Warm ocean processes and carbon cycling in the Eocene
Sea surface and subsurface temperatures over large parts of the ocean during the Eocene
epoch (55.5–33.7 Ma) exceeded modern values by several degrees, which must have …
epoch (55.5–33.7 Ma) exceeded modern values by several degrees, which must have …
Temperature-dependent remineralization and carbon cycling in the warm Eocene oceans
Metabolic rates in heterotrophic bacteria are more sensitive to temperature than rates of
primary production (eg, López-Urrutia et al., 2006; Regaudie-de-Gioux and Duarte, 2012) …
primary production (eg, López-Urrutia et al., 2006; Regaudie-de-Gioux and Duarte, 2012) …
[HTML][HTML] Prolonged deep-ocean carbonate chemistry recovery after the Paleocene-Eocene Thermal Maximum
Abstract The Paleocene-Eocene Thermal Maximum (PETM) is a hyperthermal event at∼ 56
Ma ago, caused by rapid and massive carbon releases into the ocean-atmosphere system …
Ma ago, caused by rapid and massive carbon releases into the ocean-atmosphere system …
Organic carbon and barium in Eocene sediments: Possible controls on nutrient recycling in the Eocene equatorial Pacific Ocean
AO Lyle, M Lyle - Proc. Ocean Drill. Program Sci. Results, 2005 - www-odp.tamu.edu
We present the first high-resolution organic carbon mass accumulation rate (MAR) data set
for the Eocene equatorial Pacific upwelling region, from Sites 1218 and 1219 of the Ocean …
for the Eocene equatorial Pacific upwelling region, from Sites 1218 and 1219 of the Ocean …
A continental shelf perspective of ocean acidification and temperature evolution during the Paleocene-Eocene Thermal Maximum
A rapid and large injection of isotopically light carbon into the ocean-atmosphere reservoirs
is signaled by a negative carbon isotope excursion (CIE) at the Paleocene-Eocene …
is signaled by a negative carbon isotope excursion (CIE) at the Paleocene-Eocene …
Rapid acidification of the ocean during the Paleocene-Eocene thermal maximum
The Paleocene-Eocene thermal maximum (PETM) has been attributed to the rapid release
of∼ 2000× 109 metric tons of carbon in the form of methane. In theory, oxidation and ocean …
of∼ 2000× 109 metric tons of carbon in the form of methane. In theory, oxidation and ocean …
Ocean biogeochemistry in the warm climate of the late Paleocene
M Heinze, T Ilyina - Climate of the Past, 2015 - cp.copernicus.org
The late Paleocene is characterized by warm and stable climatic conditions that served as
the background climate for the Paleocene–Eocene Thermal Maximum (PETM,~ 55 million …
the background climate for the Paleocene–Eocene Thermal Maximum (PETM,~ 55 million …
Ocean acidification and surface water carbonate production across the Paleocene–Eocene thermal maximum
The addition of massive amounts of carbon to the ocean–atmosphere system at the
Paleocene–Eocene thermal maximum (PETM,∼ 55Ma) caused deep-ocean acidification …
Paleocene–Eocene thermal maximum (PETM,∼ 55Ma) caused deep-ocean acidification …
Coupled greenhouse warming and deep‐sea acidification in the middle Eocene
The Middle Eocene Climatic Optimum (MECO) is an enigmatic warming event that
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …
represents an abrupt reversal in long‐term cooling through the Eocene. In order to further …