Upper Ordovician continuous lithological succession in outer‐shelf facies, Yangtze Platform, South China: Facies changes and oceanographic reconstruction up to the Late Ordovician Hirnantian glaciation-Reference-Cited by-同舟云学术

Upper Ordovician continuous lithological succession in outer‐shelf facies, Yangtze Platform, South China: Facies changes and oceanographic reconstruction up to the Late Ordovician Hirnantian glaciation

Published:2018-06-06 Issue:5 Volume:27 Page:e12259
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Yu Shenyang¹²^ORCID,Chen Qing¹,Kershaw Stephen³,Li Yue¹,Li Chao¹

Affiliation:

1. Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and PaleontologyChinese Academy of Sciences 39 East Beijing Road, Nanjing 210008 China

2. Nanjing Institute of Geology and Paleontology, University of Science and Technology of China 96 Jinzhai Road, Hefei 230026 China

3. Department of Life Sciences, Halsbury BuildingBrunel University Uxbridge UB8 3PH UK

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/iar.12259

Reference94 articles.

1. Ordovician of China 1982 Geological Publishing House Beijing China T. X. An C. G. Lai Conodonts 213 222

2. Progressive ventilation of the oceans; an explanation for the distribution of the lower Paleozoic black shales

3. Ordovician odyssey 1995 A. J. Boucot X. Chen C. R. Scotese J. Cooper M. Droser S. Finney Ibexian and post‐Iberian paleogeography based on climatically sensitive sediments and biogeographic data 291 296

4. Pre-Hirnantian Ashgill climatically warm event in the Mediterranean region

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