TY - JOUR AU - Hably, Lilla AU - Sebe, Krisztina TI - A late Miocene termophilous flora from Pécs-Danitzpuszta, Mecsek Mts., Hungary JF - NEUES JAHRBUCH FÜR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN J2 - NEUES JAHRB GEOL P-A VL - 279 PY - 2016 IS - 3 SP - 261 EP - 271 PG - 11 SN - 0077-7749 DO - 10.1127/njgpa/2016/0554 UR - https://m2.mtmt.hu/api/publication/3022749 ID - 3022749 LA - English DB - MTMT ER - TY - CHAP AU - Sebe, Krisztina AU - Csillag, Gábor AU - Dulai, Alfréd AU - Gasparik, Mihály AU - Magyar, Imre AU - Selmeczi, Ildikó AU - Szabó, Márton AU - Sztanó, Orsolya AU - Szuromi-Korecz, A ED - Bartha, I-R ED - Kriván, Á ED - Magyar, Imre ED - Sebe, Krisztina TI - Neogene stratigraphy in the Mecsek region. Hetvehely, Badenian rocky shore and fossiliferous shorface sand TS - Hetvehely, Badenian rocky shore and fossiliferous shorface sand T2 - Neogene of the Paratethyan Region: 6th Workshop on the Neogene of Central and South-Eastern Europe. An RCMNS Interim Colloquium PB - Magyarhoni Földtani Társulat CY - Budapest SN - 9789638221575 PY - 2015 SP - 102 EP - 124 PG - 23 UR - https://m2.mtmt.hu/api/publication/2906290 ID - 2906290 LA - English DB - MTMT ER - TY - CHAP AU - Sebe, Krisztina AU - Magyar, Imre AU - Csillag, Gábor AU - Sztanó, Orsolya ED - Dályay, Virág ED - Sámson, Margit TI - A mecseki pannóniai üledékek rétegtana: új adatok, eredmények és kérdések T2 - Tisia Konferencia PB - Molnár Nyomda és Kiadó CY - Pécs SN - 9789638221568 PY - 2015 SP - 72 EP - 76 PG - 5 UR - https://m2.mtmt.hu/api/publication/2852176 ID - 2852176 LA - Hungarian DB - MTMT ER - TY - CHAP AU - Magyar, Imre AU - Geary, DH ED - Baganz, OW ED - Bartov, Y ED - Bohacs, K ED - Nummedal, D TI - Biostratigraphy in a late Neogene Caspian-Type Lacustrine Basin: Lake Pannon, Hungary T2 - Lacustrine sandstone reservoirs and hydrocarbon systems PB - American Association of Petroleum Geologists (AAPG) CY - Tulsa (OK) SN - 9780891813774 T3 - AAPG Memoir, ISSN 0271-8529 ; 95. PY - 2012 SP - 255 EP - 264 PG - 10 DO - 10.1306/13291392M953142 UR - https://m2.mtmt.hu/api/publication/2145538 ID - 2145538 N1 - Cited By :33 Export Date: 15 February 2022 LA - English DB - MTMT ER - TY - JOUR AU - Erdei, Boglárka AU - Hably, Lilla AU - Kázmér, Miklós AU - Utescher, T AU - Bruch, AA TI - Neogene flora and vegetation development of the Pannonian domain in relation to palaeoclimate and palaeogeography JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 253 PY - 2007 IS - 1-2 SP - 115 EP - 140 PG - 26 SN - 0031-0182 DO - 10.1016/j.palaeo.2007.03.036 UR - https://m2.mtmt.hu/api/publication/1782867 ID - 1782867 N1 - Botanical Department, Hungarian Natural History Museum, P.O.Box 222, H-1476 Budapest, Hungary Department of Palaeontology, Eötvös Lóránd University, P.O.Box 120, H-1518 Budapest, Hungary Institut für Geologie, Nussallee 8, 53115 Bonn, Germany Senckenberg Research Institute, Senckenberganlage 25, 60325 Frankfurt am Main, Germany Cited By :87 Export Date: 24 February 2023 CODEN: PPPYA Correspondence Address: Erdei, B.; Botanical Department, P.O.Box 222, H-1476 Budapest, Hungary; email: erdei@bot.nhmus.hu AB - A survey of the Neogene flora and vegetation pattern of the Pannonian domain based on selected fossil plant assemblages is given. The paper aims to reveal the complex interrelation of tectonic-palaeogeographic evolution, climate, flora and vegetation development through the Neogene of the Pannonian domain. Flora and vegetation patterns are based on well-documented and studied fossil plant assemblages (macrofloras, primarily leaves). There are time intervals well-represented in the fossil record, e.g. the Pannonian or the Sarmatian and others with relatively few localities, e.g. the Badenian. A general but slow cooling trend is definitely observable after the Early Miocene as reflected by both quantitative climate reconstructions and floristic change, i.e. decrease of diversity, slow disappearance of thermophilous and exotic elements, as well as decrease in the variety of vegetation types. A significant decline of coldest month temperatures (as compared to warmest month temperatures) must have played a defining role in forming flora and vegetation through the Neogene. As compared to climate estimates for the Middle/Late Miocene fossil floras, warmer climate conditions are indicated by the Ipolytarnoc flora and vegetation comprising an extremely high number of thermophilous taxa as well as complex vegetation structure. The Early and Middle Miocene fossil assemblages bear a significant relevance to the tectonic pattern of the Pannonian domain. A transitional character in both flora and vegetation is indicated by the Karpatian Magyaregregy locality. Knowledge of the Badenian flora and vegetation is limited to the Middle Badenian Nogradszakal assemblage indicating cooler climate conditions which contrasts with global climate change. In contrast to the relatively poor azonal vegetation of Nogradszakal and most Pannonian localities, the more diverse Sarmatian and Pliocene floras display a strong relation to each other - attributable to palaeogeographic constraints. (C) 2007 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Magyar, Imre AU - Geary, DH AU - Muller, P TI - Paleogeographic evolution of the Late Miocene Lake Pannon in Central Europe JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 147 PY - 1999 IS - 3-4 SP - 151 EP - 167 PG - 17 SN - 0031-0182 DO - 10.1016/S0031-0182(98)00155-2 UR - https://m2.mtmt.hu/api/publication/1890263 ID - 1890263 N1 - Cited By :351 Export Date: 24 February 2023 CODEN: PPPYA Correspondence Address: Geary, D.H.; Department of Geology and Geophysics, 1215 West Dayton Street, Madison, WI 53706, United States; email: dana@geology.wisc.edu AB - The paleogeographic evolution of Lake Pannon within the Pannonian basin is reconstructed with eight maps, ranging from the Middle Miocene to the Early Pliocene. The maps are based on the distribution of selected biozones and specific fossils, and on complementary sedimentological and seismic information. Our reconstruction shows that the history of Lake Pannon can be divided into three distinct intervals: an initial stage with low water level, which resulted in isolation from the sea at about 12 Ma and might have led to temporary fragmentation of the lake; an interval of gradual transgression lasting until ca. 9.5 Ma; and a long late interval of shrinkage and infilling of sediments that persisted into the Early Pliocene. The deep subbasins of the lake formed during the transgressive interval, in more basinward locations than the deep basins of the preceding Sarmatian age. The southern shoreline, running parallel with the Sava and Danube rivers along the northern foot of the Dinarides, changed very Little during the Lifetime of the lake, while the northern shoreline underwent profound changes. (C) 1999 Elsevier Science B.V. All rights reserved. LA - English DB - MTMT ER -