{"refrec":{"BRefID":395805,"RR":"<b>Judd, E.J.; Tierney, J.E.; Lunt, D.J.; Montañez, I.P.; Huber, B.T.; Wing, S.L.; Valdes, P.J.</b> (2024). A 485-million-year history of Earth’s surface temperature. <i>Science (Wash.) 385(6715)</i>: eadk3705. <a href=\"https://dx.doi.org/10.1126/science.adk3705\" target=\"_blank\">https://dx.doi.org/10.1126/science.adk3705</a>","BEntID":393593,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 385(6715)</i>: eadk3705. <a href=\"https://dx.doi.org/10.1126/science.adk3705\" target=\"_blank\">https://dx.doi.org/10.1126/science.adk3705</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Judd, E.J.; Tierney, J.E.; Lunt, D.J.; Montañez, I.P.; Huber, B.T.; Wing, S.L.; Valdes, P.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Judd, E.J. <i>et al.</i>","Englishabstract":"A long-term record of global mean surface temperature (GMST) provides critical insight into the<br>dynamical limits of Earth’s climate and the complex feedbacks between temperature and the<br>broader Earth system. Here, we present PhanDA, a reconstruction of GMST over the past 485 million<br>years, generated by statistically integrating proxy data with climate model simulations. PhanDA<br>exhibits a large range of GMST, spanning 11° to 36°C. Partitioning the reconstruction into climate<br>states indicates that more time was spent in warmer rather than colder climates and reveals<br>consistent latitudinal temperature gradients within each state. There is a strong correlation between<br>atmospheric carbon dioxide (CO<sub>2</sub>) concentrations and GMST, identifying CO<sub>2</sub> as the dominant control on variations in Phanerozoic global climate and suggesting an apparent Earth system sensitivity of ~8°C.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A 485-million-year history of Earth’s surface temperature","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-22 01:32:39.811217","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2024,"MonPub":null,"DateUpdate":"2024-09-23","DateCreate":"2024-09-23","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1126/science.adk3705"},"refs":null,"anarec":{"AnaID":395805,"PubliDate":2024,"Pagination":"eadk3705","XtraPublOfAnaID":null,"ISBN":null,"Volume":"385","Issue":"6715","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43776,"SerRR":"Science (Washington). American Association for the Advancement of Science: New York, N.Y.  ISSN 0036-8075; e-ISSN 1095-9203","StandardTitleSer":"Science (Washington)","ISSN":"0036-8075","AbbrevSer":"Science (Wash.)","StandardTitleMon":null,"StartPage":null,"Pages":null,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":[{"XBRefID":395804,"RefStrFull":"<b>Mills, B.J.W.</b> (2024). Hot and cold Earth through time. <i>Science (Wash.) 385(6715)</i>: 1276-1278. <a href=\"https://dx.doi.org/10.1126/science.ads1526\" target=\"_blank\">https://dx.doi.org/10.1126/science.ads1526</a>","RelID":4,"RelationY":"Related to","StandardTitle":"Hot and cold Earth through 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