{"refrec":{"BRefID":350470,"RR":"<b>Babila, T.L.; Penman, D.E.; Standish, C.D.; Doubrawa, M.; Bralower, T.J.; Robinson, M.M.; Self-Trail, J.M.; Speijer, R.P.; Stassen, P.; Foster, G.L.; Zachos, J.C.</b> (2022). Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum. <i>Science Advances 8(11)</i>: eabg1025. <a href=\"https://dx.doi.org/10.1126/sciadv.abg1025\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.abg1025</a>","BEntID":348166,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Science Advances 8(11)</i>: eabg1025. <a href=\"https://dx.doi.org/10.1126/sciadv.abg1025\" target=\"_blank\">https://dx.doi.org/10.1126/sciadv.abg1025</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Babila, T.L.; Penman, D.E.; Standish, C.D.; Doubrawa, M.; Bralower, T.J.; Robinson, M.M.; Self-Trail, J.M.; Speijer, R.P.; Stassen, P.; Foster, G.L.; Zachos, J.C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Babila, T.L. <i>et al.</i>","Englishabstract":"The Paleocene-Eocene Thermal Maximum (PETM) is recognized by a major negative carbon isotope (δ<sup>13</sup>C) excursion (CIE) signifying an injection of isotopically light carbon into exogenic reservoirs, the mass, source, and tempo of which continue to be debated. Evidence of a transient precursor carbon release(s) has been identified in a few localities, although it remains equivocal whether there is a global signal. Here, we present foraminiferal δ<sup>13</sup>C records from a marine continental margin section, which reveal a 1.0 to 1.5‰ negative pre-onset excursion (POE), and concomitant rise in sea surface temperature of at least 2°C and a decline in ocean pH. The recovery of both δ<sup>13</sup>C and pH before the CIE onset and apparent absence of a POE in deep-sea records suggests a rapid (&lt; ocean mixing time scales) carbon release, followed by recovery driven by deep-sea mixing. Carbon released during the POE is therefore likely more similar to ongoing anthropogenic emissions in mass and rate than the main CIE.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-03-17","DateCreate":"2022-03-17","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000770280500002","VABBcode":null,"OpenAcc":1,"DOI":"10.1126/sciadv.abg1025"},"refs":null,"anarec":{"AnaID":350470,"PubliDate":2022,"Pagination":"eabg1025","XtraPublOfAnaID":null,"ISBN":null,"Volume":"8","Issue":"11","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":248966,"SerRR":"Science Advances. 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