{"refrec":{"BRefID":284787,"RR":"<b>Lattaud, J.; Kim, J.-H; de Jonge, C.; Zell, C.; Sinninghe Damsté, J.S.; Schouten, S.</b> (2017). The C<sub>32</sub> alkane-1,15-diol as a tracer for riverine input in coastal seas. <i>Geochim. Cosmochim. Acta 202</i>: 146-158. <a href=\"https://dx.doi.org/10.1016/j.gca.2016.12.030\" target=\"_blank\">https://dx.doi.org/10.1016/j.gca.2016.12.030</a>","BEntID":276811,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geochim. Cosmochim. Acta 202</i>: 146-158. <a href=\"https://dx.doi.org/10.1016/j.gca.2016.12.030\" target=\"_blank\">https://dx.doi.org/10.1016/j.gca.2016.12.030</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lattaud, J.; Kim, J.-H; de Jonge, C.; Zell, C.; Sinninghe Damsté, J.S.; Schouten, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lattaud, J. <i>et al.</i>","Englishabstract":"Long chain alkyl diols are lipids that occur ubiquitously in marine sediments and are used as a proxy for sea surface temperature (SST), using the Long chain Diol Index (LDI), and for upwelling intensity/high nutrient conditions. The distribution of 1,13- and 1,15-diols has been documented in open marine and lacustrine sediments and suspended particulate matter, but rarely in coastal seas receiving a significant riverine, and thus continental organic matter, input. Here we studied the distribution of diols in four shelf seas with major river outflows: the Gulf of Lion, the Kara Sea, the Amazon shelf and the Berau delta, covering a wide range of climate conditions. The relative abundance of the C32 1,15-diol is consistently higher close to the river mouth and particularly in the suspended particulate matter of the rivers suggesting a terrigenous source. This is supported by statistical analysis which points out a significant positive correlation between the C32 1,15-diol and the Branched and Isoprenoid Tetraether index, a proxy reflecting soil and riverine input in marine environments. However, the C32 1,15-diol was not detected in soils and is unlikely to be derived from vegetation, suggesting that the C32 1,15-diol is mainly produced in rivers. This agrees with the observation that it is a dominant diol in most cultivated freshwater eustigmatophyte algae. We, therefore, suggest that the relative abundance of the C<sub>32</sub> 1,15-diol can potentially be used as a proxy for riverine organic matter input in shelf seas. Our results also show that long chain alkyl diols delivered by rivers can substantially affect LDI-reconstructed SSTs in coastal regions close to river mouths.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The C<sub>32</sub> alkane-1,15-diol as a tracer for riverine input in coastal seas","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":"Long chain diols; Long chain Diol Index; 1,13-,1,14- and 1,15-diols; C32 1, 15-diol; River outflow; Terrigenous output; Sea Surface Temperature    ","OtherDescriptors":null,"Notes":null,"AnaPub":2017,"MonPub":null,"DateUpdate":"2019-05-27","DateCreate":"2017-05-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000396794300008","VABBcode":null,"OpenAcc":1,"DOI":"10.1016/j.gca.2016.12.030"},"refs":null,"anarec":{"AnaID":284787,"PubliDate":2017,"Pagination":"146-158","XtraPublOfAnaID":null,"ISBN":null,"Volume":"202","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42901,"SerRR":"Geochimica et Cosmochimica Acta. Elsevier: Oxford,New York etc..  ISSN 0016-7037; e-ISSN 1872-9533","StandardTitleSer":"Geochimica et Cosmochimica Acta","ISSN":"0016-7037","AbbrevSer":"Geochim. Cosmochim. 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