HARZHAUSER, Mathias, Johanna KOVAR-EDER, Slavomír NEHYBA, Margit STROBITZER-HERMANN, Jurgen SCHWARZ, Jan WOJCICKI a Irene ZORN. An Early Pannonian (Late Miocene) transgression in the Northern Vienna Basin. The paleoecological feedback. Geologica Carpathica. Bratislava, roč. 54, č. 1, s. 41-52. ISSN 1335-0552. 2003.
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Základní údaje
Originální název An Early Pannonian (Late Miocene) transgression in the Northern Vienna Basin. The paleoecological feedback.
Autoři HARZHAUSER, Mathias (40 Rakousko, garant), Johanna KOVAR-EDER (40 Rakousko), Slavomír NEHYBA (203 Česká republika), Margit STROBITZER-HERMANN (40 Rakousko), Jurgen SCHWARZ (276 Německo), Jan WOJCICKI (616 Polsko) a Irene ZORN (40 Rakousko).
Vydání Geologica Carpathica, Bratislava, 2003, 1335-0552.
Další údaje
Originální jazyk angličtina
Typ výsledku Článek v odborném periodiku
Obor 10500 1.5. Earth and related environmental sciences
Stát vydavatele Slovensko
Utajení není předmětem státního či obchodního tajemství
Impakt faktor Impact factor: 0.397
Kód RIV RIV/00216224:14310/03:00030514
Organizační jednotka Přírodovědecká fakulta
Klíčová slova anglicky Late Miocene; Pannonian; Lake Pannon; Northern Vienna Basin; hydrophytes; paleoecology
Štítky hydrophytes, Lake Pannon, Late Miocene, Northern Vienna Basin, paleoecology, Pannonian
Změnil Změnil: prof. RNDr. Slavomír Nehyba, Dr., učo 2710. Změněno: 27. 3. 2010 10:50.
Anotace
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.
Anotace česky
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.
Návaznosti
MSM 143100004, záměrNázev: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid
Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Geologické procesy a jejich environmentální vyústění - styk variscid a alpid
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