Depauperate survival bryozoans following the first episode of the end-Ordovician mass extinction in the Kuanyinchiao Bed (Hirnantian, Upper Ordovician) of northern Guizhou, South China-Reference-Cited by-同舟云学术

Depauperate survival bryozoans following the first episode of the end-Ordovician mass extinction in the Kuanyinchiao Bed (Hirnantian, Upper Ordovician) of northern Guizhou, South China

Published:2022-03-08 Issue:1 Volume:103 Page:95-107
ISSN:1867-1594
Container-title:Palaeobiodiversity and Palaeoenvironments
language:en
Short-container-title:Palaeobio Palaeoenv

Author:

Ma Junye^ORCID,Buttler Caroline J.,Taylor Paul D.,Huang Bing,Zhao Zhen,Xia Fengsheng

Funder

National Natural Science Foundation of China

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Geology,Ecology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Link

https://link.springer.com/content/pdf/10.1007/s12549-021-00520-0.pdf

Reference77 articles.

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2. Astrova, G. G. & Morozova, I. P. (1956). O sistematike mshanok otryada Cryptostomata [On systematics of the bryozoans of the Order Cryptostomata]. Doklady Akademii Nauk SSSR, 110, 661–664. [in Russian]

3. Bassler, R. S. (1903). The structural features of the bryozoan Homotrypa, with descriptions of species from the Cincinnatian Group. United States National Museum Proceedings, 26, 565–591.

4. Bassler, R. S. (1911). The Early Paleozoic Bryozoa of the Baltic Provinces. Bulletin of the United States National Museum, 77, 1–382.

5. Billings, E. (1866). Catalogues of the Silurian fossils of the island of Anticosti, with descriptions of some new genera and species. Geological Survey of Canada, 427, 1–93. [Separate Report]