{"refrec":{"BRefID":210715,"RR":"<b>Poulain, C.; Lorrain, A.; Mas, R.; Gillikin, D.P.; Dehairs, F.; Robert, R.; Paulet, Y.M.</b> (2010). Experimental shift of diet and DIC stable carbon isotopes: Influence on shell d<sup>13</sup>C values in the Manila clam <i>Ruditapes philippinarum</i>. <i>Chem. Geol. 272(1-4)</i>: 75-82. <a href=\"http://dx.doi.org/10.1016/j.chemgeo.2010.02.006\" target=\"_blank\">dx.doi.org/10.1016/j.chemgeo.2010.02.006</a>","BEntID":202637,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Chem. Geol. 272(1-4)</i>: 75-82. <a href=\"https://dx.doi.org/10.1016/j.chemgeo.2010.02.006\" target=\"_blank\">https://dx.doi.org/10.1016/j.chemgeo.2010.02.006</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Poulain, C.; Lorrain, A.; Mas, R.; Gillikin, D.P.; Dehairs, F.; Robert, R.; Paulet, Y.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Poulain, C. <i>et al.</i>","Englishabstract":"The influences of diet and seawater dissolved inorganic carbon (DIC) on the carbon isotope composition of shell aragonite d<sup>13</sup>C<sub>shell</sub> in the Manila clam <i>Ruditapes philippinarum</i> reared under laboratory conditions were investigated. Clams were exposed to two successive negative carbon isotope shifts: a first shift in diet (d<sup>13</sup>C<sub>phytoplankton</sub>) and a second shift, 35 days later, in DIC (d<sup>13</sup>C<sub>DIC</sub>). Both successive shifts induced a decrease in d<sup>13</sup>C<sub>shell</sub>. These results are the first to experimentally confirm an incorporation of respired carbon derived from food and carbon from DIC into shell carbonate of adult bivalves. Skeletal d<sup>13</sup>C responded to changes in the d<sup>13</sup>C of both diet and DIC in less than 7 days. Consequently, proxies based on d<sup>13</sup>C<sub>shell</sub> may be used with high temporal resolution. Using d<sup>13</sup>C<sub>phycoplankton</sub> as a proxy for the carbon isotope composition of respired carbon (d<sup>13</sup>C<sub>R</sub>) resulted in a rather constant percentage of metabolic carbon (C<sub>M</sub>) into the shell carbonate over time (close to 12%). However, an accurate estimation of d<sup>13</sup>C<sub>R</sub> is required in order to precisely estimate the percentage of metabolic carbon incorporated into the shell. Despite the significant incorporation of metabolic carbon into shell carbonate, our experimental results revealed that d<sup>13</sup>C<sub>shell</sub> was highly correlated with d<sup>13</sup>C<sub>DIC</sub> (r<sup>2</sup>=0.77, p<0.0001). Thus it seems that d<sup>13</sup>C<sub>shell</sub> is a promising proxy of large scale variations in d<sup>13</sup>C<sub>DIC</sub> and therefore of salinity in estuarine water.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Experimental shift of diet and DIC stable carbon isotopes: Influence on shell d<sup>13</sup>C values in the Manila clam <i>Ruditapes philippinarum</i>","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"delta(13)C(shell); DIC; Salinity; Metabolic carbon; Ruditapes","OtherDescriptors":null,"Notes":null,"AnaPub":2010,"MonPub":null,"DateUpdate":"2012-06-08","DateCreate":"2011-12-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000277220700009","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.chemgeo.2010.02.006"},"refs":null,"anarec":{"AnaID":210715,"PubliDate":2010,"Pagination":"75-82","XtraPublOfAnaID":null,"ISBN":null,"Volume":"272","Issue":"1-4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42560,"SerRR":"Chemical Geology. Elsevier: New York; London; Amsterdam.  ISSN 0009-2541; e-ISSN 1872-6836","StandardTitleSer":"Chemical Geology","ISSN":"0009-2541","AbbrevSer":"Chem. 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