{"refrec":{"BRefID":348431,"RR":"<b>Erdem, Z.; Lattaud, J.; van Erk, M.R.; Mezger, E.M.; Reichart, G.-J.; Lückge, A.; Sinninghe Damste, J.S.; Schouten, S.</b> (2021). Applicability of the long chain diol index (LDI) as a sea surface temperature proxy in the Arabian Sea. <i>Paleoceanography and Paleoclimatology 36(12)</i>: e2021PA004255. <a href=\"https://dx.doi.org/10.1029/2021pa004255\" target=\"_blank\">https://dx.doi.org/10.1029/2021pa004255</a>","BEntID":346125,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Paleoceanography and Paleoclimatology 36(12)</i>: e2021PA004255. <a href=\"https://dx.doi.org/10.1029/2021pa004255\" target=\"_blank\">https://dx.doi.org/10.1029/2021pa004255</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Erdem, Z.; Lattaud, J.; van Erk, M.R.; Mezger, E.M.; Reichart, G.-J.; Lückge, A.; Sinninghe Damste, J.S.; Schouten, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Erdem, Z. <i>et al.</i>","Englishabstract":"<p>    The long-chain diol index (LDI) is a relatively new proxy for sea surface    temperature (SST) which has been rarely applied in upwelling regions. Here,    we evaluated its application by comparison with other SST records obtained    by commonly used proxies, that is, the Mg/Ca ratio of the planktonic    foraminifera species <em>Globigerinoides ruber</em> and the alkenone    paleothermometer U<sup>K´</sup><sub>37</sub>. We focused on the last    glacial–interglacial transition of four different sedimentary archives from    the western and northern Arabian Sea, which are currently under the    influence of monsoon-induced upwelling and the associated development of an    oxygen minimum zone. The    <img        width=\"26\"        height=\"24\"        src=\"file:///C:/Users/LVDWEE~1/AppData/Local/Temp/msohtmlclip1/01/clip_image001.png\"        alt=\"urn:x-wiley:25724517:media:palo21117:palo21117-math-0004\"    />    and Mg/Ca<em><sub>G.ruber</sub></em> SST records revealed an increase of    0.6–3.4°C from the Last Glacial Maximum to the late Holocene with somewhat    higher amplitude in the northern part of the Arabian Sea than compared to    the western part. In contrast, the LDI SSTs did not reveal major changes    during the last glacial–interglacial transition which was followed by a    decreasing trend during the Holocene. The LGM versus the Holocene LDI SSTs    ranged between −0.2 and −2.7°C. Particularly at one record, offshore Oman,    the SST decrease during the Holocene was high in amplitude, suggesting a    potential cold bias, possibly related to changes in upwelling intensity.    This indicates that care has to be taken when applying the LDI for annual    mean SST reconstruction in upwelling regions.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Applicability of the long chain diol index (LDI) as a sea surface temperature proxy in the Arabian Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:01.897972","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2022-01-10","DateCreate":"2022-01-02","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000735924600004","VABBcode":null,"OpenAcc":0,"DOI":"10.1029/2021pa004255"},"refs":null,"anarec":{"AnaID":348431,"PubliDate":2021,"Pagination":"e2021PA004255","XtraPublOfAnaID":null,"ISBN":null,"Volume":"36","Issue":"12","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":292301,"SerRR":"Paleoceanography and Paleoclimatology. 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