@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:33917923,
	title = {Day‐To‐Day Quantification of Changes in Global Lightning Activity Based on Schumann Resonances},
	url = {https://m2.mtmt.hu/api/publication/33917923},
	author = {Bozóki, Tamás and Sátori, Gabriella and Williams, E. and Guha, A. and Liu, Y. and Steinbach, Péter and Leal, A. and Herein, Mátyás and Atkinson, M. and Beggan, C. D. and DiGangi, E. and Koloskov, A. and Kulak, A. and LaPierre, J. and Milling, D. K. and Mlynarczyk, J. and Neska, A. and Potapov, A. and Raita, T. and Rawat, R. and Said, R. and Sinha, A. K. and Yampolski, Y.},
	doi = {10.1029/2023JD038557},
	journal-iso = {J GEOPHYS RES ATMOS},
	journal = {JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES},
	volume = {128},
	unique-id = {33917923},
	issn = {2169-897X},
	year = {2023},
	eissn = {2169-8996},
	orcid-numbers = {Bozóki, Tamás/0000-0002-1672-1510; Liu, Y./0000-0002-8460-5191; Steinbach, Péter/0000-0003-2524-8494; Leal, A./0000-0003-0606-2950; Herein, Mátyás/0000-0003-1903-3761; Beggan, C. D./0000-0002-2298-0578; DiGangi, E./0000-0001-9665-5738; Mlynarczyk, J./0000-0002-0076-759X; Potapov, A./0000-0002-4864-0993; Said, R./0000-0002-8095-4204}
}

@inproceedings{MTMT:33811202,
	title = {ELF-viharok ég fölött és föld alatt},
	url = {https://m2.mtmt.hu/api/publication/33811202},
	author = {Bór, József and Szabóné André, Karolina and Novák, Attila and Bozóki, Tamás and Janusz, Mlynarczyk and Steinbach, Péter and Lemperger, István},
	booktitle = {Magyar Űrkutatási Fórum 2021 - Válogatott közlemények},
	unique-id = {33811202},
	year = {2023},
	orcid-numbers = {Szabóné André, Karolina/0000-0002-2465-1620; Bozóki, Tamás/0000-0002-1672-1510; Steinbach, Péter/0000-0003-2524-8494}
}

@article{MTMT:33611038,
	title = {Seismic Activity in the Celje Basin (Slovenia) in Roman Times—Archaeoseismological Evidence from Celeia},
	url = {https://m2.mtmt.hu/api/publication/33611038},
	author = {Kázmér, Miklós and Jamšek Rupnik, Petra and Gaidzik, Krzysztof},
	doi = {10.3390/quat6010010},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {6},
	unique-id = {33611038},
	issn = {2571-550X},
	abstract = {Searching for unknown earthquakes in Slovenia in the first millennium, we performed archaeoseismological analysis of Roman settlements. The Mesto pod mestom museum in Celje exhibits a paved Roman road, which suffered severe deformation. Built on fine gravel and sand from the Savinja River, the road displays a bulge and trench, pop-up structures, and pavement slabs tilted up to 40°. The city wall was built over the deformed road in Late Roman times, supported by a foundation containing recycled material (spolia) from public buildings, including an emperor’s statue. We hypothesize that a severe earthquake hit the town before 350 AD, causing widespread destruction. Seismic-induced liquefaction caused differential subsidence, deforming the road. One of the nearby faults from the strike-slip Periadriatic fault system was the seismic source of this event.},
	year = {2023},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316; Jamšek Rupnik, Petra/0000-0003-0809-1739; Gaidzik, Krzysztof/0000-0003-3286-0833}
}

@article{MTMT:33126810,
	title = {Origin, timing and paleogeographic implications of Paleogene karst bauxites in the northern Transdanubian range, Hungary},
	url = {https://m2.mtmt.hu/api/publication/33126810},
	author = {Kelemen, Péter and Dunkl, István and Csillag, Gábor and Mindszenty, Andrea and Józsa, Sándor and Fodor, László and von Eynatten, Hilmar},
	doi = {10.1007/s00531-022-02249-3},
	journal-iso = {INT J EARTH SCI},
	journal = {INTERNATIONAL JOURNAL OF EARTH SCIENCES},
	volume = {112},
	unique-id = {33126810},
	issn = {1437-3254},
	abstract = {Paleogene karst bauxites in the northeastern Transdanubian Range and their cover sequences provide valuable sedimentary archives, despite their weathered nature and vague paleontological records. U–Pb detrital zircon geochronology combined with heavy mineral analysis indicates ‘local’ Alpine aeolian and fluvial sources and ‘distant’ aeolian sources connected to the Bohemian Massif. Records of episodic Paleogene volcanic eruptions related to igneous complexes of the Adamello and probably also the Bergell, Recsk and Balkan Peninsula, are reflected by euhedral zircon crystals. Their U–Pb geochronology supplies age constraints for the phases of subaerial exposure of the karstic surface and the accumulation of bauxitic protoliths and helps to improve the existing stratigraphic records and to define stages of denudation in the northeastern Transdanubian Range. Distinct phases of subaerial exposure and accumulation of the bauxite's protoliths are identified as ca. 42, 35 and 31 Ma; alternating with episodes of subsidence, represented by siliciclastic and carbonatic sequences at ca. 38, 32 and 31 Ma. Besides Paleogene volcanism, zircon dating also revealed contributions from the Middle Triassic tuffs of the Transdanubian Range. Garnet, epidote, kyanite, staurolite, and xenotime/monazite crystals suggest fluvial drainage of diverse metamorphic units of the Austroalpine basement from the Eastern- and Southern Alps, which also supplied most of the pre-Mesozoic zircons. However, the unexpectedly high proportion of Variscan ages in the bauxites most likely relate to igneous rocks of the Bohemian Massif, thus suggesting additional long-distance aeolian sources. The new data allow for detailed reconstructions of the Paleogene evolution and palaeogeography of the northeastern Transdanubian range.},
	year = {2023},
	eissn = {1437-3262},
	pages = {243-264},
	orcid-numbers = {Mindszenty, Andrea/0000-0001-8927-3053; Józsa, Sándor/0000-0001-8219-0044}
}

@CONFERENCE{MTMT:34082836,
	title = {Detection of crystallinity changes in speleothem calcite and},
	url = {https://m2.mtmt.hu/api/publication/34082836},
	author = {Demény, Attila and Németh, Péter and Frisia, S and Lange-Enyedi, Nóra and Makk, Judit and Czuppon, György and Surányi, Gergely and Leél-Őssy, Szabolcs},
	booktitle = {Climate Change: The Karst Record IX (KR9)},
	unique-id = {34082836},
	year = {2022},
	pages = {191},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Németh, Péter/0000-0001-5592-5877; Makk, Judit/0000-0001-5768-7622; Czuppon, György/0000-0002-7231-6042}
}

@CONFERENCE{MTMT:34082768,
	title = {Climate change event at 8.5 ka detected from Oman to the Carpathian Basin: teleconnections with the Indian ocean},
	url = {https://m2.mtmt.hu/api/publication/34082768},
	author = {Demény, Attila and Topál, Dániel and Surányi, Gergely and Czuppon, György and Berentés, Á and Molnár, Mihály and Leél-Őssy, Szabolcs and Kovács, R},
	booktitle = {Climate Change: The Karst Record IX (KR9)},
	unique-id = {34082768},
	year = {2022},
	pages = {101},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Czuppon, György/0000-0002-7231-6042}
}

@article{MTMT:34065081,
	title = {Két földrengés az ókori Palesztinában : Capitolias római színházának archeoszeizmológiája},
	url = {https://m2.mtmt.hu/api/publication/34065081},
	author = {Lakatos, Szilvia and Al-Tawalbeh, Mohammad Ibrahim Abed and Khrisat, Bilal and Kázmér, Miklós},
	journal-iso = {ÓKOR},
	journal = {ÓKOR: FOLYÓIRAT AZ ANTIK KULTÚRÁRÓL},
	volume = {21},
	unique-id = {34065081},
	issn = {1589-2700},
	year = {2022},
	pages = {66-77},
	orcid-numbers = {Kázmér, Miklós/0000-0003-1092-1316}
}

@{MTMT:33803819,
	title = {Outcrop-scale structures observed in the Upper Jurassic–Early Cretaceous sections of the Bakony Mountains (Transdanubian Range, Hungary).},
	url = {https://m2.mtmt.hu/api/publication/33803819},
	author = {Fodor, László},
	booktitle = {Fauna, biostratigraphy, facies and paleotectonic evolution of the Late Jurassic–Early Cretaceous formations in the Bakony Mountains (Transdanubian Range, Hungary).},
	unique-id = {33803819},
	year = {2022},
	pages = {101-110}
}

@{MTMT:33803803,
	title = {The place of the Bakony Mountains and the Transdanubian Range in plate tectonic configurations during the Late Jurassic to Early Cretaceous},
	url = {https://m2.mtmt.hu/api/publication/33803803},
	author = {Fodor, László},
	booktitle = {Fauna, biostratigraphy, facies and paleotectonic evolution of the Late Jurassic–Early Cretaceous formations in the Bakony Mountains (Transdanubian Range, Hungary).},
	unique-id = {33803803},
	year = {2022},
	pages = {17-23}
}