{"refrec":{"BRefID":133992,"RR":"<b>van Oevelen, D.; Soetaert, K.; Franco, M.A.; Moodley, L.; van Ijzerloo, L.; Vincx, M.; Vanaverbeke, J.</b> (2009). Organic matter input and processing in two contrasting North Sea sediments: insights from stable isotope and biomass data. <i>Mar. Ecol. Prog. Ser. 380</i>: 19-32. <a href=\"http://dx.doi.org/10.3354/meps07921\" target=\"_blank\">dx.doi.org/10.3354/meps07921</a>","BEntID":127940,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Mar. Ecol. Prog. Ser. 380</i>: 19-32. <a href=\"https://dx.doi.org/10.3354/meps07921\" target=\"_blank\">https://dx.doi.org/10.3354/meps07921</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van Oevelen, D.; Soetaert, K.; Franco, M.A.; Moodley, L.; van Ijzerloo, L.; Vincx, M.; Vanaverbeke, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van Oevelen, D. <i>et al.</i>","Englishabstract":"Organic matter input and processing was studied in 2 contrasting sediments (Stn 115<sub>FINE</sub> and Stn 330<sub>COARSE</sub>) in the southern North Sea. The sediments are subjected to similar hydrodynamic conditions, but Stn 115<sub>FINE</sub> underlies a high turbidity zone, making it a fine, low-permeability sediment. Monthly data on chlorophyll a (chl a), d<sup>13</sup>C and d<sup>15</sup>N of particulate organic matter in the water column and sediment showed that the algal spring bloom deposition created a strong vertical gradient of sedimentary chl a at Stn 115<sub>FINE</sub>. Macrobenthic biomass (78 ± 60 g Cm<sup>-2</sup>, mean ± SD) was dominated by suspension feeders, suggesting biological mediation of the organic matter input. In contrast, the offshore Stn 330<sub>COARSE</sub> is a coarse, high-permeability sediment in which chl a penetrated centimeters deep due to physically mediated input. The macrobenthic community, low in biomass (3.8 ± 2.4 g Cm<sup>-2</sup>), was dominated by mobile polychaetes and epibenthic amphipods, which is characteristic of physically disturbed sediments. Overall, sediment characteristics played an important but indirect role in the organic matter input and processing. At Stn 115<sub>FINE</sub>, a large macrobenthic community developed that mediated the input of organic matter to the sediment through herbivore and predatory pathways. At Stn 330<sub>COARSE</sub>, in contrast, organic matter input seemed to be dominated by physical processes. Overall, the fraction of algal carbon degraded in the sediment was higher at Stn 115<sub>FINE</sub> than at Stn 330<sub>COARSE</sub>, indicating that the physical input at Stn 330<sub>COARSE</sub> was less efficient than the biological input at Stn 115<sub>FINE</sub>.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Organic matter input and processing in two contrasting North Sea sediments: insights from stable isotope and biomass data","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-02 08:33:14.980000","timezone_type":1,"timezone":"+00:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Food web; Carbon isotope; Nitrogen isotope; Coastal sediment; North sea; Permeable sediment; Benthic; Pelagic coupling","OtherDescriptors":null,"Notes":null,"AnaPub":2009,"MonPub":null,"DateUpdate":"2016-06-12","DateCreate":"2009-04-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000265907000002","VABBcode":null,"OpenAcc":0,"DOI":"10.3354/meps07921"},"refs":null,"anarec":{"AnaID":133992,"PubliDate":2009,"Pagination":"19-32","XtraPublOfAnaID":null,"ISBN":null,"Volume":"380","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43354,"SerRR":"Marine Ecology Progress Series. 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