{"refrec":{"BRefID":203037,"RR":"<b>Nolf, D.; Cappetta, H.</b> (1988). Otolithes de poissons pliocènes du sud-est de la France. <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 58</i>: 209-271","BEntID":195264,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Bull. Kon. Belg. Inst. Natuurwet. Aardwet. = Bull. - Inst. r. sci. nat. Belg., Sci. Terre 58</i>: 209-271","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Nolf, D.; Cappetta, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Nolf, D.; Cappetta, H.","Englishabstract":"Otoliths collected from nine localities in the Lower and Middle Pliocene blue marls of southern France revealed the presence of 118 teleost taxa, including 80 named species. Three new species are introduced: <i>Pseudophichthys escaravatierensis</i>, \"genus Bythitinorum\" <i>vonhachti</i> and <i>Cepola neogenica</i>. The associations studied belong to five different biozones of planktonic foraminifera in the Lower and Middle Pliocene. The relationships of these Pliocene teleost faunas to the Tortonian and Recent Mediterranean faunas are analysed. Because major problems exist in matching otolith-based species with those erected for osteological material from Messinian localities, our comparisons are based exclusively on data obtained from the otoliths. Fifty of our 80 identified species appear only in the Pliocene. This indicates that at the beginning of the Piocene, the Mediterranean realm was subject to extensive faunal replacement. All the studied associations indicate higher temperatures than those of the present day Mediterranean. In the studied area, the associations from the basal Pliocene (<i>Spaeroidinellopsis</i> Acme-zone) at Saint-Martin-du-Var clearly indicate a bathyal environment, corresponding to depths of 300-500 m or even more. Ascending the stratigraphic column, the successive associations in the Pliocene rias of Southeastern France indicate decreasing depths, corresponding to the progressive filling of these basins. In the studied area, data on the teleosts of the terminal Pliocene are lacking, but faunas of this age are known from Southern Italy. They show that the Paleomediterranean fauna, which was substantially modified at the beginning of the Pliocene, appears near the end of this period as a warm water fauna, trapped in a basin where deterioration of climatic conditions led progressively to extinction. The Recent bathyal fauna of the Mediterranean appears extremely impoverished, but the littoral fauna conserves certain aspects of warmer waters, as is apparent in the prolific evolution of gobiids, labrids and blenniids.","AbstractOtherLang":"L'étude des otolithes provenant de neuf gisements situés dans les marnes bleues du Pliocène inférieur et moyen du Sud-Est de la France a permis d'identifier 118 taxa de téléostéens dont 80 espèces nominales. Parmi ces dernières, trois sont nouvelles: <i>Pseudophichthys escaravatierensis</i>, \"genus Bythitinorum\" <i>vonhachti</i> et <i>Cepola neogenica</i>. Les gisements se répartissent dans cinq biozones de foraminifères planctoniques successives, du Pliocène inférieur à moyen. Les rapports des faunes de téléostéens pliocènes avec celles du Tortonien et de la Méditerranée actuelle sont analysés. En raison des nombreux problèmes qui subsistent dans la mise en synonymie de faunes établies sur des otolithes et celles établies sur des squelettes dans des gisements messiniens, notre analyse est exclusivement basée sur des données obtenues à partir des otolithes. Cinquante des 80 espèces nominales identifiées n'apparaissent qu'au Pliocène; il faut donc conclure à un très important renouvellement de la faune méditerranéenne au début du Pliocène. Toutes les associations étudiées indiquent une faune d'eaux plus chaudes que celles de la Méditerranée actuelle. Dans la région étudiée, l'association du Pliocène basai (acmé à <i>Sphaeroidinellopsis</i>) de Saint-Martin-du-Var a livré une association franchement bathyale, correspondant à un environnement situé entre 300 et 500 m de profondeur, ou même plus. A mesure que l'on monte dans la stratigraphie, des associations indiquant des environnements de moins en moins profonds se succèdent dans les rias pliocènes du sud-est de la France, ce qui correspond au comblement progressif de ces bassins. On ne possède pas de données sur les faunes ichthyologiques du Pliocène terminal ou du Pleistocène dans la région étudiée, mais en Italie méridionale, des faunes de cet âge sont connues. Elles nous apprennent que la faune subtropicale paléoméditerranéenne, modifiée profondément au début du Pliocène, se présente vers la fin de cette époque comme une faune d'eau chaude piégée dans un bassin où la détérioration des conditions climatiques conduit progressivement à sa disparition. La faune bathyale actuelle de la Méditerranée apparaît comme extrêmement appauvrie, mais la faune littorale garde certains aspects d'une faune d'eaux plus chaudes, comme en témoigne l'évolution prolifique des gobiidés, labridés et blenniidés.","BibLvlCode":"AS","StandardTitle":"Otolithes de poissons pliocènes du sud-est de la France","OrigTitleLangCode":"fr","OrigTitleLangCodeExtended":"fre","OrigTitleLangID":22,"DateLastModified":{"date":"2025-07-02 08:33:14.980000","timezone_type":1,"timezone":"+00:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"teleostean fishes, Pliocene, Paleomediterranean, poissons téléostéens, Pliocène, Paléoméditerranée","OtherDescriptors":null,"Notes":null,"AnaPub":1988,"MonPub":null,"DateUpdate":"2015-09-02","DateCreate":"2011-03-02","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":203037,"PubliDate":1988,"Pagination":"209-271","XtraPublOfAnaID":null,"ISBN":null,"Volume":"58","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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