Constraining the biotic transitions across the end‐Ordovician mass extinction in South China: Bio‐ and chemostratigraphy of the Wulipo Formation in the Meitan area of northern Guizhou-Reference-Cited by-同舟云学术

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Constraining the biotic transitions across the end‐Ordovician mass extinction in South China: Bio‐ and chemostratigraphy of the Wulipo Formation in the Meitan area of northern Guizhou

Published:2020-03-17 Issue:9 Volume:55 Page:6399-6411
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Wang Guangxu¹^ORCID,Wei Xin¹²,Luan Xiaocong¹,Wu Rongchang¹,Percival Ian G.³,Zhan Renbin¹⁴

Affiliation:

1. State Key Laboratory of Palaeobiology and Stratigraphy, Center for Excellence in Life and Paleoenvironment, Nanjing Institute of Geology and PalaeontologyChinese Academy of Sciences Nanjing China

2. University of Science and Technology of China Hefei China

3. Geological Survey of New South Wales Sydney New South Wales Australia

4. University of Chinese Academy of Sciences Beijing China

Funder

Chinese Academy of Sciences

National Natural Science Foundation of China

State Key Laboratory of Palaeobiology and Stratigraphy

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3816

Reference39 articles.

1. The Position of the Ordovician–Silurian Boundary in Estonia Tested by High-Resolution δ13C Chemostratigraphic Correlation

2. Late Ordovician–Early Silurian δ13C chemostratigraphy in the Upper Mississippi Valley: implications for chronostratigraphy and depositional interpretations

3. High-resolution stable isotope stratigraphy of Upper Ordovician sequences: Constraints on the timing of bioevents and environmental changes associated with mass extinction and glaciation

4. The Global Boundary Stratotype Section and Point (GSSP) for the base of the Hirnantian Stage (the uppermost of the Ordovician System)

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1. Stromatoporoids of the upper Hirnantian (Upper Ordovician) Shiqian Formation of South China: implications for environmental interpretation and the Ordovician–Silurian stromatoporoid transition;Journal of Systematic Palaeontology;2024-07-05

2. Bedrock geological map predictions for Phanerozoic fossil occurrences;Paleobiology;2023-01-27

3. Nearshore warm-water biota development in the aftermath of the Late Ordovician Mass Extinction in South China;Palaeogeography, Palaeoclimatology, Palaeoecology;2022-10

4. Amsassia (calcareous alga) from the Lower Ordovician (Tremadocian) of western Newfoundland, and the biologic affinity and geologic history of the genus;Journal of Paleontology;2021-09-21

5. Middle to Late Ordovician (late Darriwilian to early Sandbian) ostracods from the Meitan area of northern Guizhou, SW China;Alcheringa: An Australasian Journal of Palaeontology;2020-10-01

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