Occurrence of the Lower Cambrian anemone-style trace fossils in the Zabuk Formation (Mardin-Derik, SE Turkey)

Date

2018-10-01

Author

Hosgor, Izzet
Yılmaz, İsmail Ömer

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The Zabuk Formation of the Derik Group exposed over much of south-eastern Turkey presents a succession composed of shallow marine and fluvial siliciclastic sedimentary rocks. The Lower Cambrian assemblages containing abundant anemone-style trace fossils are known from most major palaeocontinents such as Laurentia, Baltica, and Gondwana. These have possible affinities with semi-infaunal dwelling anemones on siliciclastic midlatitude shelves of West Gondwana in early Fortunian deposits. Among them is Bergaueria, characterized by plug-shaped burrows as exemplified by Bergaueria perata, that is, a characteristic trace fossil of the Cambrian globally. (C) 2018 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.

Subject Keywords

SE Turkey, Gondwana, Lower Cambrian, Palaeoenvironment, Trace fossils, Bergaueria

URI

https://hdl.handle.net/11511/41084

Journal

COMPTES RENDUS PALEVOL

DOI

https://doi.org/10.1016/j.crpv.2018.02.004

Collections

Department of Geological Engineering, Article

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Citation Formats

I. Hosgor and İ. Ö. Yılmaz, “Occurrence of the Lower Cambrian anemone-style trace fossils in the Zabuk Formation (Mardin-Derik, SE Turkey),” COMPTES RENDUS PALEVOL, pp. 495–503, 2018, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/41084.