{"refrec":{"BRefID":331960,"RR":"<b>Livsey, C.M.; Kozdon, R.; Bauch, D.; Brummer, G.-J. A.; Jonkers, L.; Orland, I.; Hill, T.M.; Spero, H.J.</b> (2020). High‐Resolution Mg/Ca and δ<sup>18</sup>O patterns in modern <i>Neogloboquadrina pachyderma</i> from the Fram Strait and Irminger Sea. <i>Paleoceanography and Paleoclimatology 35(9)</i>. <a href=\"https://doi.org/10.1029/2020pa003969\" target=\"_blank\">https://doi.org/10.1029/2020pa003969</a>","BEntID":325572,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Paleoceanography and Paleoclimatology 35(9)</i>. <a href=\"https://doi.org/10.1029/2020pa003969\" target=\"_blank\">https://doi.org/10.1029/2020pa003969</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Livsey, C.M.; Kozdon, R.; Bauch, D.; Brummer, G.-J. A.; Jonkers, L.; Orland, I.; Hill, T.M.; Spero, H.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Livsey, C.M. <i>et al.</i>","Englishabstract":"<i>Neogloboquadrina pachyderma</i>    is the dominant species of planktonic foraminifera found in polar waters    and is therefore invaluable for paleoceanographic studies of the high    latitudes. However, the geochemistry of this species is complicated due to    the development of a thick calcite crust in its final growth stage and atgreater depths within the water column. We analyzed the in situ Mg/Ca and δ    <sup>18</sup>O in discrete calcite zones using laser ablation‐inductively    coupled plasma‐mass spectrometry, electron probe microanalysis, and    secondary ion mass spectrometry within modern <i>N. pachyderma</i> shells    from the highly dynamic Fram Strait and the seasonally isothermal/isohaline    Irminger Sea. Here we compare shell geochemistry to the measured    temperature, salinity, and δ<sup>18</sup>O<sub>sw</sub> in which the shells    calcified to better understand the controls on <i>N. pachyderma</i>    geochemical heterogeneity. We present a relationship between Mg/Ca and    temperature in <i>N. pachyderma</i> lamellar calcite that is significantly    different than published equations for shells that contained both crust and    lamellar calcite. We also document highly variable secondary ion mass    spectrometry δ<sup>18</sup>O results (up to a 3.3‰ range in single shells)    on plankton tow samples which we hypothesize is due to the granular texture    of shell walls. Finally, we document that the δ<sup>18</sup>O of the crust    and lamellar calcite of <i>N. pachyderma</i> from an isothermal/isohaline    environment are indistinguishable from each other, indicating that shifts    in <i>N. pachyderma</i> δ<sup>18</sup>O are primarily controlled by changes    in environmental temperature and/or salinity rather than differences in the    sensitivities of the two calcite types to environmental conditions.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"High‐Resolution Mg/Ca and δ<sup>18</sup>O patterns in modern <i>Neogloboquadrina pachyderma</i> from the Fram Strait and Irminger Sea","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":"foraminiferal geochemistry; SST proxy; stable isotopes; planktonic foraminifera; Mg/Ca","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2020-12-14","DateCreate":"2020-12-14","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000576397200005","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2020pa003969"},"refs":null,"anarec":{"AnaID":331960,"PubliDate":2020,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"35","Issue":"9","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":292301,"SerRR":"Paleoceanography and Paleoclimatology. 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