaria digitata</italic>, we sampled six populations, from the Arctic to Brittany (Spitsbergen, Troms&#xf8;, Bod&#xf8; [all Norway], Helgoland [Germany], Roscoff and Quiberon [both France]), across the species&#x2019; entire distribution range, spanning 31.5&#xb0; latitude and 12-13&#xb0;C difference in mean summer sea surface temperature. We used pooled vegetative gametophytes derived from several sporophytes to approximate the genetic diversity of each location. Gametophytes were exposed to (sub-) lethal high (20-25&#xb0;C) and (sub-) optimal low (0-15&#xb0;C) temperature gradients in two full-factorial, common-garden experiments, subjecting subsets of populations from different origins to the same conditions. We assessed survival of gametophytes, their ability to develop microscopic sporophytes, and subsequent growth. We hypothesized that the thermal performance of gametophytes and microscopic sporophytes corresponds to their local long-term thermal history. Integrated gametophyte survival revealed a uniform upper survival temperature (UST) of 24&#xb0;C among five tested populations (Troms&#xf8; to Quiberon). In contrast, following two weeks of thermal priming of gametophytes at 20-22&#xb0;C, sporophyte formation at 15&#xb0;C was significantly higher in southern populations (Quiberon and Roscoff) compared to the high-latitude population of Troms&#xf8;. Between 0-15&#xb0;C, survival of the Arctic population (Spitsbergen) was negatively correlated with increasing temperatures, while the southern-most population (Quiberon) showed the opposite. Thus, responses of survival at low, and sporophyte formation at high temperatures, support the concept of local adaption. On the other hand, sporophyte formation between 0-15&#xb0;C peaked at 6-9&#xb0;C in the Quiberon and at 9-12&#xb0;C in the Spitsbergen population. Sporophyte growth rates (GR) both in length and width were similar for Spitsbergen, Troms&#xf8; and Quiberon; all had maximum GRs at 12-15&#xb0;C and low GRs at 0-6&#xb0;C. Therefore, responses of sporophyte formation and growth at low temperatures do not reflect ecotypic adaptation. We conclude that <italic>L. digitata</italic> populations display trait-dependent adaptation, partly corresponding to their local temperature histories and partly manifesting uniform or unpredictable responses. This suggests differential selection pressures on the ontogenetic development of kelps such as <italic>L. digitata</italic>.</p>
</abstract>
<kwd-group>
<kwd>kelp</kwd>
<kwd>gametophytes</kwd>
<kwd>temperature</kwd>
<kwd>local adaptation</kwd>
<kwd>North Atlantic</kwd>
<kwd>latitudinal gradient</kwd>
<kwd>populations</kwd>
<kwd>thermal priming</kwd>
</kwd-group>
<contract-num rid="cn001">VA 105/25-1</contract-num>
<contract-sponsor id="cn001">Deutsche Forschungsgemeinschaft<named-content content-type="fundref-id">10.13039/501100001659</named-content>
</contract-sponsor>
<counts>
<fig-count count="6"/>
<table-count count="5"/>
<equation-count count="1"/>
<ref-count count="97"/>
<page-count count="17"/>
<word-count count="10441"/>
</counts>
</article-meta>
</front>
<body>
<sec id="s1">
<title>1 Introduction</title>    <p>Kelp forests are complex, biodiverse, and highly productive ecosystems that occur globally between warm-temperate and polar regions (<xref ref-type="bibr" rid="B87">Teagle et&#xa0;al., 2017</xref>), and in deep tropical waters (<xref ref-type="bibr" rid="B33">Graham et&#xa0;al., 2007</xref>). Even though they provide important ecosystem services, their socio-economic value is only starting to be recognized (e.g., <xref ref-type="bibr" rid="B92">V&#xe1;squez et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B10">Blamey and Bolton, 2018</xref>; <xref ref-type="bibr" rid="B21">Eger et&#xa0;al., 2021</xref>). Kelp forests benefit humankind directly (e.g., kelp harvesting, fishing, tourism), indirectly (e.g., habitat provision, climate regulation, nutrient cycling, carbon capture), and through cultural and spiritual value itself (biodiversity, recreation, science; <xref ref-type="bibr" rid="B27">Filbee-Dexter and Wernberg, 2018</xref>). A key, habitat-forming kelp is the digitate brown alga <italic>Laminaria digitata</italic>, which occurs on the upper subtidal rocky shore in cold-temperate to Arctic regions of the North Atlantic (<xref ref-type="bibr" rid="B51">L&#xfc;ning, 1990</xref>). Its distribution is limited between Spitsbergen (Norway) in the north, and southern Brittany (France) in the south, but it also inhabits the western North Atlantic between the northeast coast of the US and Greenland (<xref ref-type="bibr" rid="B51">L&#xfc;ning, 1990</xref>; <xref ref-type="bibr" rid="B2">Assis et&#xa0;al., 2017a</xref>). It therefore occurs in a broad range of temperatures stretching from the 0&#xb0;C February to the 18&#xb0;C August sea-surface isotherm (<xref ref-type="bibr" rid="B60">M&#xfc;ller et&#xa0;al., 2009</xref>).</p>
<p>Various abiotic factors influence the life cycle and productivity of kelps; however, temperature is one of the major factors determining their biogeographical distribution (<xref ref-type="bibr" rid="B50">L&#xfc;ning, 1984</xref>; <xref ref-type="bibr" rid="B51">L&#xfc;ning, 1990</xref>; <xref ref-type="bibr" rid="B1">Adey and Steneck, 2001</xref>). <italic>Laminaria digitata</italic> displays a haplo-diplontic, heteromorphic life cycle with an alternation between diploid, macroscopic sporophytes and haploid, microscopic gametophytes, where the latter are dioecious and sexually dimorphic (<xref ref-type="bibr" rid="B91">van den Hoek et&#xa0;al., 1995</xref>). Physiological processes differ in their thermal characteristics between ontogenetic stages, but both macro- and microscopic stages are similar in that they reveal a wider temperature range for growth than for reproduction (e.g., <xref ref-type="bibr" rid="B88">tom Dieck (Bartsch), 1992</xref>; <xref ref-type="bibr" rid="B7">Bartsch et&#xa0;al., 2013</xref>). The sporophytic phase of <italic>L. digitata</italic> shows maximal growth at 10-15&#xb0;C (<xref ref-type="bibr" rid="B88">tom Dieck (Bartsch), 1992</xref>) and reproduces best at 5-10&#xb0;C (<xref ref-type="bibr" rid="B7">Bartsch et&#xa0;al., 2013</xref>), whereas gametophyte growth is greatest at 15-18&#xb0;C (<xref ref-type="bibr" rid="B49">L&#xfc;ning, 1980</xref>) and gametogenesis best at 5-15&#xb0;C (<xref ref-type="bibr" rid="B55">Martins et&#xa0;al., 2017</xref>). Ocean warming could thus negatively impact growth and photosynthesis of kelps (<xref ref-type="bibr" rid="B73">Roleda, 2009</xref>; <xref ref-type="bibr" rid="B74">Roleda, 2016</xref>), may result in delayed sporophyte recruitment due to prolonged vegetative growth of gametophytes, and could even lead to inhibition of reproduction and reduction in geographic range of the species (<xref ref-type="bibr" rid="B64">Oppliger et&#xa0;al., 2012</xref>).</p>
<p>In low nutrient and irradiance (white or red light) laboratory settings, gametophytes have, in most cases, survived and grown vegetatively for several months to decades and reproduced sexually when they were returned to optimal conditions (<xref ref-type="bibr" rid="B89">tom Dieck (Bartsch), 1993</xref>; <xref ref-type="bibr" rid="B13">Carney and Edwards, 2010</xref>; <xref ref-type="bibr" rid="B82">Silva et&#xa0;al., 2022</xref>). The ability to maintain such microscopic seed banks (<xref ref-type="bibr" rid="B19">Edwards, 2000</xref>) underlines the principal role that gametophytes play in controlling the species&#x2019; distribution and survival (<xref ref-type="bibr" rid="B20">Edwards, 2022</xref>). This survival mechanism can be vital at warm distribution margins, after prolonged summer heat stress, or after extreme thermal fluctuations (<xref ref-type="bibr" rid="B43">Ladah and Zertuche-Gonz&#xe1;lez, 2007</xref>; <xref ref-type="bibr" rid="B5">Barradas et&#xa0;al., 2011</xref>). The exact contribution of the gametophyte phase to the persistence of kelp forests, however, remains partially speculative due to the difficulty of studying gametophytes <italic>in situ</italic> (<xref ref-type="bibr" rid="B77">Santelices et&#xa0;al., 1995</xref>; <xref ref-type="bibr" rid="B18">Destombe and Oppliger, 2011</xref>; <xref ref-type="bibr" rid="B20">Edwards, 2022</xref>).</p>
<p>Polar and cold-temperate regions have been heavily affected by anthropogenic climate change (<xref ref-type="bibr" rid="B38">Jueterbock et&#xa0;al., 2013</xref>; <xref ref-type="bibr" rid="B28">Filbee-Dexter et&#xa0;al., 2019</xref>) with mean sea surface temperature (SST) increases of ~0.11&#xb0;C per decade between 1971 to 2010 (<xref ref-type="bibr" rid="B35">IPCC, 2014</xref>). Accordingly, SST isotherms have shifted predominantly poleward by 30-100 km per decade (<xref ref-type="bibr" rid="B34">Hansen et&#xa0;al., 2006</xref>). Future projections indicate further isotherm shifts of up to 600 km northwards (<xref ref-type="bibr" rid="B34">Hansen et&#xa0;al., 2006</xref>) and rising annual average SSTs of up to 3-4&#xb0;C by 2100 (<xref ref-type="bibr" rid="B35">IPCC, 2014</xref>). Many coastal organisms, including kelps, will struggle to shift their ranges fast enough to match the current rapid warming projections, given their limited dispersal ability (<xref ref-type="bibr" rid="B56">Merzouk and Johnson, 2011</xref>; <xref ref-type="bibr" rid="B3">Assis et&#xa0;al., 2017b</xref>). More importantly, the increasing occurrence and intensity of marine heat waves may prove to be even more problematic for kelps (<xref ref-type="bibr" rid="B84">Smale et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B29">Filbee-Dexter et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B63">Oliver et&#xa0;al., 2021</xref>). Kelps respond differently, depending on the duration and magnitude of the heat stress (<xref ref-type="bibr" rid="B23">Eggert, 2012</xref>), but are vulnerable to temperature fluctuations that surpass their upper survival threshold for more than a day, particularly toward low-latitude range edges (<xref ref-type="bibr" rid="B17">Dayton and Tegner, 1984</xref>; <xref ref-type="bibr" rid="B83">Smale and Wernberg, 2013</xref>). Several large-scale range shifts have already been documented in the Northeast Atlantic for various kelp species such as <italic>Saccharina latissima</italic> in Norway (<xref ref-type="bibr" rid="B59">Moy and Christie, 2012</xref>) and <italic>Laminaria ochroleuca</italic> in southern Britain (<xref ref-type="bibr" rid="B85">Smale et&#xa0;al., 2015</xref>). In Spain, <italic>Saccorhiza polyschides</italic>, <italic>L. ochroleuca</italic> and <italic>Laminaria hyperborea</italic> have experienced severe regional contractions (<xref ref-type="bibr" rid="B26">Fern&#xe1;ndez, 2011</xref>; <xref ref-type="bibr" rid="B93">Voerman et&#xa0;al., 2013</xref>). A progressive disappearance of <italic>L. digitata</italic> has also been described in France as early as 1999 (<xref ref-type="bibr" rid="B16">Cosson, 1999</xref>), and on Helgoland, considerable biomass loss of <italic>L. digitata</italic> in the shallow sub-tidal was observed between 1968 and 2005 (<xref ref-type="bibr" rid="B66">Pehlke and Bartsch, 2008</xref>). Ecological niche modelling (ENM) and recent analysis of spatio-temporal distribution have shown and predicted northward range shifts of kelps, including <italic>L. digitata</italic> populations (<xref ref-type="bibr" rid="B60">M&#xfc;ller et&#xa0;al., 2009</xref>; <xref ref-type="bibr" rid="B69">Raybaud et&#xa0;al., 2013</xref>; <xref ref-type="bibr" rid="B2">Assis et&#xa0;al., 2017a</xref>; <xref ref-type="bibr" rid="B3">Assis et&#xa0;al., 2017b</xref>; <xref ref-type="bibr" rid="B42">Krause-Jensen et&#xa0;al., 2020</xref>).</p>
<p>Even though projected shifts in distribution patterns frequently presume that individuals of a species respond uniformly to climate change, there is evidence for intraspecific variation among populations of kelps (<xref ref-type="bibr" rid="B40">King et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B41">King et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>; <xref ref-type="bibr" rid="B8">Becheler et&#xa0;al., 2022</xref>). In <italic>S. latissima</italic>, local mortality thresholds of sporophytes differ by ~3&#xb0;C between populations from the NE and NW Atlantic, so single temperature tolerances should not be assumed to apply over an entire species&#x2019; distribution (<xref ref-type="bibr" rid="B29">Filbee-Dexter et&#xa0;al., 2020</xref>). Populations at the warm range edge are expected to contain unique genetic diversity that was maintained across glacial cycles (<xref ref-type="bibr" rid="B52">Maggs et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B2">Assis et&#xa0;al., 2017a</xref>), which may provide them with high physiological versatility and resilience (<xref ref-type="bibr" rid="B95">Wernberg et&#xa0;al., 2018</xref>), but these are especially threatened in the face of climate change. Furthermore, species with broad spatial distributions, occupying a range of thermal niches, may also have evolved unique genetic and phenotypic characteristics (<xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B8">Becheler et&#xa0;al., 2022</xref>). One of the best methods to study adaptive changes along latitudinal gradients are common-garden experiments (<xref ref-type="bibr" rid="B40">King et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B8">Becheler et&#xa0;al., 2022</xref>), in which material from different populations is subjected to the same environment, regardless of the geographical and environmental origin of populations. However, rather than dealing with multiple parental strains to yield substantial genetic representation, past studies have primarily used single clonal strains, but this has changed lately (e.g., <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>; <xref ref-type="bibr" rid="B47">Liesner et&#xa0;al., 2020b</xref>; <xref ref-type="bibr" rid="B8">Becheler et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B32">Gauci et&#xa0;al., 2022</xref>).</p>
<p>In this study, we investigated whether <italic>L. digitata</italic> gametophyte progeny derived from multiple local sporophytes from across their entire latitudinal distribution range are locally adapted to their long-term temperature history. Bearing in mind that <italic>L. digitata</italic> populations are genetically structured into a northern and southern clade (<xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>; <xref ref-type="bibr" rid="B62">Neiva et&#xa0;al., 2020</xref>), we hypothesized that gametophytes derived from southern populations, which are regularly subjected to high summer temperatures &#x2265;18&#xb0;C (Quiberon, Roscoff [both France], and Helgoland [Germany]), will perform better at high temperatures, while gametophytes from northern populations, occasionally exposed to summer temperatures &gt;8-12&#xb0;C (Bod&#xf8;, Troms&#xf8; and Spitsbergen [all Norway]), will perform better at low temperatures. To this end, two full-factorial, common-garden laboratory experiments were conducted on microscopic stages across populations, each with a different subset of populations, to investigate the fitness-related parameters of 1) upper survival temperatures (UST) of gametophytes integrated over time and sporophyte formation following thermal priming at sub-lethal high temperatures, and 2) gametophyte survival, sporophyte formation and sporophyte growth at low to optimum temperatures.</p>
</sec>
<sec id="s2" sec-type="materials|methods">
<title>2 Materials and Methods</title>
<sec id="s2_1">
<title>2.1 Study Sites</title>
<p>Samples were collected from the following six locations along the European NE Atlantic coast during summer, from north, in the Arctic, to south, on the coast of Brittany: Spitsbergen (SPT), Troms&#xf8; (TRM), Bod&#xf8; (BOD), Helgoland (HLG), Roscoff (ROS) and Quiberon (QUI; <xref ref-type="fig" rid="f1">
<bold>Figures&#xa0;1</bold>
</xref>, <xref ref-type="fig" rid="f2">
<bold>2</bold>
</xref>; for sampling details see <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>). Spitsbergen and Quiberon, respectively, correspond to the northern and southern distribution boundaries of <italic>L. digitata</italic>. Maps were generated using a European Environment Agency coastline shapefile (<xref ref-type="bibr" rid="B25">European Environment Agency, 2021</xref>) and QGIS 3.8.2-Zanzibar software (<xref ref-type="bibr" rid="B68">QGIS Development Team, 2019</xref>).</p>
<fig id="f1" position="float">
<label>Figure&#xa0;1</label>
<caption>
<p>Sampling sites along the NE Atlantic coast. Inset maps show more precise locations within each area. Sampling sites were Spitsbergen, Norway (SPT), Troms&#xf8;, Norway (TRM), Bod&#xf8;, Norway (BOD), Helgoland, Germany (HLG), Roscoff, France (ROS) and Quiberon, France (QUI).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-870792-g001.tif"/>
</fig>
<fig id="f2" position="float">
<label>Figure&#xa0;2</label>
<caption>
<p>
<bold>(A)</bold> Average annual sea surface temperatures (SSTs) for each month between 2010 and 2020 and <bold>(B)</bold> overall averages between 2010 and 2020. Satellite-derived data were obtained from the <xref ref-type="bibr" rid="B24">E.U. Copernicus Marine Service (2021)</xref>. SPT, Spitsbergen; TRM, Troms&#xf8;; BOD, Bod&#xf8;; HLG, Helgoland; ROS, Roscoff; QUI, Quiberon.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-870792-g002.tif"/>
</fig>
</sec>
<sec id="s2_2">
<title>2.2 Sampling and Culture Conditions</title>
<p>Fertile <italic>L. digitata</italic> sporophytes (n=30-35, for Helgoland n=15), spaced &#x2265;1 m apart, were collected at low tide in the infralittoral fringe at each location, and stored in ambient seawater flow-through tanks for immediate processing not lasting more than three days. Two soral discs per individual (&#xd8;=20 mm) were cut out, briefly rinsed with fresh water, and placed in a 50 ml centrifuge tube containing two microscope slides and 45 ml sterile seawater. They were left for 1-3 days to allow released spores to settle. In samples from Bod&#xf8;, sporulation was induced by leaving discs in a wet chamber overnight before adding sterile seawater. Saturated germanium dioxide solution (GeO<sub>2</sub>) was added (0.5 ml/l) to prevent diatom growth (<xref ref-type="bibr" rid="B81">Shea and Chopin, 2007</xref>). Tubes were transported in dark, cooled (&lt;15&#xb0;C) boxes from the respective locations to the Alfred Wegener Institute in Bremerhaven, Germany, within two days. Samples were stored at 5&#xb0;C with a maximum irradiance of 5 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> white light (LED Mitras Lightbar Daylight 150 controlled by a ProfiLux 3 computer, GHL Advanced Technology, Kaiserslautern, Germany), measured using a LI 190SB quantum sensor coupled to a LI-185B photometer (LI-COR-Biosciences, Lincoln, NE, USA) in a 16:8 h light:dark (LD) photoperiod. Microscope slides were then transferred to Petri dishes (&#xd8;=9 cm) filled with iron-free, half strength Provasoli enriched seawater (PES) to inhibit gametogenesis (<xref ref-type="bibr" rid="B67">Provasoli, 1968</xref>; <xref ref-type="bibr" rid="B45">Lewis et&#xa0;al., 2013</xref>; iodide enrichment according to <xref ref-type="bibr" rid="B86">Tatewaki (1966)</xref>, double concentration of Na<sub>2</sub>glycerophosphate) and GeO<sub>2</sub>, and stored at 15&#xb0;C in 3-4 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> red LED light to allow germination into vegetative gametophytes until start of experiment 1 (for details see <xref ref-type="supplementary-material" rid="SM1">
<bold>Table S1</bold>
</xref>). For experiment 2, pairs of male and female gametophytes, each originating from a single sporophyte, were isolated in 2016 (Spitsbergen) and in 2019 (Troms&#xf8;, Quiberon) into unialgal stock cultures and cultivated in 3 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> red light at 15&#xb0;C in &#xbd; PES until start of the experiment in 2020 (for details see <xref ref-type="supplementary-material" rid="SM1">
<bold>Table S2</bold>
</xref>). This approach was needed, as long-term cultivation of dense, mixed gametophytes is often prone to hidden contamination that causes experimental bias, and because one sex may overgrow the other, resulting in an increasingly skewed sex-ratio (see <xref ref-type="bibr" rid="B55">Martins et&#xa0;al., 2017</xref>).</p>
</sec>
<sec id="s2_3">
<title>2.3 Experiment 1 &#x2013; Upper Temperature Performance of <italic>Laminaria digitata</italic> Gametophytes</title>
<sec id="s2_3_1">
<title>2.3.1 Stock Cultures</title>
<p>Five replicate gametophyte stock cultures were prepared for the Troms&#xf8;, Bod&#xf8;, Roscoff and Quiberon populations (<xref ref-type="supplementary-material" rid="SM1">
<bold>Table S1</bold>
</xref>). Each stock contained gametophyte progeny derived from meiospores that originated from three distinct sporophytes and thus consisted of families of hundreds of sibling gametophytes. Replicates were therefore true biological replicates. Equal quantities of gametophyte material were gently fragmented with a sterile pestle and mortar, sieved to obtain a size fraction &lt;100 &#xb5;m and kept in suspension on a magnetic mixer at ~250 rpm. The density of each stock culture was estimated under an inverted microscope (Olympus CKX41, Olympus Co., Tokyo, Japan). Stock cultures were seeded into Petri dishes (&#xd8;=6 cm) filled with 100 ml &#xbd; PES to achieve a target density of 600 gametophytes cm<sup>-2</sup>. This density allows for good distinction between gametophytes and does not inhibit gametogenesis (<xref ref-type="bibr" rid="B55">Martins et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>).</p>
<p>Samples from the Helgoland population had been collected a year before establishment of the standardized experimental protocol. Meiospores from Helgoland were released from sori after being stored for 1-2 days in &lt;5 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> white light in plastic bags filled with sterilized natural seawater, following the method of <xref ref-type="bibr" rid="B6">Bartsch (2018)</xref>. Spore suspensions obtained from five individual sporophytes were used to inoculate four replicate dishes at a target density of 15,000 spores cm<sup>-2</sup>. Following meiospore germination in 15 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> for four days, dishes were stored in darkness at 15&#xb0;C for four weeks before initiation of the experiment. For each of the five lineages, four replicate dishes were placed into five temperature treatments (n=4 for five lineages; n=20 in total).</p>
</sec>
<sec id="s2_3_2">
<title>2.3.2 Experimental Set-up</title>
<p>Gametophytes from Troms&#xf8;, Bod&#xf8;, Roscoff and Quiberon were acclimated for six days (three days at 15&#xb0;C and three days at 20&#xb0;C) in an irradiance of 2-3 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> white LED light in a 16:8 h LD regime. Gametophytes were incubated in temperature-controlled water baths (Huber Variostat CC + Pilot ONE, Peter Huber K&#xe4;ltemaschinen GmbH, Offenburg, Germany). With the beginning of the priming period on day 0, the irradiance was raised to 15 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> and gametophytes were exposed to high temperatures spanning 20&#xb0;C, 21&#xb0;C, 22&#xb0;C, 23&#xb0;C, 24&#xb0;C and 25&#xb0;C &#xb1; 0.1&#xb0;C for 14 days. A 15&#xb0;C treatment served as control to monitor gametogenesis in optimum conditions (<xref ref-type="bibr" rid="B49">L&#xfc;ning, 1980</xref>). On day 14, gametophytes from all priming treatments were transferred to 15&#xb0;C for 14 days under the same irradiance conditions, to observe potential recovery and sporophyte formation. Medium exchange took place on day 14 and 28. Spitsbergen material was excluded here, as the temperature tolerance of this population has been determined before (<xref ref-type="bibr" rid="B31">Franke et&#xa0;al., 2021</xref>).</p>
<p>Material from Helgoland was acclimated to low light (3-5 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup>) for five days and brighter light (15 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup>) for one day before start of the experiment. The experiment started immediately for the 15&#xb0;C and 20&#xb0;C treatments, while the remaining treatments underwent a temperature ramping period: 22&#xb0;C (one day at 20&#xb0;C), 24&#xb0;C (one day at 20&#xb0;C) and 25&#xb0;C (one day at 20&#xb0;C, two days at 24&#xb0;C). There were no 21&#xb0;C and 23&#xb0;C treatments for the Helgoland population. Following the 14-day priming period, gametophytes were transferred to 20&#xb0;C in 5 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> for 14 days of post-culture.</p>
<p>In all populations, long-term post-cultivation in apparently lethal temperatures (24&#xb0;C and 25&#xb0;C) was checked against control (20&#xb0;C) after approximately 3 to 15 weeks at 15&#xb0;C in low red light and iron-free &#xbd; PES.</p>
</sec>
<sec id="s2_3_3">
<title>2.3.3 Gametophyte Survival Under Heat Stress</title>
<p>Total gametophyte density was quantified on day 0, 4, 8, 11, 14 and after recovery on day 21 and 28 (day 0, 7, 14 and 28 for Helgoland; no day 28 for Bod&#xf8;) under an inverted microscope. The mean number of randomly selected fields of view required to quantify &#x2265;200 female gametophytes was estimated on day 0 and used as a standard for subsequent measurements. Cells were considered alive when they still showed pigmentation.</p>
<p>Due to differences in methodology between the direct seeding of spores from Helgoland and the use of multi-cellular, vegetative gametophyte progeny for the other populations, Helgoland had a significantly higher initial gametophyte density (single cells) on day 0 than Troms&#xf8;, Bod&#xf8;, Roscoff and Quiberon (Kruskal-Wallis, <italic>X</italic>
<sup>2</sup> = 193.69, <italic>p</italic>&lt;0.0001, df = 4). However, the absolute number of cells per dish was similar (<xref ref-type="supplementary-material" rid="SM1">
<bold>Table S3</bold>
</xref>). We therefore calculated integrated gametophyte survival over time as follows: for each priming treatment and population, we averaged gametophyte survival between day 4 and 28, based on six (BOD: five; HLG: three) points in time, to yield overall gametophyte survival over the entire experimental phase. Some replicates were excluded from statistical analysis when contaminations through diatoms or filamentous brown algae became visible.</p>
</sec>
<sec id="s2_3_4">
<title>2.3.4 Sporophyte Formation During Recovery From Thermal Priming</title>
<p>The formation of microscopic sporophytes (% of female gametophytes with sporophytes) at 15&#xb0;C, following the 2-week-long thermal priming period, was quantified on day 28. Microscopic sporophytes were distinguished from released eggs when they were no longer spherical or showed first cell divisions.</p>
</sec>
</sec>
<sec id="s2_4">
<title>2.4 Experiment 2 - Lower Temperature Performance of <italic>Laminaria digitata</italic> Gametophytes</title>
<sec id="s2_4_1">
<title>2.4.1 Stock Cultures</title>
<p>Five male and five female stock cultures were prepared for the Spitsbergen, Troms&#xf8; and Quiberon populations, each containing equal quantities of pooled gametophyte material from five clonal isolates (always one pair of male and female gametophytes derived from one sporophyte) which had been obtained from different sporophytes (<xref ref-type="supplementary-material" rid="SM1">
<bold>Table S2</bold>
</xref>). A density of 300 male and 300 female gametophytes cm<sup>-2</sup> was targeted. As these gametophytes were fragmented pieces of the five clonal cultures, the actual fraction of each clone per replicate was not controllable, however we assumed a random dispersal. Fragmentation, sieving, and density determination was conducted as described above. Due to logistical reasons, we only chose representatives of the coldest, warmest, and intermediate temperature environments of the species (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>).</p>
</sec>
<sec id="s2_4_2">
<title>2.4.2 Experimental Set-up</title>
<p>For gametophytes from Spitsbergen, Troms&#xf8; and Quiberon, the temperature was ramped down over the course of six days, starting with a temperature of 15&#xb0;C which was lowered daily by 3&#xb0;C until the respective experimental temperature (0&#xb0;C, 3&#xb0;C, 6&#xb0;C, 9&#xb0;C, 12&#xb0;C and 15&#xb0;C &#xb1; 0.1&#xb0;C) was reached one day before the start of the treatment period. These temperatures were chosen as they approximately correspond to the different local long-term SST averages (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>). Ramping took place in 1-2 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> white light in a 16:8 h LD cycle to suppress fertility. With the start of the 21-day long treatment period, the irradiance was increased to 15 &#xb1; 1 &#xb5;mol photons m<sup>-2</sup> s<sup>-1</sup> white light with the same photoperiod, and the medium (&#xbd; PES) was exchanged once on day 14.</p>
</sec>
<sec id="s2_4_3">
<title>2.4.3 Gametophyte and Sporophyte Quantification</title>
<p>Counting of the gametophytes was conducted as described for experiment 1. The required number of fields of view to be counted was based on quantifying &#x2265;400 total male and female gametophytes on day 0, as sexual dimorphism was not yet entirely evident. Due to significant differences in initial gametophyte densities (ANOVA, <italic>F</italic>
<sub>(2,87)</sub>=24.95, <italic>p</italic>&lt;0.0001; <xref ref-type="supplementary-material" rid="SM1">
<bold>Table S3</bold>
</xref>), percentage survival of gametophytes was quantified on day 0, 7, 14 and 21 relative to day 0. The formation of microscopic sporophytes (% of female gametophytes with sporophytes) and sporophyte density (sporophytes cm <sup>-2</sup>) were quantified on day 7, 14 and 21.</p>
</sec>
<sec id="s2_4_4">
<title>2.4.4 Sporophyte Size and Growth</title>
<p>The size of microscopic sporophytes was measured on day 7 and 21 <italic>via</italic> photographic images (camera: AxioCam ERc5s mounted on an inverted microscope). Per replicate, ten fields of view containing at least one sporophyte were randomly photographed. The length and width of the longest sporophyte in each photograph was measured using the imaging software ZEN 2 Blue Edition version 2.3. If only one sporophyte was present, this one was selected. As sporophyte formation is a continuous process stretching over several weeks, we assumed that the longest sporophytes in each photograph represented the oldest ones and thus provided the best proxy for maximal growth. Length to width ratio (L:W ratio) was derived for day 21. In addition, the linear length (GR <sub>length</sub>) and linear width growth rates (GR <sub>length</sub> and GR <sub>width</sub>), were calculated separately between day 7 and 21 as follows:</p>
<disp-formula>
<mml:math display="block" id="M1">
<mml:mrow>
<mml:mi>G</mml:mi>
<mml:mi>R</mml:mi>
<mml:mo>&#xa0;</mml:mo>
<mml:mrow>
<mml:mo>(</mml:mo>
<mml:mrow>
<mml:mi>&#x3bc;</mml:mi>
<mml:mi>m</mml:mi>
<mml:mi>w</mml:mi>
<mml:msup>
<mml:mi>k</mml:mi>
<mml:mrow>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>1</mml:mn>
</mml:mrow>
</mml:msup>
</mml:mrow>
<mml:mo>)</mml:mo>
</mml:mrow>
<mml:mo>=</mml:mo>
<mml:mfrac>
<mml:mrow>
<mml:msub>
<mml:mi>x</mml:mi>
<mml:mn>2</mml:mn>
</mml:msub>
<mml:mo>&#x2212;</mml:mo>
<mml:msub>
<mml:mi>x</mml:mi>
<mml:mn>1</mml:mn>
</mml:msub>
</mml:mrow>
<mml:mrow>
<mml:msub>
<mml:mi>t</mml:mi>
<mml:mn>2</mml:mn>
</mml:msub>
<mml:mo>&#x2212;</mml:mo>
<mml:msub>
<mml:mi>t</mml:mi>
<mml:mn>1</mml:mn>
</mml:msub>
</mml:mrow>
</mml:mfrac>
</mml:mrow>
</mml:math>
</disp-formula>
<p>where x is the length or width (<italic>&#x3bc;</italic>m), and t is the time in weeks (wk) at time point 1 and 2.</p>
</sec>
</sec>
<sec id="s2_5">
<title>2.5 Statistical Analysis</title>
<p>Statistics were performed using R version 3.6.3 (<xref ref-type="bibr" rid="B70">R Core Team, 2020</xref>). One-way ANOVA was performed to test initial gametophyte densities in experiment 2 and gametophyte survival at 24&#xb0;C and 25&#xb0;C on day 8 (HLG, day 7) in experiment 1. Initial densities in experiment 1 did not meet assumptions of homogeneity, so a non-parametric Kruskal-Wallis test was performed, with subsequent pairwise Wilcoxon rank sum testing and Bonferroni correction of <italic>p</italic>-values to reduce the probability of type I errors. Sporophyte GR <sub>length</sub>, GR <sub>width</sub> and L:W ratio were analyzed using ANCOVA, with sporophyte density (day 7) as a covariate, as density may influence growth rates. All other parameters were evaluated by two-way ANOVA. Statistically significant differences were compared with the <italic>post hoc</italic> Tukey honest significance difference (HSD) test using the &#x201c;emmeans&#x201d; package. Prior to analysis, data were tested for homogeneity of variance using the Levene&#x2019;s test. Data with heterogeneous variances were either square-root, fourth-root or logarithmically transformed (<xref ref-type="bibr" rid="B90">Underwood, 1996</xref>). If assumptions of homogeneity were still not met, the significance level was lowered to <italic>p</italic>&lt;0.01, as there is no non-parametric alternative for two-way ANOVA with <italic>post hoc</italic> tests. Reports of pairwise comparisons are described by the highest <italic>p</italic>-value.</p>
</sec>
</sec>
<sec id="s3">
<title>3 Results</title>
<sec id="s3_1">
<title>3.1 Experiment 1</title>
<sec id="s3_1_1">
<title>3.1.1 Gametophyte Survival</title>
<p>Integrated survival of <italic>L. digitata</italic> gametophytes at (sub-) lethal high temperatures (20-25&#xb0;C) over time (day 4-28) was significantly influenced by population and temperature, but there was no interaction (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>; <xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>). Thus, all populations responded to temperature in the same way. Gametophytes from all populations suffered a loss of pigmentation at 24&#xb0;C and 25&#xb0;C, resulting in a significantly lower mean survival in the 24&#xb0;C (19.9%-40.8%) and 25&#xb0;C treatments (0.1%-24.3%) than in the 15-23&#xb0;C treatments (70.4%-104.5%; [15&#xb0;C = 20&#xb0;C = 21&#xb0;C = 22&#xb0;C = 23&#xb0;C] &gt; [24&#xb0;C = 25&#xb0;C]; Tukey tests, <italic>p</italic>&lt;0.05). Between populations, there were statistically significant differences in integrated gametophyte survival at 15&#xb0;C ([ROS = BOD = TRM] &gt; [QUI = HLG = BOD = TRM]; Tukey tests, <italic>p</italic>&lt;0.05), at 20&#xb0;C ([QUI = ROS = BOD =TRM] &gt; [QUI = HLG]; Tukey tests, <italic>p</italic>&lt;0.01) and at 22&#xb0;C ([ROS = BOD = TRM] &gt; [QUI = ROS = HLG]; Tukey tests, <italic>p</italic>&lt;0.05). In gametophytes from all populations except for Helgoland, the survival rate intermittently rose above 100%, which probably indicates fragmentation of vegetative gametophytes into smaller pieces by die-off of intercalary gametophyte cells. However, this process was not quantified.</p>
<table-wrap id="T1" position="float">
<label>Table&#xa0;1</label>
<caption>
<p>Two-way ANOVA to assess the effects of priming temperature and population on integrated survival of <italic>Laminaria digitata</italic> gametophytes over time in experiment 1.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left">Parameter</th>
<th valign="top" align="center">numDf</th>
<th valign="top" align="center">denDF</th>
<th valign="top" align="center">
<italic>F</italic>-value</th>
<th valign="top" align="center">
<italic>p</italic>-value</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Population</td>
<td valign="top" align="center">4</td>
<td valign="top" align="center">143</td>
<td valign="top" align="center">6.671</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Priming temperature</td>
<td valign="top" align="center">6</td>
<td valign="top" align="center">143</td>
<td valign="top" align="center">83.06</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Population &#xd7; priming temperature</td>
<td valign="top" align="center">22</td>
<td valign="top" align="center">143</td>
<td valign="top" align="center">0.459</td>
<td valign="top" align="center">0.982</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>Statistically significant values (p &lt; 0.01) are highlighted in bold. numDf, numerator degrees of freedom; denDf, denominator degrees of freedom.</p>
</fn>
</table-wrap-foot>
</table-wrap>
<fig id="f3" position="float">
<label>Figure&#xa0;3</label>
<caption>
<p>Integrated gametophyte survival over time of <italic>Laminaria digitata</italic> along a temperature gradient in experiment 1. Mean relative gametophyte survival between day 4 and 28 for priming treatments 15-25&#xb0;C for Troms&#xf8; (TRM; n = 5; day 28, n = 4), Bod&#xf8; (BOD; n = 5), Helgoland (HLG; n = 4), Roscoff (ROS; n = 5; day 21-28, n = 3) and Quiberon (QUI; n = 5; day 21-28, n = 4) averaged over six (BOD: five; HLG: three) points in time. Letters indicate statistical differences in survival between treatments within each population (ANOVA; Tukey test, <italic>p</italic> &lt; 0.01). Asterisks and dashed boxes denote the degree of significant differences between populations within treatments (ANOVA, Tukey test, <italic>p</italic> &lt; 0.05). Values are expressed as the mean of means &#xb1; SD.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-870792-g003.tif"/>
</fig>
<p>With respect to percentage survival, gametophytes from all populations survived between 57%-100% in the 15-23&#xb0;C treatments for 28 days (<xref ref-type="supplementary-material" rid="SM1">
<bold>Figure S1</bold>
</xref>). At higher temperatures, gametophytes from all populations suffered a loss of pigmentation with low survival at 24&#xb0;C (&lt;7.6% on day 14 and &lt;2.2% on day 28) and no survival at 25&#xb0;C (<xref ref-type="supplementary-material" rid="SM1">
<bold>Figure S1</bold>
</xref>). A noteworthy disparity was visible on day 8 (HLG, day 7) at 24&#xb0;C and 25&#xb0;C. In the 24&#xb0;C treatment, gametophytes from Troms&#xf8; maintained a significantly higher survival than gametophytes from Bod&#xf8;, Helgoland and Quiberon, while survival of gametophytes from Roscoff was intermediate (ANOVA, <italic>F</italic>
<sub>(4,35)</sub>=6.42, <italic>p</italic>&lt;0.001). After 8 days at 25&#xb0;C, survival declined to &lt;3.7% in gametophytes from all populations except for Troms&#xf8;, which displayed a significantly higher gametophyte survival of 51.7% at this point (<italic>F</italic>
<sub>(4,35)</sub>=59.34, <italic>p</italic>&lt;0.0001).</p>
<p>The long-term post-cultivation of the 24&#xb0;C treatment (data not shown) revealed that single gametophyte cells from all populations survived and proliferated vegetatively again after a few weeks at 15&#xb0;C (QUI, 3 weeks: 0.01%-0.14% males, 0% females; ROS, 5 weeks: 0%-0.1% males, 0%-0.03% females; HLG, 15 weeks: 0%-2.3% total gametophytes; BOD, 4 weeks: 0.01%-0.21% males, 0%-0.08% females; TRM: no data). However, at 25&#xb0;C no gametophyte cells had survived at all.</p>
</sec>
<sec id="s3_1_2">
<title>3.1.2 Sporophyte Formation</title>
<p>During the 14-day thermal priming period, female gametophytes in the 20-25&#xb0;C treatments from all populations remained in a vegetative state or died, while in the 15&#xb0;C treatment eggs and sporophytes developed as expected. In all populations, only females that were primed at 20-23&#xb0;C developed eggs and sporophytes after transfer to 15&#xb0;C (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>).</p>
<fig id="f4" position="float">
<label>Figure&#xa0;4</label>
<caption>
<p>Formation of microscopic sporophytes of <italic>Laminaria digitata</italic> on day 28, after 14 days of thermal priming at (sub)-lethal non-fertilizing temperatures (20&#xb0;C, 21&#xb0;C, 22&#xb0;C and 23&#xb0;C) followed by 14 days of recovery at 15&#xb0;C in the three populations Troms&#xf8; (TRM; n = 4), Roscoff (ROS; n = 3) and Quiberon (QUI; n = 4) in experiment 1. 15&#xb0;C served as control temperature over 28 days. The 24&#xb0;C treatment was excluded, as only 0%-3% of gametophytes survived and they did not become fertile during recovery at 15&#xb0;C. There were no surviving gametophytes at 25&#xb0;C. Values are expressed as the mean &#xb1; SD.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-870792-g004.tif"/>
</fig>
<p>Sporophyte formation on day 28, 14 days after transfer to 15&#xb0;C, was significantly influenced by priming temperature, population, and their interaction (<xref ref-type="table" rid="T2">
<bold>Table&#xa0;2</bold>
</xref>), and decreased with increasing priming temperature in samples from all populations (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>). Significant differences between populations were evident at priming temperatures of 20&#xb0;C, 21&#xb0;C and 22&#xb0;C while at 23&#xb0;C, female gametophytes from all populations showed no or very low mean sporophyte development (0%-12.3% females with sporophytes). At 24&#xb0;C, gametophyte survival was only 0%-3% and gametophytes did not become fertile during recovery at 15&#xb0;C. In the 20&#xb0;C priming treatment, females from the southern populations Quiberon (98.0 &#xb1; 2.4%) and Roscoff (83.4 &#xb1; 8.7%) developed significantly more microscopic sporophytes per female gametophyte than the northern population Troms&#xf8; (48.1 &#xb1; 13.4%; Tukey test, <italic>p</italic>&lt;0.0001). In the 21&#xb0;C and 22&#xb0;C priming treatments, respective sporophyte formation differed significantly among all populations (QUI [21&#xb0;C: 100 &#xb1; 0%; 22&#xb0;C: 89.1 &#xb1; 15.3%] &gt; ROS [21&#xb0;C: 58.7 &#xb1; 12.1%; 22&#xb0;C: 42.0 &#xb1; 10.1%] &gt;TRM [21&#xb0;C: 10.2 &#xb1; 5.0%; 22&#xb0;C: 8.8 &#xb1; 5.6%]; Tukey test, <italic>p</italic>&lt;0.0001).</p>
<table-wrap id="T2" position="float">
<label>Table&#xa0;2</label>
<caption>
<p>Two-way ANOVA to examine the effects of priming temperature and population on the sporophyte formation of <italic>Laminaria digitata</italic> gametophytes from Troms&#xf8;, Roscoff and Quiberon on day 28 during experiment 1.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left">Parameter</th>
<th valign="top" align="center">numDF</th>
<th valign="top" align="center">denDF</th>
<th valign="top" align="center">
<italic>F</italic>-value</th>
<th valign="top" align="center">
<italic>p</italic>-value</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Population</td>
<td valign="top" align="center">2</td>
<td valign="top" align="center">39</td>
<td valign="top" align="center">178.22</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Priming temperature</td>
<td valign="top" align="center">4</td>
<td valign="top" align="center">39</td>
<td valign="top" align="center">190.57</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Population &#xd7; priming temperature</td>
<td valign="top" align="center">8</td>
<td valign="top" align="center">39</td>
<td valign="top" align="center">24.53</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>Statistically significant values (p &lt; 0.05) are highlighted in bold. numDF, numerator degrees of freedom; denDf, denominator degrees of freedom. Included in the analysis are the 15&#xb0;C and 20-23&#xb0;C priming temperatures.</p>
</fn>
</table-wrap-foot>
</table-wrap>
<p>Within populations, female gametophytes from Quiberon showed the broadest temperature window for sporophyte formation (89.1%-100%) between 15&#xb0;C and the 22&#xb0;C priming treatment ([15&#xb0;C = 20&#xb0;C = 21&#xb0;C = 22&#xb0;C] &gt; 23&#xb0;C; Tukey test, <italic>p</italic>&lt;0.0001). Sporophyte formation in females from Roscoff was highest at 15&#xb0;C and in the 20&#xb0;C priming treatment (99.6%-83.4%) and decreased linearly with warmer priming temperatures ([15&#xb0;C = 20&#xb0;C] &gt; [21&#xb0;C = 22&#xb0;C] &gt; 23&#xb0;C; Tukey test, <italic>p</italic>&lt;0.05). Reproductive success in the Troms&#xf8; population was highest at 15&#xb0;C (86.9% &#xb1; 9.4%), intermediate at the 20&#xb0;C priming temperature (48.1 &#xb1; 13.4%) and decreasing sharply to 8.8%-10.2% at the 21-23&#xb0;C priming temperatures (15&#xb0;C &gt; 20&#xb0;C &gt; [21&#xb0;C = 22&#xb0;C = 23&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.0001).</p>
</sec>
</sec>
<sec id="s3_2">
<title>3.2 Experiment 2</title>
<sec id="s3_2_1">
<title>3.2.1 Gametophyte Survival</title>
<p>Survival of <italic>L. digitata</italic> gametophytes from Spitsbergen, Troms&#xf8; and Quiberon at lower temperatures (0-15&#xb0;C) is shown in <xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5A</bold>
</xref>. There was a significant population &#xd7; temperature interaction for the survival of gametophytes after 21 days (<xref ref-type="table" rid="T3">
<bold>Table&#xa0;3</bold>
</xref>). The significant population differences corresponded to the latitudinal origin of gametophytes. Gametophytes from the northern-most population of Spitsbergen survived better at lower temperatures, with significantly higher survival at 0&#xb0;C (57.3% &#xb1; 8.4%) and 3&#xb0;C (58.0% &#xb1; 8.6%) than at 12&#xb0;C (35.3% &#xb1; 2.4%) and 15&#xb0;C (36.9% &#xb1; 9.7%; [0&#xb0;C = 3&#xb0;C = 6&#xb0;C = 9&#xb0;C] &gt; [6&#xb0;C = 9&#xb0;C = 15&#xb0;C] &gt; [6&#xb0;C = 12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). The southern population of Quiberon on the other hand showed significantly higher survival at 9-15&#xb0;C (87.1%-88.4%) than at 0&#xb0;C (66.1% &#xb1; 6.5%; [0&#xb0;C = 3&#xb0;C = 6&#xb0;C] &lt; [3&#xb0;C = 6&#xb0;C = 9&#xb0;C = 12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). Gametophytes from Troms&#xf8; showed significantly lower survival at 3&#xb0;C (56.1% &#xb1; 7.3%) and 12&#xb0;C (56.5% &#xb1; 5.6%) than at 15&#xb0;C (78.0% &#xb1; 10.2%; [0&#xb0;C = 3&#xb0;C = 6&#xb0;C = 9&#xb0;C = 12&#xb0;C] &lt; [0&#xb0;C = 6&#xb0;C = 9&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05).</p>
<fig id="f5" position="float">
<label>Figure&#xa0;5</label>
<caption>
<p>Effect of temperature on <bold>(A)</bold> the gametophyte survival (%), <bold>(B)</bold> females with microscopic sporophytes (%) and <bold>(C)</bold> absolute sporophyte density of <italic>Laminaria digitata</italic> on day 21 in three populations (Spitsbergen, SPT; Troms&#xf8;, TRM; Quiberon, QUI) along a temperature gradient between 0&#xb0;C and 15&#xb0;C during experiment 2. The Troms&#xf8; population was excluded in <bold>(B)</bold> and <bold>(C)</bold>, due to high egg mortality after 14 days. Values are expressed as the mean &#xb1; SD (n = 5).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-870792-g005.tif"/>
</fig>
<table-wrap id="T3" position="float">
<label>Table&#xa0;3</label>
<caption>
<p>Results of two-way ANOVAs to examine the effects of temperature and population on the response variables gametophyte survival, sporophyte formation and sporophyte density of Laminaria digitata from Spitsbergen, Troms&#xf8; and Quiberon on day 21 along the lower temperature gradient (0-15&#xb0;C) in experiment 2.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left">Response variable</th>
<th valign="top" align="center">Parameter</th>
<th valign="top" align="center">numDF</th>
<th valign="top" align="center">denDF</th>
<th valign="top" align="center">
<italic>F</italic>-value</th>
<th valign="top" align="center">
<italic>p</italic>-value</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Gametophyte survival</td>
<td valign="top" align="left">Population</td>
<td valign="top" align="left">2</td>
<td valign="top" align="left">72</td>
<td valign="top" align="left">84.14</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">
</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">5</td>
<td valign="top" align="left">72</td>
<td valign="top" align="left">1.98</td>
<td valign="top" align="left">0.0917</td>
</tr>
<tr>
<td valign="top" align="left">
</td>
<td valign="top" align="left">Population &#xd7; temperature</td>
<td valign="top" align="left">10</td>
<td valign="top" align="left">72</td>
<td valign="top" align="left">5.96</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Sporophyte formation</td>
<td valign="top" align="left">Population</td>
<td valign="top" align="left">1</td>
<td valign="top" align="left">48</td>
<td valign="top" align="left">11.14</td>
<td valign="top" align="left">
<bold>&lt;0.01</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">
</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">5</td>
<td valign="top" align="left">48</td>
<td valign="top" align="left">178.84</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">
</td>
<td valign="top" align="left">Population &#xd7; temperature</td>
<td valign="top" align="left">5</td>
<td valign="top" align="left">48</td>
<td valign="top" align="left">20.56</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Sporophyte density</td>
<td valign="top" align="left">Population</td>
<td valign="top" align="left">1</td>
<td valign="top" align="left">48</td>
<td valign="top" align="left">117.76</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">
</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">5</td>
<td valign="top" align="left">48</td>
<td valign="top" align="left">91.41</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">
</td>
<td valign="top" align="left">Population &#xd7; temperature</td>
<td valign="top" align="left">5</td>
<td valign="top" align="left">48</td>
<td valign="top" align="left">24.18</td>
<td valign="top" align="left">
<bold>&lt;0.0001</bold>
</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>Statistically significant values (p&lt;0.05) are highlighted in bold. numDF, numerator degrees of freedom; denDf, denominator degrees of freedom. Note that gametophytes from Troms&#xf8; were excluded from the sporophyte formation and density analysis, as most eggs had died after 14 days between 6&#xb0;C and 15&#xb0;C.</p>
</fn>
</table-wrap-foot>
</table-wrap>
</sec>
<sec id="s3_2_2">
<title>3.2.2 Sporophyte Formation</title>
<p>The formation of microscopic sporophytes on day 21 was significantly affected by an interaction of population and temperature (<xref ref-type="table" rid="T3">
<bold>Table&#xa0;3</bold>
</xref>; <xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5B</bold>
</xref>). Due to unknown reasons, many eggs in the Troms&#xf8; population disintegrated after 14 days between 6&#xb0;C and 15&#xb0;C, resulting in low numbers of offspring, so this population was excluded from the statistical analysis. In samples from Spitsbergen, the percentage of female gametophytes with sporophytes at 0&#xb0;C (42.8% &#xb1; 4.0%) and 3&#xb0;C (72.1% &#xb1; 7.3%) was significantly lower than between 6&#xb0;C and 15&#xb0;C (84.0%-96.0%; 0&#xb0;C &lt; 3&#xb0;C &lt; [6&#xb0;C = 9&#xb0;C = 15&#xb0;C] &lt; [9&#xb0;C = 12&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). In the Quiberon population, the highest proportion of females with sporophytes was observed in the mid temperatures between 3&#xb0;C and 12&#xb0;C (79.5%-95.2%), with maxima at 6&#xb0;C and 9&#xb0;C, which were significantly higher than at 0&#xb0;C (24.9% &#xb1; 10.9%) and 15&#xb0;C (59.7% &#xb1; 3.1%; 0&#xb0;C &lt; 15&#xb0;C &lt; [3&#xb0;C = 12&#xb0;C] &lt; [9&#xb0;C = 12&#xb0;C] &lt; [6&#xb0;C = 9&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). It is also noteworthy that relative sporophyte formation per female gametophyte in the northern-most population of Spitsbergen was significantly higher than in the southern population of Quiberon at 0&#xb0;C, 12&#xb0;C and 15&#xb0;C, while there were no significant differences between the two populations at 3&#xb0;C, 6&#xb0;C and 9&#xb0;C (Tukey test, <italic>p</italic>&lt;0.05).</p>
</sec>
<sec id="s3_2_3">
<title>3.2.3 Sporophyte Density</title>
<p>Sporophyte density on day 21 was significantly affected by a population &#xd7; temperature interaction for the Quiberon and Spitsbergen population, and the overall sporophyte density in the Spitsbergen population was much lower than for the Quiberon population (<xref ref-type="table" rid="T3">
<bold>Table&#xa0;3</bold>
</xref>; <xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5C</bold>
</xref>). Sporophyte density in the Quiberon population was at its peak at 9&#xb0;C (1094 sporophytes cm<sup>-2</sup>), which was significantly higher than in all other temperature treatments (0&#xb0;C &lt; 15&#xb0;C &lt; [3&#xb0;C =12&#xb0;C] &lt; [6&#xb0;C = 12&#xb0;C] &lt; 9&#xb0;C; Tukey test, <italic>p</italic>&lt;0.05). In the Spitsbergen population, sporophyte density was significantly higher at 9&#xb0;C and 12&#xb0;C (515 and 639 sporophytes cm<sup>-2</sup>) than at the other temperatures ([0&#xb0;C = 3&#xb0;C] &lt; [3&#xb0;C = 6&#xb0;C = 15&#xb0;C] &lt; [9&#xb0;C = 12&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). At 3&#xb0;C, 6&#xb0;C and 9&#xb0;C, sporophyte density was significantly higher in the Quiberon, compared to Spitsbergen population (Tukey test, <italic>p</italic>&lt;0.0001), while there were no significant differences at 0&#xb0;C, 12&#xb0;C and 15&#xb0;C.</p>
</sec>
<sec id="s3_2_4">
<title>3.2.4 Sporophyte Length and Width Growth</title>
<p>Linear GR <sub>length</sub> and GR <sub>width</sub> of sporophytes integrated between day 7 and day 21 revealed a significant population &#xd7; temperature interaction, taking into account the significantly different sporophyte densities in all populations on day 7 (<xref ref-type="table" rid="T4">
<bold>Table&#xa0;4</bold>
</xref>; <xref ref-type="fig" rid="f6">
<bold>Figures&#xa0;6A, B</bold>
</xref>). The overall sporophyte GR <sub>length</sub> (<xref ref-type="fig" rid="f6">
<bold>Figure&#xa0;6A</bold>
</xref>) was generally very low in cold temperatures and increased significantly towards higher temperatures, with the highest GRs <sub>length</sub> between 9&#xb0;C and 15&#xb0;C, irrespective of location (SPT: 0&#xb0;C &lt; 3&#xb0;C &lt; 6&#xb0;C &lt; 9&#xb0;C &lt; [12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05; TRM: 0&#xb0;C &lt; 3&#xb0;C &lt; 6&#xb0;C &lt; [9&#xb0;C =15&#xb0;C] &lt; 12&#xb0;C; Tukey test, <italic>p</italic>&lt;0.01; QUI: 0&#xb0;C &lt; 3&#xb0;C &lt; 6&#xb0;C &lt; [9&#xb0;C = 15&#xb0;C] &lt; [12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.001). However, the GR <sub>length</sub> at 9&#xb0;C, 12&#xb0;C and 15&#xb0;C was significantly higher in sporophytes from Troms&#xf8; (423 to 562 &#xb5;m <sub>length</sub> week<sup>-1</sup>) and Quiberon (328 to 469 &#xb5;m <sub>length</sub> week<sup>-1</sup>) than from Spitsbergen (210 to 317 &#xb5;m <sub>length</sub> week<sup>-1</sup>; Tukey test, <italic>p</italic>&lt;0.01). In cold temperatures, at 0&#xb0;C and 3&#xb0;C, GR <sub>length</sub> did not differ significantly between populations (26 to 52 &#xb5;m <sub>length</sub> week<sup>-1</sup>). At 6&#xb0;C, there was a significantly higher sporophyte GR <sub>length</sub> in the Troms&#xf8; population (174 &#xb5;m <sub>length</sub> week<sup>-1</sup>) than in the Quiberon and Spitsbergen populations (112 and 104 &#xb5;m <sub>length</sub> week<sup>-1</sup>; Tukey test, <italic>p</italic>&lt;0.01).</p>
<table-wrap id="T4" position="float">
<label>Table&#xa0;4</label>
<caption>
<p>Two-way ANCOVA to examine the effects of temperature and population on sporophyte growth parameters of <italic>Laminaria digitata</italic> on day 21 along a lower temperature gradient (0-15&#xb0;C) in experiment 2, with sporophyte density on day 7 as a covariate.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left"/>
<th valign="top" align="center"/>
<th valign="top" align="center"/>
<th valign="top" colspan="2" align="center">GR<sub>length</sub>
</th>
<th valign="top" colspan="2" align="center">GR<sub>width</sub>
</th>
<th valign="top" colspan="2" align="center">L:W ratio</th>
</tr>
<tr>
<th valign="top" align="left">Parameter</th>
<th valign="top" align="center">numDF</th>
<th valign="top" align="center">denDF</th>
<th valign="top" align="center">
<italic>F</italic>-value</th>
<th valign="top" align="center">
<italic>p-</italic>value</th>
<th valign="top" align="center">
<italic>F</italic>-value</th>
<th valign="top" align="center">
<italic>p</italic>-value</th>
<th valign="top" align="center">
<italic>F</italic>-value</th>
<th valign="top" align="center">
<italic>p</italic>-value</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Density</td>
<td valign="top" align="center">1</td>
<td valign="top" align="center">71</td>
<td valign="top" align="center">2332.45</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">1341.64</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">383.18</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Population</td>
<td valign="top" align="center">2</td>
<td valign="top" align="center">71</td>
<td valign="top" align="center">92.98</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">70.03</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">161.95</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="center">5</td>
<td valign="top" align="center">71</td>
<td valign="top" align="center">581.48</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">594.73</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">15.63</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
<tr>
<td valign="top" align="left">Population &#xd7; temperature</td>
<td valign="top" align="center">10</td>
<td valign="top" align="center">71</td>
<td valign="top" align="center">9.6</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">11.88</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
<td valign="top" align="center">16.58</td>
<td valign="top" align="center">
<bold>&lt;0.0001</bold>
</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>Statistically significant values (p &lt; 0.05) are highlighted in bold. numDF, numerator degrees of freedom; denDf, denominator degrees of freedom; GR, growth rate; L:W ratio, length:width ratio.</p>
</fn>
</table-wrap-foot>
</table-wrap>
<fig id="f6" position="float">
<label>Figure&#xa0;6</label>
<caption>
<p>Sporophyte growth parameters of <italic>Laminaria digitata</italic> in three populations (Spitsbergen, SPT; Troms&#xf8;, TRM; Quiberon, QUI) on day 21 between 0&#xb0;C and 15&#xb0;C in experiment 2. <bold>(A)</bold> Linear sporophyte growth rate (GR) in length, <bold>(B)</bold> in width and <bold>(C)</bold> sporophyte length:width (L:W) ratio. Values are expressed as the mean of means &#xb1; SD (n = 5).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-870792-g006.tif"/>
</fig>
<p>A similar pattern was observed in sporophyte GR <sub>width</sub> across all populations (<xref ref-type="fig" rid="f6">
<bold>Figure&#xa0;6B</bold>
</xref>). The GRs <sub>width</sub> were low at low temperatures and increased towards higher temperatures, but with differences between temperatures per population (SPT and TRM: [0&#xb0;C = 3&#xb0;C] &lt; 6&#xb0;C &lt; 9&#xb0;C &lt; [12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05; QUI: 0&#xb0;C &lt; 3&#xb0;C &lt; 6&#xb0;C &lt; 9&#xb0;C &lt; [12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). In the 9&#xb0;C, 12&#xb0;C and 15&#xb0;C treatments, Troms&#xf8; sporophytes showed significantly higher GRs <sub>width</sub> (90 to 127 &#xb5;m <sub>width</sub> week<sup>-1</sup>) than Spitsbergen (54 to 84 &#xb5;m <sub>width</sub> week<sup>-1</sup>) and Quiberon sporophytes (42 to 83 &#xb5;m <sub>width</sub> week<sup>-1</sup>; Tukey test, <italic>p</italic>&lt;0.05). At 0&#xb0;C and 3&#xb0;C however, GRs <sub>width</sub> were very low and were same between populations (8 to 12 &#xb5;m <sub>width</sub> week<sup>-1</sup>). At 6&#xb0;C, there was a significantly higher sporophyte GR <sub>width</sub> in the Troms&#xf8; and Spitsbergen population (29 and 27 &#xb5;m <sub>width</sub> week<sup>-1</sup>) than in the Quiberon population (18 &#xb5;m <sub>width</sub> week<sup>-1</sup>; Tukey test, <italic>p</italic>&lt;0.05).</p>
<p>A significant temperature &#xd7; population interaction also became apparent for the L:W ratio on day 21 (<xref ref-type="fig" rid="f6">
<bold>Figure&#xa0;6C</bold>
</xref>; <xref ref-type="table" rid="T4">
<bold>Table&#xa0;4</bold>
</xref>). Spitsbergen sporophytes showed a relatively constant L:W ratio of 3.0-4.1, but with a significantly lower L:W ratio at 0&#xb0;C compared to the other populations (0&#xb0;C &lt; [3&#xb0;C = 9&#xb0;C = 12&#xb0;C = 15&#xb0;C] &lt; [6&#xb0;C = 9&#xb0;C = 12&#xb0;C = 15&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). In sporophytes from Troms&#xf8;, the L:W ratio spiked at 6&#xb0;C (5.9 &#xb1; 0.7) and was lowest at 0&#xb0;C, 3&#xb0;C and 12&#xb0;C (3.5-4.6; [0&#xb0;C = 3&#xb0;C = 12&#xb0;C] &lt; [3&#xb0;C = 9&#xb0;C = 12&#xb0;C = 15&#xb0;C] &lt; [6&#xb0;C = 9&#xb0;C]; Tukey test, <italic>p</italic>&lt;0.05). Quiberon showed the lowest L:W ratio at 0&#xb0;C (3.3 &#xb1; 0.2) and the highest at 9&#xb0;C (7.6 &#xb1; 0.3; 0&#xb0;C &lt; 3&#xb0;C &lt; [6&#xb0;C = 15&#xb0;C] &lt; 12&#xb0;C &lt; 9&#xb0;C; Tukey test, <italic>p</italic>&lt;0.05).</p>
</sec>
</sec>
</sec>
<sec id="s4">
<title>4 Discussion</title>
<p>This study highlights the importance of holistic approaches for the identification of intraspecific variation and local adaptation. Particularly sessile species with extensive latitudinal ranges may exhibit ecotypic adaptation as a means of survival, and so cannot be assumed to respond uniformly throughout their range and across different fitness-related parameters (<xref ref-type="bibr" rid="B4">Atkins and Travis, 2010</xref>; <xref ref-type="bibr" rid="B57">Mohring et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B29">Filbee-Dexter et&#xa0;al., 2020</xref>). The use of full-factorial, common-garden experiments, along with the usage of gametophyte progeny from several sporophytes, presents a sound method for studying adaptive changes in kelp populations from varying <italic>in situ</italic> environmental conditions, while also ensuring wider genetic diversity of populations, than studies based on single clonal cultures (<xref ref-type="bibr" rid="B40">King et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>). Here, we provide evidence for ecotypic differentiation of microscopic stages of the key habitat-forming kelp <italic>Laminaria digitata</italic> along its NE Atlantic distribution range. By investigating microscopic stages and several associated life cycle processes, we highlight that the response pattern across populations towards (sub)-lethal high and (sub)-optimum low temperatures is partly uniform across populations and partly reflects the long-term local temperature history of the respective population and thus their biogeographic distribution patterns, indicating local adaptation. However, some responses varied in an unpredictable manner, deviating from their local long-term temperature history, which warrants further investigation.</p>
<sec id="s4_1">
<title>4.1 Uniform Upper Survival Temperature of Gametophytes</title>
<p>Gametophytes from the five tested populations (Quiberon in the south, to Troms&#xf8; in the north), spanning a wide distribution range in the NE Atlantic, exhibited a similar response in the upper temperature gradient with a uniform UST of 24&#xb0;C after a two-week exposure, with no short-term recovery and limited long-term recovery. Gametophytes from Spitsbergen have been investigated before and exhibited the same upper lethal temperature limit (<xref ref-type="bibr" rid="B31">Franke et&#xa0;al., 2021</xref>). This is despite local mean summer SSTs differing by ~12-13&#xb0;C between the southern (<xref ref-type="bibr" rid="B65">Oppliger et&#xa0;al., 2014</xref>) and northern distribution margins (<xref ref-type="bibr" rid="B30">Fischer et&#xa0;al., 2019</xref>; <xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>). Although none of the populations are likely to experience such high SSTs over 14 days in their natural environment, it should be noted that our experimental priming temperature of 24&#xb0;C only exceeds the mean summer SST at the southern-most location in Quiberon by ~6&#xb0;C, but by 18-19&#xb0;C at the northern-most limit of the species in Spitsbergen (<xref ref-type="bibr" rid="B65">Oppliger et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B30">Fischer et&#xa0;al., 2019</xref>). Few studies have examined the intra-specific thermal response of microscopic gametophyte and sporophyte stages throughout their distribution gradient (<xref ref-type="bibr" rid="B53">Martinez, 1999</xref>; <xref ref-type="bibr" rid="B64">Oppliger et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B57">Mohring et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B8">Becheler et&#xa0;al., 2022</xref>). However, several previous studies have shown that the upper lethal limit with respect to survival and growth of gametophytes of Atlantic <italic>Laminaria</italic> spp. and <italic>Saccharina</italic> spp. was also similar across sites with different thermal environments (<xref ref-type="bibr" rid="B11">Bolton and L&#xfc;ning, 1982</xref>; <xref ref-type="bibr" rid="B88">tom Dieck (Bartsch), 1992</xref>; <xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>); but these authors only worked with single clonal isolates. With recent insights into the genetic heterogeneity of <italic>L. digitata</italic>, its reduced gene flow in marginal populations (e.g., <xref ref-type="bibr" rid="B9">Billot et&#xa0;al., 2003</xref>; <xref ref-type="bibr" rid="B39">King et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>) and latitudinal adaptation of sporophytes towards heat stress (e.g., <xref ref-type="bibr" rid="B41">King et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>), it became questionable whether this single-clonal approach was sufficient to understand the full tolerance width within a single kelp species. By applying a population approach and assuming that we incorporated several genetic lineages per location, our study now confirms that the upper thermal limit of <italic>L. digitata</italic> gametophytes is conserved along its whole distribution gradient in the NE, irrespective of the local long-term thermal environment. This supports early assumptions of <xref ref-type="bibr" rid="B96">Wiencke et&#xa0;al. (1994)</xref> that the upper survival limit of seaweed species is relatively fixed and illustrates that neutral genetic diversity is not always a good indicator for intra-specific performance plasticity (<xref ref-type="bibr" rid="B39">King et&#xa0;al., 2020</xref>).</p>
<p>Polar and temperate kelp species exhibit a complex alternation of generations between microscopic gametophytes and macroscopic sporophytes, where each life cycle stage exploits different ecological niches according to its physiological needs. This strategy is thought to provide an adaptive advantage, especially in variable environments (<xref ref-type="bibr" rid="B43">Ladah and Zertuche-Gonz&#xe1;lez, 2007</xref>; <xref ref-type="bibr" rid="B5">Barradas et&#xa0;al., 2011</xref>). Microscopic gametophytes of kelps have been shown to be the most heat tolerant stage, regardless of population or species (<xref ref-type="bibr" rid="B89">tom Dieck (Bartsch), 1993</xref>; <xref ref-type="bibr" rid="B43">Ladah and Zertuche-Gonz&#xe1;lez, 2007</xref>), highlighting their widespread ability to persist as hardy, long-lived seed banks, that can exist for up to decades without losing their fertility (<xref ref-type="bibr" rid="B89">tom Dieck (Bartsch), 1993</xref>; <xref ref-type="bibr" rid="B19">Edwards, 2000</xref>; <xref ref-type="bibr" rid="B12">Carney and Edwards, 2006</xref>; <xref ref-type="bibr" rid="B20">Edwards, 2022</xref>; <xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>). The fact that such a high UST has been preserved in <italic>L. digitata</italic> gametophytes underlines the importance of this parameter as a survival mechanism in which persisting gametophytes can replenish sporophyte populations following die-off events (e.g., <xref ref-type="bibr" rid="B7">Bartsch et&#xa0;al., 2013</xref>). This may be especially important for southern populations that have in fact faced large-scale extirpation in the past (<xref ref-type="bibr" rid="B48">Lima et&#xa0;al., 2007</xref>; <xref ref-type="bibr" rid="B26">Fern&#xe1;ndez, 2011</xref>; <xref ref-type="bibr" rid="B59">Moy and Christie, 2012</xref>; <xref ref-type="bibr" rid="B93">Voerman et&#xa0;al., 2013</xref>; <xref ref-type="bibr" rid="B85">Smale et&#xa0;al., 2015</xref>).</p>
<p>After several weeks of post-cultivation at 15&#xb0;C, gametophytes previously exposed to 24&#xb0;C were observed to grow again. These may have arisen from single living cells in damaged multicellular gametophyte filaments or from unaccounted surviving gametophytes that we missed in our monitoring protocol, where we only sampled random areas of the petri dishes. Therefore, we highlight the importance of allowing long-term cultivation under growth-supporting conditions after exposure to environmental stressors, as we might be underestimating the survival potential of microscopic stages of kelps at near lethal conditions.</p>
<p>Interestingly, the few gametophytes that survived the 24&#xb0;C priming treatment were primarily male. These results suggest differential survival capacities between sexes, with female gametophytes being more sensitive to heat than male gametophytes. In several species of the genus <italic>Laminaria</italic>, male gametophytes were reported to survive better in high temperatures than female gametophytes, (<xref ref-type="bibr" rid="B89">tom Dieck (Bartsch), 1993</xref>). Likewise, Arctic isolates of the morphologically similar species <italic>L. digitata</italic> and <italic>Hedophyllum nigripes</italic>, revealed higher heat tolerance in male than female gametophytes (<xref ref-type="bibr" rid="B31">Franke et&#xa0;al., 2021</xref>). <xref ref-type="bibr" rid="B11">Bolton and L&#xfc;ning (1982)</xref> also found a 1&#xb0;C higher UST in male <italic>L. digitata</italic> gametophytes compared to females, but not for the other N-Atlantic kelp species <italic>L. hyperborea</italic>, S<italic>. latissima</italic> and Arctic <italic>Laminaria solidungula</italic>. One explanation for the differential survival capacity of sexes is the ability of male gametophytes to reproduce vegetatively through fragmentation (<xref ref-type="bibr" rid="B18">Destombe and Oppliger, 2011</xref>), giving an illusion of higher survival. This is thought to act as a dispersal mechanism by reducing male to female distances (to &lt;1 mm) to facilitate pheromone signaling and thereby enhancing reproductive success (<xref ref-type="bibr" rid="B71">Reed et&#xa0;al., 1997</xref>; <xref ref-type="bibr" rid="B18">Destombe and Oppliger, 2011</xref>). In the wild, more male survivors may increase the chance of females being fertilized, as an oogonium and antheridium only produce one egg and sperm, respectively (<xref ref-type="bibr" rid="B18">Destombe and Oppliger, 2011</xref>). Why sex-ratio is especially male-skewed at high temperatures (see also <xref ref-type="bibr" rid="B44">Lee and Brinkhuis, 1988</xref>; <xref ref-type="bibr" rid="B36">Izquierdo et&#xa0;al., 2002</xref>), however, is not clear, but may be linked to better stress resistance of males. In fact, gene expression profiles in vegetative <italic>S. latissima</italic> gametophytes have been shown to be different between temperatures and sexes (<xref ref-type="bibr" rid="B58">Monteiro et&#xa0;al., 2019</xref>). Only a small proportion (7-12%) of differentially expressed genes were consistent across temperatures, indicating that temperature strongly influences development. In general, functional categories linked to responses to stress and external and abiotic stimuli were over-represented in females. Females also responded more strongly at higher temperatures than males, suggesting a lower heat tolerance of females (<xref ref-type="bibr" rid="B58">Monteiro et&#xa0;al., 2019</xref>). These hypotheses may explain the significantly slower gametophyte mortality of the Troms&#xf8; population at 24&#xb0;C and 25&#xb0;C within the priming period compared to all other populations, as only this population was male-dominated (1.74 &#xd7; more males than females on day 0 - an artificial effect of inconsistent seeding), which could have provided a survival advantage.</p>
</sec>
<sec id="s4_2">
<title>4.2 Ecotypic Survival of Gametophytes at Low to Optimum Temperatures</title>
<p>In contrast to the uniform lethal limit at high temperatures across populations, we discovered that gametophyte survival from three populations in the lower temperature gradient between 0-15&#xb0;C was clearly reflective of the thermal environment from which they originated. The southern-most population of Quiberon showed a positive relationship of survival with increasing temperature, whereas the northern-most population Spitsbergen showed a negative relationship with increasing temperature. Gametophytes from both populations survived best near their <italic>in situ</italic> annual average SSTs at 15&#xb0;C (Quiberon) and 0-3&#xb0;C (Spitsbergen). Gametophytes from Troms&#xf8;, located in between, where the mean annual SSTs are ~7&#xb0;C (<xref ref-type="bibr" rid="B14">Chepurin and Carton, 2012</xref>; <xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>), revealed rather constant survival over temperatures, with significantly lower survival only at 3&#xb0;C and 12&#xb0;C compared to 15&#xb0;C. This suggests that <italic>L. digitata</italic> populations have adapted in response to local long-term environmental conditions and that selection pressure towards local mean temperatures was higher than for USTs. A study by <xref ref-type="bibr" rid="B57">Mohring et&#xa0;al. (2014)</xref>, that examined the thermal performance of microscopic stages of the warm-temperate kelp <italic>Ecklonia radiata</italic> from three regions across its latitudinal distribution in southern Australia, came to similar conclusions. Gametophyte survival (density) and growth (area of gametophytes) was optimal in conditions reflective of the environment in which they persist. These findings support the hypothesis that variability in the thermal performance of kelps with broad latitudinal distributions is influenced by biogeography and ecotypic adaptation to local temperature regimes, but that this adaptation is only reflected in naturally-occurring temperature ranges, shaping optimal responses towards local conditions rather than altering physiological thresholds.</p>
<p>North Atlantic kelps are generally quite young. The Arctic endemic kelp <italic>L. solidungula</italic> likely originated from the first major migration event of Pacific <italic>Laminaria</italic> through the Bering Strait around 5.3 Mya (<xref ref-type="bibr" rid="B75">Rothman et&#xa0;al., 2017</xref>). The cold-temperate species, such as <italic>L. digitata</italic>, followed later from a second migration event, which also gave rise to the warm-temperate species (<xref ref-type="bibr" rid="B75">Rothman et&#xa0;al., 2017</xref>). So, despite their ancestors crossing the Arctic from the Pacific to the Atlantic, North Atlantic kelps are mostly not Arctic in their temperature profile, except for the more distantly related <italic>L. solidungula</italic> (<xref ref-type="bibr" rid="B88">tom Dieck (Bartsch), 1992</xref>; <xref ref-type="bibr" rid="B89">tom Dieck (Bartsch), 1993</xref>; <xref ref-type="bibr" rid="B74">Roleda, 2016</xref>). The uniform UST of <italic>L. digitata</italic> gametophytes shown here, in combination with the ecotypic adaptation at lower temperatures, indicate that populations of this species are likely in an early stage of adaptation to cold environments, due to their relatively short cold-water history since around 3 My (<italic>sensu</italic> <xref ref-type="bibr" rid="B96">Wiencke et&#xa0;al., 1994</xref>).</p>
<p>Phylogeographic studies of NE Atlantic <italic>L. digitata</italic> have identified genetically distinct northern and southern clusters (<xref ref-type="bibr" rid="B39">King et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>; <xref ref-type="bibr" rid="B62">Neiva et&#xa0;al., 2020</xref>). This genetic structure corresponds to the differentiation of thermal traits in <italic>L. digitata</italic> sporophytes (<xref ref-type="bibr" rid="B41">King et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>) and might also explain the location-specific gametophyte survival at lower temperatures (this study). This divergence can be traced back to different post-glacial redistribution histories after the Last Glacial Maximum (20,000 YBP; <xref ref-type="bibr" rid="B2">Assis et&#xa0;al., 2017a</xref>; <xref ref-type="bibr" rid="B62">Neiva et&#xa0;al., 2020</xref>). Potential glacial refugia have been suggested near the unglaciated coastlines of the Armorican and Celtic Seas (Brittany and SW Britain; <xref ref-type="bibr" rid="B52">Maggs et&#xa0;al., 2008</xref>), and close to Ireland (<xref ref-type="bibr" rid="B62">Neiva et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B80">Schoenrock et&#xa0;al., 2020</xref>), which was at the border of former, heavily glaciated regions. Repeated range contractions into and expansions from these refugia may have maintained unique gene pools and facilitated genetic diversification across glacial cycles (<xref ref-type="bibr" rid="B2">Assis et&#xa0;al., 2017a</xref>; <xref ref-type="bibr" rid="B62">Neiva et&#xa0;al., 2020</xref>).</p>
</sec>
<sec id="s4_3">
<title>4.3 Location-Specific Temperature Effects on Sporophyte Development</title>
<p>Similarly, as for survival at the lower temperature end, gametophytes from Troms&#xf8;, Roscoff and Quiberon showed ecotypic responses in relative microscopic sporophyte formation per female gametophytes at the upper temperature end. This was apparent after thermal priming in high (sub)-lethal temperatures with subsequent transfer to fertility-inducing 15&#xb0;C. While all three populations showed 87% to 99.8% reproductive success at continuous 15&#xb0;C, indicating an optimum response, the limiting priming temperature for reproduction was 23&#xb0;C in all populations. Gametophytes from the southern populations Quiberon and Roscoff exposed to priming temperatures of 20-22&#xb0;C exhibited significantly higher reproductive success during recovery in optimal conditions compared to the northern population of Troms&#xf8;. Furthermore, female gametophytes from the southern-most population Quiberon showed no decline in sporophyte formation in these priming temperatures, whereas Roscoff revealed a clear negative relationship with increasing priming temperature. This variation towards thermal priming at high temperatures points towards thermal adaptation to local conditions. The impact of thermal priming on subsequent trait performance seems to be vital in explaining some of the observed trait plasticity in kelps. Recent discoveries revealed that <italic>L. digitata</italic> gametophytes from the North Sea and the Arctic (same locations as in this study) also behaved differently after recovery from short heatwave priming treatments (20-25&#xb0;C), indicating ecotypic responses (<xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>).</p>
<p>Within the same set of results, we additionally noted that reproductive success in gametophytes exposed to the 21&#xb0;C and 22&#xb0;C priming treatments was significantly different among all three populations in latitudinal sequence. Given the close geographic proximity (~1&#xb0; latitude apart) and similarity in thermal environments (2&#xb0;C difference in maximum monthly mean SSTs) of the two French sites, it is surprising that such a considerable difference was observed between the two. For comparison, Troms&#xf8; is situated roughly 22&#xb0; latitude further north and the local annual average SST is approximately 7-8&#xb0;C lower than in northern France (<xref ref-type="bibr" rid="B14">Chepurin and Carton, 2012</xref>; <xref ref-type="bibr" rid="B65">Oppliger et&#xa0;al., 2014</xref>). Therefore, it is likely that intraspecific variation not only plays a role between populations from the two opposite distribution edges, but also among neighboring populations themselves (<xref ref-type="bibr" rid="B9">Billot et&#xa0;al., 2003</xref>). Gene flow is low among <italic>L. digitata</italic> populations from Roscoff and Quiberon (<xref ref-type="bibr" rid="B9">Billot et&#xa0;al., 2003</xref>; <xref ref-type="bibr" rid="B72">Robuchon et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>), which potentially facilitated differentiation between populations. The southern-most European <italic>L. digitata</italic> population of Quiberon might be under especially high selection pressure.</p>
<p>In the lower temperature gradient, relative sporophyte formation per female gametophyte also varied between populations, but not in a pattern that indicated adaptation to local temperatures. In fact, female gametophytes from the high-latitude population of Spitsbergen had a high relative sporophyte formation between 6-15&#xb0;C, with optima at 9-12&#xb0;C, compared to the low-latitude population of Quiberon which produced most sporophytes between 3-12&#xb0;C, with optima at 6-9&#xb0;C. The fact that reproduction in <italic>L. digitata</italic> gametophytes appears to be adapted to such a wide temperature window (3-15&#xb0;C; <xref ref-type="bibr" rid="B88">tom Dieck (Bartsch), 1992</xref>; <xref ref-type="bibr" rid="B61">M&#xfc;ller et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B55">Martins et&#xa0;al., 2017</xref>), but not to low temperatures of 0&#xb0;C, further supports the idea that the migration of <italic>L. digitata</italic> to the Arctic may have been a rather recent event (<italic>sensu</italic> <xref ref-type="bibr" rid="B96">Wiencke et&#xa0;al., 1994</xref>). On the other hand, absolute sporophyte development showed a different pattern. The Quiberon population produced more sporophytes per area at 3-9&#xb0;C than the Spitsbergen population. This was likely influenced by the initial gametophyte density which was &gt;100 gametophytes cm<sup>-2</sup> higher in the former compared to the latter population (<xref ref-type="supplementary-material" rid="SM1">
<bold>Table S3</bold>
</xref>), providing Quiberon with more female cells that could potentially develop sporophytes. Aside from this difference between the two populations, and contrary to their relative ability to form sporophytes, absolute sporophyte development clearly peaked in a narrow range of intermediate temperatures (Quiberon at 9&#xb0;C and Spitsbergen at 9-12&#xb0;C). A similar mismatch between speed of gametogenesis and recruitment optima has been described before (<xref ref-type="bibr" rid="B55">Martins et&#xa0;al., 2017</xref>), pointing towards differential selection pressure on proximate ontogenetic processes, distinctively controlled by temperature.</p>
</sec>
<sec id="s4_4">
<title>4.4 Microscopic Sporophyte Growth Reveals No Local Adaptation</title>
<p>Linear GR <sub>length</sub> and GR <sub>width</sub> of microscopic sporophytes from different populations of <italic>L. digitata</italic> at 0-15&#xb0;C were not obviously related to the thermal environment in which the populations occur. Although we found differences in GR <sub>length</sub> and GR <sub>width</sub> among populations (Spitsbergen, Troms&#xf8; and Quiberon), the general growth patterns were similar, with &gt;4-fold higher GRs <sub>length</sub> and GRs <sub>width</sub> at 9-15&#xb0;C than at 0-3&#xb0;C. Thus, sporophyte growth at cool conditions is clearly not favored, irrespective of location. The higher GR <sub>length</sub> of the Troms&#xf8; population compared to Spitsbergen and Quiberon was likely attributable to the low reproductive success and consequently low sporophyte density of the Troms&#xf8; population, providing more space and nutrients for growth. Our results are in line with former studies that consistently showed maximum growth of juvenile <italic>L. digitata</italic> sporophytes between 10&#xb0;C and 15&#xb0;C (<xref ref-type="bibr" rid="B11">Bolton and L&#xfc;ning, 1982</xref>; <xref ref-type="bibr" rid="B88">tom Dieck (Bartsch), 1992</xref>) and therefore do not suggest prominent ecotypic responses for this trait. The only other study investigating juvenile kelp sporophyte growth along latitudes in a common-garden approach dealt with <italic>Lessonia nigrescens</italic>. The reported thermal ecotypes in growth of microscopic sporophytes from three Chilean locations spanning 21&#xb0; latitude (<xref ref-type="bibr" rid="B53">Martinez, 1999</xref>), were probably due to the presence of two cryptic species (<xref ref-type="bibr" rid="B64">Oppliger et&#xa0;al., 2012</xref>) and thus also do not suggest intraspecific, ecotypic adaptation of this trait.</p>
<p>Results of our study reveal that low-latitude populations of <italic>L. digitata</italic>, might rely on faster reproduction and sporophyte growth to minimize exposure of gametophytes to unpredictable thermal fluctuations in summer, whereas colder, high-latitude populations, that generally experience more stable thermal conditions, may benefit from delayed maturation and increased vegetative growth of gametophytes, resulting in multicellular gametophytes that can bear more offspring (<xref ref-type="bibr" rid="B18">Destombe and Oppliger, 2011</xref>; <xref ref-type="bibr" rid="B64">Oppliger et&#xa0;al., 2012</xref>). If slow recruitment is better in the cold, and fast recruitment better in warm temperatures, maybe it is this plasticity that is selected for. As temperatures of &gt;9&#xb0;C have not yet been encountered in the Arctic, the high temperature recruitment optimum of the Spitsbergen population may suggest that this trait has not been under selection pressure yet.</p>
</sec>
<sec id="s4_5">
<title>4.5 Sporophyte Morphology May Suggest Local Adaptation</title>
<p>In contrast to GRs, sporophyte morphology, expressed as L:W ratio, might suggest local adaptation. The southern range edge population of Quiberon showed the widest range in L:W ratio, with a maximum at 9&#xb0;C. Sporophytes from Troms&#xf8; were less variable over the thermal treatments but peaked at 6&#xb0;C. Spitsbergen sporophytes on the other hand, displayed a constantly low L:W ratio across all temperatures. Morphologically, this may imply that adult sporophytes from Quiberon generally grow long and thin at intermediate temperatures, whereas sporophytes from Spitsbergen grow wider rather than longer blades. It is, however, unclear whether these differences reflect local adaptation, or why a broad range in sporophyte morphology may be advantageous in warm environments as opposed to consistent morphology in cold environments. Nonetheless, whether this feature is plastic or genetically determined may have significant implications in selecting seedstocks for farming and domestication.</p>
</sec>
<sec id="s4_6">
<title>4.6 Implications of Thermal Responses of Gametophytes for Kelp Ecology</title>
<p>Intraspecific variation in thermal responses is prevalent among widely-distributed kelp species (<xref ref-type="bibr" rid="B57">Mohring et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B76">Saada et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B40">King et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B41">King et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>; <xref ref-type="bibr" rid="B54">Martins et&#xa0;al., 2020</xref>). Yet, the specific mechanisms acting on different life history stages are not well-understood. We have shown that temperature-dependent responses of microscopic stages of <italic>L. digitata</italic> vary among life history stages and populations. The clear pattern of local adaptation we have identified in some traits, but not in others, may shed light on the crucial developmental processes under selection pressure and the fundamental niche of the species.</p>
<p>Gametophyte survival in lower (sub-) optimal temperatures and sporophyte formation after thermal priming at upper temperatures between 15&#xb0;C and 23&#xb0;C showed ecotypic responses across populations (<xref ref-type="table" rid="T5">
<bold>Table&#xa0;5</bold>
</xref>). Phenotypic divergence in these traits may highlight their importance for survival in the natural environment. On the other hand, the upper survival limit of gametophytes was uniform across populations. Adapting the UST does not seem to have been under selection pressure in the past, and current evidence suggests that ocean warming is outpacing the adaptive capacity of kelp forests (<xref ref-type="bibr" rid="B94">Vranken et&#xa0;al., 2021</xref>). Sporophyte formation and growth at low temperatures showed a random response, potentially concurring with the overall low levels of local adaptation found in adult sporophytes (<xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>). Consequently, variation manifests itself in different traits both in haploid and diploid stages. Examining only single parameters or life cycle stages might therefore lead to incomplete or even false interpretations, and so whole-life-cycle approaches, using a range of different fitness-related traits, are vital to reveal the complex survival strategies of kelps.</p>
<table-wrap id="T5" position="float">
<label>Table&#xa0;5</label>
<caption>
<p>Indication of local adaptation in <italic>Laminaria digitata</italic> gametophyte populations from across the species entire NE Atlantic distribution range with respect to different experimental temperatures and life history stages.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left">Response variable</th>
<th valign="top" align="center">Upper (sub-) lethal temperatures (20-25&#xb0;C - Exp. 1)</th>
<th valign="top" align="center">Lower temperatures (0-15&#xb0;C - Exp. 2)</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Survival</td>
<td valign="top" align="center">O</td>
<td valign="top" align="center">&#x221a;</td>
</tr>
<tr>
<td valign="top" align="left">Sporophyte formation</td>
<td valign="top" align="center">&#x221a;</td>
<td valign="top" align="center">X</td>
</tr>
<tr>
<td valign="top" align="left">Growth and morphology</td>
<td valign="top" align="center">nd</td>
<td valign="top" align="center">X</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>Exp., Experiment; O, uniform response, probably not under selection; &#x221a;, intuitive pattern, may represent local adaptation according to our hypotheses; X, counterintuitive pattern, no hypothesis for selective forces behind these patterns; nd, no data.</p>
</fn>
</table-wrap-foot>
</table-wrap>
<p>In conclusion, our study demonstrates trait-dependent ecotypic adaptation in the thermal performance of different microscopic life history stages of <italic>L. digitata</italic> across its entire NE Atlantic distribution. In the future, kelp forests will struggle to thermally acclimate, adapt, or shift their distribution ranges fast enough to keep up with the rising temperatures and marine heatwaves (<xref ref-type="bibr" rid="B56">Merzouk and Johnson, 2011</xref>). While local adaptation may delay the regional contractions of marginal populations, it is unlikely that they will cope with global warming in the long term (<xref ref-type="bibr" rid="B46">Liesner et&#xa0;al., 2020a</xref>; <xref ref-type="bibr" rid="B62">Neiva et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B94">Vranken et&#xa0;al., 2021</xref>). The potential for fast adaptation of kelps <italic>via</italic> thermal priming or trans-generational and epigenetic inheritance, is only starting to be understood (<xref ref-type="bibr" rid="B47">Liesner et&#xa0;al., 2020b</xref>; <xref ref-type="bibr" rid="B32">Gauci et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B78">Scheschonk et&#xa0;al., 2022</xref>). Therefore, the development of strategies to future-proof and restore kelp forests is of utmost importance (<xref ref-type="bibr" rid="B97">Wood et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B15">Coleman et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B22">Eger et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B37">Jueterbock et&#xa0;al., 2021</xref>).</p>
</sec>
</sec>
<sec id="s5" sec-type="data-availability">
<title>Data Availability Statement</title>
<p>Data for this study were published open access (<xref ref-type="bibr" rid="B79">Schimpf et al., 2022</xref>) and can be found in the PANGAEA database: <uri xlink:href="https://doi.org/10.1594/PANGAEA.943526">https://doi.org/10.1594/PANGAEA.943526</uri>.</p>
</sec>
<sec id="s6" sec-type="ethics-statement">
<title>Ethics Statement</title>
<p>
<bold>Nagoya Protocol statement:</bold> Sampling in France and handling of data was conducted in accordance with the French legislation on Access and Benefit-Sharing of genetic resources (ABSCH-IRCC-FR-252418-1). With respect to Norway, we complied with our due diligence by sending an inquiry to the national authorities. In 2020, they replied that no permits were required and in late 2021 this statement was officially confirmed to the Alfred Wegener Institute by the Norwegian National Focal Point. The Norwegian regulation on the Nagoya Protocol has not yet entered into force.</p>
</sec>
<sec id="s7" sec-type="author-contributions">
<title>Author Contributions</title>
<p>NS and IB designed the study, with contributions from DL and KF. DL, IB, and MR carried out field sampling. NS, KF, and DL conducted the experiments. NS analyzed the data. NS, IB, DL, KF, and MR contributed to the data interpretation and discussion. NS wrote the first draft of the manuscript. All authors contributed to manuscript revision and read and approved the submitted version.</p>
</sec>
<sec id="s8" sec-type="funding-information">
<title>Funding</title>
<p>This work was supported by the 2015-2016 BiodivERsA COFUND call for research proposals (program MARFOR), with the national funder German Research Foundation (DFG; grant no. VA 105/25-1). We acknowledge support by the Open Access Publication Funds of the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research.</p>
</sec>
<sec id="s9" sec-type="COI-statement">
<title>Conflict of Interest</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.</p>
</sec>
<sec id="s10" sec-type="disclaimer">
<title>Publisher&#x2019;s Note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
</body>
<back>
<ack>
<title>Acknowledgments</title>
<p>We would like to thank A. Wagner for the sampling and clonal isolation of kelp material and technical assistance in the laboratory, C. Daniel for support with the image analysis, L. Foqueau for the SST data, C. Gauci for statistical advice and S. DeAmicis for supervision in this BSc Thesis.</p>
</ack>
<sec id="s11" sec-type="supplementary-material">
<title>Supplementary Material</title>
<p>The Supplementary Material for this article can be found online at: <ext-link ext-link-type="uri" xlink:href="https://www.frontiersin.org/articles/10.3389/fmars.2022.870792/full#supplementary-material">https://www.frontiersin.org/articles/10.3389/fmars.2022.870792/full#supplementary-material</ext-link>
</p>
<supplementary-material xlink:href="DataSheet_1.docx" id="SM1" mimetype="application/vnd.openxmlformats-officedocument.wordprocessingml.document"/>
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