{"refrec":{"BRefID":352732,"RR":"<b>Agterhuis, T.; Ziegler, M.; de Winter, N.J.; Lourens, L.J.</b> (2022). Warm deep-sea temperatures across Eocene Thermal Maximum 2 from clumped isotope thermometry. <i>Commun. Earth Environ. 3</i>: 39. <a href=\"https://dx.doi.org/10.1038/s43247-022-00350-8\" target=\"_blank\">https://dx.doi.org/10.1038/s43247-022-00350-8</a>","BEntID":350441,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Commun. Earth Environ. 3</i>: 39. <a href=\"https://dx.doi.org/10.1038/s43247-022-00350-8\" target=\"_blank\">https://dx.doi.org/10.1038/s43247-022-00350-8</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Agterhuis, T.; Ziegler, M.; de Winter, N.J.; Lourens, L.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Agterhuis, T. <i>et al.</i>","Englishabstract":"The early Eocene hothouse experienced highly elevated atmospheric CO<sub>2</sub> levels and multiple transient global warming events, so-called hyperthermals. The deep ocean constitutes an assumed setting to estimate past global mean temperatures. However, available deep-sea temperature reconstructions from conventional benthic foraminiferal oxygen isotopes and magnesium/calcium ratios rely on uncertain assumptions of non-thermal influences, associated with seawater chemistry and species-specific physiological effects. Here we apply the carbonate clumped isotope thermometer, a proxy not governed by these uncertainties, to evaluate South Atlantic deep-sea temperatures across two hyperthermal events in the early Eocene (Eocene Thermal Maximum 2/H1 and H2; ~54 Myr ago). Our independent reconstructions indicate deep-sea temperatures of 13.5 ± 1.9 °C (95% CI) for the background conditions and average hyperthermal peak temperatures of 16.9 ± 2.3 °C (95% CI). On average, these absolute temperatures are three degrees warmer than estimates from benthic oxygen isotopes. This finding implies a necessary reassessment of (1) the Eocene seawater isotope composition and (2) pH changes in the deep ocean and its potential influence on benthic foraminiferal oxygen isotope records.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Warm deep-sea temperatures across Eocene Thermal Maximum 2 from clumped isotope thermometry","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-23 01:33:16.899974","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-06-21","DateCreate":"2022-06-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000760962300001","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s43247-022-00350-8"},"refs":null,"anarec":{"AnaID":352732,"PubliDate":2022,"Pagination":"39","XtraPublOfAnaID":null,"ISBN":null,"Volume":"3","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":337093,"SerRR":"Communications Earth & Environment. 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