{"refrec":{"BRefID":295919,"RR":"<b>de Winter, N.J.; Zeeden, C.; Hilgen, F.J.</b> (2014). Low-latitude climate variability in the Heinrich frequency band of the Late Cretaceous greenhouse world. <i>Clim. Past 10(3)</i>: 1001-1015. <a href=\"https://dx.doi.org/10.5194/cp-10-1001-2014\" target=\"_blank\">https://dx.doi.org/10.5194/cp-10-1001-2014</a>","BEntID":288007,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Clim. Past 10(3)</i>: 1001-1015. <a href=\"https://dx.doi.org/10.5194/cp-10-1001-2014\" target=\"_blank\">https://dx.doi.org/10.5194/cp-10-1001-2014</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"de Winter, N.J.; Zeeden, C.; Hilgen, F.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"de Winter, N.J. <i>et al.</i>","Englishabstract":"Deep marine successions of early Campanian age from DSDP (Deep Sea Drilling Project) site 516F drilled at low paleolatitudes in the South Atlantic reveal distinct sub-Milankovitch variability in addition to precession, obliquity and eccentricity-related variations. Elemental abundance ratios point to a similar climatic origin for these variations and exclude a quadripartite structure as an explanation for the inferred semi-precession cyclicity in the magnetic susceptibility (MS) signal as observed in the Mediterranean Neogene for precession-related cycles. However, semi-precession cycles as suggested by previous work are likely an artifact reflecting the first harmonic of the precession signal. The sub-Milankovitch variability, especially in MS, is best approximated by a similar to 7 kyr cycle as shown by spectral analysis and bandpass filtering. The presence of sub-Milankovitch cycles with a period similar to that of Heinrich events of the last glacial cycle is consistent with linking the latter to low-latitude climate change caused by a non-linear response to precession-induced variations in insolation between the tropics.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Low-latitude climate variability in the Heinrich frequency band of the Late Cretaceous greenhouse world","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:32:04.270074","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2014,"MonPub":null,"DateUpdate":"2018-06-08","DateCreate":"2018-05-15","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000338761600006","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/cp-10-1001-2014"},"refs":null,"anarec":{"AnaID":295919,"PubliDate":2014,"Pagination":"1001-1015","XtraPublOfAnaID":null,"ISBN":null,"Volume":"10","Issue":"3","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":220505,"SerRR":"Climate of the Past. 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