@article{MTMT:3168106,
	title = {Late Cretaceous (Maastrichtian) Chondrichthyes and Osteichthyes from northeastern Iberia},
	url = {https://m2.mtmt.hu/api/publication/3168106},
	author = {Blanco, A and Szabó, Márton and Blanco-Lapaz, A and Marmi, J},
	doi = {10.1016/j.palaeo.2016.10.039},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {465},
	unique-id = {3168106},
	issn = {0031-0182},
	year = {2017},
	eissn = {1872-616X},
	pages = {278-294}
}

@article{MTMT:33257668,
	title = {A new family of teiioid lizards from the Upper Cretaceous of Romania with notes on the evolutionary history of early teiioids},
	url = {https://m2.mtmt.hu/api/publication/33257668},
	author = {Codrea, Vlad A. and Venczel, Márton and Solomon, Alexandru},
	doi = {10.1093/zoolinnean/zlx008},
	journal-iso = {ZOOL J LINN SOC-LOND},
	journal = {ZOOLOGICAL JOURNAL OF THE LINNEAN SOCIETY},
	volume = {181},
	unique-id = {33257668},
	issn = {0024-4082},
	year = {2017},
	eissn = {1096-3642},
	pages = {385-399},
	orcid-numbers = {Venczel, Márton/0000-0003-2200-3619}
}

@article{MTMT:3277587,
	title = {The continental fish fauna of the Late Cretaceous (Santonian) Iharkút locality (Bakony Mountains, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3277587},
	author = {Szabó, Márton and Ősi, Attila},
	doi = {10.1556/24.60.2017.009},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {60},
	unique-id = {3277587},
	issn = {1788-2281},
	year = {2017},
	eissn = {1789-3348},
	pages = {230-287},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:2986714,
	title = {Facies architecture and palaeoenvironmental implications of the upper Cretaceous (Santonian) Csehbánya formation at the Iharkút vertebrate locality (Bakony Mountains, Northwestern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2986714},
	author = {Botfalvai, Gábor and Haas, János and Bodor, Emese Réka and Mindszenty, Andrea and Ősi, Attila},
	doi = {10.1016/j.palaeo.2015.10.018},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {441},
	unique-id = {2986714},
	issn = {0031-0182},
	year = {2016},
	eissn = {1872-616X},
	pages = {659-678},
	orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Haas, János/0000-0003-0929-8889; Bodor, Emese Réka/0000-0003-3894-2506; Mindszenty, Andrea/0000-0001-8927-3053; Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:2951460,
	title = {Vertebrate remains from the Upper Cretaceous (Santonian) Ajka Coal Formation, western Hungary},
	url = {https://m2.mtmt.hu/api/publication/2951460},
	author = {Ősi, Attila and Bodor, Emese Réka and Makádi, László and Rabi, Márton},
	doi = {10.1016/j.cretres.2015.04.014},
	journal-iso = {CRETACEOUS RES},
	journal = {CRETACEOUS RESEARCH},
	volume = {57},
	unique-id = {2951460},
	issn = {0195-6671},
	abstract = {Vertebrate remains from the Upper Cretaceous (Santonian) Ajka Coal Formation (Bakony Mountains, western Hungary) are described. Macro- and microfossils collected from two boreholes and from isolated chunks of sediment/matrix dumped on spoil heaps of the Jókai Mine represent pycnodontiform and lepisosteiform fishes, bothremydid turtles, the mosasauroid Pannoniasaurus inexpectatus, the crocodyliforms cf. Theriosuchus, Iharkutosuchus makadii and cf. Allodaposuchus, as well as ankylosaurian and theropod dinosaurs. This unit was deposited in a swampy lacustrine environment, in contrast with the neighbouring and contemporaneous floodplain deposit of the vertebrate-bearing Csehbánya Formation at Iharkút. Despite significant environmental differences, the faunal composition of the Ajka Coal Formation assemblage completely overlaps with that of the Csehbánya Formation, suggesting the occurrence of the same semi-aquatic and terrestrial species in both settings. The ankylosaurian remains further strengthen the previous view that ankylosaurus preferred wetland habitats such as fluvial systems and coastal regions. © 2015 Elsevier Ltd.},
	keywords = {Hungary; Late cretaceous; Dinosaurs; Swampy environment; Continental vertebrates},
	year = {2016},
	eissn = {1095-998X},
	pages = {228-238},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X; Bodor, Emese Réka/0000-0003-3894-2506}
}

@article{MTMT:2999644,
	title = {Late Cretaceous (Santonian) Atractosteus (Actinopterygii, Lepisosteidae) remains from Hungary (Iharkút, Bakony Mountains)},
	url = {https://m2.mtmt.hu/api/publication/2999644},
	author = {Szabó, Márton and Gulyás, P and Ősi, Attila},
	doi = {10.1016/j.cretres.2015.12.002},
	journal-iso = {CRETACEOUS RES},
	journal = {CRETACEOUS RESEARCH},
	volume = {60},
	unique-id = {2999644},
	issn = {0195-6671},
	year = {2016},
	eissn = {1095-998X},
	pages = {239-252},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:3071287,
	title = {Late Cretaceous (Santonian) pycnodontid (Actinopterygii, Pycnodontidae) remains from the freshwater deposits of the Csehbánya Formation, (Iharkút, Bakony Mountains, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3071287},
	author = {Szabó, Márton and Gulyás, P and Ősi, Attila},
	doi = {10.1016/j.annpal.2016.04.001},
	journal-iso = {ANN PALEONTOL},
	journal = {ANNALES DE PALEONTOLOGIE},
	volume = {102},
	unique-id = {3071287},
	issn = {0753-3969},
	abstract = {Isolated but well-preserved remains of pycnodontiform fishes from the Upper Cretaceous (Santonian) Csehbánya Formation at Iharkút, western Hungary are described here. The assemblage contains cranial (premaxilla/dentary, vomers, prearticulars, teeth) and postcranial (possible contour scales) remains allowing the identification of the Iharkút pycnodontiforms as cf. Coelodus sp. Supported by sedimentological and stable isotope studies, the Iharkút fossils represent one of the few certainly freshwater occurrences of the group in the Upper Cretaceous of Europe. An estimated value of minimum number of individuals indicates that the remains of at least 28 individuals were hitherto discovered, suggesting that these medium-sized hard-shelled prey consuming fishes were quite abundant in the Iharkút freshwater habitats. © 2016 Elsevier Masson SAS.},
	keywords = {palaeoecology; Late cretaceous; Csehbanya Formation; Vomer; Pycnodontidae; Prearticular; Molariform teeth; Incisiform teeth; Coelodus},
	year = {2016},
	eissn = {1778-3666},
	pages = {123-134},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:3126163,
	title = {A new teiid lizard from the Late Cretaceous of the Haţeg Basin, Romania and its phylogenetic and palaeobiogeographical relationships},
	url = {https://m2.mtmt.hu/api/publication/3126163},
	author = {Venczel, Márton and Codrea, VA},
	doi = {10.1080/14772019.2015.1025869},
	journal-iso = {J SYST PALAEONTOL},
	journal = {JOURNAL OF SYSTEMATIC PALAEONTOLOGY},
	volume = {14},
	unique-id = {3126163},
	issn = {1477-2019},
	year = {2016},
	eissn = {1478-0941},
	pages = {219-237},
	orcid-numbers = {Venczel, Márton/0000-0003-2200-3619}
}

@CONFERENCE{MTMT:2918690,
	title = {Facies architecture and palaeoenvironment implications of the Upper Cretaceous (Santonian) Csehbánya Formation at the Iharkút vertebrate locality (Bakony Mts., Northwestern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2918690},
	author = {Botfalvai, Gábor and Haas, J and Mindszenty, A and Bodor, Emese Réka and Ősi, Attila},
	booktitle = {31st IAS Meeting of Sedimentology Abstract Volume},
	unique-id = {2918690},
	year = {2015},
	pages = {82},
	orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Bodor, Emese Réka/0000-0003-3894-2506; Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:2782588,
	title = {Taphonomic and paleoecologic investigations of the Late Cretaceous (Santonian) Iharkút vertebrate assemblage (Bakony Mts, Northwestern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2782588},
	author = {Botfalvai, Gábor and Ősi, Attila and Mindszenty, Andrea},
	doi = {10.1016/j.palaeo.2014.09.032},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {417},
	unique-id = {2782588},
	issn = {0031-0182},
	year = {2015},
	eissn = {1872-616X},
	pages = {379-405},
	orcid-numbers = {Botfalvai, Gábor/0000-0002-5479-9036; Ősi, Attila/0000-0003-2967-997X; Mindszenty, Andrea/0000-0001-8927-3053}
}

@article{MTMT:2782593,
	title = {Island life in the Cretaceous - faunal composition, biogeography, evolution, and extinction of land-living vertebrates on the Late Cretaceous European archipelago},
	url = {https://m2.mtmt.hu/api/publication/2782593},
	author = {Csiki-Sava, Z and Buffetaut, E and Ősi, Attila and Pereda-Suberbiola, X and Brusatte, SL},
	doi = {10.3897/zookeys.469.8439},
	journal-iso = {ZOOKEYS},
	journal = {ZOOKEYS},
	volume = {469},
	unique-id = {2782593},
	issn = {1313-2989},
	year = {2015},
	eissn = {1313-2970},
	pages = {1-161},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:2960986,
	title = {A new durophagous scincomorphan lizard genus from the Late Cretaceous Iharkút locality (Hungary, Bakony Mts)},
	url = {https://m2.mtmt.hu/api/publication/2960986},
	author = {Makádi, László and Nydam, RL},
	doi = {10.1007/s12542-014-0253-1},
	journal-iso = {PALAEONTOL Z},
	journal = {PALAEONTOLOGISCHE ZEITSCHRIFT},
	volume = {89},
	unique-id = {2960986},
	issn = {0031-0220},
	year = {2015},
	eissn = {1867-6812},
	pages = {925-941}
}

@article{MTMT:2960354,
	title = {An enigmatic crocodyliform tooth from the bauxites of western Hungary suggests hidden mesoeucrocodylian diversity in the Early Cretaceous European archipelago},
	url = {https://m2.mtmt.hu/api/publication/2960354},
	author = {Ősi, Attila and Rabi, Márton and Makádi, László},
	doi = {10.7717/peerj.1160},
	journal-iso = {PEERJ},
	journal = {PEERJ},
	volume = {3},
	unique-id = {2960354},
	issn = {2167-8359},
	abstract = {Background. The Cretaceous of southern Europe was characterized by an archipelago setting with faunas of mixed composition of endemic, Laurasian and Gondwanan elements. However, little is known about the relative timing of these faunal influences. The Lower Cretaceous of East-Central Europe holds a great promise for understanding the biogeographic history of Cretaceous European biotas because of the former proximity of the area to Gondwana (as part of the Apulian microcontinent). However, East-Central European vertebrates are typically poorly known from this time period. Here, we report on a ziphodont crocodyliform tooth discovered in the Lower Cretaceous (Albian) Alsopere Bauxite Formation of Olaszfalu, western Hungary. Methods. The morphology of the tooth is described and compared with that of other similar Cretaceous crocodyliforms. Results. Based on the triangular, slightly distally curved, constricted and labiolingually flattened crown, the small, subequal-sized true serrations on the carinae mesially and distally, the longitudinal fluting labially, and the extended shelves along the carinae lingually the tooth is most similar to some peirosaurid, non-baurusuchian sebecosuchian, and uruguaysuchid notosuchians. In addition, the paralligatorid Wannchampsus also possesses similar anterior teeth, thus the Hungarian tooth is referred here to Mesoeucrocodylia indet. Discussion. Supposing a notosuchian affinity, this tooth is the earliest occurrence of the group in Europe and one of the earliest in Laurasia. In case of a paralligatorid relationship the Hungarian tooth would represent their first European record, further expanding their cosmopolitan distribution. In any case, the ziphodont tooth from the Albian bauxite deposit of western Hungary belongs to a group still unknown from the Early Cretaceous European archipelago and therefore implies a hidden diversity of crocodyliforms in the area.},
	year = {2015},
	eissn = {2167-8359},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:2792909,
	title = {A revised Eurogondwana model: Late Cretaceous notosuchian crocodyliforms and other vertebrate taxa suggest the retention of episodic faunal links between Europe and Gondwana during most of the Cretaceous},
	url = {https://m2.mtmt.hu/api/publication/2792909},
	author = {Rabi, Márton and Sebők, N},
	doi = {10.1016/j.gr.2014.09.015},
	journal-iso = {GONDWANA RES},
	journal = {GONDWANA RESEARCH},
	volume = {28},
	unique-id = {2792909},
	issn = {1342-937X},
	year = {2015},
	eissn = {1878-0571},
	pages = {1197-1211}
}

@article{MTMT:2596650,
	title = {Cranial morphology of Theriosuchus sympiestodon (Mesoeucrocodylia, Atoposauridae) and the widespread occurrence of Theriosuchus in the Late Cretaceous of Europe},
	url = {https://m2.mtmt.hu/api/publication/2596650},
	author = {Martin, JE and Rabi, Márton and Csiki-Sava, Z and Vasile, Ş},
	doi = {10.1666/13-106},
	journal-iso = {J PALEONTOL},
	journal = {JOURNAL OF PALEONTOLOGY},
	volume = {88},
	unique-id = {2596650},
	issn = {0022-3360},
	year = {2014},
	eissn = {1937-2337},
	pages = {444-456}
}

@article{MTMT:2960980,
	title = {A new polyglyphanodontine lizard (Squamata: Borioteiioidea) from the Late Cretaceous Iharkut locality (Santonian, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2960980},
	author = {Makádi, László},
	doi = {10.1016/j.cretres.2013.08.001},
	journal-iso = {CRETACEOUS RES},
	journal = {CRETACEOUS RESEARCH},
	volume = {46},
	unique-id = {2960980},
	issn = {0195-6671},
	abstract = {In recent years the Late Cretaceous (Santonian) terrestrial vertebrate locality at Iharkut (western Hungary) has yielded well-preserved remains of lizard taxa besides the remains of fishes, amphibians, turtles, crocodiles, pterosaurs and dinosaurs. Previously the polyglyphanodontine lizard Bicuspidon aff. hatzegiensis has been reported from Iharkut. However, recent excavations at this site produced more lacertilian remains including new polyglyphanodontine material, namely a maxilla and two dentaries which suggest the presence of a new genus in the Iharkut fauna. This previously unknown lizard (described here as Distortodon rhomboideus n. g. n. sp.) is distinct from other polyglyphanodontines such as Bicuspidon, Paraglyphanodon, Polyglyphanodon, Dicothodon and Peneteius. It differs from these genera mainly in having the lingual cusp situated more distally compared to the labial one on its bicuspid teeth located in the distal part of the tooth row, thus the crowns having a unique rhomboidal shape in occlusal view. Distortodon rhomboideus further strengthens the dominance of borioteiioid lizards in the Iharkut fauna. The growing presence of borioteiioids in European localities supports previous theories which suggest some paleobiogeographic connections between the western Tethyan archipelago and North America in the Late Cretaceous. (C) 2013 Elsevier Ltd. All rights reserved.},
	year = {2013},
	eissn = {1095-998X},
	pages = {166-176}
}

@article{MTMT:2960981,
	title = {The first known chamopsiid lizard (Squamata) from the Upper Cretaceous of Europe (Csehbanya Formation; Hungary, Bakony Mts)},
	url = {https://m2.mtmt.hu/api/publication/2960981},
	author = {Makádi, László},
	doi = {10.1016/j.annpal.2013.07.002},
	journal-iso = {ANN PALEONTOL},
	journal = {ANNALES DE PALEONTOLOGIE},
	volume = {99},
	unique-id = {2960981},
	issn = {0753-3969},
	abstract = {The Upper Cretaceous (Santonian) Iharkut terrestrial vertebrate locality, in Hungary, has yielded several lacertilian taxa since its discovery in 2000. One of these is represented by a left mandible fragment and two dentary fragments. The characters observed on these remains support assignment to the family Chamopsiidae (Scincomorpha). Moreover, the remains belong to a new genus and species, Pelsochamops infrequens n. g. n. sp. Pelsochamops is the first known occurrence of chamopsiids outside North America and adds another scincomorphan lizard to the Iharkut fauna. It represents an additional evidence for dispersal routes between North America and Europe. (C) 2013 Elsevier Masson SAS. All rights reserved.},
	year = {2013},
	eissn = {1778-3666},
	pages = {261-274}
}

@article{MTMT:2359717,
	title = {The First Freshwater Mosasauroid (Upper Cretaceous, Hungary) and a New Clade of Basal Mosasauroids},
	url = {https://m2.mtmt.hu/api/publication/2359717},
	author = {Makádi, László and Caldwell, MW and Ősi, Attila},
	doi = {10.1371/journal.pone.0051781},
	journal-iso = {PLOS ONE},
	journal = {PLOS ONE},
	volume = {7},
	unique-id = {2359717},
	issn = {1932-6203},
	abstract = {Mosasauroids are conventionally conceived of as gigantic, obligatorily aquatic marine lizards (1000s of specimens from marine deposited rocks) with a cosmopolitan distribution in the Late Cretaceous (90-65 million years ago [mya]) oceans and seas of the world. Here we report on the fossilized remains of numerous individuals (small juveniles to large adults) of a new taxon, Pannoniasaurus inexpectatus gen. et sp. nov. from the Csehbanya Formation, Hungary (Santonian, Upper Cretaceous, 85.3-83.5 mya) that represent the first known mosasauroid that lived in freshwater environments. Previous to this find, only one specimen of a marine mosasauroid, cf. Plioplatecarpus sp., is known from non-marine rocks in Western Canada. Pannoniasaurus inexpectatus gen. et sp. nov. uniquely possesses a plesiomorphic pelvic anatomy, a non-mosasauroid but pontosaur-like tail osteology, possibly limbs like a terrestrial lizard, and a flattened, crocodile-like skull. Cladistic analysis reconstructs P. inexpectatus in a new clade of mosasauroids: (Pannoniasaurus (Tethysaurus (Yaguarasaurus, Russellosaurus))). P. inexpectatus is part of a mixed terrestrial and freshwater faunal assemblage that includes fishes, amphibians turtles, terrestrial lizards, crocodiles, pterosaurs, dinosaurs and birds.},
	keywords = {PHYLOGENY; phosphates; SLOVENIA; LIZARD; Dinosauria; Squamata; SPECIMEN; MOROCCO; HALISAURUS; HUNGAROSAURUS-TORMAI},
	year = {2012},
	eissn = {1932-6203},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@inbook{MTMT:1464155,
	title = {The Late Cretaceous continental vertebrate fauna from Iharkút, western Hungary: a review},
	url = {https://m2.mtmt.hu/api/publication/1464155},
	author = {Ősi, Attila and Makádi, László and Rabi, Márton and Szentesi, Zoltán and Botfalvai, Gábor and Gulyás, P},
	booktitle = {Bernissart Dinosaurs and Early Cretaceous Terrestrial Ecosystems},
	unique-id = {1464155},
	year = {2012},
	pages = {533-570},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X; Szentesi, Zoltán/0000-0002-7019-5478; Botfalvai, Gábor/0000-0002-5479-9036}
}

@article{MTMT:2523293,
	title = {Survival of Theriosuchus (Mesoeucrocodylia: Atoposauridae) in a Late Cretaceous archipelago: a new species from the Maastrichtian of Romania},
	url = {https://m2.mtmt.hu/api/publication/2523293},
	author = {Martin, JE and Rabi, Márton and Csiki, Z},
	doi = {10.1007/s00114-010-0702-y},
	journal-iso = {SCI NAT-HEIDELBERG},
	journal = {NATURWISSENSCHAFTEN},
	volume = {97},
	unique-id = {2523293},
	issn = {0028-1042},
	abstract = {Small terrestrial non-eusuchian mesoeucrocodylians are common components of Cretaceous assemblages of Gondwanan provinces with notosuchians and araripesuchids as flagship taxa in South America, Africa and Madagascar, well into the Late Cretaceous. On the other hand, these are exceedingly rare in Laurasian landmasses during the Late Cretaceous. Small terrestrial mesoeucrocodylians from Europe were often referred to the genus Theriosuchus, a taxon with stratigraphic range extending from the Late Jurassic to the late Early Cretaceous. Theriosuchus is abundantly reported from various European localities, although Asiatic and possibly North American members are also known. It has often been closely associated with the first modern crocodilians, members of the Eusuchia, because of the presence of procoelous vertebrae, a widespread key character diagnosing the Eusuchia. Nevertheless, the relationships of Theriosuchus have not been explored in detail although one species, Theriosuchus pusillus, has been extensively described and referred in numerous works. Here, we describe a new basal mesoeucrocodylian, Theriosuchus sympiestodon sp. nov. from the Maastrichtian of the HaA eg pound Basin, Romania, suggesting a large temporal gap (about 58 myr) in the fossil record of the genus. Inclusion of the new taxon, along with Theriosuchus guimarotae, in a phylogenetic analysis confirms its referral to the genus Theriosuchus, within a monophyletic atoposaurid clade. Although phylogenetic resolution within this clade is still poor, the new taxon appears, on morphological grounds, to be most closely related to T. pusillus. The relationships of Atoposauridae within Mesoeucrocodylia and especially to Neosuchia are discussed in light of the results of the present contribution as well as from recent work. Our results raise the possibility that Atoposauridae might not be regarded as a derived neosuchian clade anymore, although further investigation of the neosuchian interrelationships is needed. Reports of isolated teeth referable to a closely related taxon from the Upper Cretaceous of Romania and France, together with the presence of Doratodon and Ischyrochampsa, indicate a previously unsuspected diverse assemblage of non-eusuchian mesoeucrocodylians in the Late Cretaceous European archipelago.},
	year = {2010},
	eissn = {1432-1904},
	pages = {845-854}
}

@CONFERENCE{MTMT:2524708,
	title = {Specialized basal eusuchian crocodilians in the Late Cretaceous of Europe: evidence for the hylaeochampsid affinites of Acynodon and its implication on alligatoroid biogeography},
	url = {https://m2.mtmt.hu/api/publication/2524708},
	author = {Rabi, Márton and Ősi, Attila},
	booktitle = {Abstract volume of the 8th Annual Meeting of the EAVP, Aix-en-Provance},
	unique-id = {2524708},
	year = {2010},
	pages = {71},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:1926615,
	title = {An advanced anuran from the Late Cretaceous (Santonian) of Hungary},
	url = {https://m2.mtmt.hu/api/publication/1926615},
	author = {Szentesi, Zoltán and Venczel, Márton},
	doi = {10.1127/0077-7749/2010/0054},
	journal-iso = {NEUES JAHRB GEOL P-A},
	journal = {NEUES JAHRBUCH FÜR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN},
	volume = {256},
	unique-id = {1926615},
	issn = {0077-7749},
	year = {2010},
	eissn = {2363-717X},
	pages = {291-302},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478; Venczel, Márton/0000-0003-2200-3619}
}

@article{MTMT:151959,
	title = {New remains of Hungarosaurus tormai (Ankylosauria, Dinosauria) from the Upper Cretaceous of Hungary: skeletal reconstruction and body mass estimation},
	url = {https://m2.mtmt.hu/api/publication/151959},
	author = {Ősi, Attila and Makádi, László},
	doi = {10.1007/s12542-009-0017-5},
	journal-iso = {PALAEONTOL Z},
	journal = {PALAEONTOLOGISCHE ZEITSCHRIFT},
	volume = {83},
	unique-id = {151959},
	issn = {0031-0220},
	year = {2009},
	eissn = {1867-6812},
	pages = {227-245},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:2960991,
	title = {Bicuspidon aff. hatzegiensis (Squamata: Scincomorpha: Teiidae) from the Upper Cretaceous Csehbánya Formation (Hungary, Bakony Mts)},
	url = {https://m2.mtmt.hu/api/publication/2960991},
	author = {Makádi, László},
	doi = {10.1556/AGeol.49.2006.4.5},
	journal-iso = {ACTA GEOL HUNG},
	journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES},
	volume = {49},
	unique-id = {2960991},
	issn = {0236-5278},
	year = {2006},
	pages = {373-385}
}

@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}
}