{"refrec":{"BRefID":220716,"RR":"<b>Kennedy, W.J.</b> (1993). Campanian and Maastrichtian ammonites from the Mons Basin and adjacent areas (Belgium). <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 63</i>: 99-131","BEntID":212449,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 63</i>: 99-131","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kennedy, W.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kennedy, W.J.","Englishabstract":"Upper Cretaceous chalks of the Mons Basin and adjacent areas in Belgium have yielded small but stratigraphically significant ammonite assemblages, as has the reworked basal conglomerate of the succeeding Palaeocene Tuffeau de Ciply. Twenty two species are described on the basis of specimens housed in the collections of the Institut Royal des Sciences Naturelles de Belgique, Brussels. They indicate Campanian and Lower Maastrichtian ages that are compatible with the belemnite and foraminiferal evidence of ROBASZYNSKI & CHRISTENSEN (1989). Of great interest is the presence of three <i>Baculites</i> species previously known only from the United States Western Interior, where they are upper Lower Campanian and Lower Maastrichtian zonal indicators.","AbstractOtherLang":"En Belgique, dans la Bassin de Mons et les régions avoisinantes, les craies du Crétacé Supérieur ainsi que le conglomérat basai remanié du Tuffeau de Ciply sus-jacent ont livré des assemblages pauvres en espèces, mais à valeur stratigraphique importante. Vingt et une espèce sont décrites sur base de spécimens conservés dans les collections de l'Institut Royal des Sciences Naturelles de Belgique à Bruxelles. Elles indiquent des âges Campanien et Maastrichtien inférieur, en accord avec les conclusions de ROBASZYNSKI & CHRISTENFENSEN (1989) basées sur l'étude des bélemnites et des forminifères. La présence de trois espèces de <i>Baculites</i> est d'un grand intérêt car cellesci n'étaient jusqu'à présent connues que dans le \"Western Interior\" des Etats-Unis où elles caractérisent la partie supérieure du Campanien inférieur et le Maastrichtien inférieur.","BibLvlCode":"AS","StandardTitle":"Campanian and Maastrichtian ammonites from the Mons Basin and adjacent areas (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":"Cephalopods: Ammonites, Taxonomy; Upper Cretaceous; Belgium; Taxinomie; Crétacé supérieur; Belgique ","OtherDescriptors":null,"Notes":null,"AnaPub":1993,"MonPub":null,"DateUpdate":"2015-09-04","DateCreate":"2012-12-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":220716,"PubliDate":1993,"Pagination":"99-131","XtraPublOfAnaID":null,"ISBN":null,"Volume":"63","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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