{"refrec":{"BRefID":230895,"RR":"<b>van der Meer, M.T.J.; Benthien, A.; Bijma, J.; Schouten, S.; Sinninghe Damsté, J.S.</b> (2013). Alkenone distribution impacts the hydrogen isotopic composition of the C<sub>37:2</sub> and C<sub>37:3</sub> alkan-2-ones in <i>Emiliania huxleyi</i>. <i>Geochim. Cosmochim. Acta 111</i>: 162-166. <a href=\"http://dx.doi.org/10.1016/j.gca.2012.10.041\" target=\"_blank\">dx.doi.org/10.1016/j.gca.2012.10.041</a>","BEntID":222607,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geochim. Cosmochim. Acta 111</i>: 162-166. <a href=\"https://dx.doi.org/10.1016/j.gca.2012.10.041\" target=\"_blank\">https://dx.doi.org/10.1016/j.gca.2012.10.041</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"van der Meer, M.T.J.; Benthien, A.; Bijma, J.; Schouten, S.; Sinninghe Damsté, J.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"van der Meer, M.T.J. <i>et al.</i>","Englishabstract":"The hydrogen isotopic composition (delta D) of long-chain alkenones derived from haptophyte algae has recently been applied as paleo sea surface salinity proxy, but this application has been complicated by reported differences in delta D of individual C-37 alkenones of up to 45 parts per thousand. Here we show that this difference in D/H ratios is the result of the desaturation of the C-37:2 alkenone to form the C-37:3 alkenone and related to the relative abundance of the individual alkenones, and, therefore, the U-37(K)'. For the purpose of reconstructing paleo sea surface salinities it is recommended to determine the delta D of combined rather than individual C-37 alkenones.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Alkenone distribution impacts the hydrogen isotopic composition of the C<sub>37:2</sub> and C<sub>37:3</sub> alkan-2-ones in <i>Emiliania huxleyi</i>","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:32:52.928458","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2013,"MonPub":null,"DateUpdate":"2014-07-16","DateCreate":"2013-12-01","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000317746800013","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.gca.2012.10.041"},"refs":null,"anarec":{"AnaID":230895,"PubliDate":2013,"Pagination":"162-166","XtraPublOfAnaID":null,"ISBN":null,"Volume":"111","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42901,"SerRR":"Geochimica et Cosmochimica Acta. 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