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- W4288045104 abstract "The global End-Devonian Hangenberg Event was one of the most important mass extinction events during the Phanerozoic eon. The stratigraphical, paleontological, and sedimentological evolution of strata equivalent to the Hangenberg Event have been widely investigated in three depositional environments of shallow-marine platform, of margin and upper slope, and of deep-water facies along the South China Platform. In this representative region within the eastern Paleotethys, the volcanic tuffs, storm deposits, and microbialites deposited during the time of the Hangenberg Event differ from the record of the Hangenberg Crisis in the Rhenish Slate Mountains of Germany, which is a standard for the western Paleotethys. The Upper Crisis Interval (so-called Stockum Limestone Event) in the Rhenish record is interpreted as correlative to the aftermath of the Hangenberg Event in South China rather than a crisis record per se. The unique Cap Microbialite of peloids and oncoids in South China is linked to onset of a new shallow-marine ecosystem characterized by microbe resurgence during a delayed biotic recovery. This microbialite resurgence in association with low-diversity metazoan ecosystems may be a common feature of post-extinction episodes. The new synthesis of records from South China provide insights into global changes that contributed to the Hangenberg biotic extinctions." @default.
- W4288045104 created "2022-07-27" @default.
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- W4288045104 date "2022-09-01" @default.
- W4288045104 modified "2023-10-16" @default.
- W4288045104 title "The End-Devonian Hangenberg Event and its aftermath in South China: Stratigraphic and sedimentary records from shallow to deep water facies" @default.
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- W4288045104 doi "https://doi.org/10.1016/j.earscirev.2022.104137" @default.
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