HARZHAUSER, Mathias, Johanna KOVAR-EDER, Slavomír NEHYBA, Margit STROBITZER-HERMANN, Jurgen SCHWARZ, Jan WOJCICKI and Irene ZORN. An Early Pannonian (Late Miocene) transgression in the Northern Vienna Basin. The paleoecological feedback. Geologica Carpathica. Bratislava, 2003, vol. 54, No 1, p. 41-52. ISSN 1335-0552.
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Basic information
Original name An Early Pannonian (Late Miocene) transgression in the Northern Vienna Basin. The paleoecological feedback.
Authors HARZHAUSER, Mathias (40 Austria, guarantor), Johanna KOVAR-EDER (40 Austria), Slavomír NEHYBA (203 Czech Republic), Margit STROBITZER-HERMANN (40 Austria), Jurgen SCHWARZ (276 Germany), Jan WOJCICKI (616 Poland) and Irene ZORN (40 Austria).
Edition Geologica Carpathica, Bratislava, 2003, 1335-0552.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Slovakia
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 0.397
RIV identification code RIV/00216224:14310/03:00030514
Organization unit Faculty of Science
Keywords in English Late Miocene; Pannonian; Lake Pannon; Northern Vienna Basin; hydrophytes; paleoecology
Tags hydrophytes, Lake Pannon, Late Miocene, Northern Vienna Basin, paleoecology, Pannonian
Changed by Changed by: prof. RNDr. Slavomír Nehyba, Dr., učo 2710. Changed: 27/3/2010 10:50.
Abstract
The studied sections are situated on the northwestern margin of the Vienna Basin. They represent a characteristic marginal facies of Lake Pannon in the late Miocene Pannonian stage. Biofacies as well as lithofacies point to a transgressive event resulting in the shift from deltaic, riverine conditions to the formation of freshwater marshes and lakes and, finally, in the deposition of offshore clays. Biostratigraphically, the logged sequences correspond to the regional Pannonian mollusc zone C. The extraordinarily fine-scaled Paleoecological resolution might serve as a basis for a correlation of 4th order changes reported from basinal settings of the northern Vienna Basin. Thus the rapid facies succession on the northwestern margin of the Vienna Basin is interpreted as being linked to major lake level changes rather than to solely local changes in the riverine system.
Abstract (in Czech)
The studied sections are situated on the northwestern margin of the Vienna Basin. They represent a characteristic marginal facies of Lake Pannon in the late Miocene Pannonian stage. Biofacies as well as lithofacies point to a transgressive event resulting in the shift from deltaic, riverine conditions to the formation of freshwater marshes and lakes and, finally, in the deposition of offshore clays. Biostratigraphically, the logged sequences correspond to the regional Pannonian mollusc zone C. The extraordinarily fine-scaled Paleoecological resolution might serve as a basis for a correlation of 4th order changes reported from basinal settings of the northern Vienna Basin. Thus the rapid facies succession on the northwestern margin of the Vienna Basin is interpreted as being linked to major lake level changes rather than to solely local changes in the riverine system.
Links
MSM 143100004, plan (intention)Name: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid
Investor: Ministry of Education, Youth and Sports of the CR, Geological Processes and their Environmental Impact - Contact of the Variscides and Alpides
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