Автор |
Michalík, Jozef |
Автор |
Šimo, Vladimír |
dc.description |
ABSTRACTZavitokichnus fusiformis n. igen. et n. isp. occurs in Lower Cretaceous (Valanginian to Hauterivian) limestones of the Fatric Superunit in the Western Carpathians. Typical cross sections of this more or less spiral trace fossil are sometimes U–O–C–S-shaped. In cross-section the trace fossil passes from a simple linear form, and spreads to a wider rolled-up or rolled-out form and then it returns to a linear trace. Spreite-like lamellae are distinguishable on several cross-section examples. The trace fossil was produced by a deposit feeder and it might be classified as a fodinichnion. Z. fusiformis co-occurs with trace fossil associations of Zoophycos, Chondrites, Planolites, Hormosiroidea and Palaeophycus in carbonate sediments of a deep-seated ramp along the margin of the Fatric intrashelf basin. |
Формат |
application.pdf |
Издатель |
Royal Society of Edinburgh Scotland Foundation |
Копирайт |
Copyright © Royal Society of Edinburgh 2010 |
Тема |
Early Cretaceous |
Тема |
serial sectioning |
Тема |
spreite structure |
Тема |
Zavitokichnus fusiformis |
Тема |
3D reconstruction |
Название |
A new spreite trace fossil from Lower Cretaceous limestone (Western Carpathians, Slovakia) |
Тип |
research-article |
DOI |
10.1017/S1755691009008068 |
Electronic ISSN |
1755-6929 |
Print ISSN |
1755-6910 |
Журнал |
Earth and Environmental Science Transactions of the Royal Society of Edinburgh |
Том |
100 |
Первая страница |
417 |
Последняя страница |
427 |
Аффилиация |
Michalík Jozef; Dúbravská cesta 9, P.O. Box 106, 840 05, Bratislava, Slovakia Email: vladosimo@yahoo.com; geolmich@savba.sk |
Аффилиация |
Šimo Vladimír; Dúbravská cesta 9, P.O. Box 106, 840 05, Bratislava, Slovakia Email: vladosimo@yahoo.com; geolmich@savba.sk |
Выпуск |
4 |