Reconstruction of oceanic redox conditions across the Palaeocene-Eocene Thermal
Maximum (PETM,∼ 55.93 Ma) provides crucial information on potential PETM triggers and …

Abstract The Paleocene‐Eocene Thermal Maximum (PETM,∼ 56 Ma) presents a past
analog for future global warming. Previous studies provided evidence for major loss of …

Large amounts of 13C‐depleted carbon were released to the oceans and atmosphere
during a period of abrupt global warming at the Paleocene‐Eocene thermal maximum …

Understanding marine environmental change and associated biological turnover across the
Palaeocene–Eocene Thermal Maximum (PETM;~ 56 Ma)—the most pronounced Cenozoic …

The Paleocene–Eocene Thermal Maximum (PETM,~ 56 Ma) was a~ 200 kyr episode of
global warming, associated with massive injections of 13 C-depleted carbon into the ocean …

The Paleocene–Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a period of rapid and
sustained global warming associated with significant carbon emissions. It coincided with the …

Anthropogenic global warming affects marine ecosystems in complex ways, and declining
ocean oxygenation is a growing concern. Forecasting the geographical and bathymetric …

A rapid increase in greenhouse gas levels is thought to have fueled global warming at the
Paleocene-Eocene Thermal Maximum (PETM). Foraminiferal magnesium/calcium ratios …

Geological records reveal a major perturbation in carbon cycling during the Paleocene–
Eocene Thermal Maximum (PETM,∼ 56 Ma), marked by global warming of more than 5° C …

The degree to which ocean deoxygenation will alter the function of marine communities
remains unclear but may be best constrained by detailed study of intervals of rapid warming …