{"refrec":{"BRefID":260936,"RR":"<b>Woulds, C.; Bouillon, S.; Cowie, G.L.; Drake, E.; Middelburg, J.J.; Witte, U.</b> (2016). Patterns of carbon processing at the seafloor: the role of faunal and microbial communities in moderating carbon flows. <i>Biogeosciences 13(15)</i>: 4343-4357. <a href=\"https://dx.doi.org/10.5194/bg-13-4343-2016\" target=\"_blank\">https://dx.doi.org/10.5194/bg-13-4343-2016</a>","BEntID":252954,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Biogeosciences 13(15)</i>: 4343-4357. <a href=\"https://dx.doi.org/10.5194/bg-13-4343-2016\" target=\"_blank\">https://dx.doi.org/10.5194/bg-13-4343-2016</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Woulds, C.; Bouillon, S.; Cowie, G.L.; Drake, E.; Middelburg, J.J.; Witte, U.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Woulds, C. <i>et al.</i>","Englishabstract":"Marine sediments, particularly those located in estuarine and coastal zones, are key locations for the burial of organic carbon (C). However, organic C delivered to the sediment is subjected to a range of biological C-cycling processes, the rates and relative importance of which vary markedly between sites, and which are thus difficult to predict. <br><br> In this study, stable isotope tracer experiments were used to quantify the processing of C by microbial and faunal communities in two contrasting Scottish estuarine sites: a subtidal, organic C rich site in Loch Etive with cohesive fine-grained sediment, and an intertidal, organic C poor site on an Ythan estuary sand flat with coarse-grained permeable sediments. <br><br> In both experiments, sediment cores were recovered and amended with <sup>13</sup>C labelled phytodetritus to quantify whole community respiration of the added C and to trace the isotope label into faunal and bacterial biomass. Similar respiration rates were found in Loch Etive and on the Ythan sand flat (0.64 ± 0.04 and 0.63 ± 0.12 mg C m<sup>−2</sup>h<sup>−1</sup>, respectively), which we attribute to the experiments being conducted at the same temperature. Faunal uptake of added C over the whole experiment was markedly greater in Loch Etive (204 ± 72 mg C m<sup>−2</sup>) than on the Ythan sand flat (0.96 ± 0.3 mg C m<sup>−2</sup>), and this difference was driven by a difference in both faunal biomass and activity. Conversely, bacterial C uptake over the whole experiment in Loch Etive was much lower than that on the Ythan sand flat (1.80 ± 1.66 and 127 ± 89 mg C m<sup>−2</sup>, respectively). This was not driven by differences in biomass, indicating that the bacterial community in the permeable Ythan sediments was particularly active, being responsible for 48 ± 18 % of total biologically processed C. This type of biological C processing appears to be favoured in permeable sediments. The total amount of biologically processed C was greatest in Loch Etive, largely due to greater faunal C uptake, which was in turn a result of higher faunal biomass. When comparing results from this study with a wide range of previously published isotope tracing experiments, we found a strong correlation between total benthic biomass (fauna plus bacteria) and total biological C processing rates. Therefore, we suggest that the total C-cycling capacity of benthic environments is primarily determined by total biomass.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Patterns of carbon processing at the seafloor: the role of faunal and microbial communities in moderating carbon flows","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":2016,"MonPub":null,"DateUpdate":"2021-06-02","DateCreate":"2016-08-04","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000383050600001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/bg-13-4343-2016"},"refs":null,"anarec":{"AnaID":260936,"PubliDate":2016,"Pagination":"4343-4357","XtraPublOfAnaID":null,"ISBN":null,"Volume":"13","Issue":"15","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":68092,"SerRR":"<b>Gattuso, J.P.; Kesselmeier, J. (Ed.)</b> Biogeosciences. Copernicus Publications: Göttingen.  ISSN 1726-4170; e-ISSN 1726-4189","StandardTitleSer":"Biogeosciences","ISSN":"1726-4170","AbbrevSer":"Biogeosciences","StandardTitleMon":null,"StartPage":4343,"Pages":15,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Woulds","Firstname":"Clare","Initials":"C.","Affiliation":"School of Geography, University of Leeds","Discriminator":null,"CorporateFlag":0,"BEntID":252954,"AutID":171897,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Bouillon","Firstname":"Steven","Initials":"S.","Affiliation":"Department of Earth and Environmental Sciences, KU Leuven","Discriminator":null,"CorporateFlag":0,"BEntID":252954,"AutID":177718,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":"Katholieke Universiteit Leuven; 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