Late Ordovician Reefs and the Biological Crisis at the Ordovician–Silurian Boundary
- 作者: Kuznetsov V.G.1
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隶属关系:
- Gubkin State University of Oil and Gas
- 期: 卷 26, 编号 3 (2018)
- 页面: 261-266
- 栏目: Article
- URL: https://ogarev-online.ru/0869-5938/article/view/177900
- DOI: https://doi.org/10.1134/S0869593818030085
- ID: 177900
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详细
Reef formation in the Late Ordovician was relatively widespread in the Sandbian and Katian times. In the late Katian, it gradually reduced and ended in the Hirnantian, before the end of the Ordovician. In parallel, reef-building skeleton frame-building biota disappeared and was replaced with algae and calcimicrobes.
作者简介
V. Kuznetsov
Gubkin State University of Oil and Gas
编辑信件的主要联系方式.
Email: vgkuz@yandex.ru
俄罗斯联邦, Moscow
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