Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle
Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …
[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 …
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum
The Paleocene-Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a geologically rapid
warming period associated with carbon release, which caused a marked increase in the …
warming period associated with carbon release, which caused a marked increase in the …
[PDF][PDF] Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other …
Mercury (Hg) is increasingly being used as a sedimentary tracer of Large Igneous Province
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
(LIP) volcanism, and supports hypotheses of a coincidence between the formation of several …
Osmium isotope evidence for two pulses of increased continental weathering linked to Early Jurassic volcanism and climate change
LME Percival, AS Cohen, MK Davies… - …, 2016 - pubs.geoscienceworld.org
Large igneous provinces (LIPs) are proposed to have caused a number of episodes of
abrupt environmental change by increasing atmospheric CO2 levels, which were …
abrupt environmental change by increasing atmospheric CO2 levels, which were …
Flood basalts and mass extinctions
ME Clapham, PR Renne - Annual Review of Earth and …, 2019 - annualreviews.org
Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …
Mercury anomalies across the Palaeocene–Eocene thermal maximum
Large-scale magmatic events like the emplacement of the North Atlantic Igneous Province
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …
The seawater carbon inventory at the Paleocene–Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum (PETM)(55.6 Mya) was a geologically rapid
carbon-release event that is considered the closest natural analog to anthropogenic CO2 …
carbon-release event that is considered the closest natural analog to anthropogenic CO2 …
Mercury isotope evidence for protracted North Atlantic magmatism during the Paleocene-Eocene Thermal Maximum
Abstract The Paleocene-Eocene Thermal Maximum (PETM,∼ 56 Ma) was a major
hyperthermal event that has been linked to CO 2 release from the North Atlantic Igneous …
hyperthermal event that has been linked to CO 2 release from the North Atlantic Igneous …
Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a)
LME Percival, LR Tedeschi, RA Creaser… - Global and Planetary …, 2021 - Elsevier
Large igneous province (LIP) volcanism has been proposed as a key trigger of several
major climate and environmental perturbations during the Phanerozoic Aeon. Large-scale …
major climate and environmental perturbations during the Phanerozoic Aeon. Large-scale …