@article{MTMT:34521274,
	title = {Prospalax priscus jaw from the site of Węże 2 (southern Poland, Pliocene)},
	url = {https://m2.mtmt.hu/api/publication/34521274},
	author = {Czernielewski, Michał},
	doi = {10.5474/geologija.2023.011},
	journal-iso = {GEOLOGIJA (LJUBLJANA)},
	journal = {GEOLOGIJA (LJUBLJANA)},
	volume = {66},
	unique-id = {34521274},
	issn = {0016-7789},
	abstract = {The ecology and adaptations of the Anomalomyidae (Muroidea) have been long debated in the scientific literature. A jaw belonging to Prospalax priscus (Anomalomyidae) was found at the Late Pliocene site of Węże 2 in southern Poland. The presence of this species at the site agrees with the interpretation of P. priscus and the Anomalomyidae in general as adapted to forest environments.},
	year = {2023},
	eissn = {1854-620X},
	pages = {247-255}
}

@article{MTMT:34134323,
	title = {New Pleistocene vertebrate assemblages from the Villány Hills (SW Hungary): Siklós and Palkonya},
	url = {https://m2.mtmt.hu/api/publication/34134323},
	author = {Sebe, Krisztina and Gasparik, Mihály and Szentesi, Zoltán and Surányi, Gergely and Novothny, Ágnes and Pandolfi, Luca},
	doi = {10.17111/FragmPalHung.2023.38.75},
	journal-iso = {FRAGM PALAEONTOL HUNG},
	journal = {FRAGMENTA PALAEONTOLOGICA HUNGARICA},
	volume = {38},
	unique-id = {34134323},
	issn = {1586-930X},
	abstract = {The Villány Hills in SW Hungary have the richest archive of Pliocene–Quaternary vertebrate faunas in the Pannonian Basin, mostly in karstic cavities. Here we present three new sites that extend the list of Pleistocene vertebrate locations for the area and add information to the evolution history of the region. In the northern part of the Siklós quarry, bone breccia was found coming from fissures in Jurassic or Cretaceous limestones. Its lithofacies and fossil content are similar to those of other well-known Plio-Pleistocene karst infills of the region. As it contained mostly snake vertebrae, its age could not be constrained precisely. In the southern part of the same quarry, two vertical shaft s were discovered, which are unusual in several respects. Th ey formed in a Middle Triassic dolomite succession, a rock type generally not prone to karstification. Th ey might have been created by gravitational deformation of the relatively steep slope, probably at diff erent times. One of them was closed from above and contained fl owstones precipitated during the late Middle Pleistocene, during the late Rissian MIS7 interglacial. The other one was filled from above with loess, rock fragments and remains of large mammals – Equus cf. ferus, Bos primigenius and Coelodonta antiquitatis –, possibly between 140–40 ka, during one of the stadials of the Weichselian or the latest Saalian. The site shows that fossil-bearing cavities could also form in lithologies not favourable for karstification, which then trapped fossils in a similar way karstic cavities do. In contrast with the previous two and with most of the other known vertebrate sites of the Villány Hills, the Palkonya outcrop is not a karst cavity fill but was deposited on the (palaeo)surface. Bison sp., possibly B. schoetensacki remains were found between the Triassic basement and Quaternary slope sediments, and within the latter succession. The Bison bones are probably Middle Pleistocene or late Early Pleistocene, older than ~300 ka. The overlying slope sediments originate from the reworking of various older deposits. Th ey were covered with loess in the Weichselian (~22 ka ago), then again with slope deposits. The abundance of bones in and around the outcrop suggests that this site acted as a fossil trap as well. Bones probably enriched in the sediments during reworking of older deposits. In cold periods, loess deposition decreased (subdued) the relief through infilling the depressions. With 21 figures and 3 tables.},
	year = {2023},
	pages = {75-94},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Szentesi, Zoltán/0000-0002-7019-5478; Novothny, Ágnes/0000-0003-3513-0406}
}

@article{MTMT:32819051,
	title = {Amphibian and reptilian fauna from the early Miocene of Echzell, Germany},
	url = {https://m2.mtmt.hu/api/publication/32819051},
	author = {Vasilyan, Davit and Čerňanský, Andrej and Szyndlar, Zbigniew and Mörs, Thomas},
	doi = {10.3897/fr.25.83781},
	journal-iso = {FOSS REC},
	journal = {FOSSIL RECORD: AN INTERNATIONAL JOURNAL OF GEOSCIENCE},
	volume = {25},
	unique-id = {32819051},
	issn = {2193-0066},
	year = {2022},
	eissn = {1860-1014},
	pages = {99-145},
	orcid-numbers = {Vasilyan, Davit/0000-0001-8712-0678; Čerňanský, Andrej/0000-0001-8920-2503; Mörs, Thomas/0000-0003-2268-5824}
}

@article{MTMT:32106197,
	title = {A Messinian (latest Miocene) occurrence for Albanerpeton Estes & Hoffstetter, 1976 (Lissamphibia: Albanerpetontidae) at Moncucco Torinese, Piedmont Basin, northwestern Italy, and a review of the European Cenozoic record for albanerpetontids},
	url = {https://m2.mtmt.hu/api/publication/32106197},
	author = {Gardner, James D. and Villa, Andrea and Colombero, Simone and Venczel, Márton and Delfino, Massimo},
	doi = {10.5252/geodiversitas2021v43a14},
	journal-iso = {GEODIVERSITAS},
	journal = {GEODIVERSITAS},
	volume = {43},
	unique-id = {32106197},
	issn = {1280-9659},
	year = {2021},
	eissn = {1638-9395},
	pages = {391-404},
	orcid-numbers = {Venczel, Márton/0000-0003-2200-3619}
}

@article{MTMT:32638333,
	title = {A late Pleistocene fossiliferous paleokarst site in the Western Mecsek Mts (Bükkösd, SW Hungary)},
	url = {https://m2.mtmt.hu/api/publication/32638333},
	author = {Sebe, Krisztina and Szentesi, Zoltán and Pazonyi, Piroska and Surányi, Gergely and Csillag, Gábor},
	doi = {10.17111/FragmPalHung.2021.37.127},
	journal-iso = {FRAGM PALAEONTOL HUNG},
	journal = {FRAGMENTA PALAEONTOLOGICA HUNGARICA},
	volume = {37},
	unique-id = {32638333},
	issn = {1586-930X},
	year = {2021},
	pages = {127-144},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Szentesi, Zoltán/0000-0002-7019-5478}
}

@article{MTMT:31342357,
	title = {Plio-Pleistocene dust traps on paleokarst surfaces: a case study from the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/31342357},
	author = {Kovács, János and Újvári, Gábor and Varga, György and Seelos, K and Szabó, Péter and Dezső, József and Gammoudi, Nadia},
	doi = {10.3389/feart.2020.00189},
	journal-iso = {FRONT EARTH SC-SWITZ},
	journal = {FRONTIERS IN EARTH SCIENCE},
	volume = {8},
	unique-id = {31342357},
	abstract = {Plio-Pleistocene silt/clay-rich deposits and paleo-karst fissure sediments from sites of the northern and southern parts of the Carpathian Basin were investigated. These materials were supposed to be mixed during transport before being captured in karstified fissures. Evidence that the eolian fissure sediments of Plio-Pleistocene age in the older Triassic-Cretaceous limestones are derived from eolian silt and clay includes compositional and textural matches, especially decreasing grain-size trends observed downwards from the paleo-surface of the former landscape. Various environmental factors could be recognized by the statistical evaluation of grain-size distribution curves of fissure fillings sediments, such as the effects of eolian transport, parent rock type, weathering, and other sediment transport processes. Grain-size distribution curves with a single maximum in the silt size range are typical for the overlying siltstone debris, for the redeposited loess and red paleosol underlying the loess. Red clay fissure fillings yield bimodal grain-size distribution curves with maxima both in the clay and silt fractions. The research reported in this paper identifies for the first time the presence of eolian deposits in karst fissures of the Carpathian Basin and investigates the characteristics and origin.},
	year = {2020},
	eissn = {2296-6463},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515; Újvári, Gábor/0000-0002-2816-6155; Varga, György/0000-0003-4784-6372; Szabó, Péter/0000-0003-0827-3583}
}

@mastersthesis{MTMT:33090779,
	title = {Kovács J. 2020: Plio-pleisztocén vörösagyagok üledékföldtani, ásványtani, geokémiai és őskörnyezeti aspektusai. – MTA doktori értekezés, 127pp. dc_1801_20},
	url = {https://m2.mtmt.hu/api/publication/33090779},
	author = {Kovács, János},
	unique-id = {33090779},
	year = {2020}
}

@article{MTMT:31618154,
	title = {Gerinces fosszíliák és kutatásuk a Kárpát-medencében},
	url = {https://m2.mtmt.hu/api/publication/31618154},
	author = {Ősi, Attila and Mészáros, Lukács},
	doi = {10.23928/foldt.kozl.2020.150.3.375},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {150},
	unique-id = {31618154},
	issn = {0015-542X},
	year = {2020},
	eissn = {2559-902X},
	pages = {375-396},
	orcid-numbers = {Ősi, Attila/0000-0003-2967-997X}
}

@article{MTMT:32062657,
	title = {Új albanerpetontida (Allocaudata: Albanerpetontidae) leletek az iharkúti késő-kréta szárazföldi ősgerinces lelőhelyről},
	url = {https://m2.mtmt.hu/api/publication/32062657},
	author = {Szentesi, Zoltán},
	doi = {10.53019/AnnlsMusHistNatHung.2020.112.37},
	journal-iso = {ANNLS MUS HIST-NAT HUNG},
	journal = {ANNALES MUSEI HISTORICO-NATURALIS HUNGARICI},
	volume = {112},
	unique-id = {32062657},
	issn = {0521-4726},
	year = {2020},
	pages = {37-55},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478}
}

@mastersthesis{MTMT:30755277,
	title = {Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal), Dissertação para obtenção do Grau de Mestre em Paleontologia},
	url = {https://m2.mtmt.hu/api/publication/30755277},
	author = {Guillaume, A.R.D.},
	unique-id = {30755277},
	year = {2017}
}