Published November 9, 2020 | Version v1
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Text-fig. 1. Geological map of the Staniantsi Coal Basin (redrawn from Angelov et al. 1993): 1 – Pleistocene sediments, 2 – Neogen sediments, 3 – Cretaceous sediments, 4 – Jurassic sediments, 5 – Triassic sediments. in Castor-Like Postcranial Adaptation In An Uppermost Miocene Beaver From The Staniantsi Basin (Nw Bulgaria)

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Text-fig. 1. Geological map of the Staniantsi Coal Basin (redrawn from Angelov et al. 1993): 1 – Pleistocene sediments, 2 – Neogen sediments, 3 – Cretaceous sediments, 4 – Jurassic sediments, 5 – Triassic sediments.

Notes

Published as part of Lechner, Thomas Sebastian & Böhme, Madelaine, 2020, Castor-Like Postcranial Adaptation In An Uppermost Miocene Beaver From The Staniantsi Basin (Nw Bulgaria), pp. 128-164 in Fossil Imprint 76 (1) on page 129, DOI: 10.37520/fi.2020.009, http://zenodo.org/record/5382632

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Journal article: 10.37520/fi.2020.009 (DOI)
Journal article: urn:lsid:plazi.org:pub:5437FFA12233FF922A77FF3AE627FFD4 (LSID)
Journal article: https://zenodo.org/record/5382632 (URL)