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Journal articles on the topic 'Karpatian'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

Gebhardt, Holger, Bettina Schenk, Annekatrin Enge, Stjepan Ćorić, Eva-Maria Ranftl, and Petra Heinz. "The Lower - Middle Miocene transition (Karpatian – Badenian) in the Krems Embayment (Central Paratethys, Lower Austria): a multistrati-graphic approach and the role of the Diendorf-Boskovice Fault System." Austrian Journal of Earth Sciences 116, no. 1 (2023): 117–34. http://dx.doi.org/10.17738/ajes.2023.0006.

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Abstract The Krems Embayment contains the westernmost fully marine depositional environments of the Karpatian and Bade-nian transgressions in the Central Paratethys. Four drill cores were investigated to analyse the bio- and lithostratigraphic, and tectonic relations. The investigated core sections cover the Karpatian Laa Formation (bio-zones M4, NN4) and the Badenian Gaindorf Formation (M5b-M6, NN4-NN5). Important biostratigraphic indicators identified are Praeorbulina glomerosa glomerosa, Praeorbulina glomerosa circularis and Orbulina suturalis for the Gaindorf Formation. The Laa Formation i

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2

Hajek-Tadesse, Valentina, Mirko Belak, Jasenka Sremac, Davor Vrsaljko, and Lara Wacha. "Early Miocene ostracods from the Sadovi section (Mt Požeška gora, Croatia)." Geologica Carpathica 60, no. 3 (2009): 251–62. http://dx.doi.org/10.2478/v10096-009-0017-0.

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Early Miocene ostracods from the Sadovi section (Mt Požeška gora, Croatia)The study of the Early Miocene (Late Ottnangian/Early Karpatian) ostracod fauna from the Sadovi section (Mt Požeška gora, Croatia) led to several results concerning Neogene paleobiogeography and paleoecology. Brackish deposits of Late Ottnangian and Early Karpatian age have been recognized for the first time in the North Croatian Basin. These deposits indicate the first marine ingression into the Early Miocene lake in this area. Twenty-nine ostracod species were determined, including the new taxaFabaeformiscandona slavon

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3

Palzer-Khomenko, Markus, Michael Wagreich, Mădălina-Elena Kallanxhi, et al. "Facies, palaeogeography and stratigraphy of the lower Miocene Traisen Formation and Wildendürnbach Formation (former “Oncophora Beds”) in the Molasse Zone of Lower Austria." Austrian Journal of Earth Sciences 111, no. 1 (2018): 75–91. http://dx.doi.org/10.17738/ajes.2018.0006.

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Abstract A detailed study of OMV wells throughout the Lower Austrian Molasse Basin demonstrates the existence of a distinct and synchronous upper Ottnangian (lower Miocene) stratigraphic signal, the Calcite Minimum Interval (CMI). It corresponds to the depositional phase of the Rzehakia Lake System. This signal is interpreted to be of chronostratigraphic importance as an expression of palaeoclimate and related sea-level change. It is represented by the brackish Traisen Formation, which crops out south of the Danube. The Traisen Formation correlates with sands and shales in OMV wells to the nor

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GRANADO, P., W. THÖNY, N. CARRERA, O. GRATZER, P. STRAUSS, and J. A. MUÑOZ. "Basement-involved reactivation in foreland fold-and-thrust belts: the Alpine–Carpathian Junction (Austria)." Geological Magazine 153, no. 5-6 (2016): 1110–35. http://dx.doi.org/10.1017/s0016756816000066.

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AbstractThe late Eocene – early Miocene Alpine–Carpathian fold-and-thrust belt (FTB) lies in the transition between the Eastern Alps and the Western Carpathians, SE of the Bohemian crystalline massif. Our study shows the involvement of crystalline basement from the former European Jurassic continental margin in two distinct events. A first extensional event coeval with Eggerian–Karpatian (c. 28–16 Ma) thin-skinned thrusting reactivated the rift basement fault array and resulted from the large degree of lower plate bending promoted by high lateral gradients of lithospheric strength and slab pul

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Gašparič, Rok, Dale Tshudy, Tin-Yam Chan, and Stjepan Ćorić. "A new deepwater lobster, Metanephrops serendipitus sp. nov. (Crustacea, Decapoda, Nephropidae), from lower Miocene of Meljski hrib (Maribor, Slovenia)." Boletín de la Sociedad Geológica Mexicana 73, no. 3 (2021): A240521. http://dx.doi.org/10.18268/bsgm2021v73n3a240521.

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A new species of nephropid lobster, Metanephrops serendipitus sp. nov., is described from the lower Miocene (Ottnangian/Karpatian) in beds of Central Paratethys. Metanephrops serendipitus sp. nov. represents the first fossil representative of the genus from the northern hemisphere and thus extends its known palaeobiogeographical distribution. Additionally, the palaeoecology of the new species is discussed. Similar to extant species of Metanephrops, the fossil nephropid inhabited a fine-grained deep-sea environment, associated with frequent brittle stars.

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6

Hyžný, Matúš, Mathias Harzhauser, and Wolfgang Danninger. "Decapod Crustacea of the Central Paratethyan Ottnangian Stage (middle Burdigalian): implications for systematics and biogeography." Geologica Carpathica 66, no. 3 (2015): 217–33. http://dx.doi.org/10.1515/geoca-2015-0021.

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AbstractDecapod crustaceans from the Ottnangian (middle Burdigalian, Lower Miocene) of the Western and Central Paratethys remain poorly known. In this study, we review and re-describe mud shrimps (Jaxea kuemeli), ghost shrimps (Gourretiasp.,Calliax michelottii) and brachyuran crabs of the families Leucosiidae, Polybiidae and Portunidae. A dorsal carapace of the genusCalliaxis reported for the first time in the fossil record. Re-examination of the type material ofRandallia strouhali(Leucosiidae) andGeryon ottnangensis(Geryonidae) resulted in a transfer of these species intoPalaeomyra(Leucosiida

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7

Pelech, Ondrej, Katarína Žecová, Michal Jamrich, et al. "Trenčianska kotlina and Ilavská kotlina basins – Remnants of an inverted Early Miocene wedge top basin (Western Carpathians, Slovakia)." Mineralia Slovaca 52, no. 1 (2020): 1–22. https://doi.org/10.5281/zenodo.3994146.

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Paper summarizes the latest knowledge about the Early Miocene Trenčianska kotlina and Ilavská kotlina basins, Slovakia. The studied basins are located at the boundary between the Internal and External Western Carpathians and overlie the Pieniny Klippen Belt and Internal Carpathian Mesozoic nappes (Tatricum, Fatricum and Hronicum). This research is based on the results of geological mapping in the northwestern Trenčianska kotlina Basin and westernmost part of the Ilavská kotlina Basin and summarizes all previous (bio)stratigraphic, sedimentological, geophysical and borehole (PB-1,

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8

Ivančič, Kristina, Mirka Trajanova, Stjepan Ćorić, Boštjan Rožič, and Andrej Šmuc. "Miocene paleogeography and biostratigraphy of the Slovenj Gradec Basin: a marine corridor between the Mediterranean and Central Paratethys." Geologica Carpathica 69, no. 6 (2018): 528–44. http://dx.doi.org/10.1515/geoca-2018-0031.

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Abstract The Miocene evolution of the area transitional from the Eastern Alps to the Pannonian Basin System was studied through the paleogeographic evolution of the Slovenj Gradec Basin in northern Slovenia. It is based on mapping, section logging, nannoplankton biostratigraphy, and petrography. The results are correlated with the lithological column of the borehole MD-1/05. The evolution of the basin is connected with the development of the Pannonian Basin System, and the global 3rd order cycles, which influenced the connection with the Mediterranean Sea. Sedimentation started in the Karpatia

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Piller, Werner E., Mathias Harzhauser, and Oleg Mandic. "Miocene Central Paratethys stratigraphy – current status and future directions." Stratigraphy 4, no. 2-3 (2007): 151–68. http://dx.doi.org/10.29041/strat.04.2.09.

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The complex geodynamic history of the Paratethys periodically fostered the evolution of a highly endemic biota with only limited exchange between the neighboring Mediterranean and Indo-Pacific provinces. The resulting very peculiar fossil assemblages forced the introduction of a regional chronostratigraphic subdivision for the Western/Central and Eastern Paratethys respectively. For the Central Paratethys we present a summarized and updated database for the individual stages, and we review the current status for correlation with the Mediterranean stratigraphic framework. The Miocene Central Pa

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Tibljaš, Darko, Vanja Loparić, and Mirko Belak. "Discriminant Function Analysis of Miocene Volcaniclastic Rocks from North-Western Croatia Based on Geochemical Data." Geologia Croatica 55, no. 1 (2002): 39–44. http://dx.doi.org/10.4154/gc.2002.04.

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Preliminary results of discriminant function analysis of geochemical data of Miocene volcanic and volcaniclastic rocks revealed that it ispossible to distinguish rocks of different ages, namely Egerian -Eggenburgian, Karpatian and Badenian. On the basis of calculated coefficients of classification functions, presented in the paper, it is possible to indicate the age of Miocene volcanic and volcaniclastic rocks if their trace element content is known. The analysis also showed that, especially in the case of volcaniclastic rocks, the mineral and petrological composition of the rocks should also

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11

Šarinová, Katarína, Samuel Rybár, Fred Jourdan, et al. "40Ar/39Ar geochronology of Burdigalian paleobotanical localities in the central Paratethys (south Slovakia)." Geologica Acta 19 (May 21, 2021): 1–19. http://dx.doi.org/10.1344/geologicaacta2021.19.5.

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The Lipovany and Mučín paleobotanical localities contain important floral associations within the tuff horizons, which were used for determination of subtropical to tropical climatic conditions during the Early Miocene. Based on the combination of results from plagioclase and biotite 40Ar/39Ar dating, the age of the tuff deposition is around 17.3Ma. For the Lipovany locality, single-grain 40Ar/39Ar convergent ages of 17.49±0.54Ma and 17.28±0.06Ma, for plagioclase and biotite were obtained, respectively. The Mučín locality only provide an imprecise convergent age of 16.5±1.4Ma due to the small

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12

Hyžný, Matúš. "Diversity and distribution patterns of the Oligocene and Miocene decapod crustaceans (Crustacea: Malacostraca) of the Western and Central Paratethys." Geologica Carpathica 67, no. 5 (2016): 471–94. http://dx.doi.org/10.1515/geoca-2016-0030.

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AbstractDecapod associations have been significant components of marine habitats throughout the Cenozoic when the major diversification of the group occurred. In this respect, the circum-Mediterranean area is of particular interest due to its complex palaeogeographic history. During the Oligo-Miocene, it was divided in two major areas, Mediterranean and Paratethys. Decapod crustaceans from the Paratethys Sea have been reported in the literature since the 19thcentury, but only recent research advances allow evaluation of the diversity and distribution patterns of the group. Altogether 176 speci

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13

Reichenbacher, Bettina, Daniel Kälin, and Jürg Jost. "A fourth St. Gallen Formation cycle (?) in the Karpatian Upper Marine Molasse of central Switzerland." Facies 51, no. 1-4 (2005): 160–72. http://dx.doi.org/10.1007/s10347-005-0056-7.

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14

Harzhauser, Mathias, Matthias Kranner, Oleg Mandic, Philipp Strauss, Wolfgang Siedl, and Werner E. Piller. "Miocene lithostratigraphy of the northern and central Vienna Basin (Austria)." Austrian Journal of Earth Sciences 113, no. 1-2 (2020): 169–99. http://dx.doi.org/10.17738/ajes.2020.0011.

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Abstract For the first time, a concise lithostratigraphic scheme for the lower and middle Miocene (Ottnangian – Badenian) of the northern and central Vienna Basin is proposed, which is based on the integration of core-material, well-log data and seismic information from OMV. For all formations and members type sections are proposed, geographic distribution and thickness are provided, typical depositional environments and fossils are described and age constraints are discussed. This time frame allows for a more reliable calculation of sedimentation rates. This in turn might be important for the

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15

Hohenegger, Johann, Stjepan Ćorić, and Michael Wagreich. "Timing of the Middle Miocene Badenian Stage of the Central Paratethys." Geologica Carpathica 65, no. 1 (2014): 55–66. http://dx.doi.org/10.2478/geoca-2014-0004.

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Abstract A new and precisely defined chronometric subdivision of the Badenian (Middle Miocene, regional stage of Central Paratethys) is proposed. This uses global events, mainly geomagnetic polarity reversals as correlated chronometric boundaries, supported by climatic and sea-level changes in addition to isotope events and biostratigraphic data. The Karpatian/ Badenian boundary lies at 16.303 Ma, at the top of Chron C5Cn.2n, which is near the base of the Praeorbulina sicana Lowest-occurrence Zone (LOZ). The Badenian/Sarmatian boundary is placed at the top of polarity Chron C5Ar.2n, thus at 12

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Prokop, Jakub, Günther Fleck, and André Nel. "New dragonflies from the Lower Miocene (Ottnangian/Karpatian) of the Cypris Shale in western Bohemia (Odonata: Libellulidae)." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2003, no. 9 (2003): 561–76. http://dx.doi.org/10.1127/njgpm/2003/2003/561.

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17

Görög, Ágnes, Eszter Balassi, and Tamás Váczi. "Nothia ex gr. excelsa (Grzybowski, 1898), ‘flysch-type’ agglutinated foraminifera from the Karpatian (Early-Miocene) of Hungary." Historical Biology 30, no. 3 (2017): 327–35. http://dx.doi.org/10.1080/08912963.2016.1278444.

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18

Reichenbacher, Bettina, Wout Krijgsman, Yannick Lataster, et al. "A new magnetostratigraphic framework for the Lower Miocene (Burdigalian/Ottnangian, Karpatian) in the North Alpine Foreland Basin." Swiss Journal of Geosciences 106, no. 2 (2013): 309–34. http://dx.doi.org/10.1007/s00015-013-0142-8.

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19

Rundic, Ljupko, Nebojsa Vasic, Miodrag Banjesevic, et al. "Facies analyses, biostratigraphy and radiometric dating of the Lower-Middle Miocene succession near Zajecar (Dacian basin, eastern Serbia)." Annales g?ologiques de la Peninsule balkanique 80, no. 2 (2019): 13–37. http://dx.doi.org/10.2298/gabp1902013r.

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Lower-Middle Miocene sedimentary succession and the conformable/ unconformable relationships between the lacustrine-continental systems (i.e. DLS, SLS) and Badenian marine transgression represents one of the intrigue topics. Herein, we studied five exploration boreholes (eastern Serbia) and analyzed the main facies pattern, biostratigraphic characteristics of the Miocene succession, and applied the U-Pb radiometric dating of volcanic tuffs interstratified in the sedimentary series with coal layers (borehole NRKR- 17002). The obtained concordia age of 16.9 ?0.2 Ma for all the analysed zircon gr

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Kvaček, Zlatko, Vasilis Teodoridis, Marianna Kováčová, Ján Schlögl, and Viliam Sitár. "Lower Miocene plant assemblage with coastal-marsh herbaceous monocots from the Vienna Basin (Slovakia)." Geologica Carpathica 65, no. 3 (2014): 229–41. http://dx.doi.org/10.2478/geoca-2014-0016.

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Abstract A new plant assemblage of Cerová-Lieskové from Lower Miocene (Karpatian) deposits in the Vienna Basin (western Slovakia) is preserved in a relatively deep, upper-slope marine environment. Depositional conditions with high sedimentation rates allowed exceptional preservation of plant remains. The plant assemblage consists of (1) conifers represented by foliage of Pinus hepios and Tetraclinis salicornioides, a seed cone of Pinus cf. ornata, and by pollen of the Cupressaceae, Pinaceae, Pinus sp. and Cathaya sp., and (2) angiosperms represented by Cinnamomum polymorphum, Platanus neptuni,

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Saftić, Bruno, Josipa Velić, Orsolya Sztano, Györgyi Juhasz, and Željko Ivković. "Tertiary Subsurface Facies, Source Rocks and Hydrocarbon Reservoirs in the SW Part of the Pannonian Basin (Northern Croatia and South-Western Hungary)." Geologia Croatica 56, no. 1 (2003): 101–22. http://dx.doi.org/10.4154/232.

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The Neogene sedimentary successions of the Drava, Sava and Slavonija–Srijem depressions in the SW part of the Pannonian Basin Systemare built up of three 2nd order megacycles separated by four majorerosional unconformities. The first megacycle contains terrestrial tomarine syn-rift and early post-rift sediments of Early to Mid-Mioceneage. The second is built up of Late Miocene Lake Pannon deposits,while the third contains those sediments which were deposited inthe remnants of Lake Pannon and in the subsequent fluvial systems,in areas of continuous subsidence associated with basin inversionfrom

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Spezzaferri, Silvia, Stjepan Coric, Johann Hohenegger, and Fred Rögl. "Basin-scale paleobiogeography and paleoecology: an example from Karpatian (Latest Burdigalian) benthic and planktonic foraminifera and calcareous nannofossils from the Central Paratethys." Geobios 35 (December 2002): 241–56. http://dx.doi.org/10.1016/s0016-6995(02)00063-3.

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23

Meszar, Maria, Susanne Gier, Markus Palzer-Khomenko, Wolfgang Knierzinger, and Michael Wagreich. "Clay mineralogy of Miocene mudstones from the Lower Austrian Molasse Basin." Austrian Journal of Earth Sciences 113, no. 1 (2020): 125–38. http://dx.doi.org/10.17738/ajes.2020.0008.

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Abstract Recent studies established the lithological and chemical sediment evolution in the Lower Austrian Molasse Basin (LAMB), a part of the North Alpine foreland basin, during the Early Miocene. In this study, we aim to integrate the clay mineralogy of seven wells across the LAMB with a newly proposed lithostratigraphy, and to infer implications for provenance, palaeo-geography and palaeoclimate. The results of our qualitative and quantitative evaluation of the clay-sized fraction with x-ray diffractometry largely support the stratigraphic model. The early stage of foreland basin formation

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Gusterhuber, Juergen, István Dunkl, Ralph Hinsch, Hans-Gert Linzer, and Reinhard Sachsenhofer. "Neogene uplift and erosion in the Alpine Foreland Basin (Upper Austria and Salzburg)." Geologica Carpathica 63, no. 4 (2012): 295–305. http://dx.doi.org/10.2478/v10096-012-0023-5.

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Neogene uplift and erosion in the Alpine Foreland Basin (Upper Austria and Salzburg)In the present paper we apply a multi-technique approach (shale compaction data, seismic stratigraphy, isopach maps, moisture content of lignite, fission track data) to assess timing and amount of uplift and erosion of the Alpine Foreland Basin. The combination of the different techniques allows us to discriminate the effects of two different erosion events during the Neogene: (1) Seismic stratigraphy and isopach maps indicate a Karpatian (Early Miocene) regional tilting of the basin to the west (slope of about

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Hók, Jozef, Michal Kováč, Ondrej Pelech, Ivana Pešková, Rastislav Vojtko, and Silvia Králiková. "The Alpine tectonic evolution of the Danube Basin and its northern periphery (southwestern Slovakia)." Geologica Carpathica 67, no. 5 (2016): 495–505. http://dx.doi.org/10.1515/geoca-2016-0031.

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AbstractThe tectonic evolution of the pre-Cenozoic basement, as well as the Cenozoic structures within the Danube Basin (DB) and its northern periphery are presented. The lowermost portion of the pre-Cenozoic basement is formed by the Tatricum Unit which was tectonically affected by the subduction of the Vahicum / Penninicum distal continental crust during the Turonian. Tectonically disintegrated Tatricum overlaid the post-Turonian to Lower Eocene sediments that are considered a part of the Vahicum wedge-top basin. These sediments are overthrust with the Fatricum and Hronicum cover nappes. The

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Palzer-Khomenko, Markus, Michael Wagreich, Wolfgang Knierzinger, et al. "A calcite crisis unravelling Early Miocene (Ottnangian) stratigraphy in the North Alpine–Carpathian Foreland Basin: a litho- and chemostratigraphic marker for the Rzehakia Lake System." Geologica Carpathica 69, no. 4 (2018): 315–34. http://dx.doi.org/10.1515/geoca-2018-0019.

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Abstract Within the Lower Austrian part of the North Alpine Foreland Basin (NAFB), up to 1000 m of sediments were deposited throughout the Ottnangian (Early Miocene, Burdigalian). According to homogeneous compositions and sparse biostratigraphic resolution, a consistent stratigraphic concept from the basin margins into the foreland depocenter was still lacking. New investigations on several deep drill cores throughout the basin provide comprehensive sedimentological, mineralogical, chemical and micropaleontological data. A calcite poor, fossil- and pyrite-free, smectite-rich, up to 800 m thick

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Reichenbacher, Bettina, and Jerome Prieto. "Lacustrine fish faunas (Teleostei) from the Karpatian of the northern Alpine Molasse Basin, with a description of two new species of Prolebias Sauvage." Palaeontographica Abteilung A 278, no. 1-6 (2006): 87–95. http://dx.doi.org/10.1127/pala/278/2006/87.

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Nazarchuk, Oleksandr, and Pavlo Satskyi. "KARPATIAN UKRAINE AS A FACTOR IN THE PROCESS OF TRANSFORMATION THE POLITICAL CONFIGURATION IN CENTRAL EUROPE ON THE EVE OF WORLD WAR II." Kyiv Historical Studies, no. 2 (2019): 74–82. http://dx.doi.org/10.28925/2524-0757.2019.2.9.

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Pavelić, Davor. "ALLUVIAL-LACUSTRINE-MARINE COMPLEX OF MOUNT MEDVEDNICA: THE EARLY SYN-RIFT DEPOSITION AND PALAEOGEOGRAPHY (EARLY TO MIDDLE MIOCENE, NORTH CROATIAN BASIN)." Rudarsko-geološko-naftni zbornik 39, no. 1 (2024): 65–85. http://dx.doi.org/10.17794/rgn.2024.1.7.

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Mt. Medvednica belongs to the western part of the Neogene rift-type North Croatian Basin that occupies the south-western Pannonian Basin System. The Lower to Middle Miocene continental to marine sedimentary complex was studied on Mt. Medvednica in order to interpret the early syn-rift depositional environment and reconstruct palaeogeography of the North Croatian Basin. Based on facies analysis, deposits are grouped into 16 facies based on their lithological characteristics. Six of the facies belong to the alluvial environment that is characterized by coarse-grained bedload siliciclastics. Nine

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Lemberkovics, Viktor, Edina Kissné Pável, Balázs Badics, Katalin Lőrincz, Alexander Rodionov, and Iskander Galimullin. "Petroleum system of Miocene troughs of the Pannonian Basin in southern Hungary, based on 3D basin modeling." Interpretation 6, no. 1 (2018): SB37—SB50. http://dx.doi.org/10.1190/int-2017-0075.1.

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The role of the Middle-Upper Miocene source rocks in the Late Neogene petroleum system of the Pannonian Basin is undoubtedly significant, but it is not entirely understood. Only a few general publications exist that describe these sediments and their importance. We have focused on understanding the Neogene tectono-stratigraphic development and petroleum systems of these relatively small syn-rift grabens in southern Hungary. We have developed a workflow for organic geochemical, seismic, and facies interpretation; basin subsidence; and 3D basin modeling to better understand the Miocene-Pliocene-

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Sóron, András Szabolcs. "Paleoenvironmental and stratigraphic investigations of the foraminiferal fauna from the Karpatian (Lower Miocene) Garáb Schlier Formation of the Mátraverebély-122 (Mv-122) borehole (North Hungary)." Central European Geology 54, no. 3 (2011): 211–31. http://dx.doi.org/10.1556/ceugeol.54.2011.3.1.

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Ivančič, Kristina, Miloš Bartol, Miha Marinšek, et al. "A review of the Neogene formations and beds in Slovenia, Western Central Paratethys." Geologija 67, no. 2 (2024): 193–215. https://doi.org/10.5474/geologija.2024.009.

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Neogene sedimentary successions are found in eastern and northeastern Slovenia. Their formation was closely related to the evolution of the western part of the Pannonian Basin System and the Central Paratethys; it was influenced by global transgressive and regressive cycles as well as by global, regional and local tectonics. Several formations and beds were defined within the Neogene sedimentary successions which can be found in three separate areas. The first one includes the formations north of two major fault systems, the Periadriatic Fault System and the Mid-Hungarian Zone, which were asso

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Sebe, Krisztina, Marton Szabo, Zoltan Szentesi, Luca Pandolfi, Noémi Jankó, and Imre Magyar. "Fossils from the Upper Miocene (Pannonian) sands of the Pécsvárad sand pit (Eastern Mecsek Mts., SW Hungary)." Annales g?ologiques de la Peninsule balkanique, no. 00 (2024): 7. http://dx.doi.org/10.2298/gabp240228007s.

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The Mecsek Mountains in SW Hungary represent an uplifted basement block of the Pannonian Basin. Their Neogene cover includes deposits both from the Middle Miocene Central Paratethys and from its Late Miocene (Pannonian) brackish-water descendant, Lake Pannon. Along the mountain front, the Pannonian sands of the Pecsvarad sand pit contain a mixed vertebrate fossil assemblage, which gives insight into terrestrial and aquatic biota during various time intervals of the Miocene. The fossil-bearing sands accumulated between 7.6-6.8 Ma, in a high-energy littoral setting of Lake Pannon, as indicated b

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Auer, G., W. E. Piller, and M. Harzhauser. "Two distinct decadal and centennial cyclicities forced marine upwelling intensity and precipitation during the late Early Miocene in Central Europe." Climate of the Past Discussions 10, no. 2 (2014): 1223–64. http://dx.doi.org/10.5194/cpd-10-1223-2014.

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Abstract. Within a 5.5 m-thick succession of Upper Burdigalian (Karpatian) sediments in the North Alpine Foreland Basin (NAFB; Austria), dated to CNP-zone NN4, a high-resolution section was logged continuously. 100 samples were taken with a resolution of ~10 mm per layer and analysed using an integrated multi-proxy approach. Earlier analyses of geochemistry and calcareous nannoplankton assemblages hint at small-scale, short-term variations in palaeoenvironmental conditions, such as water-column stratification, primary productivity, organic matter flux, bottom-water oxygenation, freshwater infl

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Auer, G., W. E. Piller, and M. Harzhauser. "Two distinct decadal and centennial cyclicities forced marine upwelling intensity and precipitation during the late Early Miocene in central Europe." Climate of the Past 11, no. 2 (2015): 283–303. http://dx.doi.org/10.5194/cp-11-283-2015.

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Abstract. Within a 5.5 m thick succession of Upper Burdigalian (Karpatian) sediments in the North Alpine Foreland Basin (NAFB; Austria), dated to CNP-zone NN4, a high-resolution section was logged continuously. One hundred samples were taken with a resolution of ~10 mm (approximating ~17 years) per layer and analyzed using an integrated multi-proxy approach. Earlier analyses of geochemistry and calcareous nannoplankton assemblages hint at small-scale, short-term variations in paleoenvironmental conditions, such as water-column stratification, primary productivity, organic matter flux, bottom-w

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Francírek, Michal, and Slavomír Nehyba. "Evolution of the passive margin of the peripheral foreland basin: an example from the Lower Miocene Carpathian Foredeep (Czech Republic)." Geologica Carpathica 67, no. 1 (2016): 41–68. http://dx.doi.org/10.1515/geoca-2016-0003.

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Abstract The Karpatian deposits of the central part of the Carpathian Foredeep in Moravia, which are deeply buried under the Outer Western Carpathians, provide a unique opportunity to reconstruct the former evolutionary stages of this peripheral foreland basin and its paleogeography. A succession of three depositional units characterized by a distinct depositional environment, provenance, and partly also foreland basin depozone, have been identified. The first depositional unit represents a proximal forebulge depozone and consists of lagoon-estuary and barred coastline deposits. The source fro

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Petrik, Attila, Barbara Beke, László Fodor, and Réka Lukács. "Cenozoic structural evolution of the southwestern Bükk Mts. and the southern part of the Darnó Deformation Belt (NE Hungary)." Geologica Carpathica 67, no. 1 (2016): 83–104. http://dx.doi.org/10.1515/geoca-2016-0005.

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Abstract Extensive structural field observations and seismic interpretation allowed us to delineate 7 deformation phases in the study area for the Cenozoic period. Phase D1 indicates NW–SE compression and perpendicular extension in the Late Oligocene–early Eggenburgian and it was responsible for the development of a wedge-shaped Paleogene sequence in front of north-westward propagating blind reverse faults. D2 is represented by E–W compression and perpendicular extension in the middle Eggenburgian–early Ottnangian. The D1 and D2 phases resulted in the erosion of Paleogene suites on elevated hi

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Nehyba, Slavomír. "Lower Badenian coarse-grained Gilbert deltas in the southern margin of the Western Carpathian Foredeep basin." Geologica Carpathica 69, no. 1 (2018): 89–113. http://dx.doi.org/10.1515/geoca-2018-0006.

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AbstractTwo coarse-grained Gilbert-type deltas in the Lower Badenian deposits along the southern margin of the Western Carpathian Foredeep (peripheral foreland basin) were newly interpreted. Facies characterizing a range of depositional processes are assigned to four facies associations — topset, foreset, bottomset and offshore marine pelagic deposits. The evidence of Gilbert deltas within open marine deposits reflects the formation of a basin with relatively steep margins connected with a relative sea level fall, erosion and incision. Formation, progradation and aggradation of the thick coars

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Grabowski, Jacek, Jozef Michalík, Andrzej Pszczółkowski, and Otília Lintnerová. "Magneto-, and isotope stratigraphy around the Jurassic/Cretaceous boundary in the Vysoká Unit (Malé Karpaty Mountains, Slovakia): correlations and tectonic implications." Geologica Carpathica 61, no. 4 (2010): 309–26. http://dx.doi.org/10.2478/v10096-010-0018-z.

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Magneto-, and isotope stratigraphy around the Jurassic/Cretaceous boundary in the Vysoká Unit (Malé Karpaty Mountains, Slovakia): correlations and tectonic implications Magneto- and isotope stratigraphic studies in the Vysoká Nappe (Hlboča section, Fatric Unit, Malé Karpaty Mts, Slovakia) were performed. A generally decreasing δ13C isotope curve is interpreted as a primary trend from the Late Oxfordian (3.3 ‰ V-PDB) to the Late Tithonian (1.8-1.4 ‰ V-PDB). Data from the Tithonian part of the Tegernsee Formation probably reflect "local" basin processes connected with the breccia formation in th

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Mohan, Gh. "Trochobryum carniolicum Breidl. & Beck., ein für die Bryoflora Rumäniens neu aufgefundenes Relikt." Feddes Repertorium 97, no. 5-6 (1986): 313–18. http://dx.doi.org/10.1002/j.1522-239x.1986.tb00307.x.

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ZusammenfassungBei Aufsammlungen im Rotnei‐Gebirge (nördlicher Teil der rumänischen Karpathen) fand der Autor eine Moosart – Trochobryum carniolocum Bheidl & Beck., die neu für die Karpathen und für die rumänische Bryoflora ist.

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Webster, Paul. "George Karpati." Lancet 373, no. 9671 (2009): 1246. http://dx.doi.org/10.1016/s0140-6736(09)60716-9.

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Paško, Oksana. "Krim, Karpaten, Capri." osteuropa 72, no. 6-8 (2022): 225. http://dx.doi.org/10.35998/oe-2022-0157.

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Krzeminski, Wieslaw, and Jakub Prokop. "Ptychoptera deleta Novák, 1877 from the Early Miocene of the Czech Republic: redescription of the first fossil attributed to Ptychopteridae (Diptera)." ZooKeys 130 (September 24, 2011): 299–305. https://doi.org/10.3897/zookeys.130.1401.

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The first fossil that was described in Ptychopteridae, <i>Ptychoptera deleta</i><b> </b>Novák, 1877 from the classical Early Miocene locality Mokřina (Krottensee) in western Bohemia is re-examined. The re-description of the holotype including a new line drawing and remarks summarizing the scarce fossil record of this group is provided.

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Sinnreich, Michael, and Frederick Andermann. "George Karpati (1934-2009)." Canadian Journal of Neurological Sciences / Journal Canadien des Sciences Neurologiques 36, no. 03 (2009): 282. http://dx.doi.org/10.1017/s0317167100006983.

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Hastings, Kenneth. "George Karpati (1934-2009)." Muscle & Nerve 40, no. 2 (2009): 169–70. http://dx.doi.org/10.1002/mus.21437.

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Zajączkowski, Maciej. "Die Reliktfohre in den polnischen Karpathen." Acta Societatis Botanicorum Poloniae 13, no. 1 (2017): 1–22. http://dx.doi.org/10.5586/asbp.1936.001.

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Coldea, Gh. "Phytozönologisches Studium der Krummholzgebüsche in den Südostkarpaten." Feddes Repertorium 96, no. 5-6 (1985): 397–405. http://dx.doi.org/10.1002/j.1522-239x.1985.tb00455.x.

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ZusammenfassungIn der Arbeit werden Ergebnisse eines vergleichenden phytozönologischen Studiums der Krummholzgebüsche aus den südöstlichen Karpaten im Vergleich mit den Krummholzgebüschen Zentraleuropas) und der Balkanhalbinsel gebracht. Auf der Grundlage von 45 eigenen phytozönologischen Aufnahmen, die in verschiedenen Gebirgsmassiven (Rodna, Căliman. Retezat‐Gebirge) vorgenommen wurden, und der 100 vollständigen, von verschiedenen rumänischen Botanikern veröffentlichten Aufnahmen aus einigen Gebirgszonen, bearbeitet der Verfasser das Rhododendro kotschyi‐Pinetum mugi Borza 1959 emend, h. 1.

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Schulte-Umberg, Thomas. "Serbien 1914, Karpaten – San – Bložewkasumpf 1915." Mitteilungen des Instituts für Österreichische Geschichtsforschung 127, no. 1 (2019): 88–140. http://dx.doi.org/10.7767/miog.2019.127.1.88.

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Täuber, Ferdinand. "Endemische Phytoassoziationen aus den Rumänischen Karpaten." Folia Geobotanica et Phytotaxonomica 20, no. 1 (1985): 1–16. http://dx.doi.org/10.1007/bf02856461.

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Rowland, Lewis P. "George Karpati, MD (1934–2009)." Journal of the Neurological Sciences 281, no. 1-2 (2009): 1. http://dx.doi.org/10.1016/j.jns.2009.02.372.

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