[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum

MJ Carmichael, GN Inglis, MPS Badger… - Global and Planetary …, 2017 - Elsevier
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …

Intergovernmental Panel on Climate Change (IPCC). Global carbon and other biogeochemical cycles and feedbacks

JG Canadell, PMS Monteiro, MH Costa… - Climate change 2021 …, 2023 - cambridge.org
It is unequivocal that the increases in atmospheric carbon dioxide (CO2), methane (CH4)
and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …

Identifying oxygen minimum zone-type biogeochemical cycling in Earth history using inorganic geochemical proxies

F Scholz - Earth-Science Reviews, 2018 - Elsevier
Because of anthropogenic global warming, the world ocean is currently losing oxygen. This
trend called ocean deoxygenation is particularly pronounced in low-latitude upwelling …

Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2

MO Clarkson, CH Stirling, HC Jenkyns… - Proceedings of the …, 2018 - National Acad Sciences
Oceanic Anoxic Event 2 (OAE 2), occurring∼ 94 million years ago, was one of the most
extreme carbon cycle and climatic perturbations of the Phanerozoic Eon. It was typified by a …

Upper limits on the extent of seafloor anoxia during the PETM from uranium isotopes

MO Clarkson, TM Lenton, MB Andersen… - Nature …, 2021 - nature.com
Abstract The Paleocene Eocene Thermal Maximum (PETM) represents a major carbon cycle
and climate perturbation that was associated with ocean de-oxygenation, in a qualitatively …

Cycles of~ 32.5 My and~ 26.2 My in correlated episodes of continental flood basalts (CFBs), hyper-thermal climate pulses, anoxic oceans, and mass extinctions over …

MR Rampino, K Caldeira, S Rodriguez - Earth-Science Reviews, 2023 - Elsevier
Potential temporal and causal connections among various geologic events have long been
discussed in the geological literature. More recently, signs of common periodicities in these …

Ocean circulation in the Toarcian (Early Jurassic): a key control on deoxygenation and carbon burial on the European Shelf

I Ruvalcaba Baroni, A Pohl… - Paleoceanography …, 2018 - Wiley Online Library
Abstract The Toarcian Oceanic Anoxic Event (T‐OAE,∼ 183 Myr) was a long‐lasting
episode of ocean deoxygenation during the Early Jurassic. The event is related to a period …

Cretaceous large igneous provinces: from volcanic formation to environmental catastrophes and biological crises

LME Percival, H Matsumoto, S Callegaro… - Geological Society …, 2025 - lyellcollection.org
Abstract The Cretaceous Period was marked by the formation of numerous large igneous
provinces (LIPs), several of which were associated with geologically rapid climate …

Enhanced phosphorus recycling during past oceanic anoxia amplified by low rates of apatite authigenesis

NM Papadomanolaki, WK Lenstra, M Wolthers… - Science …, 2022 - science.org
Enhanced recycling of phosphorus as ocean deoxygenation expanded under past
greenhouse climates contributed to widespread organic carbon burial and drawdown of …

What controls the duration and intensity of ocean anoxic events in the Paleozoic and the Mesozoic?

T Reershemius, NJ Planavsky - Earth-Science Reviews, 2021 - Elsevier
The sedimentological and geochemical expression of Mesozoic ocean anoxic events
(OAEs) in the geologic record is reasonably well-characterized and the causal mechanisms …