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- W2077029429 abstract "The Upper Cretaceous (Middle Cenomanian-Coniacian) successions of the Bey Dağları Carbonate Platform (Western Taurides, SW Turkey) are represented by rudist-bearing shallow-water limestones. Four rudist lithosomes are distinguished for the first time from the Eastern, Northern and Southern Areas of the Bey Dağları Autochthon. The oldest rudist assemblages dominated by caprinids are observed in the Eastern (Katran Dağ) Area (caprinid lithosomes) and suggest a Middle-Late Cenomanian age. The uppermost part of the platform carbonates in the Northern Area is characterized by an association of hippuritid and radiolitid rudist bivalves dominated by Vaccinites praegiganteus (Toucas) (hippuritid lithosomes). The rudist fauna indicates the Late Turonian age, which is confirmed by the previously obtained 87Sr/86Sr values of well-preserved low-Mg calcite of Vaccinites praegiganteus (Toucas) shells. The rudist associations of the Southern (Susuzdağ) Area are represented by two rudist formations. The lower lithosomes are mainly made up of hippuritids and radiolitids (hippuritid-radiolitid lithosomes). The stratigraphical distributions of the species of the assemblage indicate a Santonian-Early Campanian age. The rudist associations of the upper lithosomes are dominated by species of Joufia and Gorjanovicia (Joufia-Gorjanovicia lithosomes), which suggest a Late Campanian-Maastrichtian age. Identification of the rudist lithosomes yields information on the palaeobiogeographic distribution of the rudist species in the eastern Mediterranean region and also on the biostratigraphic frame of the Upper Cretaceous successions of the Bey Dağları Carbonate Platform. Les séries d’âge crétacé supérieur (Cénomanien moyen-Coniacien) de la plate-forme carbonatée de Bey Dağları (Taurides occidentales, SO de la Turquie) sont représentées par des calcaires peu profonds à rudistes. Quatre lithosomes à rudistes sont distingués pour la première fois dans les régions autochtones Est, Nord et Sud de Bey Dağları. Les plus anciens assemblages à rudistes dominés par les caprinidés (lithosomes à caprinidés) sont observés dans la région Est (Katran Dağ) et suggèrent un âge cénomanien moyen à supérieur. La partie la plus supérieure des carbonates de plate-forme est caractérisée dans la région Nord par une association à bivalves rudistes hippuritidés et radiolitidés (lithosomes à hippuritidés) dominés par Vaccinites praegiganteus (Toucas). La faune à rudistes indique un âge turonien supérieur, confirmé par les valeurs 87Sr/86Sr obtenues précédemment sur des coquilles bien préservées en calcite faiblement magnésienne de Vaccinites praegiganteus (Toucas). Les associations à rudistes de la région Sud (Susuzdağ) sont représentées par deux formations à rudistes. Les lithosomes inférieurs sont principalement caractérisés par des hippuritidés et des radiolitidés (lithosomes à hippuritidé-radiolitidé). La distribution stratigraphique des espèces de l’assemblage indique un âge santonien à campanien inférieur. L’association à rudistes du lithosome supérieur est dominée par les espèces des genres Joufia et Gorjanovicia (lithosomes à Joufia-Gorjanovicia), ce qui suggère un âge campanien supérieur à maestrichtien. L’identification des lithosomes à rudistes fournit des informations sur la distribution paléobiogéographique des espèces de rudistes en Méditerranée occidentale et sur le canevas biostratigraphique des successions du Crétacé supérieur de la plate-forme carbonatée de Bey Dağları." @default.
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- W2077029429 date "2009-05-01" @default.
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- W2077029429 title "Upper Cretaceous rudist biostratigraphy of the Bey Dağları Carbonate Platform, Western Taurides, SW Turkey" @default.
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- W2077029429 doi "https://doi.org/10.1016/j.geobios.2008.10.006" @default.
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