Persistent environmental change after the Paleocene–Eocene Thermal Maximum in the eastern North Atlantic
A Bornemann, RD Norris, JA Lyman… - Earth and Planetary …, 2014 - Elsevier
Abstract The Paleocene–Eocene Thermal Maximum (PETM;∼ 56 Ma) is associated with
abrupt climate change, carbon cycle perturbation, ocean acidification, as well as …
abrupt climate change, carbon cycle perturbation, ocean acidification, as well as …
South Pacific intermediate water oxygen depletion at the onset of the Paleocene‐Eocene thermal maximum as depicted in New Zealand margin sections
MJ Nicolo, GR Dickens, CJ Hollis - Paleoceanography, 2010 - Wiley Online Library
Extreme global warming and massive input of 13C‐depleted carbon into the exogenic
carbon cycle characterize the Paleocene‐Eocene thermal maximum (PETM) circa 55.5 Ma …
carbon cycle characterize the Paleocene‐Eocene thermal maximum (PETM) circa 55.5 Ma …
Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic coastal plain
The chronology of the Paleocene-Eocene Thermal Maximum (PETM,~ 56 Ma) remains
disputed, hampering complete understanding of the possible trigger mechanisms of this …
disputed, hampering complete understanding of the possible trigger mechanisms of this …
Paleoredox changes across the Paleocene‐Eocene thermal maximum, Walvis Ridge (ODP Sites 1262, 1263, and 1266): Evidence from Mn and U enrichment factors
COJ Chun, ML Delaney, JC Zachos - Paleoceanography, 2010 - Wiley Online Library
An understanding of sediment redox conditions across the Paleocene‐Eocene thermal
maximum (PETM)(∼ 55 Ma) is essential for evaluating changes in processes that control …
maximum (PETM)(∼ 55 Ma) is essential for evaluating changes in processes that control …
Southern ocean warming, sea level and hydrological change during the Paleocene-Eocene thermal maximum
A brief (~ 150 kyr) period of widespread global average surface warming marks the
transition between the Paleocene and Eocene epochs,~ 56 million years ago. This so …
transition between the Paleocene and Eocene epochs,~ 56 million years ago. This so …
Active Pacific meridional overturning circulation (PMOC) during the warm Pliocene
An essential element of modern ocean circulation and climate is the Atlantic meridional
overturning circulation (AMOC), which includes deep-water formation in the subarctic North …
overturning circulation (AMOC), which includes deep-water formation in the subarctic North …
A transient deep‐sea circulation switch during Eocene Thermal Maximum 2
Ever since its discovery, Eocene Thermal Maximum 2 (ETM2;~ 53.7 Ma) has been
considered as one of the “little brothers” of the Paleocene‐Eocene Thermal Maximum …
considered as one of the “little brothers” of the Paleocene‐Eocene Thermal Maximum …
The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future
FA McInerney, SL Wing - Annual Review of Earth and Planetary …, 2011 - annualreviews.org
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …
petagrams of carbon were released into the ocean-atmosphere system with attendant …
A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2
The mid-Cretaceous is thought to be a greenhouse world with significantly higher
atmospheric pCO2 and sea-surface temperatures as well as a much flatter latitudinal …
atmospheric pCO2 and sea-surface temperatures as well as a much flatter latitudinal …