@article{MTMT:1203330, title = {Enantiornithine bird remains from the Late Cretaceous of Hungary}, url = {https://m2.mtmt.hu/api/publication/1203330}, author = {Ősi, Attila}, journal-iso = {ORYCTOS}, journal = {ORYCTOS}, volume = {7}, unique-id = {1203330}, issn = {1290-4805}, year = {2008}, pages = {55-60}, orcid-numbers = {Ősi, Attila/0000-0003-2967-997X} } @{MTMT:2470274, title = {Non-avian theropod dinosaur remains from the Upper Cretaceous (Santonian) Csehbánya Formation (Iharkút, Bakony Mountains, western Hungary)}, url = {https://m2.mtmt.hu/api/publication/2470274}, author = {Ősi, Attila and Apesteguía, S}, booktitle = {6th Meeting of the European Association of Vertebrate Palaeontologist}, unique-id = {2470274}, year = {2008}, pages = {78-79}, orcid-numbers = {Ősi, Attila/0000-0003-2967-997X} } @article{MTMT:2112410, title = {A new bothremydid (Chelonia: Pleurodira) fossil assemblage from the Late Cretaceous (Santonian) of Hungary - Additional studies in the historical paleobiogeography of Late Cretaceous bothremydids}, url = {https://m2.mtmt.hu/api/publication/2112410}, author = {Rabi, Márton and Botfalvai, Gábor}, journal-iso = {HANTKENIANA}, journal = {HANTKENIANA}, volume = {5}, unique-id = {2112410}, issn = {1219-3933}, abstract = {At the only Late Cretaceous (Santonian) dinosaur locality of Hungary in the Bakony Mountains (Iharkút locality) turtle remains are the most abundant fossils and because, of their preservation they are also the best represented group so far. Since 2000 three partial skulls, two isolated lower jaws, several hind limbs, two partial plastrons, numerous shell fragments and other postcranial bones have been discovered. The skulls and the lower jaws belong to a presently unnamed new bothremydid taxon while the identification of the isolated postcranial material is in progress. The Iharkút bothremydid is a new taxon and a member of the so-called Bothremys-group. According to a preliminary cladistir analysis this is the sister taxon of Foxemys mechinorum from the Late Cretaceous deposits of southern France. The newly discovered material suggests that members of the Bothremys-group First appeared in the Mediterraneum and the appearance of bothmemydids in North America at the same period can be explained by a sudden migrational event from Europe.}, keywords = {Europe; Hungary; taxonomy; Eurasia; Central Europe; paleoecology; cladistics; turtle; fossil assemblage; Dinosauria; PALEOBIOGEOGRAPHY; Santonian; Testudines; Pleurodira; Bothremydidae}, year = {2006}, pages = {61-65}, orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036} } @article{MTMT:1236932, title = {Mesozoic plate tectonic reconstruction of the carpathian region}, url = {https://m2.mtmt.hu/api/publication/1236932}, author = {Csontos, L and Vörös, Attila}, doi = {10.1016/j.palaeo.2004.02.033}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {210}, unique-id = {1236932}, issn = {0031-0182}, abstract = {Palaeomagnetic, palaeobiogeographic and structural comparisons of different parts of the Alpine-Carpathian region suggest that four terranes comprise this area: the Alcapa, Tisza, Dacia and Adria terranes. These terranes are composed of different Mesozoic continental and oceanic fragments that were each assembled during a complex Late Jurassic-Cretaceous Palaeogene history. Palaeomagnetic and tectonic data suggest that the Carpathians are built up by two major oroclinal bends. The Alcapa bend has the Meliata oceanic unit, correlated with the Dinaric Vardar ophiolite, in its core. It is composed of the Western Carpathians, Eastern Alps and Southern Alcapa units (Transdanubian Range, Bukk). This terrane finds its continuation in the High Karst margin of the Dinarides. Further elements of the Alcapa terrane are thought to be derived from collided microcontinents: Czorsztyn in the N and a carbonate unit (Tisza?) in the SE. The Tisza-Dacia bend has the Vardar oceanic unit in its core. It is composed of the Bihor and Getic microcontinents. This terrane finds its continuation in the Serbo-Macedonian Massif of the Balkans. The Bihor-Getic microcontinent originally laid east of the Western Carpathians and filled the present Carpathian embayment in the Late Palaeozoic-Early Mesozoic. The Vardar ocean occupied an intermediate position between the Western Carpathian-Austroalpine-Transdanubian-High Karst margin and the Bihor-Getic-Serbo-Macedonian microcontinent. The Vardar and Pindos oceans were opened in the heart of the Mediterranean-Adriatic microcontinent in the Late Permian-Middle Triassic. Vardar subducted by the end of Jurassic, causing the Bihor-Getic-Serbo-Macedonian microcontinent to collide with the internal Dinaric-Western Carpathian margin. An external Penninic-Vahic ocean tract began opening in the Early Jurassic, separating the Austroalpine-Western Carpathian microcontinent (and its fauna) from the European shelf. Further east, the Severin-Ceahlau-Magura also began opening in the Early Jurassic, but final separation of the Bihor-Getic ribbon (and its fauna) from the European shelf did not take place until the late Middle Jurassic. The Alcapa and the Tisza-Dacia were bending during the Albian-Maastrichtian. The two oroclinal bends were finally opposed and pushed into the gates of the Carpathian embayment during the Palaeogene and Neogene. At that time, the main NS shortening in distant Alpine and Hellenic sectors was linked by a broader right-lateral shear zone along the former Vardar suture. (C) 2004 Elsevier B.V. All rights reserved.}, year = {2004}, eissn = {1872-616X}, pages = {1-56} }