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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
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