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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.2022.984569</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>Inter-individual variability of early life stages of a model marine invertebrate with a bi-phasic life cycle is shaped by contrasting oceanographic conditions</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Leal</surname>
<given-names>Miguel Costa</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/949295"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Rey</surname>
<given-names>Felisa</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/275066"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Ferreira</surname>
<given-names>Guilherme Duarte</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/342877"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Domingues</surname>
<given-names>M. Ros&#xe1;rio</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1083383"/>
</contrib>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Calado</surname>
<given-names>Ricardo</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="author-notes" rid="fn001">
<sup>*</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/654278"/>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>Laborat&#xf3;rio para a Inova&#xe7;&#xe3;o e Sustentabilidade dos Recursos Biol&#xf3;gicos Marinhos e da Universidade de Aveiro (ECOMARE) &amp; Centro de Estudos do Ambiente e do Mar (CESAM) Centre for Environmental and Marine Studies, Department of Biology, University of Aveiro, Campus Universit&#xe1;rio de Santiago</institution>, <addr-line>Aveiro</addr-line>, <country>Portugal</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>Department of Fish Ecology and Evolution, Swiss Federal Institute of Aquatic Science and Technology (Eawag), Center for Ecology, Evolution, and Biogeochemistry</institution>, <addr-line>Kastanienbaum</addr-line>, <country>Switzerland</country>
</aff>
<aff id="aff3">
<sup>3</sup>
<institution>Mass Spectrometry Centre &amp; Laborat&#xf3;rio Associado para a Qu&#xed;mica Verde (LAQV-REQUIMTE), Department of Chemistry, University of Aveiro, Campus Universit&#xe1;rio de Santiago</institution>, <addr-line>Aveiro</addr-line>, <country>Portugal</country>
</aff>
<aff id="aff4">
<sup>4</sup>
<institution>MARE - Marine and Environmental Science Centre, Escola Superior de Turismo e Tecnologia do Mar (ESTM), Polytechnic of Leiria</institution>, <addr-line>Peniche</addr-line>, <country>Portugal</country>
</aff>
<aff id="aff5">
<sup>5</sup>
<institution>Centre for Environmental and Marine Studies (CESAM), Department of Chemistry, University of Aveiro, Santiago University Campus</institution>, <addr-line>Aveiro</addr-line>, <country>Portugal</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>Edited by: Francesca Porri, South African Institute for Aquatic Biodiversity, South Africa</p>
</fn>
<fn fn-type="edited-by">
<p>Reviewed by: Nancy O&#x0027;Connor, University of Massachusetts Dartmouth, United States; Simone Baldanzi, Universidad de Valparaiso, Chile</p>
</fn>
<fn fn-type="corresp" id="fn001">
<p>*Correspondence: Miguel Costa Leal, <email xlink:href="mailto:miguelcleal@gmail.com">miguelcleal@gmail.com</email>; Ricardo Calado, <email xlink:href="mailto:rjcalado@ua.pt">rjcalado@ua.pt</email>
</p>
</fn>
<fn fn-type="other" id="fn002">
<p>This article was submitted to Marine Biology, a section of the journal Frontiers in Marine Science</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>12</day>
<month>09</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="collection">
<year>2022</year>
</pub-date>
<volume>9</volume>
<elocation-id>984569</elocation-id>
<history>
<date date-type="received">
<day>02</day>
<month>07</month>
<year>2022</year>
</date>
<date date-type="accepted">
<day>22</day>
<month>08</month>
<year>2022</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2022 Leal, Rey, Ferreira, Domingues and Calado</copyright-statement>
<copyright-year>2022</copyright-year>
<copyright-holder>Leal, Rey, Ferreira, Domingues and Calado</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>Inter-individual variability plays a key role in species resilience. This, however, is difficult to assess in marine invertebrates with complex life cycles due to the inherent difficulty of sampling individuals in oceanic environments throughout their ontogeny. This study monitored the effect of contrasting oceanographic conditions, namely downwelling and upwelling, on the inter-variability of embryos and megalopae (the final larval stage) of the model brachyuran crab <italic>Carcinus maenas</italic>. We assessed i) the heterogeneity of energetic reserves, biomass, elemental composition, and isotopic niche in these early life stages, and ii) the effect of oceanographic conditions (up- and downwelling) on inter-individual variability. Indeed, organisms developing during downwelling consistently exhibited a higher heterogeneity than those developing during upwelling. While this finding suggests a higher resilience during downwelling, the overall condition of individuals was better during upwelling (i.e., higher C:N), irrespective of the developmental stage. Altogether, our data suggests that trophic history experienced under contrasting oceanographic conditions shape the plasticity of <italic>C. maenas</italic> populations and cascades over different life stages.</p>
</abstract>
<kwd-group>
<kwd>downwelling</kwd>
<kwd>upwelling</kwd>
<kwd>
<italic>carcinus maenas</italic>
</kwd>
<kwd>inter-individual variability</kwd>
<kwd>maternal effects</kwd>
<kwd>isotopic niche</kwd>
<kwd>developmental stages</kwd>
</kwd-group>
<contract-sponsor id="cn001">Funda&#xe7;&#xe3;o para a Ci&#xea;ncia e a Tecnologia<named-content content-type="fundref-id">10.13039/501100001871</named-content>
</contract-sponsor>
<contract-sponsor id="cn002">Funda&#xe7;&#xe3;o para a Ci&#xea;ncia e a Tecnologia<named-content content-type="fundref-id">10.13039/501100001871</named-content>
</contract-sponsor>
<contract-sponsor id="cn003">Funda&#xe7;&#xe3;o para a Ci&#xea;ncia e a Tecnologia<named-content content-type="fundref-id">10.13039/501100001871</named-content>
</contract-sponsor>
<contract-sponsor id="cn004">Funda&#xe7;&#xe3;o para a Ci&#xea;ncia e a Tecnologia<named-content content-type="fundref-id">10.13039/501100001871</named-content>
</contract-sponsor>
<counts>
<fig-count count="5"/>
<table-count count="2"/>
<equation-count count="1"/>
<ref-count count="84"/>
<page-count count="12"/>
<word-count count="6353"/>
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</article-meta>
</front>
<body>
<sec id="s1" sec-type="intro">
<title>Introduction</title>
<p>A &#x201c;deep trench of knowledge&#x201d; separates developmental and ecological biologists focusing on marine crustaceans (<xref ref-type="bibr" rid="B75">Torres et&#xa0;al., 2019</xref>). The former mostly focus on specific processes that occur within a given developmental stage (e.g., neurogenesis) under optimal conditions. In contrast, ecological biologists usually attempt to link plastic responses (e.g., growth rates or trophic ecology consequences) to some key (yet specific) factors. Nevertheless, these two research lines share the need for information on real-world environmental contexts. Such information is key to address questions that link environmental conditions to inter-individual variability and its fitness consequences (<xref ref-type="bibr" rid="B7">Bosch et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B26">Gilbert, 2017</xref>; <xref ref-type="bibr" rid="B68">Sultan, 2017</xref>). In particular, inter-individual variability is typically associated with the levels of adaptability and resilience for a given species (<xref ref-type="bibr" rid="B69">Sunday et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B22">Foo et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B66">Schlegel et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B23">Forsman and Wennersten, 2016</xref>), which highlights the importance of understanding the key drivers of variability for both developmental and ecological disciplines.</p>
<p>Studying inter-individual variability in marine invertebrates with complex life cycles (i.e., those who experience metamorphosis from pelagic larvae to benthonic juveniles) is, however, beset by <italic>in situ</italic> logistic limitations to secure the monitoring of complete larval periods, and by the inherent difficulty of sampling in oceanic environments (<xref ref-type="bibr" rid="B60">Rey et&#xa0;al., 2019</xref>). As such, the extent of inter-individual variability in this type of organisms and the possible effects of varying environmental conditions on this trait have been largely overlooked (<xref ref-type="bibr" rid="B9">Calado and Leal, 2015</xref>). Indeed, marine invertebrates with complex life cycles often inhabit contrasting environments in their larval and adult forms, and shift dramatically from a pelagic to a benthic environment (e.g., <xref ref-type="bibr" rid="B74">Torres et&#xa0;al., 2021</xref> and references therein). This change results in multiple potential drivers of inter-individual variability throughout their life cycle, thus highlighting the role of marine invertebrates with this type of development as model species to assess phenotypic variability throughout ontogeny (<xref ref-type="bibr" rid="B17">Duarte et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B75">Torres et&#xa0;al., 2019</xref>).</p>
<p>Aside from environmental drivers, inter-individual variability can also be affected by developmental processes. When considering embryogenesis, for example, it is important to know if the natural variability present in newly extruded embryos is propagated to later embryonic stages (<xref ref-type="bibr" rid="B20">Fern&#xe1;ndez et&#xa0;al., 2000</xref>; <xref ref-type="bibr" rid="B33">Leal et&#xa0;al., 2013</xref>) or if, on the other hand, initial embryonic inter-individual variability decreases over embryogenesis (<xref ref-type="bibr" rid="B65">Rosa et&#xa0;al., 2003</xref>; <xref ref-type="bibr" rid="B58">Rey et&#xa0;al., 2016a</xref>). Embryogenesis in marine invertebrates with complex life cycles, such as decapod crustaceans, is heavily dependent on lipidic reserves (<xref ref-type="bibr" rid="B49">Petersen and Anger, 1997</xref> and references therein), which are known to vary throughout embryogenesis (<xref ref-type="bibr" rid="B55">Rey et&#xa0;al., 2015a</xref>) and with environmental conditions (e.g., <xref ref-type="bibr" rid="B8">Brillon et&#xa0;al., 2005</xref>) and/or with the nutritional status of females (e.g., <xref ref-type="bibr" rid="B76">Tuck et&#xa0;al., 1997</xref>; <xref ref-type="bibr" rid="B53">Racotta et&#xa0;al., 2003</xref>; <xref ref-type="bibr" rid="B10">Calado et&#xa0;al., 2010</xref>). A contrasting allocation of lipids from females to their embryos due to environmental or dietary drivers can determine the level of initial lipidic reserves available to fuel embryogenesis. Thence, the fitness of subsequent life stages can either be compromised or enhanced, and this effect likely repercusses on inter-individual variability throughout embryonic development (e.g., <xref ref-type="bibr" rid="B64">Rosa et&#xa0;al., 2007</xref>; <xref ref-type="bibr" rid="B58">Rey et&#xa0;al., 2016a</xref>). Ultimately, the performance and survival of decapod crustaceans with complex life cycles can be already compromised at hatching (e.g., <xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B61">Rey et&#xa0;al., 2015b</xref>; <xref ref-type="bibr" rid="B59">Rey et&#xa0;al., 2016b</xref>) or even at oviposition if maternal effects are taken into consideration (see review by <xref ref-type="bibr" rid="B9">Calado and Leal, 2015</xref>). Indeed, early life stages can provide key information on how contrasting environmental conditions affect inter-individual variability (and performance) of these invertebrates with bi-phasic life cycles (<xref ref-type="bibr" rid="B48">Pechenik, 2006</xref>; <xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B60">Rey et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B57">Rey et&#xa0;al., 2022</xref>).</p>
<p>The green crab <italic>Carcinus maenas</italic> develops through four planktonic zoeal stages, a single megalopae stage (semi-benthonic), and then undergoes metamorphosis to settle as a benthic juvenile that grows onto adulthood (<xref ref-type="bibr" rid="B62">Rice and Ingle, 1975</xref>). This species is a highly successful global invader (<xref ref-type="bibr" rid="B12">Carlton and Cohen, 2003</xref>; <xref ref-type="bibr" rid="B84">Young and Elliott, 2019</xref>), which makes it an optimal candidate to study the influence of environmental parameters (such as contrasting oceanographic conditions, namely downwelling and upwelling) as drivers of inter-individual variability. For instance, downwelling and upwelling repercuss on planktonic community composition and abundance (e.g., <xref ref-type="bibr" rid="B43">Ospina-Alvarez et&#xa0;al., 2010</xref>; <xref ref-type="bibr" rid="B82">Wilson et&#xa0;al., 2021</xref>). In turn, this affects <italic>C. maenas</italic> throughout its different life stages, as they ingest plankton during larval life (<xref ref-type="bibr" rid="B50">Pihl, 1985</xref>) and predate on important planktotrophs as adults (<xref ref-type="bibr" rid="B44">Palacios and Ferraro, 2003</xref>). Consequently, the variability experienced by <italic>C. maenas</italic> in such natural settings provides an excellent opportunity to investigate how these oceanographic events shape the inter-individual variability of this model species (<xref ref-type="bibr" rid="B15">Domingues et&#xa0;al., 2011</xref>).</p>
<p>The present study determined the effects of different developmental and environmental factors on inter-individual variability throughout the early life stages of the model species <italic>C</italic>. <italic>maenas</italic>. The following hypotheses were tested: i) the dominant oceanographic condition (up- or downwelling) is an important determinant of heterogeneity among embryos, and ii) variability at hatching (irrespective of the source) affects the degree of inter-individual variability of later developmental stages. The hypotheses were addressed by assessing the stable isotopic niche variability of both individual embryos and megalopae, and the elemental composition of the latter, sampled during contrasting oceanographic events (downwelling and upwelling). We also determined the biochemical profile (phospholipid, elemental composition and isotopic signature) of newly extruded and late-stage embryos to assess maternal effects and embryogenesis as potential sources of inter-individual variability. Altogether, the collected data provide an overview of different sources of inter-individual variability and their potential fitness consequences (e.g., <xref ref-type="bibr" rid="B72">Tang and Dam, 1999</xref>).</p>
</sec>
<sec id="s2" sec-type="materials|methods">
<title>Materials and methods</title>
<sec id="s2_1">
<title>Sampling procedure and location</title>
<p>Ovigerous <italic>C. maenas</italic> females and megalopae were collected at Ria de Aveiro, a shallow coastal lagoon on the north-western Portuguese coast (40&#xb0;37&#x2019;17&#x2019;&#x2019; N, 8&#xb0;44&#x2019;56&#x2019;&#x2019; W) influenced by downwelling and upwelling conditions (<xref ref-type="bibr" rid="B21">Fi&#xfa;za et&#xa0;al., 1998</xref>). The ovigerous females were sampled in periods of downwelling (28<sup>th</sup> of March to 17<sup>th</sup> of April 2013) and upwelling (3<sup>rd</sup> and 4<sup>th</sup> of July 2013) events (see <xref ref-type="bibr" rid="B59">Rey et&#xa0;al., 2016b</xref> for a detailed analysis of the upwelling index during this period).</p>
<p>Ovigerous females were collected by trawling at low tide at ca. 2 m depth and pools of embryos were obtained by carefully removing them from their brooding chambers using forceps. Embryos were subsequently identified either as stage 1 (newly extruded embryos &#x2013; characterised by uniform yolk and no embryonic structures visible, <italic>n</italic> = 10 females per oceanographic event) or stage 3 (embryos ready to hatch in less than 48 h &#x2013; characterised by nearly no yolk and a fully developed embryo, <italic>n</italic> = 10 females per oceanographic event) according to <xref ref-type="bibr" rid="B64">Rosa et&#xa0;al. (2007)</xref>. Accordingly, a total of 40 ovigerous females were sampled for this study, and individual carapace widths (CW, mm &#x2013; measured between the first pair of lateral spines of the carapace) were recorded, ranging between 26.55 and 49.79 mm. These measurements were then converted to wet weight (WW, g) to minimize the effects of allometric growth following Equation 1 (<xref ref-type="bibr" rid="B29">Jungblut et&#xa0;al., 2017</xref>):</p>
<disp-formula>
<label>(1)</label>
<mml:math display="block" id="M1">
<mml:mrow>
<mml:mtext>WW</mml:mtext>
<mml:mo>=</mml:mo>
<mml:mo>&#xa0;</mml:mo>
<mml:mo>&#x2212;</mml:mo>
<mml:mn>0.01172</mml:mn>
<mml:mtext>CW</mml:mtext>
<mml:mo>+</mml:mo>
<mml:mn>0.002300</mml:mn>
<mml:msup>
<mml:mrow>
<mml:mtext>CW</mml:mtext>
</mml:mrow>
<mml:mn>2</mml:mn>
</mml:msup>
<mml:mo>+</mml:mo>
<mml:mn>0.0001759</mml:mn>
<mml:msup>
<mml:mrow>
<mml:mtext>CW</mml:mtext>
</mml:mrow>
<mml:mn>3</mml:mn>
</mml:msup>
</mml:mrow>
</mml:math>
</disp-formula>
<p>Immediately after collection, 30 embryos were randomly selected from the pool of embryos sampled from each female and measured using a calibrated micrometer eyepiece mounted on a stereomicroscope. Embryos were assumed to be approximately spheric (Rosa et&#xa0;al., 2007;Rey et&#xa0;al., 2016a). The remaining embryos pooled from each female were freeze-dried and stored at -32&#xb0;C until biochemical analysis.</p>
<p>Megalopae were sampled by deploying two plankton nets with their entrance facing the inlet of the lagoon (constant depth of 0.1 m, as described by <xref ref-type="bibr" rid="B52">Queiroga et&#xa0;al. (2006)</xref>) for 24 h over several consecutive days within a period of downwelling (24<sup>th</sup> of March to 14<sup>th</sup> of April) and a period of upwelling (7<sup>th</sup> of May to 21<sup>st</sup> of May). The nets were allowed to passively collect plankton onto a collector cup, with specimens being gently transferred to a bucket with seawater and transported to the laboratory. Upon arrival, <italic>C. maenas</italic> megalopae were sorted live from the mixed plankton assemblage using a plastic pipette, rinsed with freshwater to remove salt, flash-frozen and freeze-dried. A total of 226 megalopae were collected during downwelling and 307 during upwelling conditions.</p>
</sec>
<sec id="s2_2">
<title>Isotopic signatures and elemental composition</title>
<p>Currently, one of the best methods for the characterisation of a species&#x2019; trophic niche is the determination of its isotopic niche, as the two are tightly correlated (<xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>). The isotopic niche is typically inferred from a bi-plot that represents stable isotopic signatures (the variation in heavy to light ratios &#x2013; <sup>13</sup>C/<sup>12</sup>C and <sup>15</sup>N/<sup>14</sup>N &#x2013; i.e., &#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N values) in a &#x3b4;-space (<xref ref-type="bibr" rid="B42">Newsome et&#xa0;al., 2007</xref>). The stable isotopic signatures of <italic>C. maenas</italic> embryos and megalopae were thus determined. The information from embryos was used as a proxy to infer the isotopic niche of ovigerous females following previous studies (e.g., <xref ref-type="bibr" rid="B30">Kaufman et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B14">Dimitrijevi&#x107; et&#xa0;al., 2018</xref>).</p>
<p>Stable isotopic signatures were measured using a Thermo Fisher Delta V Advantage Isotope Ratio mass spectrometer coupled to a Thermo Flash 2000 Organic elemental analyser. The isotopic reference materials (acetanilide; Stable Isotope Research Facility, Indiana University, USA) were assessed at the beginning of each run and after every 10 samples. The average precision standards for &#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N were 0.05 and 0.14&#x2030;, respectively. Carbon and nitrogen contents were also determined using this equipment. Before being processed (for isotopic and elemental analysis), a sub-sample of the pool of embryos sampled from each female (<italic>n</italic> = 40) were ground into a fine powder using a tissue lyser paired with tungsten beads (TissueLyser II, Qiagen, Hombrechtikon, Switzerland). Megalopas were individually placed and weighed in the tin cups before analysis in the mass spectrometer.</p>
<p>Decapod crustaceans possess a chitin-calcite exoskeleton and, therefore, their isotopic signature can be affected by the presence of inorganic C (<xref ref-type="bibr" rid="B18">Fantle et&#xa0;al., 1999</xref>; <xref ref-type="bibr" rid="B31">Kolasinski et&#xa0;al., 2008</xref>). We conducted a preliminary analysis to assess the effect of acidification (HCl) on megalopae &#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N (<xref ref-type="bibr" rid="B11">Carabel et&#xa0;al., 2006</xref>). Although the &#x3b4;<sup>15</sup>N remained unaltered (<italic>t</italic> = 1.42, df = 11.58. <italic>p</italic> = 0.2), &#x3b4;<sup>13</sup>C changed, as expected, with acidification (<italic>t</italic> = 5.05, df = 11.53, <italic>p</italic>&lt; 0.01). However, we decided not to acidify megalopa samples because i) the changes in &#x3b4;<sup>13</sup>C with acidification were lower than the range of an average trophic level (ca. 0.39&#x2030;, whereas the average trophic level shift is 0.5 to 1&#x2030; &#x2013; see for instance <xref ref-type="bibr" rid="B14">Dimitrijevi&#x107; et&#xa0;al. (2018)</xref>; ii) acidifying samples significantly (<italic>p&lt;</italic> 0.05) affected the C and N content (C = 28.62% &#xb1; 6.62, N = 6.23% &#xb1; 0.91 in acidified samples versus C = 35.50% &#xb1; 0.49, N = 7.60% &#xb1; 0.16 in non-acidified samples) but not the C:N ratio (<italic>t</italic> = -1.72, df = 7.8113, <italic>p</italic> = 0.12); and iii) acidification decreased the dry weight of individual megalopae by ca. 18% (from 0.260 &#xb1; 0.039 to 0.213 &#xb1; 0.012) and, as a consequence, the accuracy of the &#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N isotopic signatures were affected by the decrease in dry weight to values close to the detection limit of the mass spectrometer and elemental analyser, which in turn artificially increased the variability of results. Given that the main goal of this study was to assess sources of inter-individual variability, we have decided to mitigate any additional variability driven by technical artefacts, i.e., the detection limit of the equipment.</p>
<p>Phosphorus (P) content was only determined in embryos because megalopae could not be divided for different analyses. A sub-sample of ground embryonic tissue was diluted in potassium peroxydisulfate (10 g K<sub>2</sub>O<sub>8</sub>S<sub>2</sub>, 1.5 g NaOH, 1 L Milli-Q water) and autoclaved for 2 h at 121&#xb0;C for P digestion prior to quantification. The concentration of P was determined colourimetrically using a continuous flow analyser (Skalar Analytical B.V., Breda, The Netherlands) following the ammonium molybdate method (<xref ref-type="bibr" rid="B41">Murphy and Riley, 1962</xref>; <xref ref-type="bibr" rid="B47">Parsons et&#xa0;al., 1984</xref>) and standard procedure ISO 13395:1996. Drift and baseline corrections were programmed every 18 samples.</p>
</sec>
<sec id="s2_3">
<title>Lipid analysis</title>
<p>Total lipids were extracted and quantified for the embryo samples, following the method by <xref ref-type="bibr" rid="B6">Bligh and Dyer (1959)</xref> as described by <xref ref-type="bibr" rid="B58">Rey et&#xa0;al. (2016a)</xref>. For the quantification of total phospholipid (PL) content in the embryos, a phosphorus assay was conducted according to <xref ref-type="bibr" rid="B4">Bartlett and Lewis (1970)</xref>. Briefly, we incubated 5% of the total lipid volume (previously dried under a nitrogen flow) with perchloric acid (70% V/V) for 1 h at 180&#xb0;C. After this period, we added 3.3 mL of water, 0.5 mL of ammonium molybdate (2.5% w/V), and 0.5 mL of ascorbic acid (10% w/V) to each sample and incubated them for another 10 min at 100&#xb0;C. Aside from the samples of <italic>C. maenas</italic> embryos, we also prepared standard solutions from 0.1 to 3.0 &#xb5;g of phosphate (control samples) and applied the same protocol described above to them. The absorbance of both control and experimental samples was measured at room temperature (800 nm) in a microplate spectrophotometer (ultraviolet-visible).</p>
</sec>
<sec id="s2_4">
<title>Statistical analysis</title>
<p>Statistical analyses were conducted in R v 4.1.3 (<xref ref-type="bibr" rid="B54">R Development Core Team, 2021</xref>). The different physiological and biochemical parameters recorded for embryos and megalopae were compared between supply events (downwelling and upwelling) using Students&#x2019; t-test after checking for normality and homogeneity of variance. The isotopic profile (&#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N) of embryos and megalopae were compared between supply events using a two-way MANOVA with embryo stage and supply events as categorical variables. The relationship between female biomass and embryo volume was tested with a general linear model, whereas the relationship between female biomass and embryo C:N content was tested with a logistic regression (higher power than transforming proportional data to use in linear models &#x2013; <xref ref-type="bibr" rid="B80">Warton and Hui, 2011</xref>). A general linear model was used to assess how the relationship between % C and % N of megalopae interacted with supply event. Residuals for all models were tested for normality and heterogeneity of variance.</p>
<p>To infer the isotopic niche of females (using data from their embryos) and determine the isotopic niche of megalopae for each supply event, biplot ellipses were used to delineate the isotopic niche space (<xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B16">Duarte et&#xa0;al., 2017</xref>). To test whether niche space differed between supply events, we used a Bayesian estimate of the standard ellipse and its area (&#x2030;<sup>2</sup>) using the package SIAR (<xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>).</p>
</sec>
</sec>
<sec id="s3" sec-type="results">
<title>Results</title>
<sec id="s3_1">
<title>Embryos</title>
<p>Average embryonic volume and C:N content were similar across females, irrespective of their weight and sampling event (during downwelling or upwelling; <xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>). The slope of the linear or logistic regressions was not significant (<italic>p</italic> &gt; 0.05 in both cases). Irrespective of embryonic development stage and female biomass, embryonic volume did not differ significantly under downwelling or upwelling conditions (two-tailed Student&#x2019;s t-test, stage 1: <italic>t</italic>(18) = -1.43; <italic>p</italic> = 0.171; stage 3: <italic>t</italic>(18) = -1.10; <italic>p</italic> = 0.302). Nevertheless, stage 3 eggs were significantly larger than stage 1 eggs (one-tailed Student&#x2019;s t-test, <italic>t</italic>(38) = 21.63; <italic>p</italic> = 0.00).</p>
<fig id="f1" position="float">
<label>Figure&#xa0;1</label>
<caption>
<p>Relationship between female <italic>Carcinus maenas</italic> wet weight (g) and <bold>(A)</bold> average embryo volume (mm<sup>3</sup>, <italic>n</italic> = 40 females) or <bold>(B)</bold> average embryo C:N content (<italic>n</italic> = 40 females). Females collected during downwelling are depicted with white symbols, whereas upwelling ones are shown in black symbols. Squares and triangles are used to distinguish between stage 1 and stage 3 embryos, respectively.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-984569-g001.tif"/>
</fig>
<p>The PL pool of embryos differed between the two oceanographic events (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). Total PL of stage 1 and stage 3 embryos was significantly lower in females collected during downwelling, as compared to those sampled during the upwelling event (two-tailed Student&#x2019;s t-test, <italic>p</italic>&lt; 0.05 for all comparisons). In contrast, the elemental content of embryos (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>) was typically not statistically different (<italic>p</italic> &gt; 0.05) between supply events, apart from N content in stage 1 embryos, which was slightly higher during downwelling (two-tailed Student&#x2019;s t-test, <italic>t</italic>(18) = 2.18; <italic>p</italic> = 0.04).</p>
<table-wrap id="T1" position="float">
<label>Table&#xa0;1</label>
<caption>
<p>Phospholipid, elemental and isotopic content (mean &#xb1; SD) of embryos collected from wild <italic>Carcinus maenas</italic> females during downwelling (<italic>n</italic> = 10 females for stage 1 and 10 females for stage 3) and upwelling (<italic>n</italic> = 10 females for stage 1 and 10 females for stage 3).</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left">Embryo stage</th>
<th valign="top" align="center">Supply event</th>
<th valign="top" align="center">Phospholipids (&#xb5;g) PL mg Eggs<sup>-1</sup>
</th>
<th valign="top" align="center">% C</th>
<th valign="top" align="center">% N</th>
<th valign="top" align="center">% P</th>
<th valign="top" align="center">&#x3b4;<sup>13</sup>C (&#x2030;)</th>
<th valign="top" align="center">&#x3b4;<sup>15</sup>N (&#x2030;)</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" rowspan="2" align="center">1</td>
<td valign="top" align="left">Downwelling</td>
<td valign="top" align="center">77.58 &#xb1; 9.85<sup>a</sup>
</td>
<td valign="top" align="center">51.66 &#xb1; 1.15</td>
<td valign="top" align="center">10.40 &#xb1; 0.20<sup>a</sup>
</td>
<td valign="top" align="center">0.52 &#xb1; 0.10</td>
<td valign="top" align="center">-20.23 &#xb1; 1.63</td>
<td valign="top" align="center">10.82 &#xb1; 0.85<sup>a</sup>
</td>
</tr>
<tr>
<td valign="top" align="left">Upwelling</td>
<td valign="top" align="center">96.87 &#xb1; 20.72<sup>b</sup>
</td>
<td valign="top" align="center">50.55 &#xb1; 2.02</td>
<td valign="top" align="center">10.06 &#xb1; 0.45<sup>b</sup>
</td>
<td valign="top" align="center">0.56 &#xb1; 0.03</td>
<td valign="top" align="center">-19.35 &#xb1; 0.49</td>
<td valign="top" align="center">8.59 &#xb1; 0.11<sup>b</sup>
</td>
</tr>
<tr>
<td valign="top" rowspan="2" align="center">3</td>
<td valign="top" align="left">Downwelling</td>
<td valign="top" align="center">35.00 &#xb1; 3.58<sup>a</sup>
</td>
<td valign="top" align="center">43.58 &#xb1; 6.74</td>
<td valign="top" align="center">10.10 &#xb1; 1.50</td>
<td valign="top" align="center">0.56 &#xb1; 0.03</td>
<td valign="top" align="center">-19.58 &#xb1; 1.33</td>
<td valign="top" align="center">10.87 &#xb1; 1.31<sup>a</sup>
</td>
</tr>
<tr>
<td valign="top" align="left">Upwelling</td>
<td valign="top" align="center">50.20 &#xb1; 8.49<sup>b</sup>
</td>
<td valign="top" align="center">43.04 &#xb1; 1.36</td>
<td valign="top" align="center">10.20 &#xb1; 0.53</td>
<td valign="top" align="center">0.58 &#xb1; 0.02</td>
<td valign="top" align="center">-19.73 &#xb1; 1.29</td>
<td valign="top" align="center">9.19 &#xb1; 1.22<sup>b</sup>
</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>The two embryonic stages (1 and 3) were treated separately for statistical analysis. Different letters within a given column (for the same stage) indicate statistical differences between supply events (two-tailed Student&#x2019;s t-test, <italic>p</italic> &lt; 0.05). For a detailed FA profile of <italic>C. maenas</italic> embryos see <xref ref-type="bibr" rid="B58">Rey et&#xa0;al. (2016a)</xref>.</p>
</fn>
</table-wrap-foot>
</table-wrap>
<p>The isotopic profile (&#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N) of embryos was similar between developmental stages (MANOVA: <italic>F</italic> = 2.15, df = 2; <italic>p</italic> = 0.13) yet different between oceanographic event (MANOVA: <italic>F</italic> = 41.64, df = 2; <italic>p</italic>&lt; 0.01; interaction <italic>F</italic> = 1.55, df = 2; <italic>p</italic> = 0.23). Therefore, we grouped females irrespective of the developmental stage of their embryos and determined their isotopic signature during both downwelling and upwelling (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>). Ovigerous females showed a relatively similar &#x3b4;<sup>13</sup>C signature between supply events, but a higher &#x3b4;<sup>15</sup>N signature during downwelling than in the upwelling season (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). In addition, the range of isotopic signatures varied between supply events, as highlighted by the standard Bayesian ellipse areas based on both &#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N values (downwelling ellipse area = 14.14 &#x2030;<sup>2</sup>, and upwelling ellipse area = 2.30 &#x2030;<sup>2</sup>).</p>
<fig id="f2" position="float">
<label>Figure&#xa0;2</label>
<caption>
<p>Isotopic niche area of <italic>Carcinus maenas</italic> females (&#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N; &#x2030;) inferred from embryonic tissues collected during downwelling (<italic>n</italic> = 20 females) and upwelling (<italic>n</italic> = 20 females) events. Stage 1 and stage 3 embryos were combined for each event given their due to similar isotopic profiles (MANOVA, <italic>p</italic> = 0.32) The standard Bayesian Ellipse areas are shown for each supply event.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-984569-g002.tif"/>
</fig>
</sec>
<sec id="s3_2">
<title>Megalopae</title>
<p>The average ( &#xb1; SD) biomass of megalopae was significantly higher (<italic>t</italic>(531) = -20.78; <italic>p</italic>&lt; 0.01) during upwelling (0.22 &#xb1; 0.04 mg DW) as compared to the downwelling event (0.15 &#xb1; 0.04 mg DW) (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>). The two supply events surveyed also affected the C and N elemental content of megalopae (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>; %C two-tailed Students&#x2019; t-test <italic>t</italic>(531) = -9.34; <italic>p</italic>&lt; 0.01; %N two-tailed Students&#x2019; t-test <italic>t</italic>(531) = -5.32; <italic>p</italic>&lt; 0.01), as well as their C:N ratio (C:N 5.28 &#xb1; 0.31 and 5.46 &#xb1; 0.25 during downwelling and upwelling, respectively; two-tailed Students&#x2019; t-test; <italic>p</italic>&lt; 0.01). The results also demonstrate a significant interaction between the elemental profile of the megalopae and the oceanographic event (<xref ref-type="table" rid="T2">
<bold>Table&#xa0;2</bold>
</xref>).</p>
<fig id="f3" position="float">
<label>Figure&#xa0;3</label>
<caption>
<p>Biomass of <italic>Carcinus maenas</italic> megalopae (mg DW) collected during downwelling (<italic>n</italic> = 226) and upwelling (<italic>n</italic> = 307) conditions. The * denotes significant differences between supply events (one-tailed Students&#x2019; t-test, <italic>p</italic> = 0.00).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-984569-g003.tif"/>
</fig>
<fig id="f4" position="float">
<label>Figure&#xa0;4</label>
<caption>
<p>Relationship between % C and % N for <italic>Carcinus maenas</italic> megalopae collected during downwelling (<italic>n</italic> = 226) and upwelling (<italic>n</italic> = 307). The slopes of the predicted linear regressions (thick lines) represent the C:N ratio for the megalopae during the two contrasting supply events (black for downwelling, white for upwelling). The grey area depict the confidence intervals (2 times the St. Error). The C:N ratios were significantly different between supply events (two-tailed Students&#x2019; t-test, <italic>p</italic> &lt; 0.05).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-984569-g004.tif"/>
</fig>
<table-wrap id="T2" position="float">
<label>Table&#xa0;2</label>
<caption>
<p>Linear model testing the interaction between oceanographic events (downwelling and upwelling) and the elemental content of <italic>Carcinus maenas</italic> megalopae (%N as the response variable, %C and oceanographic event as explanatory variables).</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left"/>
<th valign="top" align="center">Estimate</th>
<th valign="top" align="center">St. Error</th>
<th valign="top" align="center">
<italic>t</italic>
</th>
<th valign="top" colspan="2" align="center">
<italic>P</italic>
</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Intercept</td>
<td valign="top" align="center">-1.37</td>
<td valign="top" align="center">0.23</td>
<td valign="top" align="center">-6.02</td>
<td valign="top" colspan="2" align="center">&lt;0.01</td>
</tr>
<tr>
<td valign="top" align="left">%C</td>
<td valign="top" align="center">0.27</td>
<td valign="top" align="center">0.01</td>
<td valign="top" align="center">34.60</td>
<td valign="top" colspan="2" align="center">&lt;0.01</td>
</tr>
<tr>
<td valign="top" align="left">Event (upwelling)</td>
<td valign="top" align="center">1.63</td>
<td valign="top" align="center">0.27</td>
<td valign="top" align="center">6.06</td>
<td valign="top" colspan="2" align="center">&lt;0.01</td>
</tr>
<tr>
<td valign="top" align="left">%C * Event (upwelling)</td>
<td valign="top" align="center">-0.06</td>
<td valign="top" align="center">0.01</td>
<td valign="top" align="center">-7.06</td>
<td valign="top" colspan="2" align="center">&lt;0.01</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>All parameters were statistically significant at <italic>p</italic> &lt; 0.01.</p>
</fn>
<fn><p>* denotes the interaction between the two factors (%C and event).</p></fn>
</table-wrap-foot>
</table-wrap>
<p>Megalopae showed significantly different isotopic signatures (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>) during downwelling and upwelling (MANOVA: <italic>F</italic> = 103.37, df = 2; <italic>p</italic>&lt; 0.01). The &#x3b4;<sup>13</sup>C ranged between -20.9 and -16.3&#x2030; during downwelling and -19.9 and -17.0&#x2030; during upwelling, being the average &#x3b4;<sup>13</sup>C value lower during downwelling than upwelling (-19.27 &#xb1; 0.87&#x2030; and -18.58 &#xb1; 0.49&#x2030;, respectively; <italic>p</italic>&lt; 0.01). The opposite was observed for the &#x3b4;<sup>15</sup>N signature, with an average of 7.91 &#xb1; 0.50&#x2030; during downwelling and 7.66 &#xb1; 0.49&#x2030; during upwelling (<italic>p</italic>&lt; 0.01). Yet, the isotopic signature showed a similar range in both events (6.1 to 9.1&#x2030; &#x2013; downwelling; 6.1 to 9.2&#x2030; &#x2013; upwelling). In addition, the isotopic niche space occupied by megalopae during the downwelling event was notably larger than that during upwelling, as highlighted by the standard Bayesian ellipse areas based on both &#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N values (downwelling = 1.36&#x2030;<sup>2</sup>, and upwelling = 0.71&#x2030;<sup>2</sup>).</p>
<fig id="f5" position="float">
<label>Figure&#xa0;5</label>
<caption>
<p>Isotopic niche area based on stable isotopes (&#x3b4;<sup>13</sup>C and &#x3b4;<sup>15</sup>N) of <italic>Carcinus maenas</italic> megalopae collected during downwelling (<italic>n</italic> = 226) and upwelling (<italic>n</italic> = 307) conditions. The standard Bayesian Ellipse areas were significantly different between supply events (MANOVA, <italic>p</italic> &lt; 0.01).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-09-984569-g005.tif"/>
</fig>
</sec>
</sec>
<sec id="s4" sec-type="discussion">
<title>Discussion</title>
<p>Two main questions addressed in this study using the brachyuran crab <italic>C. maenas</italic> as a model species were: i) whether downwelling and upwelling events differently affect inter-individual variability of organisms with complex life cycles, and ii) how different developmental stages can drive variability among individuals. To answer these questions we focused on the early life stages of this species, namely their embryos and megalopae, as their influence on early benthic life stages is already documented (e.g., <xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B61">Rey et&#xa0;al., 2015b</xref>; <xref ref-type="bibr" rid="B59">Rey et&#xa0;al., 2016b</xref>) through carry-over effects (also known as legacy effects) with potential phenotypic and fitness consequences (e.g., <xref ref-type="bibr" rid="B48">Pechenik, 2006</xref>; <xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B60">Rey et&#xa0;al., 2019</xref>). In summary, downwelling and upwelling events differently affected inter-individual variability, particularly through the trophic ecology of females and of megalopae during planktonic life.</p>
<p>One possible source of inter-individual variability in early life stages concerns maternal effects, which can be defined as &#x201c;the effects of adult conditioning on offspring quality&#x201d; as in <xref ref-type="bibr" rid="B48">Pechenik (2006)</xref> and references therein. Here, maternal effects were assessed through the consequences of female biomass on the volume and elemental composition of their embryos (<xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>), despite acknowledging that these effects can also be accounted using other parameters (e.g., cortisol levels in <xref ref-type="bibr" rid="B36">McCormick, 1998</xref>). The reason why female size was considered as a plausible source of maternal effects concerns the fact that larger females can secure more and/or better food, which improves the allocation of reserves to their embryos (<xref ref-type="bibr" rid="B9">Calado and Leal, 2015</xref>) and ultimately allow larvae to hatch in better conditions than those from smaller females. Indeed, energetic reserves are significantly correlated with embryonic size in various decapod species (<xref ref-type="bibr" rid="B64">Rosa et&#xa0;al., 2007</xref>). We thus hypothesized that stage 1 embryos from larger <italic>C. maenas</italic> females could be fitter than those from smaller females, and consequently display a higher volume and/or C:N ratio. However, neither the volume of stage 1 embryos (<xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1A</bold>
</xref>) nor the C:N ratio (<xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1B</bold>
</xref>) were affected by the size of the ovigerous female (<italic>p</italic> &gt; 0.05 on all cases), suggesting that female size does not significantly contribute as a driver of inter-individual variability. While this observation is in agreement with previous findings for <italic>Paralithodes camtschaticus</italic>, where female weight did not affect embryo size (<xref ref-type="bibr" rid="B71">Swiney et&#xa0;al., 2013</xref>), it contrasts with the findings for the European lobster <italic>Homarus gammarus</italic> (<xref ref-type="bibr" rid="B39">Moland et&#xa0;al., 2010</xref>).</p>
<p>A common feature of embryogenesis in crustaceans is the catabolism of lipidic reserves (<xref ref-type="bibr" rid="B49">Petersen and Anger, 1997</xref>; <xref ref-type="bibr" rid="B65">Rosa et&#xa0;al., 2003</xref>; <xref ref-type="bibr" rid="B63">Rosa et&#xa0;al., 2005</xref>), which is supported by the differences observed between the lipidic reserves of stage 1 and stage 3 embryos (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). This consumption of the available lipid pool throughout embryo development could also explain the lower C and N contents, and C:N ratios observed in late-stage embryos, when compared with newly-extruded ones (e.g., <xref ref-type="bibr" rid="B13">Dawirs, 1981</xref>; <xref ref-type="bibr" rid="B64">Rosa et&#xa0;al., 2007</xref>). Nevertheless, it is worth mentioning that the C:N ratio remained unaltered within a given embryonic stage (<italic>p</italic> &gt; 0.05 &#x2013; <xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>), despite these originating from females sampled at different oceanographic events, which is a clear sign of homeostasis in <italic>C. maenas</italic>&#x2019; embryos. Irrespective of developmental stage, different oceanographic events affected embryonic lipid content (PL content), with these being significantly lower during downwelling (<italic>p</italic>&lt; 0.05 on all cases &#x2013; <xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). These differences in energetic reserves between supply events are natural (e.g., <xref ref-type="bibr" rid="B8">Brillon et&#xa0;al., 2005</xref>; <xref ref-type="bibr" rid="B10">Calado et&#xa0;al., 2010</xref>) and are expected to repercuss on the success of larval life, as well as post-metamorphosis (e.g., <xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B61">Rey et&#xa0;al., 2015b</xref>; <xref ref-type="bibr" rid="B59">Rey et&#xa0;al., 2016b</xref>). Indeed, upwelling causes an ascent of nutrients from cooler and deeper waters to the surface, which reflects heavily on the food chain composition (e.g., <xref ref-type="bibr" rid="B82">Wilson et&#xa0;al., 2021</xref>) that becomes diatom-dominated (e.g., <xref ref-type="bibr" rid="B19">Fenchel, 1988</xref>; <xref ref-type="bibr" rid="B67">Sommer et&#xa0;al., 2002</xref>; <xref ref-type="bibr" rid="B77">Vidal et&#xa0;al., 2017</xref>). This shift in the dominant planktonic group alters the entire food chain, including the trophic ecology and nutritional status of <italic>C. maenas</italic> females that feed on planktivorous species (<xref ref-type="bibr" rid="B45">Pardal et&#xa0;al., 2006</xref>), as well as the extent of their energetic reserves (<xref ref-type="bibr" rid="B76">Tuck et&#xa0;al., 1997</xref>; <xref ref-type="bibr" rid="B53">Racotta et&#xa0;al., 2003</xref>).</p>
<p>The most prominent effect of different oceanographic events was recorded on the isotopic signature of embryos (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>). As these tissues display fast turnover rates (e.g., <xref ref-type="bibr" rid="B14">Dimitrijevi&#x107; et&#xa0;al., 2018</xref>), their isotopic signature is strongly shaped by maternal diet prior oviposition. Thus, the isotopic signature of embryos can be used as a reliable proxy to estimate the isotopic niche of ovigerous females (e.g., <xref ref-type="bibr" rid="B30">Kaufman et&#xa0;al., 2014</xref>). A species&#x2019; isotopic niche is tightly correlated with its trophic niche, despite not being the same concept (<xref ref-type="bibr" rid="B51">Post, 2002</xref>; <xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>). The trophic niche of a predator is determined by its diet (<xref ref-type="bibr" rid="B40">Moore and Semmens, 2008</xref>; <xref ref-type="bibr" rid="B46">Parnell et&#xa0;al., 2010</xref>), whereas the isotopic niche is often beset by the consumer physiology (although in predictable amounts, thus the value of such comparison &#x2013; e.g., (<xref ref-type="bibr" rid="B51">Post, 2002</xref>), <xref ref-type="bibr" rid="B5">Bearhop et&#xa0;al. (2002)</xref>; <xref ref-type="bibr" rid="B24">Fox-Dobbs et&#xa0;al. (2007)</xref>. In this regard, the &#x3b4;<sup>13</sup>C values can be used to determine the variability of dietary carbon sources (e.g., <xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B83">Yeakel et&#xa0;al., 2016</xref>) due to different incorporation rates across prey species (<xref ref-type="bibr" rid="B32">Layman et&#xa0;al., 2007</xref>). On the other hand, &#x3b4;<sup>15</sup>N values are better suited to determine the trophic level of individuals (<xref ref-type="bibr" rid="B32">Layman et&#xa0;al., 2007</xref>; <xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>). Therefore, one can observe a direct effect of the supply event on the trophic ecology of ovigerous females: during downwelling females eat more diverse food (higher &#x3b4;<sup>13</sup>C variability and range) and show a notably higher trophic level than females collected during upwelling conditions (higher &#x3b4;<sup>15</sup>N value). The average &#x3b4;<sup>15</sup>N signature during downwelling was ca. 1.97&#x2030; higher than that during upwelling, which denotes an enrichment within the expected values of a one-level trophic variation; between 1.3 and 5.3&#x2030;, with an average of ca. 3.4&#x2030; (<xref ref-type="bibr" rid="B37">Minagawa and Wada, 1984</xref>; <xref ref-type="bibr" rid="B79">Wada et&#xa0;al., 1987</xref>; <xref ref-type="bibr" rid="B25">Fry, 1988</xref>). In other words, <italic>C. maenas</italic> females predate on a shorter food chain during upwelling than they do during downwelling, with the diversity of prey items being lower. Adults <italic>C. maenas</italic> predate on important consumers of planktonic communities (e.g., <xref ref-type="bibr" rid="B50">Pihl, 1985</xref>; <xref ref-type="bibr" rid="B44">Palacios and Ferraro, 2003</xref>), whose abundance (e.g., <xref ref-type="bibr" rid="B43">Ospina-Alvarez et&#xa0;al., 2010</xref>) and composition (e.g., <xref ref-type="bibr" rid="B82">Wilson et&#xa0;al., 2021</xref>) is heavily influenced by oceanographic events and seasons (<xref ref-type="bibr" rid="B45">Pardal et&#xa0;al., 2006</xref>). Altogether, results suggest that downwelling increases the diversity of food sources being used and the length of the food chain, thus shaping the trophic ecology of adult <italic>C. maenas</italic> (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>). These consequences of downwelling are in agreement with previous studies (e.g., <xref ref-type="bibr" rid="B73">Tarran et&#xa0;al., 1999</xref>). Indeed, the lack of a dominant planktonic group during downwelling events, such as diatoms that dominate the phytoplankton community during upwelling conditions (<xref ref-type="bibr" rid="B19">Fenchel, 1988</xref>; <xref ref-type="bibr" rid="B67">Sommer et&#xa0;al., 2002</xref>), might force a diversification of prey items (and increase competition for resources &#x2013; e.g., <xref ref-type="bibr" rid="B16">Duarte et&#xa0;al., 2017</xref>); under this scenario the range of &#x3b4;<sup>13</sup>C values increases for a given species (<xref ref-type="bibr" rid="B28">Jackson et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B83">Yeakel et&#xa0;al., 2016</xref>). Therefore, the change in the trophic ecology of <italic>C. maenas</italic> in response to contrasting oceanographic events can be deemed responsible for the changes in the lipidic reserves displayed by its embryos (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). Additionally, results suggest that the higher inter-individual variability observed in the isotopic profile of ovigerous females during downwelling conditions is retained throughout embryogenesis.</p>
<p>Cascade-like effects, where early life histories determine the success or demise of later developmental stages, have been previously investigated in marine invertebrates, particularly in decapod crustaceans (e.g., <xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B61">Rey et&#xa0;al., 2015b</xref>). Yet, few studies have addressed such impacts at the individual level due to the inherently complex process of sampling and analysing individual larvae (<xref ref-type="bibr" rid="B60">Rey et&#xa0;al., 2019</xref>). Here we assessed whether the inter-individual variability during embryonic development was associated with maternal effects, as well as contrasting oceanographic conditions. One other aspect was whether megalopae would still exhibit measurable inter-individual variability that could be traced back to the influence of distinct larval supply events. It is worth noticing that despite having data from distinct developmental stages in <italic>C. maenas</italic>, our study does not provide information on the effect of development <italic>per se</italic> as a possible source of inter-individual variability, as this would require following the same individuals of a given population across multiple developmental stages.</p>
<p>The larger megalopae of <italic>C. maenas</italic> observed during upwelling (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>) suggest that the higher lipidic reserves observed in upwelling embryos (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>) likely benefited the organisms in subsequent developmental stage (also confirmed by the higher C:N ratio recorded during upwelling &#x2013; <xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>). Yet, it could have been beneficial to account for other biochemical parameters (other than lipidic reserves) that also affect a larvae&#x2019;s development into megalopae, such as the protein or carbohydrate content, for example (<xref ref-type="bibr" rid="B35">McAlister and Moran, 2012</xref>). In any case, our observations are in accordance with <xref ref-type="bibr" rid="B56">Rey et&#xa0;al. (2017)</xref>, who suggested that upwelling produced higher quality lipids in <italic>C. maenas</italic> embryos and improved larval quality and chances to successfully metamorphose. Furthermore, our results match the model predictions of <xref ref-type="bibr" rid="B59">Rey et&#xa0;al. (2016b)</xref>, where being a zoea during upwelling conditions promoted the growth of juvenile crabs. The larger an organism is, the faster it undergoes metamorphosis (<xref ref-type="bibr" rid="B27">Gim&#xe9;nez, 2010</xref>; <xref ref-type="bibr" rid="B9">Calado and Leal, 2015</xref>), which can be useful both from a prey&#x2019;s but also from a predator&#x2019;s point of view. From the prey&#x2019;s perspective, metamorphosis can make an organism large enough to attain a so called &#x201c;safe size&#x201d;, hence escape predation (<xref ref-type="bibr" rid="B81">Werner, 1991</xref>; <xref ref-type="bibr" rid="B1">Abrams et&#xa0;al., 1996</xref>) or, in the specific case of <italic>C. maenas</italic>, most likely cannibalism (<xref ref-type="bibr" rid="B38">Moksnes, 2004</xref>; <xref ref-type="bibr" rid="B2">Almeida et&#xa0;al., 2011</xref>). As a predator, metamorphosis in <italic>C. maenas</italic> involves the formation of claws and improves the overall strength of the organism, which grants it a competitive advantage over its competitors for food (<xref ref-type="bibr" rid="B17">Duarte et&#xa0;al., 2014</xref>). As such, the biomass data record (larger megalopae during upwelling conditions) suggest that individuals are better suited to deal with various biotic constraints during upwelling than during downwelling, as confirmed by the C:N ratio (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>) and the significant interaction of supply event (<xref ref-type="table" rid="T2">
<bold>Table&#xa0;2</bold>
</xref>). The reason behind having higher biomass and C:N ratios during upwelling may be explained by the dietary shifts that occur in the plankton, a direct consequence of shifting oceanographic conditions (see discussion below). Indeed, the fact that megalopae feed on plankton paired with the observations of healthy megalopae during downwelling, imply that embryonic reserves cannot completely explain the success or demise of later life stages. In other words, a lipid-poor embryo does not necessarily imply failure as megalopae since success also depends on the conditions and resources (such as food) encountered as a megalopae, thus compensating the lack of initial energetic reserves (see <xref ref-type="bibr" rid="B70">Swearer et&#xa0;al., 2019</xref> and references therein). It is also important to highlight that the higher and less variable C:N ratio (in megalopae) during upwelling suggests no absolute homeostasis and implies that these individuals are in better conditions when upwelling is the dominant oceanographic condition. Our results thus agree with previous observations that organisms deal with a changing environment by adjusting homeostatic mechanisms over time i.e., exhibit rheostasis (e.g., <xref ref-type="bibr" rid="B78">Villar-Argaiz et&#xa0;al., 2002</xref>; <xref ref-type="bibr" rid="B34">Leal et&#xa0;al., 2017</xref>).</p>
<p>Another important aspect to highlight is the lower inter-individual variability of megalopae isotopic signature during upwelling than downwelling. As previously discussed, the available range of preys greatly affects the trophic ecology of <italic>C. maenas</italic>. The trophic level of the megalopae (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>) suggests that, during upwelling, the organisms are a part of a shorter and more efficient food chain (e.g., <xref ref-type="bibr" rid="B19">Fenchel, 1988</xref>; <xref ref-type="bibr" rid="B67">Sommer et&#xa0;al., 2002</xref>). As observed by <xref ref-type="bibr" rid="B16">Duarte et&#xa0;al. (2017)</xref> for a different decapod species, a habitat with a surplus of food (equivalent to upwelling conditions in our study) enables feeding on preferred food items, which narrows down the isotopic niche of a species. In the opposite scenario (downwelling), megalopae cannot be selective and must feed on whatever preys are available. This generalist feeding behaviour often implies a higher competition for resources, with intra/inter-specific competition being known to affect the magnitude of inter-individual variability within a population (<xref ref-type="bibr" rid="B3">Ara&#xfa;jo et&#xa0;al., 2011</xref>). Altogether, this information supports our observation of a wider (i.e., more variable) isotopic niche in megalopae developing during downwelling events when contrasted to conspecifics developing during upwelling (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>).</p>
<p>Our combined observations in <italic>C. maenas</italic> adults, newly extruded and late-stage embryos, and megalopae suggest that contrasting oceanographic conditions of downwelling and upwelling greatly affect inter-individual variability. However, it must be highlighted that the conclusions attained at adult level (i.e., with ovigerous females) should be taken with caution, as sampling 20 females per oceanographic event may underestimate diversity at population level. Overall, variability was higher during downwelling irrespective of the life stage, which can indicate that organisms can be more adaptable and resilient during these oceanographic events (<xref ref-type="bibr" rid="B69">Sunday et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B22">Foo et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B66">Schlegel et&#xa0;al., 2012</xref>). However, upwelling resulted in higher lipidic reserves and C:N ratios in embryos. Altogether, it appears that hatching and growing during upwelling conditions results not only in larger individuals but also in better fitness conditions and, ultimately, more resilient populations. Nevertheless, during downwelling the higher inter-individual variability recorded highlights the remarkable ability of <italic>C. maenas</italic> to cope and thrive in highly variable environments, likely being key for this species success as a global invader.</p>
</sec>
<sec id="s5" sec-type="data-availability">
<title>Data availability statement</title>
<p>Data is available at Zenodo and can be cited using this reference: Leal, Miguel Costa, Rey, Felisa, Ferreira, Guilherme Duarte, Domingues, M. Ros&#xe1;rio, &amp; Calado, Ricardo. (2022). Inter-individual variability of early life stages of a model marine invertebrate with a bi-phasic life cycle is shaped by contrasting oceanographic conditions [Data set]. <uri xlink:href="https://doi.org/10.3389/fmars.2022.984569">https://doi.org/10.3389/fmars.2022.984569</uri>.</p>
</sec>
<sec id="s6" sec-type="author-contributions">
<title>Author contributions</title>
<p>ML, FR, MD, and RC conceptualized the experiments. RC, MD and ML acquired funding and provided materials and facilities. FR collected the samples and conducted the laboratory experiments. ML performed the laboratory analysis. ML and GF analysed the data and prepared the figures. GF and ML prepared the original draft manuscript. All authors commented and contributed to the final version of the manuscript thus justifying all authorships.</p>
</sec>
<sec id="s7" sec-type="funding-information">
<title>Funding</title>
<p>This work was supported by national funds, through Funda&#xe7;&#xe3;o para a Ci&#xea;ncia e Tecnologia (FCT), in the scope of the Individual Call to Scientific Employment Stimulus 2017 with a Junior Researcher contract [CEECIND/00580/2017 to FR] and an Assistant Researcher contract [CEECIND/01618/2020 to ML]. We also acknowledge financial support to CESAM by FCT/MCTES (UIDP/50017/2020+UIDB/50017/2020+ LA/P/0094/2020), through national funds, and to national funding through FCT, within the research project, NO RESET PTDC/BIA-BIC/116871/2010. ML was also supported by EAWAG funding. The authors also acknowledge the contribution of Serge Robert and In&#xea;s Carvalho during the laboratory analysis.</p>
</sec>
<sec id="s8" sec-type="acknowledgement">
<title>Acknowledgments</title>
<p>The authors acknowledge the contribution of Serge Robert and In&#xea;s Carvalho during the laboratory analysis.</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>
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