{"refrec":{"BRefID":233836,"RR":"<b>Marquet, R.</b> (2004). Ecology and evolution of Pliocene bivalves from the Antwerp Basin. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 74 suppl</i>: 205-212","BEntID":225521,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 74 suppl</i>: 205-212","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Marquet, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Marquet, R.","Englishabstract":"The dock construction works in the port of Antwerp at Doel and Kallo (prov. Oost-Vlaanderen, Belgium) have allowed the collection of a rich and diverse Pliocene bivalve fauna. It contains 182 taxa, 178 species and four subspecies. 90 species out of 178 (51%) are extinct. The rate of extinction does not significantly vary between the recognised strata, ranging from Lower to Upper Pliocene. The average longevity of the species is calculated at 10.7 Ma. This long range makes most of these bivalve species unfit for use in Neogene stratigraphy. The bathymetry of the different levels of the Pliocene is assessed, using the species still occurring in the Recent fauna (49% of the total number): it decreases towards the end of the Pliocene.","AbstractOtherLang":"Les travaux de construction des docks dans le port d'Anvers à Doel et à Kallo (prov, Oost-Vlaanderen, Belgique) ont permis de récolter une faune de bivalves pliocenes riche et diverse. Elle contient 182 taxa, 178 espèces et quatre sous-espèces dont 90 espèces (51 %) sont éteintes. Le pourcentage d'extinction ne varie pas de façon significative entre les différents niveaux reconnus, qui datent du Pliocène inférieur au Pliocène supérieur. La longévité moyenne des espèces est de 10,7 millions d'années. Cette longue distribution dans le temps rend impossible d'utiliser la plupart des espèces de bivalves pour la biostratigraphie du Néogène. La bathymétrie des niveaux pliocenes est calculée, en utilisant les taxa encore présents dans la faune Récente (49% du nombre total): elle diminue vers la fin du Pliocène.","BibLvlCode":"AS","StandardTitle":"Ecology and evolution of Pliocene bivalves from the Antwerp Basin","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":"Stratigraphic range, Bathymetry, Pliocene, Bivalves","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2014-02-25","DateCreate":"2014-02-25","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":233836,"PubliDate":2004,"Pagination":"205-212","XtraPublOfAnaID":null,"ISBN":null,"Volume":"74 suppl","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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