{"refrec":{"BRefID":249769,"RR":"<b>Christensen, W.K.</b> (1999). Upper Campanian and Lower Maastrichtian belemnites from the Mons Basin, Belgium. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 69</i>: 97-131","BEntID":241468,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 69</i>: 97-131","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Christensen, W.K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Christensen, W.K.","Englishabstract":"Upper Campanian <i>Belemnitella</i> and Lower Maastrichtian <i>Belemnella</i> and <i>Belemnitella</i> faunas from the chalks of the Mons Basin in Belgium are described, utilizing univariate and bivariate biométrie analyses. The Upper Campanian belemnite faunas comprise six taxa of Belemnitella, including two left in open nomenclature: <i>B. mucronata, B. woodi, B. minor</i> I, <i>B. minor</i> II, <i>B</i>. sp. 1 and <i>B</i>. sp. 2. The lower Lower Maastrichtian fauna includes <i>Belemnella (Pachybelemnella) obtusa</i> with subordinate <i>Belemnitella minor</i> II and <i>belemnitella pulchra</i>. The Upper Campanian and Lower Maastrichtian lithostratigraphical formations are placed in the international stratigraphical framework on the basis of the belemnite faunas. The Upper Campanian chalks are subdivided into four <i>Belemnitella</i> zones, and these are in ascending order: the lower Upper Campanian <i>B. mucronata</i> Zone below and <i>B. woodi</i> Zone above, in addition to the upper Upper Campanian <i>B. minor</i> I Zone below and <i>B. minor</i> II Zone above. These zones are proposed as formal zones, because they have been recognized in widely spaced areas in northwest Europe. The Craie Phosphatée de Ciply is placed in the <i>Belemnella obtusa/Belemnitella minor</i> II Zone, which is from the upper part of the lower Lower Maastrichtian.","AbstractOtherLang":"Les faunes de <i>Belemnitella</i> du Campanien supérieur et de <i>Belemnella</i> et <i>Belemnitella</i> du Maastrichticn inférieur, provenant des craies du Basin de Mons, sont décrites sur base d'analyses biométriques univariées et bivariées. Les faunes de bélemnites du Campanien supérieur incluent six taxa, dont deux laissés en nomenclature ouverte, appartenant au genre <i>Belemnitella</i>: <i>B. mucronata, B. woodi, B. minor</i> I, <i>B. minor</i> II, <i>Belemnitella</i> sp. 1 and <i>belemnitella</i> sp. 2. La faune de la partie inférieure du Maastrichtien inférieure comprend <i>belemnella (Pachybelemnella) obtusa</i> et, accessoirement, <i>Belemnitella minor</i> II et <i>B. pulchra</i>. Les formations du Campanien supérieur et Maastrichtien inférieur sont situées dans le tableau stratigraphique international sur base des faune de bélemnites. Les craies du Campanien supérieur sont subdivisées en quatre zones à <i>Belemnitella</i> qui sont en ordre ascendant: les zones à <i>B. mucronata</i> et <i>B. woodi</i> de la partie inférieure du Campanien supérieur et les zones <i>B. minor</i> I et <i>B. minor</i> II de la partie supérieure du Campanien supérieur. Ces zones sont proposées comme zones formelles car elles ont été reconnues dans des aires largement distantes les unes des autres dans le nord-ouest de l'Europe. La Craie Phosphatée de Ciply appartient à la zone à <i>Belemnella obtusa/Belemnilella minor</i> II qui fait partie du sommet de la partie supérieure du Maastrichtien inférieur.","BibLvlCode":"AS","StandardTitle":"Upper Campanian and Lower Maastrichtian belemnites from the Mons Basin, Belgium","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Belemnitellids, taxonomy, stratigraphy, Upper Campanian, Lower Maastrichtian, Mons Basin, Belgium, Bélemnitellidés, taxinomie, stratigraphie, Campanien supérieur- Maastrichtien inférieur, Basin de Mons, Belgique","OtherDescriptors":null,"Notes":null,"AnaPub":1999,"MonPub":null,"DateUpdate":"2015-09-08","DateCreate":"2015-09-08","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":249769,"PubliDate":1999,"Pagination":"97-131","XtraPublOfAnaID":null,"ISBN":null,"Volume":"69","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":64308,"SerRR":"Bulletin van het Koninklijk Belgisch Instituut voor Natuurwetenschappen. 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