{"refrec":{"BRefID":63474,"RR":"<b>Salomons, W.; Mook, W.G.</b> (1981). Field observations of the isotopic composition of particulate organic carbon in the southern North Sea and adjacent estuaries. <i>Mar. Geol. 41(3-4)</i>: M11-M20. <a href=\"http://dx.doi.org/10.1016/0025-3227(81)90079-7\" target=\"_blank\">http://dx.doi.org/10.1016/0025-3227(81)90079-7</a>","BEntID":60023,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Mar. Geol. 41(3-4)</i>: M11-M20. <a href=\"http://dx.doi.org/10.1016/0025-3227(81)90079-7\" target=\"_blank\">http://dx.doi.org/10.1016/0025-3227(81)90079-7</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Salomons, W.; Mook, W.G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Salomons, W.; Mook, W.G.","Englishabstract":"The carbon isotopic composition of the organic matter in fluvial sediments and in fluvial suspended matter falls in the range valid for continental organic matter (-25 to -28‰). The <i>d</i><sup>13</sup>C values in sediments from marine sedimentation areas and in marine suspended matter varies between -20 and -25‰. The rather low mean values for the deposited sediments of -13.2‰ suggest the presence of relatively large amounts of continental organic matter. This may be a direct supply by the present-day rivers and/or organic matter derived from the erosion of peat layers, even in the marine environment. A distinction between these two sources of detrital continental organic matter is not possible with stable isotopes studies. In the estuaries studied the organic matter contents decrease and the <i>d</i><sup>13</sup>C values of the organic matter increase in the seaward direction. 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