{"refrec":{"BRefID":353108,"RR":"<b>Iakovleva, A.I.; Quesnel, F.; Dupuis, C.</b> (2021). New insights on the Late Paleocene - Early Eocene dinoflagellate cyst zonation for the Paris and Dieppe basins. <i>Bull. Soc. Géol. Fr. 192</i>: 44. <a href=\"https://dx.doi.org/10.1051/bsgf/2021035\" target=\"_blank\">https://dx.doi.org/10.1051/bsgf/2021035</a>","BEntID":350817,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Bull. Soc. Géol. Fr. 192</i>: 44. <a href=\"https://dx.doi.org/10.1051/bsgf/2021035\" target=\"_blank\">https://dx.doi.org/10.1051/bsgf/2021035</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Iakovleva, A.I.; Quesnel, F.; Dupuis, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Iakovleva, A.I.; Quesnel, F.; Dupuis, C.","Englishabstract":"The Anglo-Belgo-Paris Basin, historical cradle of the Paleogene stratigraphy since the 19th century, is known by the presence of very specific so-called “Sparnacian” deposits (very diverse and laterally highly variable, predominantly lagoonal to terrestrial facies), which encompass the short stratigraphic interval of the Paleocene-Eocene Thermal Maximum (PETM). Due to the insufficient nature of the paleontological record, the “Sparnacian” succession of the Paris and Dieppe-Hampshire basins still needs to be robustly chronostratigraphically correlated with other Paleogene records worldwide. In order to refine the stratigraphy of the Thanetian-Lower Ypresian succession in northern France a number of cores and outcrop sections have been investigated palynologically. As a result, an updated version of the dinoflagellate cyst zonation for the Paris and Dieppe basins is proposed and contains six new or revised biozones for this stratigraphical interval: <i>Alisocysta margarita</i>, <i>Apectodinium hyperacanthum</i>, <i>Apectodinium</i>-acme, <i>Biconidinium longissimum</i>-acme, <i>Dracodinium astra</i>, and <i>Axiodinium lunare</i>/<i>Stenodinium meckelfeldense</i>. Based on combined bio-, litho- and chemostratigraphic data, it appears that the dinocyst assemblages, corresponding to the PETM event interval (“Sparnacian” deposits, Soissonnais and upper Mortemer formations), are characterized by an acme of <i>Apectodinium</i> spp. (70–98%) in both basins, sometimes alternating with an acme of a few gonyaulacoid groups in the Dieppe Basin. Dinocyst assemblages from the PETM interval contain a significant number of atypical, longer specimens of <i>Apectodinium parvum</i>, which could represent an ecological onshore substitute for <i>Axiodinium augustum</i> in the Paris and Dieppe-Hampshire basins. The establishment of a new <i>Biconidinium longissimum</i>-acme Zone suggests that the stratigraphic hiatus previously inferred within this sequence in the Paris Basin does not exist.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"New insights on the Late Paleocene - Early Eocene dinoflagellate cyst zonation for the Paris and Dieppe basins","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-26 01:32:09.578696","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"dinoflagellate cysts; Late Paleocene; Early Eocene; \"Sparnacian\"; zonation; Paris and Dieppe-Hampshire basins","OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2022-06-29","DateCreate":"2022-06-28","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000708645900005","VABBcode":null,"OpenAcc":1,"DOI":"10.1051/bsgf/2021035"},"refs":null,"anarec":{"AnaID":353108,"PubliDate":2021,"Pagination":"44","XtraPublOfAnaID":null,"ISBN":null,"Volume":"192","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":42477,"SerRR":"Bulletin de la Société Géologique de France. 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