[HTML][HTML] Shifts in magnetic mineral assemblages support ocean deoxygenation before the end-Permian mass extinction
Expansion of oceanic anoxia is a prevailing hypothesis for driving the marine end-Permian
mass extinction and is mainly based on isotopic geochemical proxies. However, long-term …
mass extinction and is mainly based on isotopic geochemical proxies. However, long-term …
Shifts in magnetic mineral assemblages support ocean deoxygenation before the end-Permian mass extinction
M Zhang, H Qin, Y Hou, K He, C Deng… - Communications …, 2024 - ui.adsabs.harvard.edu
Expansion of oceanic anoxia is a prevailing hypothesis for driving the marine end-Permian
mass extinction and is mainly based on isotopic geochemical proxies. However, long-term …
mass extinction and is mainly based on isotopic geochemical proxies. However, long-term …