Počet záznamů: 1
Microfossils accompanying some Perisphinctoid Ammonites from the Štramberk Limestone (Tithonian to Early Berriasian from the Silesian Unit, Czech Republic)
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SYSNO ASEP 0467489 Druh ASEP C - Konferenční příspěvek (mezinárodní konf.) Zařazení RIV D - Článek ve sborníku Název Microfossils accompanying some Perisphinctoid Ammonites from the Štramberk Limestone (Tithonian to Early Berriasian from the Silesian Unit, Czech Republic) Tvůrce(i) Vašíček, Zdeněk (UGN-S) RID
Reháková, D. (SK)
Skupien, P. (CZ)Celkový počet autorů 3 Zdroj.dok. Environmental, Structural and Stratigraphical Evolution of the Western Carpathians. - Bratislava : Faculty of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, 2016 / Šujan M. - ISBN 978-80-223-4201-8 Rozsah stran s. 113-114 Poč.str. 2 s. Forma vydání Tištěná - P Akce Environmental, Structural and Stratigraphical Evolution of the Western Carpathians - ESSEWECA Conference /10./ Datum konání 01.12.2016 - 02.12.2016 Místo konání Bratislava Země SK - Slovensko Typ akce EUR Jazyk dok. eng - angličtina Země vyd. SK - Slovensko Klíč. slova microfossils ; Štramberk Limestone ; ammonites Vědní obor RIV DB - Geologie a mineralogie Institucionální podpora UGN-S - RVO:68145535 Anotace In Moravian-Silesian museums in the Czech Republic, Vienna Museum of Natural History and Bayerische Staatssammlung für Paläontologie un historische Geologie of the University in Munich, ammonites collected previously in the Štramberk Limestone are deposited. A common feature of all of these older collections is that the finds miss precise localization. Museum original labels usually state only Stramberg of Štramberk. The oldest finds come before the year 1861 especially from the Castle Hill (Zámecký vrch) Quarry. This material was taxonomically processed in a monograph by Zittel (1868). Another collection was processed by Blaschke (1911). His specimens come largely from the Kotouč Quarry (formerly Gutmann Quarry. At present, the stratigraphic position of the presented ammonites can be derived in the case of well determinable species only on the basis of data in literature if such species were also found in other stratigraphically dated sections in foreign localities. Moreover, a significant auxiliary element is the occurence of guide mircrofossils provided by microfacies analysis of associated rocks surrounding or filling the ammonites. We make efforts to define a more precise stratigraphic position of the above-mentioned finds containing stratigraphically important microfossils. Pracoviště Ústav geoniky Kontakt Lucie Gurková, lucie.gurkova@ugn.cas.cz, Tel.: 596 979 354 Rok sběru 2017
Počet záznamů: 1