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The Hadim Nappe which is one of the allochthonous tectonic units in the Tauride Belt includes continuous stratigraphic successions from Middle(?)-Late Devonian to Late Cretaceous. The well exposed successions of the Moscovian to lower Kasimovian are selected for fusulinid biostratigraphy along three sections (Yassıpınar, Gölbelen and Bademli) in the Central Taurides. The Lower-Middle Pennsylvanian boundary was determined by the first appearance datum of the Aljutovella aljutovica (Rauzer-Chernousova, 1938) and Solovievaia ovata ovata (Rauzer-Chernousova, 1938). In this study, the Vereian, Kashirian, Podolskian and Myachkovian regional substages of the Moscovian stage were determined by Aljutovella aljutovica-Solovievaia ovata ovata, Aljutovella priscoidea (Rauzer-Chernousova, 1938), Eofusulina triangula (Rauzer-Chernousova & Belyaev inRauzer-Chernousova, Belyaev & Reitlinger, 1936), Fusulinella vozhgalensis devexa Rauzer-Chernousova inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951, Beedeina schellwieni (Staff inSchellwien & Staff, 1912) and Fusulinella bocki bockiMöller, 1878 in ascending order. The base of the lower Kasimovian is represented by the occurrence of Quasifusulinoides Rauzer-Chernousova & Rozovskaya inRauzer-Chernousova & Fursenko, 1959, ProtriticitesPutrya, 1948 and MontiparusRozovskaya, 1948 taxa. A total of 106 fusulinid species belonging to 19 genera were determined. One genus and ten species are new: Aljutovella typica Akbaş, n. sp., Beedeina minuta Akbaş, n. sp., Beedeina tauridiana Akbaş, n. sp., Praefusulinella guvenci Akbaş, n. gen., n. sp., Praefusulinella okuyucui Akbaş, n. gen., n. sp., Praefusulinella rhombiforma Akbaş, n. gen., n. sp., Praefusulinella tekini Akbaş, n. gen., n. sp., Fusulinella absoluta Akbaş, n. sp., Fusulinella obtusa minuta Akbaş, n. subsp. and Fusulinella propriaforma Akbaş, n. sp. The taxonomic positions of some fusulinids species (e.g., Neostaffella larionovae polasnensis (Rauzer-Chernousova & Safonova inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951), Depratina chernovi (Rauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951), Solovievaia arta (Leontovich inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951) and Beedeina paradistenta (Safonova inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951) were revised. The fusulinid assemblages recovered in this study correlate well with the Russian Platform, Cantabrian Mountains, Central Iran, southern Urals, Donets Basin, and some other regions of the Tethyan Realm.
Biostratigraphie des fusulinidés du Moscovien-Kasimovien inférieur de la nappe de Hadim, Taurides centrales, sud de la Turquie.
La nappe de Hadim, qui est l'une des unités tectoniques allochtones de la ceinture des Taurides, comprend des successions stratigraphiques continues du Dévonien moyen(?)-supérieur au Crétacé supérieur. Les successions bien exposées du Moscovien au Kasimovien inférieur sont sélectionnées pour la biostratigraphie des fusulinidés le long de trois coupes (Yassıpınar, Gölbelen et Bademli) dans les Taurides centrales. La limite Pennsylvanien inférieur-moyen a été déterminée par la date de première apparition d'Aljutovella aljutovica (Rauzer-Chernousova, 1938) et de Solovievaia ovata ovata (Rauzer-Chernousova, 1938). Dans cette étude, les sous-étages régionaux véréien, kashirien, podolskien et myachkovien de l'étage moscovien ont été déterminés par Aljutovella aljutovica-Solovievaia ovata ovata, Aljutovella priscoidea (Rauzer-Chernousova, 1938), Eofusulina triangula (Rauzer-Chernousova & Belyaev inRauzer-Chernousova, Belyaev & Reitlinger, 1936), Fusulinella vozhgalensis devexa Rauzer-Chernousova inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951, Beedeina schellwieni (Staff inSchellwien & Staff, 1912) et Fusulinella bocki bockiMöller, 1878 en ordre croissant. La base du Kasimovien inférieur est représentée par l'occurrence des taxons Quasifusulinoides Rauzer-Chernousova & Rozovskaya inRauzer-Chernousova & Fursenko, 1959, ProtriticitesPutrya, 1948 et MontiparusRozovskaya, 1948. Un total de 106 espèces de fusulinidés appartenant à 19 genres a été déterminé. Un genre et dix espèces sont nouveaux: Aljutovella typica Akbaş, n. sp., Beedeina minuta Akbaş, n. sp., Beedeina tauridiana Akbaş, n. sp., Praefusulinella guvenci Akbaş, n. gen., n. sp, Praefusulinella okuyucui Akbaş, n. gen., n. sp., Praefusulinella rhombiforma Akbaş, n. gen., n. sp., Praefusulinella tekini Akbaş, n. gen., n. sp., Fusulinella absoluta Akbaş, n. sp, Fusulinella obtusa minuta Akbaş, n. subsp. et Fusulinella propriaforma Akbaş, n. sp. La position taxonomique de certaines espèces de fusulinidés (par exemple, Neostaffella larionovae polasnensis (Rauzer-Chernousova & Safonova inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951), Depratina chernovi (Rauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951), Solovievaia arta (Leontovich inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951) et Beedeina paradistenta (Safonova inRauzer-Chernousova, Gryzlova, Kireeva, Leontovich, Safonova & Chernova, 1951) a été révisée. Les assemblages de fusulinidés retrouvés dans cette étude sont bien corrélés avec la Plate-forme Russe, les Montagnes Cantabriques, l'Iran Central, le sud de l'Oural, le bassin de Donets et quelques autres régions de la Téthys.
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