Sedimentary trace element constraints on the role of North Atlantic Igneous Province volcanism in late Paleocene–early Eocene environmental change
DJ Thomas, TJ Bralower - Marine Geology, 2005 - Elsevier
A growing body of geologic evidence suggests that emplacement of the North Atlantic
Igneous Province (NAIP) played a major role in global warming during the early Paleogene …
Igneous Province (NAIP) played a major role in global warming during the early Paleogene …
[HTML][HTML] Tracing North Atlantic volcanism and seaway connectivity across the paleocene–eocene thermal maximum (PETM)
There is a temporal correlation between the peak activity of the North Atlantic Igneous
Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the …
Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the …
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 …
Transient mobilization of subcrustal carbon coincident with Palaeocene–Eocene Thermal Maximum
Plume magmatism and continental breakup led to the opening of the northeast Atlantic
Ocean during the globally warm early Cenozoic. This warmth culminated in a transient (170 …
Ocean during the globally warm early Cenozoic. This warmth culminated in a transient (170 …
[HTML][HTML] Rapid and sustained environmental responses to global warming: the Paleocene–Eocene Thermal Maximum in the eastern North Sea
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 …
sustained global warming associated with significant carbon emissions. It coincided with the …
Uncorking the bottle: What triggered the Paleocene/Eocene thermal maximum methane release?
ME Katz, BS Cramer, GS Mountain, S Katz… - …, 2001 - Wiley Online Library
The Paleocene/Eocene thermal maximum (PETM) was a time of rapid global warming in
both marine and continental realms that has been attributed to a massive methane (CH4) …
both marine and continental realms that has been attributed to a massive methane (CH4) …
What caused the long duration of the Paleocene‐Eocene Thermal Maximum?
RE Zeebe - Paleoceanography, 2013 - Wiley Online Library
Paleorecords show that the Paleocene‐Eocene Thermal Maximum (PETM,∼ 56 Ma) was
associated with a large carbon cycle anomaly and global warming> 5 K, which persisted for …
associated with a large carbon cycle anomaly and global warming> 5 K, which persisted for …
Thermogenic methane release as a cause for the long duration of the PETM
The Paleocene–Eocene Thermal Maximum (PETM)(∼ 56 Ma) was a∼ 170,000-y (∼ 170-
kyr) period of global warming associated with rapid and massive injections of 13C-depleted …
kyr) period of global warming associated with rapid and massive injections of 13C-depleted …
Evidence for weathering and volcanism during the PETM from Arctic Ocean and Peri-Tethys osmium isotope records
AJ Dickson, AS Cohen, AL Coe, M Davies… - Palaeogeography …, 2015 - Elsevier
Sudden global warming during the Paleocene–Eocene Thermal Maximum (PETM, 55.9 Ma)
occurred because of the rapid release of several thousand gigatonnes of isotopically light …
occurred because of the rapid release of several thousand gigatonnes of isotopically light …
Marine diagenesis of tephra aided the Palaeocene-Eocene Thermal Maximum termination
Abstract The Palaeocene-Eocene Thermal Maximum (PETM) was a period of intense global
warming that began∼ 55.9 million years ago and lasted about 170,000 yrs. Various …
warming that began∼ 55.9 million years ago and lasted about 170,000 yrs. Various …