Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids-Reference-Cited by-同舟云学术

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Dynamic ocean redox conditions during the end-Triassic mass extinction: Evidence from pyrite framboids

Published:2022-11 Issue: Volume:218 Page:103981
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Li Jing,Song Huyue,Tian Li,Bond David P.G.,Song Haijun,Du Yong,Zhang Chi,Chu Daoliang,Wignall Paul B.,Tong Jinnan

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference81 articles.

1. How quick was marine recovery after the end-Triassic mass extinction and what role did anoxia play?;Atkinson;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2019

2. Biogeochemical constraints on the Triassic-Jurassic boundary carbon cycle event;Beerling;Glob. Biogeochem. Cycles,2002

3. Recurring photic zone euxinia in the northwest Tethys impinged end-Triassic extinction recovery;Beith;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2021

4. Increased fire activity at the Triassic/Jurassic boundary in Greenland due to climate-driven floral change;Belcher;Nat. Geosci.,2010

5. On the causes of mass extinctions;Bond;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2017

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2. On the occurrence of rare nannoliths (calcareous nannofossils) in the Early Jurassic and their implications for the end‐Triassic mass extinction;Papers in Palaeontology;2023-03

3. Weak and intermittent anoxia during the mid-Tournaisian (Mississippian) anoxic event in the Montagne Noire, France;Geological Magazine;2023-02-14

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