Glacio‐eustasy and δ 13 C across the Mississippian–Pennsylvanian boundary in the eastern Paleo‐Tethys Ocean (South China): Implications for mid‐Carboniferous major glaciation-Reference-Cited by-同舟云学术

Glacio‐eustasy and δ 13 C across the Mississippian–Pennsylvanian boundary in the eastern Paleo‐Tethys Ocean (South China): Implications for mid‐Carboniferous major glaciation

Published:2020-04 Issue:4 Volume:55 Page:2704-2716
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Tian Xiaoxu¹²,Chen Jitao¹³^ORCID,Yao Le¹^ORCID,Hu Keyi⁴,Qi Yuping¹,Wang Xiangdong¹⁴

Affiliation:

1. CAS Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and PaleoenvironmentChinese Academy of Sciences Nanjing China

2. Nanjing Institute of Geology and PalaeontologyUniversity of Science and Technology of China Hefei China

3. Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary MineralsShandong University of Science and Technology Qingdao China

4. Centre for Research and Education on Biological Evolution and EnvironmentNanjing University Nanjing China

Funder

National Natural Science Foundation of China

Shanghai Institutes for Biological Sciences, Chinese Academy of Sciences

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3551

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4. Global Climate Change and Intensification of Coastal Ocean Upwelling

5. The onset of the Permo-Carboniferous glaciation: reconciling global stratigraphic evidence with biogenic apatite δ18O records in the late Visean

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