{"refrec":{"BRefID":391405,"RR":"<b>De Vleeschouwer, D.; Percival, L.M.E.; Wichern, N.M.A.; Batenburg, S.J.</b> (2024). Pre-Cenozoic cyclostratigraphy and palaeoclimate responses to astronomical forcing. <i>Nat. Rev. Earth Environ. 5(1)</i>: 59-74. <a href=\"https://dx.doi.org/10.1038/s43017-023-00505-x\" target=\"_blank\">https://dx.doi.org/10.1038/s43017-023-00505-x</a>","BEntID":389152,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Nat. Rev. Earth Environ. 5(1)</i>: 59-74. <a href=\"https://dx.doi.org/10.1038/s43017-023-00505-x\" target=\"_blank\">https://dx.doi.org/10.1038/s43017-023-00505-x</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"De Vleeschouwer, D.; Percival, L.M.E.; Wichern, N.M.A.; Batenburg, S.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"De Vleeschouwer, D. <i>et al.</i>","Englishabstract":"Astronomical insolation forcing is well established as the underlying metronome of Quaternary ice ages and Cenozoic climate changes. Yet&nbsp;its effects on earlier eras (Mesozoic, Palaeozoic and pre-Cambrian) are less understood. In this Review, we explore how cyclostratigraphy can help to distinguish climate modes over the pre-Cenozoic era and aid our understanding of climate responses to astronomical forcing over geological time. The growing uncertainties with geologic age mean that pre-Cenozoic astronomical solutions cannot be used as tuning targets. However, they can be used as metronomes to identify the pacing of distinct climate states. Throughout the pre-Cenozoic, global average temperature differences between climate states were even more extreme (5–32 °C) than in the Cenozoic (14–27 °C), and these, combined with an evolving biosphere and changing plate tectonics, led to distinct Earth-system responses to astronomical forcing. The late Palaeozoic icehouse, for example, is characterized by a pronounced response to eccentricity, caused by nonlinear cryosphere and carbon-cycle behaviour. By contrast, the Devonian warmhouse and the Late Cretaceous hothouse featured recurrent episodes of marine anoxia that may have been paced by astronomical forcing. Formally defining 405,000-year eccentricity cycles as chronostratigraphic units (astrochronozones) throughout the Phanerozoic eon will enable a more comprehensive understanding of how astronomical forcing has shaped Earth’s climate over geologic time.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Pre-Cenozoic cyclostratigraphy and palaeoclimate responses to astronomical forcing","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-20 01:33:10.705624","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2024,"MonPub":null,"DateUpdate":"2024-03-26","DateCreate":"2024-03-26","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:001134921800001","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s43017-023-00505-x"},"refs":null,"anarec":{"AnaID":391405,"PubliDate":2024,"Pagination":"59-74","XtraPublOfAnaID":null,"ISBN":null,"Volume":"5","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":329518,"SerRR":"Nature Reviews Earth & Environment. 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