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Validation of the seasonality in growth lines in the shell of Macoma balthica using stable isotopes and trace elements
Individual age is a key parameter when studying population dynamics of a species. However, accurate age determination in bivalve shells is not always straightforward due to the difficulty of using external growth lines on the shell surface as a reliable method to identify annual growth patterns. In...
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Published in: | Journal of sea research 2013-09, Vol.82, p.93-102 |
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description | Individual age is a key parameter when studying population dynamics of a species. However, accurate age determination in bivalve shells is not always straightforward due to the difficulty of using external growth lines on the shell surface as a reliable method to identify annual growth patterns. In the present paper, we aimed at validating the seasonality in growth lines in the shell of Macoma balthica using stable oxygen and carbon isotopes (δ18O and δ13C) as well as trace elements (Sr, Mn, Mg and Ca).
During a 1-year growth experiment, δ18O values in the shell carbonate peaked in February/March and matched the annual line visible in the acetate peel of the shell's cross-section. Most carbonate was deposited in the months March to May, which was supported by the observed fast growth in the experiment during this period. Growth stopped between October and December indicating that annual growth lines are formed due to autumn growth stop. Fast growth occurs mainly at temperatures above 6–7°C, although growth may already start at temperatures of about 5°C.
δ13C profiles did not show any clear seasonality related to the position of the growth lines on the valve or acetate peel and, therefore, cannot be used to estimate age. Along the hinge, Sr was the only element showing variation on the growth lines. High Sr/Ca ratios in the hinge occurred near annual growth lines identified in the acetate peel, suggesting that Sr/Ca ratios may be used to identify annual growth lines and estimate age in M. balthica. Furthermore, counting external lines (on the valve) always lead to an overestimation of age and thus an underestimation of annual growth rates. Therefore, an analysis of the cross-section of the valve seems necessary to accurately estimate age and growth rate in this species. This aspect should be taken into account in studies of growth and population dynamics.
► We validate the seasonality in growth lines in the shell of Macoma balthica. ► δ18O profiles showed that annual growth lines are due to autumn growth stop. ► Internal lines visible in the cross-section give accurate estimate of age. ► Counting external lines causes overestimation of age and underestimation of growth. ► Sr/Ca ratios and δ18O can be used to estimate age of M. balthica. |
doi_str_mv | 10.1016/j.seares.2012.09.006 |
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During a 1-year growth experiment, δ18O values in the shell carbonate peaked in February/March and matched the annual line visible in the acetate peel of the shell's cross-section. Most carbonate was deposited in the months March to May, which was supported by the observed fast growth in the experiment during this period. Growth stopped between October and December indicating that annual growth lines are formed due to autumn growth stop. Fast growth occurs mainly at temperatures above 6–7°C, although growth may already start at temperatures of about 5°C.
δ13C profiles did not show any clear seasonality related to the position of the growth lines on the valve or acetate peel and, therefore, cannot be used to estimate age. Along the hinge, Sr was the only element showing variation on the growth lines. High Sr/Ca ratios in the hinge occurred near annual growth lines identified in the acetate peel, suggesting that Sr/Ca ratios may be used to identify annual growth lines and estimate age in M. balthica. Furthermore, counting external lines (on the valve) always lead to an overestimation of age and thus an underestimation of annual growth rates. Therefore, an analysis of the cross-section of the valve seems necessary to accurately estimate age and growth rate in this species. This aspect should be taken into account in studies of growth and population dynamics.
► We validate the seasonality in growth lines in the shell of Macoma balthica. ► δ18O profiles showed that annual growth lines are due to autumn growth stop. ► Internal lines visible in the cross-section give accurate estimate of age. ► Counting external lines causes overestimation of age and underestimation of growth. ► Sr/Ca ratios and δ18O can be used to estimate age of M. balthica.</description><identifier>ISSN: 1385-1101</identifier><identifier>EISSN: 1873-1414</identifier><identifier>DOI: 10.1016/j.seares.2012.09.006</identifier><language>eng</language><publisher>Oxford: Elsevier B.V</publisher><subject>Acetates ; Age ; age determination ; Animal and plant ecology ; Animal, plant and microbial ecology ; autumn ; Biological and medical sciences ; Bivalvia ; calcium ; carbon ; Dynamic tests ; Estimates ; Fundamental and applied biological sciences. Psychology ; Growth lines ; Macoma balthica ; magnesium ; manganese ; Marine ; oxygen ; Oxygen and carbon stable isotopes ; population growth ; Sea water ecosystems ; Shell ; Shells ; stable isotopes ; Strontium ; Synecology ; temperature ; Trace elements ; Valves</subject><ispartof>Journal of sea research, 2013-09, Vol.82, p.93-102</ispartof><rights>2012 Elsevier B.V.</rights><rights>2014 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c558t-ebf1409f0ae113aee11724c77ef7c32869595de256749cfb025c0fa0bf3d308d3</citedby><cites>FETCH-LOGICAL-c558t-ebf1409f0ae113aee11724c77ef7c32869595de256749cfb025c0fa0bf3d308d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>309,310,314,780,784,789,790,23930,23931,25140,27924,27925</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=27728232$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Cardoso, Joana F.M.F.</creatorcontrib><creatorcontrib>Santos, Sílvia</creatorcontrib><creatorcontrib>Witte, Johannes IJ</creatorcontrib><creatorcontrib>Witbaard, Rob</creatorcontrib><creatorcontrib>van der Veer, Henk W.</creatorcontrib><creatorcontrib>Machado, Jorge P.</creatorcontrib><title>Validation of the seasonality in growth lines in the shell of Macoma balthica using stable isotopes and trace elements</title><title>Journal of sea research</title><description>Individual age is a key parameter when studying population dynamics of a species. However, accurate age determination in bivalve shells is not always straightforward due to the difficulty of using external growth lines on the shell surface as a reliable method to identify annual growth patterns. In the present paper, we aimed at validating the seasonality in growth lines in the shell of Macoma balthica using stable oxygen and carbon isotopes (δ18O and δ13C) as well as trace elements (Sr, Mn, Mg and Ca).
During a 1-year growth experiment, δ18O values in the shell carbonate peaked in February/March and matched the annual line visible in the acetate peel of the shell's cross-section. Most carbonate was deposited in the months March to May, which was supported by the observed fast growth in the experiment during this period. Growth stopped between October and December indicating that annual growth lines are formed due to autumn growth stop. Fast growth occurs mainly at temperatures above 6–7°C, although growth may already start at temperatures of about 5°C.
δ13C profiles did not show any clear seasonality related to the position of the growth lines on the valve or acetate peel and, therefore, cannot be used to estimate age. Along the hinge, Sr was the only element showing variation on the growth lines. High Sr/Ca ratios in the hinge occurred near annual growth lines identified in the acetate peel, suggesting that Sr/Ca ratios may be used to identify annual growth lines and estimate age in M. balthica. Furthermore, counting external lines (on the valve) always lead to an overestimation of age and thus an underestimation of annual growth rates. Therefore, an analysis of the cross-section of the valve seems necessary to accurately estimate age and growth rate in this species. This aspect should be taken into account in studies of growth and population dynamics.
► We validate the seasonality in growth lines in the shell of Macoma balthica. ► δ18O profiles showed that annual growth lines are due to autumn growth stop. ► Internal lines visible in the cross-section give accurate estimate of age. ► Counting external lines causes overestimation of age and underestimation of growth. ► Sr/Ca ratios and δ18O can be used to estimate age of M. balthica.</description><subject>Acetates</subject><subject>Age</subject><subject>age determination</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>autumn</subject><subject>Biological and medical sciences</subject><subject>Bivalvia</subject><subject>calcium</subject><subject>carbon</subject><subject>Dynamic tests</subject><subject>Estimates</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Growth lines</subject><subject>Macoma balthica</subject><subject>magnesium</subject><subject>manganese</subject><subject>Marine</subject><subject>oxygen</subject><subject>Oxygen and carbon stable isotopes</subject><subject>population growth</subject><subject>Sea water ecosystems</subject><subject>Shell</subject><subject>Shells</subject><subject>stable isotopes</subject><subject>Strontium</subject><subject>Synecology</subject><subject>temperature</subject><subject>Trace elements</subject><subject>Valves</subject><issn>1385-1101</issn><issn>1873-1414</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqNkk9v1DAQxSMEEqXwDZDwBYlLgu34T3xBQlWhlYo4QLlas85416tsvNjeon57HFJxhF48tvV7b0Z60zSvGe0YZer9vssICXPHKeMdNR2l6klzxgbdt0ww8bTe-0G2rNLPmxc57yllmpr-rLn7AVMYoYQ4k-hJ2SGpXjnO9bvckzCTbYq_yo5MYca8vP8gO5ymhf8CLh6AbGAqu-CAnHKYtyQX2ExIQo4lHqsK5pGUBA4JTnjAueSXzTMPU8ZXD_W8uf10-f3iqr35-vn64uNN66QcSosbzwQ1ngIy1gPWU3PhtEavXc8HZaSRI3KptDDObyiXjnqgG9-PPR3G_rx5t_oeU_x5wlzsIWRXh4cZ4ylbpgTng6RKPg5llAv1CJRro8Wg9P9RYbhi2qjFVayoSzHnhN4eUzhAureM2iVnu7drznbJ2VJja85V9vahA2QHk08wu5D_arnWfOA9r9yblfMQLWxTZW6_VSNZd8EYPSzEh5XAmshdwGSzCzg7HENCV-wYw79H-Q142cjp</recordid><startdate>20130901</startdate><enddate>20130901</enddate><creator>Cardoso, Joana F.M.F.</creator><creator>Santos, Sílvia</creator><creator>Witte, Johannes IJ</creator><creator>Witbaard, Rob</creator><creator>van der Veer, Henk W.</creator><creator>Machado, Jorge P.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7ST</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope><scope>SOI</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20130901</creationdate><title>Validation of the seasonality in growth lines in the shell of Macoma balthica using stable isotopes and trace elements</title><author>Cardoso, Joana F.M.F. ; Santos, Sílvia ; Witte, Johannes IJ ; Witbaard, Rob ; van der Veer, Henk W. ; Machado, Jorge P.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c558t-ebf1409f0ae113aee11724c77ef7c32869595de256749cfb025c0fa0bf3d308d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Acetates</topic><topic>Age</topic><topic>age determination</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>autumn</topic><topic>Biological and medical sciences</topic><topic>Bivalvia</topic><topic>calcium</topic><topic>carbon</topic><topic>Dynamic tests</topic><topic>Estimates</topic><topic>Fundamental and applied biological sciences. 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However, accurate age determination in bivalve shells is not always straightforward due to the difficulty of using external growth lines on the shell surface as a reliable method to identify annual growth patterns. In the present paper, we aimed at validating the seasonality in growth lines in the shell of Macoma balthica using stable oxygen and carbon isotopes (δ18O and δ13C) as well as trace elements (Sr, Mn, Mg and Ca).
During a 1-year growth experiment, δ18O values in the shell carbonate peaked in February/March and matched the annual line visible in the acetate peel of the shell's cross-section. Most carbonate was deposited in the months March to May, which was supported by the observed fast growth in the experiment during this period. Growth stopped between October and December indicating that annual growth lines are formed due to autumn growth stop. Fast growth occurs mainly at temperatures above 6–7°C, although growth may already start at temperatures of about 5°C.
δ13C profiles did not show any clear seasonality related to the position of the growth lines on the valve or acetate peel and, therefore, cannot be used to estimate age. Along the hinge, Sr was the only element showing variation on the growth lines. High Sr/Ca ratios in the hinge occurred near annual growth lines identified in the acetate peel, suggesting that Sr/Ca ratios may be used to identify annual growth lines and estimate age in M. balthica. Furthermore, counting external lines (on the valve) always lead to an overestimation of age and thus an underestimation of annual growth rates. Therefore, an analysis of the cross-section of the valve seems necessary to accurately estimate age and growth rate in this species. This aspect should be taken into account in studies of growth and population dynamics.
► We validate the seasonality in growth lines in the shell of Macoma balthica. ► δ18O profiles showed that annual growth lines are due to autumn growth stop. ► Internal lines visible in the cross-section give accurate estimate of age. ► Counting external lines causes overestimation of age and underestimation of growth. ► Sr/Ca ratios and δ18O can be used to estimate age of M. balthica.</abstract><cop>Oxford</cop><pub>Elsevier B.V</pub><doi>10.1016/j.seares.2012.09.006</doi><tpages>10</tpages></addata></record> |
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subjects | Acetates Age age determination Animal and plant ecology Animal, plant and microbial ecology autumn Biological and medical sciences Bivalvia calcium carbon Dynamic tests Estimates Fundamental and applied biological sciences. Psychology Growth lines Macoma balthica magnesium manganese Marine oxygen Oxygen and carbon stable isotopes population growth Sea water ecosystems Shell Shells stable isotopes Strontium Synecology temperature Trace elements Valves |
title | Validation of the seasonality in growth lines in the shell of Macoma balthica using stable isotopes and trace elements |
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