TY - JOUR AU - Czernielewski, Michał TI - Prospalax priscus jaw from the site of Węże 2 (southern Poland, Pliocene) JF - GEOLOGIJA (LJUBLJANA) J2 - GEOLOGIJA (LJUBLJANA) VL - 66 PY - 2023 IS - 2 SP - 247 EP - 255 PG - 9 SN - 0016-7789 DO - 10.5474/geologija.2023.011 UR - https://m2.mtmt.hu/api/publication/34521274 ID - 34521274 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Sebe, Krisztina AU - Gasparik, Mihály AU - Szentesi, Zoltán AU - Surányi, Gergely AU - Novothny, Ágnes AU - Pandolfi, Luca TI - New Pleistocene vertebrate assemblages from the Villány Hills (SW Hungary): Siklós and Palkonya JF - FRAGMENTA PALAEONTOLOGICA HUNGARICA J2 - FRAGM PALAEONTOL HUNG VL - 38 PY - 2023 SP - 75 EP - 94 PG - 20 SN - 1586-930X DO - 10.17111/FragmPalHung.2023.38.75 UR - https://m2.mtmt.hu/api/publication/34134323 ID - 34134323 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Vasilyan, Davit AU - Čerňanský, Andrej AU - Szyndlar, Zbigniew AU - Mörs, Thomas TI - Amphibian and reptilian fauna from the early Miocene of Echzell, Germany JF - FOSSIL RECORD: AN INTERNATIONAL JOURNAL OF GEOSCIENCE J2 - FOSS REC VL - 25 PY - 2022 IS - 1 SP - 99 EP - 145 PG - 47 SN - 2193-0066 DO - 10.3897/fr.25.83781 UR - https://m2.mtmt.hu/api/publication/32819051 ID - 32819051 N1 - Export Date: 6 September 2023 LA - English DB - MTMT ER - TY - JOUR AU - Gardner, James D. AU - Villa, Andrea AU - Colombero, Simone AU - Venczel, Márton AU - Delfino, Massimo TI - 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 JF - GEODIVERSITAS J2 - GEODIVERSITAS VL - 43 PY - 2021 IS - 14 SP - 391 EP - 404 PG - 14 SN - 1280-9659 DO - 10.5252/geodiversitas2021v43a14 UR - https://m2.mtmt.hu/api/publication/32106197 ID - 32106197 LA - English DB - MTMT ER - TY - JOUR AU - Sebe, Krisztina AU - Szentesi, Zoltán AU - Pazonyi, Piroska AU - Surányi, Gergely AU - Csillag, Gábor TI - A late Pleistocene fossiliferous paleokarst site in the Western Mecsek Mts (Bükkösd, SW Hungary) JF - FRAGMENTA PALAEONTOLOGICA HUNGARICA J2 - FRAGM PALAEONTOL HUNG VL - 37 PY - 2021 SP - 127 EP - 144 PG - 18 SN - 1586-930X DO - 10.17111/FragmPalHung.2021.37.127 UR - https://m2.mtmt.hu/api/publication/32638333 ID - 32638333 LA - English DB - MTMT ER - TY - JOUR AU - Kovács, János AU - Újvári, Gábor AU - Varga, György AU - Seelos, K AU - Szabó, Péter AU - Dezső, József AU - Gammoudi, Nadia TI - Plio-Pleistocene dust traps on paleokarst surfaces: a case study from the Carpathian Basin JF - FRONTIERS IN EARTH SCIENCE J2 - FRONT EARTH SC-SWITZ VL - 8 PY - 2020 PG - 10 SN - 2296-6463 DO - 10.3389/feart.2020.00189 UR - https://m2.mtmt.hu/api/publication/31342357 ID - 31342357 N1 - Cited By :1 Export Date: 6 April 2021 Correspondence Address: Kovács, J.; Department of Geology and Meteorology, Hungary; email: jones@gamma.ttk.pte.hu Correspondence Address: Kovács, J.; Environmental Analytical and Geoanalytical Research Group, Hungary; email: jones@gamma.ttk.pte.hu AB - 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. LA - English DB - MTMT ER - TY - THES AU - Kovács, János TI - Kovács J. 2020: Plio-pleisztocén vörösagyagok üledékföldtani, ásványtani, geokémiai és őskörnyezeti aspektusai. – MTA doktori értekezés, 127pp. dc_1801_20 PY - 2020 UR - https://m2.mtmt.hu/api/publication/33090779 ID - 33090779 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Ősi, Attila AU - Mészáros, Lukács TI - Gerinces fosszíliák és kutatásuk a Kárpát-medencében JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 150 PY - 2020 IS - 3 SP - 375 EP - 396 PG - 22 SN - 0015-542X DO - 10.23928/foldt.kozl.2020.150.3.375 UR - https://m2.mtmt.hu/api/publication/31618154 ID - 31618154 N1 - Export Date: 16 September 2022 Correspondence Address: Ősi, A.; Eötvös Loránd Tudományegyetem, Pázmány Péter sétány 1/C, Hungary; email: hungaros@gmail.com LA - Hungarian DB - MTMT ER - TY - JOUR AU - Szentesi, Zoltán TI - Új albanerpetontida (Allocaudata: Albanerpetontidae) leletek az iharkúti késő-kréta szárazföldi ősgerinces lelőhelyről JF - ANNALES MUSEI HISTORICO-NATURALIS HUNGARICI J2 - ANNLS MUS HIST-NAT HUNG VL - 112 PY - 2020 SP - 37 EP - 55 PG - 19 SN - 0521-4726 DO - 10.53019/AnnlsMusHistNatHung.2020.112.37 UR - https://m2.mtmt.hu/api/publication/32062657 ID - 32062657 LA - Hungarian DB - MTMT ER - TY - THES AU - Guillaume, A.R.D. TI - Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal), Dissertação para obtenção do Grau de Mestre em Paleontologia PY - 2017 UR - https://m2.mtmt.hu/api/publication/30755277 ID - 30755277 N1 - Ms.C. thesis: Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa LA - Portuguese DB - MTMT ER -