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Journal articles on the topic 'Ottnangian/Karpatian'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

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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2

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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3

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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4

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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5

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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6

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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7

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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8

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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9

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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10

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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11

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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12

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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13

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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14

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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15

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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16

Bubík, Miroslav, Jiří Otava, and Šárka Hladilová. "Záznam post-paleozoického geologického vývoje uchovaný v reliktech miocénu v Brně – Líšni." Geologické výzkumy na Moravě a ve Slezsku 26, no. 1-2 (2019). http://dx.doi.org/10.5817/gvms2019-1-2-16.

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Recent operation in the Kalcit Quarry near Brno-Líšeň exposed contact of Devonian limestones with overlying Miocene sediments. Calcareous silts with chert debris and non-calcareous clays fi lling the cleft s in the limestone are Middle Miocene in age (Lower Badenian). They contained association of translucent heavy minerals derived from Drahany Culmian formations and the Brno Massif. Fossil content comprised conodonts and foraminifers weathered off the Lower Carboniferous limestones, brackish gastropods reworked from the Rzehakia Beds (Ottnangian) and foraminifers reworked from Karpatian and L

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17

Harzhauser, Mathias, Matthias Kranner, Wolfgang Siedl, Florian Conradi, and Werner E. Piller. "The Neogene of the Vienna Basin – a synthesis." Geological Society, London, Special Publications 554, no. 1 (2024). http://dx.doi.org/10.1144/sp554-2023-168.

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We present a revision of geological and paleontological data of the Vienna Basin (VB). The deposits comprise Miocene terrestrial, lacustrine and marine sediments, corresponding the Ottnangian, Karpatian, Badenian, Sarmatian and Pannonian regional stages (= Burdigalian to Tortonian). New 3D seismics and the analyses of hundreds of core samples resulted in a wealth of information. Absolute ages were published for two tuffs and the lithostratigraphy was largely formalized. The evolution of the paleoenvironments in the VB strongly reflects the impact by global climatic events such as the Miocene C

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18

Kováč, Michal, Tamás Csibri, Klement Fordinál, et al. "The Miocene to Quaternary evolution of the Vienna Basin (northeastern part): Geodynamics, eustasy, stratigraphy and depositional systems." Geological Society, London, Special Publications 554, no. 1 (2024). http://dx.doi.org/10.1144/sp554-2024-31.

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Long-term research of the Vienna Basin (Central Europe) has resulted in multiple stratigraphic concepts, though these are at least in part mutually exclusive. This contribution aims to reconsider the available information on the northeastern Vienna Basin, located in Slovakia, to create a consistent stratigraphic model. Lithostratigraphic correlations based on benthic taxa - widely used elsewhere - are omitted, since these include inherently diachronous paleoecological zones. This presumption of diachroneity is further supported by the evidence of shelf-slope scale clinoforms. The following seq

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