[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 …
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 …
Peak Cenozoic warmth enabled deep-sea sand deposition
ZFM Burton, T McHargue, CH Kremer, RB Bloch… - Scientific Reports, 2023 - nature.com
Abstract The early Eocene (~ 56–48 million years ago) was marked by peak Cenozoic
warmth and sea levels, high CO2, and largely ice-free conditions. This time has been …
warmth and sea levels, high CO2, and largely ice-free conditions. This time has been …
Climate‐driven generation of a fluvial sheet sand body at the Paleocene–Eocene boundary in north‐west Wyoming (USA)
BZ Foreman - Basin Research, 2014 - earthdoc.org
An unusually thick and laterally persistent fluvial sand body crops out at the Paleocene–
Eocene boundary within the northern part of the Bighorn Basin in northwest Wyoming, USA …
Eocene boundary within the northern part of the Bighorn Basin in northwest Wyoming, USA …
[HTML][HTML] Increased frequency of extreme precipitation events in the North Atlantic during the PETM: Observations and theory
Climate model simulations of the PETM (Paleocene-Eocene Thermal Maximum) warming
have mainly focused on replicating the global thermal response through greenhouse …
have mainly focused on replicating the global thermal response through greenhouse …
Warming, euxinia and sea level rise during the Paleocene–Eocene Thermal Maximum on the Gulf Coastal Plain: implications for ocean oxygenation and nutrient …
A Sluijs, L Van Roij, GJ Harrington, S Schouten… - Climate of the …, 2014 - cp.copernicus.org
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 …
global warming, associated with massive injections of 13 C-depleted carbon into the ocean …
A model–model and data–model comparison for the early Eocene hydrological cycle
A range of proxy observations have recently provided constraints on how Earth's
hydrological cycle responded to early Eocene climatic changes. However, comparisons of …
hydrological cycle responded to early Eocene climatic changes. However, comparisons of …
Paleocene–Eocene Thermal Maximum environmental change in the New Jersey Coastal Plain: benthic foraminiferal biotic events
The environmental impact of the Paleocene–Eocene Thermal Maximum (PETM) has been
intensively studied in the New Jersey Coastal Plain, but the benthic foraminiferal response …
intensively studied in the New Jersey Coastal Plain, but the benthic foraminiferal response …
Shallow marine response to global climate change during the Paleocene‐Eocene Thermal Maximum, Salisbury Embayment, USA
JM Self‐Trail, MM Robinson, TJ Bralower… - …, 2017 - Wiley Online Library
Abstract The Paleocene‐Eocene Thermal Maximum (PETM) was an interval of extreme
warmth that caused disruption of marine and terrestrial ecosystems on a global scale. Here …
warmth that caused disruption of marine and terrestrial ecosystems on a global scale. Here …