Anthropogenic carbon release rate unprecedented during the past 66 million years
Carbon release rates from anthropogenic sources reached a record high of∼ 10 Pg C yr− 1
in 2014. Geologic analogues from past transient climate changes could provide invaluable …
in 2014. Geologic analogues from past transient climate changes could provide invaluable …
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 …
Two massive, rapid releases of carbon during the onset of the Palaeocene–Eocene thermal maximum
The Earth's climate abruptly warmed by 5–8° C during the Palaeocene–Eocene thermal
maximum (PETM), about 55.5 million years ago,. This warming was associated with a …
maximum (PETM), about 55.5 million years ago,. This warming was associated with a …
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
The transient global warming event known as the Palaeocene–Eocene Thermal Maximum
occurred about 55.9 Myr ago. The warming was accompanied by a rapid shift in the isotopic …
occurred about 55.9 Myr ago. The warming was accompanied by a rapid shift in the isotopic …
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 …
Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming
Abstract The Palaeocene–Eocene Thermal Maximum (about 55 Myr ago) represents a
possible analogue for the future and thus may provide insight into climate system sensitivity …
possible analogue for the future and thus may provide insight into climate system sensitivity …
Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum
JD Wright, MF Schaller - Proceedings of the National …, 2013 - National Acad Sciences
The Paleocene/Eocene thermal maximum (PETM) and associated carbon isotope excursion
(CIE) are often touted as the best geologic analog for the current anthropogenic rise in …
(CIE) are often touted as the best geologic analog for the current anthropogenic rise in …
Persistence of carbon release events through the peak of early Eocene global warmth
Abstract The Early Eocene Climatic Optimum (53–50 million years ago) was preceded by
approximately six million years of progressive global warming. This warming was …
approximately six million years of progressive global warming. This warming was …
Constraints on the onset duration of the Paleocene–Eocene Thermal Maximum
SK Turner - … Transactions of the Royal Society A …, 2018 - royalsocietypublishing.org
The Paleocene–Eocene Thermal Maximum (PETM, approx. 56 Ma) provides a test case for
investigating how the Earth system responds to rapid greenhouse gas-driven warming …
investigating how the Earth system responds to rapid greenhouse gas-driven warming …
[HTML][HTML] Development of a novel empirical framework for interpreting geological carbon isotope excursions, with implications for the rate of carbon injection across the …
SK Turner, A Ridgwell - Earth and Planetary Science Letters, 2016 - Elsevier
As an episode of rapid global warming associated with the release of massive quantities of
carbon to the atmosphere and oceans, the Paleocene–Eocene Thermal Maximum (PETM,∼ …
carbon to the atmosphere and oceans, the Paleocene–Eocene Thermal Maximum (PETM,∼ …