Oxygenation in carbonate microbialites and associated facies after the end-Permian mass extinction: Problems and potential solutions
Carbonate sediments deposited in normally-oxygenated shallow ocean waters of the latest Permian period, immediately prior to the end-Permian mass extinction, contain well-developed diverse shelly faunas. After the extinction of these skeletal metazoans, the sediments commonly comprise microbialites...
Main Authors: | Stephen Kershaw, Hao Tang, Yue Li, Li Guo |
---|---|
Format: | Article |
Language: | English |
Published: |
SpringerOpen
2018-01-01
|
Series: | Journal of Palaeogeography |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S2095383617301293 |
Similar Items
-
Palaeogeographic variation in the Permian–Triassic boundary microbialites: A discussion of microbial and ocean processes after the end-Permian mass extinction
by: Stephen Kershaw
Published: (2017-04-01) -
Modern Black Sea oceanography applied to the end-Permian extinction event
by: Steve Kershaw
Published: (2015-01-01) -
Diagenesis of the microbialites in the Permian–Triassic boundary section at Laolongdong, Chongqing, South China
by: Jiang Hongxia, et al.
Published: (2013-04-01) -
Suppressed competitive exclusion enabled the proliferation of Permian/Triassic boundary microbialites
by: William J. Foster, et al.
Published: (2020-02-01) -
Ostracods (Crustacea) associated with microbialites across the Permian-Triassic boundary in Dajiang (Guizhou Province, South China)
by: Marie-Beatrice FOREL
Published: (2012-08-01)