{"refrec":{"BRefID":111335,"RR":"<b>Lorrain, A.; Paulet, Y.-M.; Chauvaud, L.; Dunbar, R.B.; Mucciarone, D.; Fontugne, M.</b> (2004). d<sup>13</sup>C variation in scallop shells: increasing metabolic carbon contribution with body size? <i>Geochim. Cosmochim. Acta 68(17)</i>: 3509-3519. <a href=\"http://dx.doi.org/10.1016/j.gca.2004.01.025\" target=\"_blank\">dx.doi.org/10.1016/j.gca.2004.01.025</a>","BEntID":105973,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":" <i>Geochim. Cosmochim. Acta 68(17)</i>: 3509-3519. <a href=\"https://dx.doi.org/10.1016/j.gca.2004.01.025\" target=\"_blank\">https://dx.doi.org/10.1016/j.gca.2004.01.025</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lorrain, A.; Paulet, Y.-M.; Chauvaud, L.; Dunbar, R.B.; Mucciarone, D.; Fontugne, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lorrain, A. <i>et al.</i>","Englishabstract":"We examined &#x3b4;<sup>13</sup>C values of shallow and deep-water scallop shells as well as &#x3b4;<sup>13</sup>C of dissolved inorganic carbon (DIC) from the Bay of Brest in western Brittany. Time series of shell calcite &#x3b4;<sup>13</sup>C do not reflect seasonal variation in seawater &#x3b4;<sup>13</sup>C, but rather show a consistent pattern of decreasing &#x3b4;<sup>13</sup>C with age, suggesting a metabolic effect rather than direct environmental control. This &#x3b4;<sup>13</sup>C trend reflects an increasing contribution of metabolic CO<sub>2</sub> to skeletal carbonate throughout ontogeny, although this respired CO<sub>2</sub> does not seem to be the major source of skeletal carbon (contribution of only 10% over the first year of life). We propose a model of this effect that depends on the availability of metabolic carbon relative to the carbon requirements for calcification. A ratio of &#x201c;respired to precipitated carbon&#x201d; is calculated, and represents the amount of metabolic carbon available for calcification. Interestingly, this ratio increases throughout ontogeny suggesting a real increase of metabolic carbon utilization into the skeleton relative to carbon from seawater DIC. This ratio allows us to separate two different populations of <i>Pecten maximus</i> of different water depth. It is therefore suggested that shell &#x3b4;<sup>13</sup>C might be used to track differences in the metabolic activity of scallops from different populations.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"d<sup>13</sup>C variation in scallop shells: increasing metabolic carbon contribution with body size?","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2012-02-16","DateCreate":"2007-06-29","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000223593700006","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.gca.2004.01.025"},"refs":null,"anarec":{"AnaID":111335,"PubliDate":2004,"Pagination":"3509-3519","XtraPublOfAnaID":null,"ISBN":null,"Volume":"68","Issue":"17","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42901,"SerRR":"Geochimica et Cosmochimica Acta. 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