Global and Planetary Change, Journal Year: 2023, Volume and Issue: 230, P. 104273 - 104273
Published: Oct. 11, 2023
Language: Английский
Global and Planetary Change, Journal Year: 2023, Volume and Issue: 230, P. 104273 - 104273
Published: Oct. 11, 2023
Language: Английский
Chemical Geology, Journal Year: 2024, Volume and Issue: 662, P. 122209 - 122209
Published: June 7, 2024
Language: Английский
Citations
2Journal of the Geological Society, Journal Year: 2024, Volume and Issue: 181(5)
Published: July 4, 2024
The cause of the Late Ordovician mass extinction (LOME) is widely debated, with glaciation, volcanism and oceanic redox fluctuations being proposed as possible drivers. Here, we apply a multi-proxy approach to deep-water Iapetus Ocean samples from Dob's Linn, Scotland, determine conditions changes in chemical weathering intensity. We document major between anoxic ferruginous oxic during first, end-Katian pulse, whereas end-Hirnantian phase witnessed more persistent anoxia. These two episodes were separated by major, short-lived decline Hirnantian suggesting that although global cooling may have placed stress on certain biota, it was unlikely be crisis. anoxia persisted into Silurian, widespread euxinia resulting drawdown redox-sensitive trace metals. Recent studies identified mid-Katian biotic crisis recovery prior LOME, precise stratigraphic position not yet defined. record at Linn shows change, dysoxic deep ocean waters giving way well-oxygenated this time. However, links these remain unclear.
Language: Английский
Citations
2Earth and Planetary Science Letters, Journal Year: 2024, Volume and Issue: 645, P. 118956 - 118956
Published: Aug. 27, 2024
Language: Английский
Citations
2Earth-Science Reviews, Journal Year: 2022, Volume and Issue: 232, P. 104101 - 104101
Published: June 30, 2022
Language: Английский
Citations
9Global and Planetary Change, Journal Year: 2023, Volume and Issue: 230, P. 104273 - 104273
Published: Oct. 11, 2023
Language: Английский
Citations
5