Rapid acidification of the ocean during the Paleocene-Eocene thermal maximum
The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release
of∼ 2000× 109 metric tons of carbon in the form of methane. In theory, oxidation and ocean …
of∼ 2000× 109 metric tons of carbon in the form of methane. In theory, oxidation and ocean …
An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum
Abstract During the Palaeocene–Eocene Thermal Maximum (PETM) about 56 million years
ago, thousands of petagrams of carbon were released into the atmosphere and ocean in just …
ago, thousands of petagrams of carbon were released into the atmosphere and ocean in just …
Enhanced terrestrial weathering/runoff and surface ocean carbonate production during the recovery stages of the Paleocene‐Eocene thermal maximum
DC Kelly, JC Zachos, TJ Bralower… - …, 2005 - Wiley Online Library
The carbonate saturation profile of the oceans shoaled markedly during a transient global
warming event known as the Paleocene‐Eocene thermal maximum (PETM)(circa 55 Ma) …
warming event known as the Paleocene‐Eocene thermal maximum (PETM)(circa 55 Ma) …
The magnitude of surface ocean acidification and carbon release during Eocene Thermal Maximum 2 (ETM‐2) and the Paleocene‐Eocene Thermal Maximum (PETM)
Abstract Eocene Thermal Maximum 2 (ETM‐2; 54.1 Ma) was the second largest Eocene
hyperthermal. Like the Paleocene‐Eocene Thermal Maximum (PETM), ETM‐2 was …
hyperthermal. Like the Paleocene‐Eocene Thermal Maximum (PETM), ETM‐2 was …
Ocean acidification and surface water carbonate production across the Paleocene–Eocene thermal maximum
The addition of massive amounts of carbon to the ocean–atmosphere system at the
Paleocene–Eocene thermal maximum (PETM,∼ 55Ma) caused deep-ocean acidification …
Paleocene–Eocene thermal maximum (PETM,∼ 55Ma) caused deep-ocean acidification …
Reversed deep‐sea carbonate ion basin gradient during Paleocene‐Eocene thermal maximum
The Paleocene‐Eocene thermal maximum (PETM,∼ 55 Ma ago) was marked by
widespread CaCO3 dissolution in deep‐sea sediments, a process that has been attributed …
widespread CaCO3 dissolution in deep‐sea sediments, a process that has been attributed …
Ocean acidification in deep time
Is there precedence in Earth history for the rapid release of carbon dioxide (CO₂) by fossil
fuel burning and its environmental consequences? Proxy evidence indicates that …
fuel burning and its environmental consequences? Proxy evidence indicates that …
Rapid carbon sequestration at the termination of the Palaeocene–Eocene Thermal Maximum
Abstract The Palaeocene–Eocene Thermal Maximum (PETM), an approximately 170,000-
year-long period of global warming about 56 million years ago, has been attributed to the …
year-long period of global warming about 56 million years ago, has been attributed to the …
Coupled greenhouse warming and deep‐sea acidification in the middle Eocene
The Middle Eocene Climatic Optimum (MECO) is an enigmatic warming event that
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …
Palaeocene–Eocene Thermal Maximum prolonged by fossil carbon oxidation
A hallmark of the rapid and massive release of carbon during the Palaeocene–Eocene
Thermal Maximum is the global negative carbon isotope excursion. The delayed recovery of …
Thermal Maximum is the global negative carbon isotope excursion. The delayed recovery of …