{"refrec":{"BRefID":64870,"RR":"<b>Bouillon, S.; Moens, T.; Koedam, N.; Dahdouh-Guebas, F.; Baeyens, W.; Dehairs, F.</b> (2004). Variability in the origin of carbon substrates for bacterial communities in mangrove sediments. <i>FEMS Microbiol. Ecol. 49(2)</i>: 171-179. <a href=\"http://dx.doi.org/10.1016/j.femsec.2004.03.004\" target=\"_blank\">dx.doi.org/10.1016/j.femsec.2004.03.004</a>","BEntID":61351,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>FEMS Microbiol. Ecol. 49(2)</i>: 171-179. <a href=\"https://dx.doi.org/10.1016/j.femsec.2004.03.004\" target=\"_blank\">https://dx.doi.org/10.1016/j.femsec.2004.03.004</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bouillon, S.; Moens, T.; Koedam, N.; Dahdouh-Guebas, F.; Baeyens, W.; Dehairs, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bouillon, S. <i>et al.</i>","Englishabstract":"Organic carbon in mangrove sediments originates from both local sources (mangroves, microphytobenthos) and tidal inputs (e.g. phytoplankton, seagrass-derived material). The relative inputs of these sources may vary strongly, both within and between different mangrove sites. We combined elemental (TOC/TN) and bulk d<sup>13</sup>C analysis on sediment cores from various mangrove sites with  d<sup>13</sup>C data of bacteria-specific phospholipid fatty acids (PLFA) in order to identify the dominant carbon substrates used by in situ bacterial communities. ?<sup>13</sup>C values of each of these markers showed a range of 10‰ or more across the different sites and sampling depths, but generally followed the d<sup>13</sup>C trend observed in bulk organic carbon. Several sediment cores show a strong vertical gradient in PLFA d<sup>13</sup>C, suggesting a selectivity for algal-derived carbon in the surface layers. 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