2024
Revize paleontologických nálezů z lokality Úsobrno
FIDLEROVÁ, Taťána; Tomáš TUREK a Nela DOLÁKOVÁZákladní údaje
Originální název
Revize paleontologických nálezů z lokality Úsobrno
Název anglicky
Revision of paleontological findings at the Úsobrno locality
Autoři
FIDLEROVÁ, Taťána; Tomáš TUREK a Nela DOLÁKOVÁ
Vydání
Geologické výzkumy na Moravě a ve Slezsku, Brno 2024, Brno, Masaryk University, 2024, 1212-6209
Další údaje
Jazyk
čeština
Typ výsledku
Článek v odborném periodiku
Obor
10506 Paleontology
Stát vydavatele
Česká republika
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Kód RIV
RIV/00216224:14310/24:00139035
Organizační jednotka
Přírodovědecká fakulta
EID Scopus
2-s2.0-85209572024
Klíčová slova česky
Karpatská předhlubeň; Spodní baden; Morava; Paleontologie; Paleoekologie; Mollusca; Anthozoa
Klíčová slova anglicky
Carpathian Foredeep; Lower Badenian; Moravia; Paleontology; Paleoecology; Mollusca; Anthozoa
Příznaky
Recenzováno
Změněno: 24. 3. 2025 10:24, Mgr. Marie Novosadová Šípková, DiS.
V originále
The Úsobrno locality is known on the basis of fossil fauna findings, which were documented and published by Vašíček (1941). Field research has not been able to find the original locality yet. In this reason paleontological material which is deposited in the collections of ÚGV PřF MU was researched. We identified a total of 573 species which belonged mainly to the classes Gastropoda, Bivalvia, Anthozoa and Scaphopoda and compared with the original findings mentioned by Vašíček (1941). The age of the samples was determined to be the Lower Badenian. Based on the findings, especially hermatypal corals, it can be assumed that the sea was warm (above 20 °C), well oxygenated with a soft and hard bottom and mostly shallow. Some findings of fauna from deeper marine areas (Ranella fragment, ahermatypal corals) indicate mixing or postmortem transport during sedimentation.
Anglicky
The Úsobrno locality is known on the basis of fossil fauna findings, which were documented and published by Vašíček (1941). Field research has not been able to find the original locality yet. In this reason paleontological material which is deposited in the collections of ÚGV PřF MU was researched. We identified a total of 573 species which belonged mainly to the classes Gastropoda, Bivalvia, Anthozoa and Scaphopoda and compared with the original findings mentioned by Vašíček (1941). The age of the samples was determined to be the Lower Badenian. Based on the findings, especially hermatypal corals, it can be assumed that the sea was warm (above 20 °C), well oxygenated with a soft and hard bottom and mostly shallow. Some findings of fauna from deeper marine areas (Ranella fragment, ahermatypal corals) indicate mixing or postmortem transport during sedimentation.
Návaznosti
| MUNI/A/1426/2023, interní kód MU |
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