TY - JOUR AU - Botfalvai, Gábor AU - Kocsis, László AU - Szabó, Márton AU - Király, Edit AU - Sebe, Krisztina TI - Preliminarily report on rare earth element taphonomy of a Miocene mixed age fossil vertebrate assemblage (Pécs-Danitzpuszta, Mecsek Mts., Hungary): uptake mechanism and possible separation of palaeocommunities JF - HISTORICAL BIOLOGY J2 - HIST BIOL VL - 35 PY - 2023 IS - 4 SP - 498 EP - 517 PG - 20 SN - 0891-2963 DO - 10.1080/08912963.2022.2049771 UR - https://m2.mtmt.hu/api/publication/32753540 ID - 32753540 LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Katona, Lajos Tamás TI - Taxonomic revision of the Lake Pannon cockle subgenus Lymnocardium (Budmania) BRUSINA, 1897 JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 76 PY - 2023 IS - 1 SP - 37 EP - 46 PG - 10 SN - 1330-030X DO - 10.4154/gc.2023.01 UR - https://m2.mtmt.hu/api/publication/34092755 ID - 34092755 N1 - Funding Agency and Grant Number: National Research, Development and Innovation Office (NKFIH) [143787] Funding text: Our work on the museum collections was supported by Klara PALOTAS, Laszlo MAKADI, Balint SZAPPANOS (SZTFH); Oleg MANDIC, Mathias HARZHAUSER (NHMW); Katarina KRIZMANIC and Marija BOSNJAK (HPM). Martin GROSS and Bernhard HUBMANN kindly provided information on the UG collection. For taxonomic and ICZN issues, we were advised by Philippe BOUCHET (Museum National d'Histoire Naturelle, Paris) and Barna PALL-GERGELY (ELKH Agrartudomanyi Ku-tatokozpont, Budapest). Reviewers Simon SCHNEIDER and Oleg MANDIC are thanked for their large effort to improve the original manuscript. This research was funded by the National Research, Development and Innovation Office (NKFIH) project 143787. This is MTA-MTM-ELTE Paleo contribution No. 368. AB - The lymnocardiine subgenus Budmania is characterized by the most unusual and spectacular morphology in the endemic mollusc fauna of the Late Miocene - Pliocene Lake Pannon. Bud -mania possessed extremely high, hollow, irregular keels on its ribs, a pattern that was long con-sidered an adaptation to the fluid, muddy substratum. Eight species were described with this pattern between 1874 and 1973. Our revision, based on the type materials and a large number of additional specimens from several collections, revealed however, that only two species can be distinguished with certainty: Lymnocardium (Budmania) ferrugineum (BRUSINA, 1874) and L. (B.) cristagalli (ROTH, 1878). The former lived in the littoral zone of Lake Pannon, on a sandy substratum, whereas the latter inhabited the sublittoral zone with a muddy bottom. This habitat partitioning challenges the interpretation of the high, hollow keels as an adaptation to a soft, muddy substratum. The occurrence of both species seems to have been restricted to the period between 7.5-7.15 Ma. LA - English DB - MTMT ER - TY - JOUR AU - Sujan, Michal AU - Aherwar, Kishan AU - Chyba, Andrej AU - Rozsova, Barbara AU - Braucher, Regis AU - Sujan, Martin AU - Sipka, Frantisek AU - Team, Aster TI - Surviving from transgression to regression of Lake Pannon: Fan deltas of the Nemcinany Fm. persisted across the rifting until the post-rift stage of the Danube Basin, western Slovakia JF - GEOLOGICA CARPATHICA J2 - GEOL CARPATH VL - 74 PY - 2023 IS - 6 SP - 469 EP - 488 PG - 20 SN - 1335-0552 DO - 10.31577/GeolCarp.2023.25 UR - https://m2.mtmt.hu/api/publication/34756026 ID - 34756026 N1 - Funding Agency and Grant Number: Slovak Research and Development Agency (APVV) [APVV-16-0121, APVV-20-0120, APVV-21-0281]; Scientific Grant Agency of the Ministry of Education, Science, Research and Sport of the Slovak Republic; Slovak Academy of Sciences (VEGA) [1/0533/21]; INSU/CNRS; ANR through the "Projets thematiques d'excellence" program for the "Equipements d'excellence" ASTER-CEREGE action; IRD Funding text: The study was supported by the Slovak Research and Development Agency (APVV) under contracts Nos. APVV-16-0121, APVV-20-0120 and APVV-21-0281, and by the Scientific Grant Agency of the Ministry of Education, Science, Research and Sport of the Slovak Republic and the Slovak Academy of Sciences (VEGA) under the contract No. 1/0533/21. The free availability of the Lidar DEM data owned by the Geodesy, Cartography and Cadaster Authority of the Slovak Republic (UGKK SR) and distributed by the Geodetic and Cartographic Institute, Bratislava (GKU) is acknowledged with gratitude. The ASTER AMS national facility (CEREGE, Aix-en-Provence, France) is supported by the INSU/CNRS, the ANR through the "Projets thematiques d'excellence" program for the "Equipements d'excellence" ASTER-CEREGE action, and IRD. We express our gratitude to the reviewers Stephanie Neuhuber and Lubomir Sliva for their constructive feedback and helpful suggestions that have substantially improved the original manuscript. AB - Successions deposited under rifting and post-rift settings of an isolated epicontinental basin often exhibit contrasting characteristics. Facies linked to transgression during basin rifting are typically locally sourced fan deltas transporting coarse-grained sediment, whereas the post-rift setup generally involves a normal regression marked by more extensive catchments, sediment sourced from greater distances, and an overall decrease in average grain size compared to the transgressive facies. In this study, we present a specific scenario based on a sedimentological, stratigraphic, and authigenic 10Be/9Be analysis of the Nemcinany Formation, an Upper Miocene fan deltaic succession in the eastern Danube Basin, Slovakia. Deposition of the Nemcinany Fm. was initiated shortly after -11.6 Ma by the fourth rifting phase of the Pannonian Basin System, triggering the transgression of Lake Pannon. The depositional system persisted until -9.6 Ma, likely balancing the increased accommodation rate with sediment supply in the shallow lake area situated on a basement high. Subsequently, a relative decrease in the accommodation rate prompted the progradation of shelf-slope scale clinoforms, originating from the Nemcinany depositional system, toward the center of the Komjatice depression at -9.4 Ma, resulting in a normal regression of Lake Pannon. The persistence of the Nemcinany fan delta system, unlike common stratigraphic patterns, was associated to the high sediment supply yielded by the paleo-Hron river, which entered the basin in the study area. These observations underscore the need for caution in predicting provenance shifts during changes in geodynamic stages of a basin. LA - English DB - MTMT ER - TY - JOUR AU - Szabó, Fanni AU - Sebe, Krisztina AU - Sztanó, Orsolya TI - Dél-zselici pannon-tavi (késő miocén) rétegsorok őskörnyezeti rekonstrukciója JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 153 PY - 2023 IS - 1 SP - 35 EP - 56 PG - 22 SN - 0015-542X DO - 10.23928/foldt.kozl.2023.153.1.35 UR - https://m2.mtmt.hu/api/publication/33775901 ID - 33775901 N1 - ELTE Eötvös Loránd Tudományegyetem, Földrajz-és Földtudományi Intézet, Általános és Alkalmazott Földtani Tanszék, Budapest, Hungary Pécsi Tudományegyetem, Földtani és Meteorológiai Tanszék, Pécs, Hungary Export Date: 23 June 2023 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Baják, Petra AU - Hegedűs-Csondor, Katalin AU - Pedretti, Daniele AU - Muniruzzaman, Muhammad AU - Surbeck, Heinz AU - Izsák, Bálint AU - Vargha, Márta AU - Horváth, Ákos AU - Pándics, Tamás AU - Erőss, Anita TI - Refining the conceptual model for radionuclide mobility in groundwater in the vicinity of a Hungarian granitic complex using geochemical modeling JF - APPLIED GEOCHEMISTRY J2 - APPL GEOCHEM VL - 137 PY - 2022 SN - 0883-2927 DO - 10.1016/j.apgeochem.2022.105201 UR - https://m2.mtmt.hu/api/publication/32597603 ID - 32597603 N1 - József and Erzsébet Tóth Endowed Hydrogeology Chair, Department of Geology, Institute of Geography and Earth Sciences, Faculty of Science, Eötvös Loránd University, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary Dipartimento di Scienze della Terra “A. Desio”, Università degli Studi di Milano, Via Mangiagalli 34, Milan, 20133, Italy Water Management Solutions, Geological Survey of Finland, Vuorimiehentie 5, Espoo, 02151, Finland Public Health Directorate, National Public Health Institute, Albert Flórián út 2-6, Budapest, 1097, Hungary Department of Atomic Physics, Institute of Physics, Eötvös Loránd University, Pázmány Péter sétány 1/a, Budapest, 1117, Hungary Export Date: 25 January 2022 CODEN: APPGE Correspondence Address: Baják, P.; József and Erzsébet Tóth Endowed Hydrogeology Chair, Pázmány Péter sétány 1/c, Hungary; email: bajakpetra@student.elte.hu AB - Groundwater is an important freshwater resource, which can be affected by geogenic radionuclide contamination. To make decisions regarding the use and management of groundwater, understanding the controls of radionuclide mobility is critical. In the southern foreland of a granitic outcrop in Hungary, high gross alpha activity concentration was measured in drinking water wells, related probably to the presence of uranium. It has been suggested that understanding of the groundwater flow system may be a key aspect to understand uranium mobility in groundwater. The goal of the present work was to elucidate the conceptual model of radionuclide mobility in the study area, focusing in particular on the geochemical controls of uranium. For this purpose, water samples were collected and nuclide-specific measurements for 226Ra and radon isotopes were carried out, in addition to 234U+238U measurements, to increase the range of radionuclides and better understand their mobility. A geochemical modeling analysis involving redox-controlling kinetic reactions and a surface complexation model was developed to support the conceptual model. The results from the sampling indicate that excess of 234U+238U (3–753 mBq L−1) contribute to the natural radioactivity measured in drinking water to a large degree. 226Ra was measured in relatively low activity concentrations (<5–63 mBq L−1) with the exception of three specific wells. Notable radon activity concentration was measured in the springwaters from Velence Hills (1.01–3.14 × 105 mBq L−1) and in interrelation with the highest (285–695 mBq L−1) 226Ra activity concentrations. The geochemical model suggests that uranium distribution is sensitive to redox changes in the aquifer. Its mobility in groundwater depends on the residence time of groundwater compared to the reaction time controlling the consumption of oxidizing species. The longer the flow path from the recharge point to an observation point where U is measured, the more likely it is that reducing conditions will be found in the aquifer and the elemental concentration U will be low. LA - English DB - MTMT ER - TY - JOUR AU - Bartha, István Róbert AU - Botka, Dániel Bálint AU - Beliczainé Csoma, Vivien AU - Katona, Lajos Tamás AU - Tóth, Emőke AU - Magyar, Imre AU - Silye, Lóránd AU - Sztanó, Orsolya TI - From marginal outcrops to basin interior: a new perspective on the sedimentary evolution of the eastern Pannonian Basin JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 111 PY - 2022 SP - 335 EP - 357 PG - 23 SN - 1437-3254 DO - 10.1007/s00531-021-02117-6 UR - https://m2.mtmt.hu/api/publication/32475967 ID - 32475967 N1 - Department of Geology, Institute of Geography and Earth Sciences, ELTE Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary Laboratories MOL, MOL Hungarian Oil & Gas Plc., Szent István utca 14, Budapest, 1039, Hungary Department of Palaeontology, Institute of Geography and Earth Sciences, ELTE Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, 1117, Hungary Hungarian Natural History Museum-BTM, Rákóczi tér 3-5, Zirc, 8420, Hungary MTA-MTM-ELTE Research Group for Paleontology, Ludovika tér 2, Budapest, 1083, Hungary MOL Hungarian Oil & Gas Plc., Október huszonharmadika u. 18, Budapest, 1117, Hungary Department of Geology and Center for Integrated Geological Studies, Babeş-Bolyai University, Cluj-Napoca, Romania Export Date: 14 February 2022 CODEN: IJESF Correspondence Address: Magyar, I.; MOL Hungarian Oil & Gas Plc., Október huszonharmadika u. 18, Hungary; email: immagyar@mol.hu LA - English DB - MTMT ER - TY - JOUR AU - Radivojević, D AU - Radonjić, M AU - Katona, Lajos Tamás AU - Magyar, Imre TI - Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania) JF - INTERNATIONAL JOURNAL OF EARTH SCIENCES J2 - INT J EARTH SCI VL - 111 PY - 2022 IS - 5 SP - 1551 EP - 1571 PG - 21 SN - 1437-3254 DO - 10.1007/s00531-022-02188-z UR - https://m2.mtmt.hu/api/publication/32816598 ID - 32816598 N1 - Export Date: 1 July 2022 CODEN: IJESF Correspondence Address: Radivojević, D.; Faculty of Mining and Geology, Kamenička 6, Serbia; email: dejan.radivojevic@rgf.bg.ac.rs AB - In the late Neogene, the Pannonian Basin in Central Europe was filled with sediments when rivers from the Alps and Carpathians shed their sediment load into Lake Pannon. The most powerful source-to-sink system was that of the paleo-Danube, transporting sediments from the NW as far as the southeastern part of the lake. In the southeastern margin of the basin, however, local sedimentary systems worked in the opposite direction, against the “tide” of the prevailing N to S sediment transport. The lifetime and advance rate of these systems were unknown. We investigated such a sedimentary system in SE Banat, SE tip of the Pannonian Basin that transported material from the westernmost Southern Carpathians towards the basin center in the NW. Following the flooding of the Southern Carpathian foothills by Lake Pannon 9.6–9.1 My ago, a shelf was built from the Southern Carpathians into the 300–500 m deep water of the adjacent local depression. The advance of the shelf-edge reached the surroundings of Vršac Island some 20–25 km to the NW about 7.5–7.0 My ago, when a small-scale transgressive–regressive cycle formed on the flanks of the Vršac Mts: coarse-grained deposits derived from local sources during the initial flooding and the overlying offshore marls representing the maximum flooding are capped by the regressive deltaic succession advancing from the Southern Carpathians. The average shelf-edge progradation rate (ca. 10 km /My) was, thus, almost an order of magnitude smaller than the progradation rate of the coeval paleo-Danube shelf on the opposite, northwestern side of the lake. LA - English DB - MTMT ER - TY - JOUR AU - Andjelkovic, Filip AU - Radivojevic, Dejan TI - The Serbian Lake Pannon formations - their significance and interregional correlation JF - ANNALES GEOLOGIQUES DE LA PENINSULA BALKANIQUE J2 - ANN GEOL PENINSULA BALKANIQUE VL - 82 PY - 2021 IS - 2 SP - 43 EP - 67 PG - 25 SN - 0350-0608 DO - 10.2298/GABP210420007A UR - https://m2.mtmt.hu/api/publication/32543082 ID - 32543082 N1 - Cited By :1 Export Date: 10 January 2023 Correspondence Address: Anbelković, F.; University of Belgrade, Kamenicka 6, Serbia LA - English DB - MTMT ER - TY - JOUR AU - Šujan, M AU - Braucher, R AU - Mandic, O AU - Fordinál, K AU - Brixová, B AU - Pipík, RK AU - Šimo, V AU - Jamrich, M AU - Rybár, S AU - Klučiar, T AU - Ruman, A AU - Zvara, I AU - Kováč, M AU - Aster, Team TI - Lake Pannon Transgression on the Westernmost Tip of the Carpathians Constrained by Biostratigraphy and Authigenic 10be/9be Dating (Central Europe) JF - RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA J2 - RIV IT PALEON STRATIG VL - 127 PY - 2021 IS - 3 SP - 627 EP - 653 PG - 27 SN - 0035-6883 DO - 10.13130/2039-4942/16620 UR - https://m2.mtmt.hu/api/publication/32461594 ID - 32461594 N1 - Funding Agency and Grant Number: Slovak Research and Development Agency (APVV)Slovak Research and Development Agency [APVV-15-0575, APVV-16-0121, APVV-16-0146, APVV-20-0120, SK-FR-2015-0017, SK-AT-2017-0010]; Scientific Grant Agency of the Ministry of Education, Science, Research and Sport of the Slovak Republic [2-0122-18]; Slovak Academy of Sciences (VEGA)Vedecka grantova agentura MSVVaS SR a SAV (VEGA) [2-0122-18]; INSU/CNRSCentre National de la Recherche Scientifique (CNRS); ANR through the "Projets thematiques d'excellence" program for the "Equipements d'excellence" ASTER-CEREGE actionFrench National Research Agency (ANR); IRD Funding text: The geophysical equipment was provided by the science Park of the comenius university in Bratislava, and is acknowledged with gratitude. maria Bielikova, the former Dean of the Faculty of informatics and information technologies of the slovak technical university is thanked for her kind agreement to the excavations behind the faculty building. The study was supported financially by the Slovak research and Development agency (aPvv) under contracts Nos. aPvv-15-0575, aPvv-16-0121, aPvv-160146, aPvv-20-0120, SK-Fr-2015-0017 and SK-aT-2017-0010, and by the Scientific Grant agency of the ministry of Education, science, Research and sport of the slovak Republic and the slovak academy of Sciences (vEGa) under the contract No. 2-0122-18. The aSTEr amS national facility (cErEGE, aix-en-Provence) is supported by the iNSu/cNrS, the aNr through the "Projets thematiques d'excellence" program for the "Equipements d'excellence" aSTEr-cErEGE action and irD. Two anonymous reviewers provided very constructive and helpful comments, which significantly improved the overall quality of the manuscript; these, also, are acknowledged with gratitude. Paul Thatcher is thanked for his efforts made during the language correction. LA - English DB - MTMT ER - TY - JOUR AU - Koroknai, B AU - Wórum, G AU - Tóth, T AU - Koroknai, Zs AU - Fekete-Németh, V AU - Kovács, Gábor TI - Geological deformations in the Pannonian Basin during the neotectonic phase: New insights from the latest regional mapping in Hungary JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 211 PY - 2020 PG - 30 SN - 0012-8252 DO - 10.1016/j.earscirev.2020.103411 UR - https://m2.mtmt.hu/api/publication/31640869 ID - 31640869 LA - English DB - MTMT ER - TY - JOUR AU - Sebe, Krisztina AU - Kovačić, M AU - Magyar, Imre AU - Krizmanić, K AU - Špelić, M AU - Bigunac, D AU - Sütő-Szentai, M AU - Kovács, Ádám AU - Szuromi-Korecz, A AU - Bakrač, K AU - Hajek-Tadesse, V AU - Troskot-Čorbić, T AU - Sztanó, Orsolya TI - Correlation of upper Miocene-Pliocene Lake Pannon deposits across the Drava Basin, Croatia and Hungary JF - GEOLOGIA CROATICA J2 - GEOL CROAT VL - 73 PY - 2020 IS - 3 SP - 177 EP - 195 PG - 19 SN - 1330-030X DO - 10.4154/gc.2020.12 UR - https://m2.mtmt.hu/api/publication/31646422 ID - 31646422 N1 - University of Pécs, Department of Geology and Meteorology, Ifjúság ú. 6, Pécs, 7624, Hungary University of Zagreb, Faculty of Science, Department of Geology, Horvatovac 95, Zagreb, 10000, Croatia MOL Hungarian Oil and Gas Plc, Október huszonharmadika utca 18, Budapest, 1117, Hungary MTA-MTM-ELTE Research Group for Paleontology, Budapest, Hungary INA-Oil Company, Plc. Exploration and Production Exploration and Upstream portfolio development, Lovinčićeva 4, Zagreb, 10 000, Croatia Croatian Geological Survey, Department of Geology, Sachsova 2, Zagreb, 10000, Croatia INA-Oil Company, Plc. Exploration and Production, Field Development, V. Holjevca 10, Zagreb, Croatia Május 1 utca 7, Komló, 7300, Hungary Eötvös Loránd University, Department of Geology, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary MOL Group EandP Laboratory, Szent István út 14, Budapest, 1039, Hungary Export Date: 1 December 2020 LA - English DB - MTMT ER - TY - JOUR AU - Fodor, László TI - Results, problems and future tasks of palaeostress and fault-slip analyses in the Pannonian Basin: the Hungarian contribution JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 149 PY - 2019 IS - 4 SP - 297 EP - 326 PG - 30 SN - 0015-542X DO - 10.23928/foldt.kozl.2019.149.4.297 UR - https://m2.mtmt.hu/api/publication/30852034 ID - 30852034 N1 - Export Date: 27 November 2019 Correspondence Address: Fodor, L.; MTA-ELTE Geological, Geophysical and Space Science Research Group, Pázmány P. sétány 1/C, Hungary; email: lasz.Fodor@yahoo.com LA - English DB - MTMT ER -