{"refrec":{"BRefID":223779,"RR":"<b>Loboziak, S.; Streel, M.; Vanguestaine, M.</b> (1983). Miospores et acritarches de la formation d'Hydrequent (Frasnien superieur à Famennien Inferieur, Boulonnais, France). <i>Ann. Soc. géol. Belg. (1968) 106(1)</i>: 173-183","BEntID":215502,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Ann. Soc. Géol. Belg. (1968) 106(1)</i>: 173-183","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Loboziak, S.; Streel, M.; Vanguestaine, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Loboziak, S. <i>et al.</i>","Englishabstract":"The upper part of the Hydrequent Shales, which are inserted between the last dolomite layer and the Ste Godeleine Sandstone, consists of at least 20 m of shaly sediments with thin sandy partings. The 44 samples studied have yielded numerous spore and acritarch species which permit a very detailed palynological zonation to be established, mainly corresponding to the upper Frasnian. The highest samples, 0.5 m below the Ste Godeleine Sandstone, can be correlated with the lower Famennian of the Belgian stratotype. The Frasnian-Famennian boundary thus falls within the Hydrequent Shales between 0.5 and 2.5 m below the Ste Godeleine Sandstone.","AbstractOtherLang":"La partie supérieure des Schistes d'Hydrequent, comprise entre le dernier banc dolomitique et les Grès de Ste Godeleine, est constituée d'au moins 20 mètres de sédiments schisteux, à fines passées plus gréseuses. Dans les 44 échantillons étudiés, un grand nombre d'espèces de spores et des acritarches ont été identifiés. Ils permettent l'élaboration d'une très fine zonation palynologique presqu'entièrement située dans le Frasnien supérieur. Les échantillons les plus supérieurs, 0 m 50 sous la base des Grès de Ste Godeleine, peuvent être corrélés avec certitude avec le Famennien inférieur de la coupe-type en Belgique ; la limite Frasnien/Famennien se place dans les Schistes d'Hydrequent entre 0 m 50 et 2 m 50 sous la base des Grès de Ste Godeleine.","BibLvlCode":"AS","StandardTitle":"Miospores et acritarches de la formation d'Hydrequent (Frasnien superieur à Famennien Inferieur, Boulonnais, France)","OrigTitleLangCode":"fr","OrigTitleLangCodeExtended":"fre","OrigTitleLangID":22,"DateLastModified":{"date":"2026-04-24 01:31:58.608245","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1983,"MonPub":null,"DateUpdate":"2014-09-05","DateCreate":"2013-03-21","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":223779,"PubliDate":1983,"Pagination":"173-183","XtraPublOfAnaID":null,"ISBN":null,"Volume":"106","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45503,"SerRR":"Annales de la Société géologique de Belgique. 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