@CONFERENCE{MTMT:34397090,
	title = {Barlang konglomerátumban: a Törökpince – Abaligeti-barlang rendszer},
	url = {https://m2.mtmt.hu/api/publication/34397090},
	author = {Sebe, Krisztina and Haász, J and Ruszkiczay-Rüdiger, Zsófia and Bauer, Márton and Pazonyi, Piroska and Szentesi, Zoltán and Gregorits, M and Szabó, M},
	booktitle = {28. Barlangkutatók ’Szablyár Péter’ Szakmai Találkozója},
	unique-id = {34397090},
	year = {2023},
	pages = {8},
	orcid-numbers = {Sebe, Krisztina/0000-0002-4647-2199; Szentesi, Zoltán/0000-0002-7019-5478}
}

@article{MTMT:33961884,
	title = {Stratigraphic and Paleoecological Significance of the Early/Middle Pleistocene Vertebrate Fauna of the Süttő 21 Site},
	url = {https://m2.mtmt.hu/api/publication/33961884},
	author = {Pazonyi, Piroska and Szentesi, Zoltán and Mészáros, Lukács and Hír, János and Gasparik, Mihály},
	doi = {10.3390/d15060736},
	journal-iso = {DIVERSITY-BASEL},
	journal = {DIVERSITY (BASEL)},
	volume = {15},
	unique-id = {33961884},
	abstract = {The Süttő 21 site is a fissure fill of the freshwater limestone of the Gazda quarry in Süttő. The material was collected between 2017 and 2019, and the results are summarised in this article, with a special focus on the small vertebrate fauna of the site and its stratigraphic and paleoecological significance. The fissure fill can be placed around the Early/Middle Pleistocene boundary (ca. 1.1 and 0.77 Ma). The paleoecological analysis of the herpeto- and mammal fauna of the sequence indicates the proximity of a permanent water body. The lower part of the sequence is dominated by open habitat indicator taxa indicating a cool, dry climate. Towards the upper part of the sequence, the climate remained cool, but became wetter, and the vegetation gradually changed to forest-steppe/open forest. The fauna of the Süttő 21 site can be compared with the material of sites that are of a similar age, thus revealing taxonomic and paleoecological differences between different areas of the country. While a warm, dry climate and open vegetation can be reconstructed in the Villány Hills around the Early/Middle Pleistocene boundary, the Northern Hungarian areas had a cooler, wetter climate and a slightly more closed (sparse forest, forest-steppe) vegetation during this period.},
	year = {2023},
	eissn = {1424-2818},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478; Mészáros, Lukács/0000-0001-8125-4149}
}

@article{MTMT:32795556,
	title = {Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe},
	url = {https://m2.mtmt.hu/api/publication/32795556},
	author = {Magyari, Enikő Katalin and Gasparik, Mihály and Major, István and Lengyel, György and Pál, Ilona and Virág, Attila and Korponai, János and Haliuc, Aritina and Szabó, Zoltán and Pazonyi, Piroska},
	doi = {10.1038/s41598-022-10714-x},
	journal-iso = {SCI REP},
	journal = {SCIENTIFIC REPORTS},
	volume = {12},
	unique-id = {32795556},
	issn = {2045-2322},
	abstract = {The study of local extinction times, together with the associated environmental and human population changes in the last glacial termination, provides insights into the causes of mega- and microfauna extinctions. In East-Central (EC) Europe, groups of Palaeolithic humans were present throughout the last glacial maximum, but disappeared suddenly around 15,200 cal BP. In this study cave sediment profiles dated using radiocarbon techniques and a large set of mammal bones dated directly by AMS 14C were used to determine local extinction times. These were, in turn, compared to changes in the total megafauna population of EC Europe derived from coprophilous fungi, the Epigravettian population decline, quantitative climate models, pollen and plant macrofossil inferred climate, as well as to biome reconstructions. The results suggest that the population size of large herbivores decreased in the area after 17,700 cal BP, when temperate tree abundance and warm continental steppe cover both increased in the lowlands. Boreal forest expansion started around 16,200 cal BP. Cave sediments show the decline of narrow-headed vole and arctic lemming populations specifically associated with a tundra environment at the same time and the expansion of the common vole, an inhabitant of steppes. The last dated appearance of arctic lemming was at ~ 16,640 cal BP, while that of the narrow-headed vole at ~ 13,340, and the estimated extinction time of woolly mammoth was either at 13,830 (GRIWM) or 15,210 (PHASE), and reindeer at 11,860 (GRIWM) or 12,550 cal BP (PHASE). The population decline of the large herbivore fauna slightly preceded changes in terrestrial vegetation, and likely facilitated it via a reduction in the intensity of grazing and the concomitant accumulation of plant biomass. Furthermore, it is possible to conclude that the Late Epigravettian population had high degree of quarry-fidelity; they left the basin when these mammals vanished.},
	year = {2022},
	eissn = {2045-2322},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Major, István/0000-0003-4675-9875; Lengyel, György/0000-0002-7803-3043; Virág, Attila/0000-0002-5530-0065; Korponai, János/0000-0003-0211-192X}
}

@article{MTMT:32638534,
	title = {A new middle Pleistocene small vertebrate fauna from the Nagyharsány Crystal Cave (Villány Hills, Southern Hungary)},
	url = {https://m2.mtmt.hu/api/publication/32638534},
	author = {Pazonyi, Piroska and Szentesi, Zoltán and Mészárosné Trembeczki, Mária and Hír, J. and Mészáros, Lukács},
	doi = {10.17111/FragmPalHung.2021.37.101},
	journal-iso = {FRAGM PALAEONTOL HUNG},
	journal = {FRAGMENTA PALAEONTOLOGICA HUNGARICA},
	volume = {37},
	unique-id = {32638534},
	issn = {1586-930X},
	year = {2021},
	pages = {101-126},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478}
}

@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}
}

@{MTMT:32341641,
	title = {Egy új középső pleisztocén kisgerinces fauna a Nagyharsányi-kristálybarlangból (Villányi-hegység)},
	url = {https://m2.mtmt.hu/api/publication/32341641},
	author = {Pazonyi, Piroska and Szentesi, Zoltán and Trembeczki, Mária and Hír, János and Mészáros, Lukács},
	booktitle = {24. Magyar Őslénytani Vándorgyűlés, Program, előadáskivonatok, kirándulásvezető},
	unique-id = {32341641},
	year = {2021},
	pages = {25-26},
	orcid-numbers = {Szentesi, Zoltán/0000-0002-7019-5478}
}

@{MTMT:32341347,
	title = {Új adatok a klasszikus Beremend 26-os lelőhely sztratigráfiájához és paleoökológiájához: pliocén denevérek és rovarevők},
	url = {https://m2.mtmt.hu/api/publication/32341347},
	author = {Mészáros, Lukács and Trembeczki, M. and Pazonyi, Piroska},
	booktitle = {24. Magyar Őslénytani Vándorgyűlés, Program, előadáskivonatok, kirándulásvezető},
	unique-id = {32341347},
	year = {2021},
	pages = {21-22}
}

@misc{MTMT:32245959,
	title = {Mammal Extinction Facilitated Biome Shift and Human Population Change During the Last Glacial Termination in East-Central Europe},
	url = {https://m2.mtmt.hu/api/publication/32245959},
	author = {Magyari, Enikő Katalin and Gasparik, Mihály and Major, István and Lengyel, György and Pál, Ilona and Virág, Attila and Korponai, János and Szabó, Zoltán and Pazonyi, Piroska},
	doi = {10.21203/rs.3.rs-778658/v1},
	unique-id = {32245959},
	year = {2021},
	pages = {1-27},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Major, István/0000-0003-4675-9875; Virág, Attila/0000-0002-5530-0065; Korponai, János/0000-0003-0211-192X}
}

@article{MTMT:31840054,
	title = {Biotic evolution and palaeogeography during the Quaternary with special reference to ground squirrels. Introduction},
	url = {https://m2.mtmt.hu/api/publication/31840054},
	author = {Popova, Lilia and Maul, Lutz Christian and Pazonyi, Piroska},
	doi = {10.1080/08912963.2020.1852402},
	journal-iso = {HIST BIOL},
	journal = {HISTORICAL BIOLOGY},
	volume = {33},
	unique-id = {31840054},
	issn = {0891-2963},
	year = {2021},
	eissn = {1029-2381},
	pages = {1-3},
	orcid-numbers = {Popova, Lilia/0000-0001-5008-8715; Maul, Lutz Christian/0000-0002-8860-2932; Pazonyi, Piroska/0000-0002-8256-8577}
}

@article{MTMT:31797540,
	title = {Pleistocene and holocene palaeoenvironmental reconstruction of the carpathian basin based on multiproxy analysis of cervid teeth},
	url = {https://m2.mtmt.hu/api/publication/31797540},
	author = {Szabó, Bence and Pazonyi, Piroska and Tóth, Emőke and Magyari, Enikő Katalin and Kiss, Gabriella Ilona and Rinyu, László and Futó, István and Virág, Attila},
	doi = {10.1080/08912963.2020.1863960},
	journal-iso = {HIST BIOL},
	journal = {HISTORICAL BIOLOGY},
	volume = {33},
	unique-id = {31797540},
	issn = {0891-2963},
	year = {2021},
	eissn = {1029-2381},
	pages = {3307-3325},
	orcid-numbers = {Pazonyi, Piroska/0000-0002-8256-8577; Tóth, Emőke/0000-0002-1733-7828; Magyari, Enikő Katalin/0000-0002-2844-8937; Virág, Attila/0000-0002-5530-0065}
}