Discovery of the late Middle Ordovician Saucrorthis fauna (Brachiopoda) from the Sibumasu palaeoplate, western Yunnan, SW China-Reference-Cited by-同舟云学术

Discovery of the late Middle Ordovician Saucrorthis fauna (Brachiopoda) from the Sibumasu palaeoplate, western Yunnan, SW China

Published:2013-10-18 Issue:1 Volume:136 Page:320-326
ISSN:1103-5897
Container-title:GFF
language:en
Short-container-title:GFF

Author:

Renbin Zhan¹,Bing Huang¹,Guangxu Wang¹,Jisuo Jin²,Yan Liang¹,Yi Wang¹,Yuandong Zhang¹,Rongyu Li³,Jianbo Liu⁴,Rongchang Wu¹

Affiliation:

1. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, P.R. China;

2. Department of Earth Sciences, Western University, London, Ontario N6A 5B7, Canada

3. Department of Earth Sciences, Brandon University, Brandon, Manitoba R7A 6A9, Canada

4. College of Earth and Space Sciences, Peking University, Beijing 100871, P.R. China

Publisher

Informa UK Limited

Subject

Paleontology,Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/11035897.2013.848232

Reference51 articles.

1. Ordovician biogeography and continental drift

2. Early-Middle Palaeozoic biogeography of Asian terranes derived from Gondwana

3. Chen, X., Rong, J.Y., Wang, X.F., Wang, Z.H., Zhang, Y.D. & Zhan, R.B., 1995: Correlation of Ordovician rocks of China. International Union of Geological Sciences Publication No. 31, Trondheim, Norway. 104 pp.

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