[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
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 …
An astronomically dated record of Earth's climate and its predictability over the last 66 million years
Much of our understanding of Earth's past climate comes from the measurement of oxygen
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …
Synchronous tropical and polar temperature evolution in the Eocene
Palaeoclimate reconstructions of periods with warm climates and high atmospheric CO2
concentrations are crucial for develo** better projections of future climate change. Deep …
concentrations are crucial for develo** better projections of future climate change. Deep …
Constraints on the onset duration of the Paleocene–Eocene Thermal Maximum
SK Turner - … Transactions of the Royal Society A …, 2018 - royalsocietypublishing.org
The Paleocene–Eocene Thermal Maximum (PETM, approx. 56 Ma) provides a test case for
investigating how the Earth system responds to rapid greenhouse gas-driven warming …
investigating how the Earth system responds to rapid greenhouse gas-driven warming …
[HTML][HTML] The DeepMIP contribution to PMIP4: Methodologies for selection, compilation and analysis of latest Paleocene and early Eocene climate proxy data …
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …
Global mean surface temperature and climate sensitivity of the EECO, PETM and latest Paleocene
Accurate estimates of past global mean surface temperature (GMST) help to contextualise
future climate change and are required to estimate the sensitivity of the climate system to …
future climate change and are required to estimate the sensitivity of the climate system to …
Global extent of early Eocene hyperthermal events: A new Pacific benthic foraminiferal isotope record from Shatsky Rise (ODP Site 1209)
Studying the dynamics of past global warming events during the late Paleocene to middle
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …
Eocene informs our understanding of Earth's carbon cycle behavior under elevated …
Proxy evidence for state-dependence of climate sensitivity in the Eocene greenhouse
Despite recent advances, the link between the evolution of atmospheric CO2 and climate
during the Eocene greenhouse remains uncertain. In particular, modelling studies suggest …
during the Eocene greenhouse remains uncertain. In particular, modelling studies suggest …
A high‐Fidelity benthic stable isotope record of late Cretaceous–early Eocene climate change and carbon‐cycling
Abstract The Late Cretaceous–Early Paleogene is the most recent period in Earth history
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
that experienced sustained global greenhouse warmth on multimillion year timescales. Yet …
Astronomical calibration of the Ypresian timescale: implications for seafloor spreading rates and the chaotic behavior of the solar system?
To fully understand the global climate dynamics of the warm early Eocene with its
reoccurring hyperthermal events, an accurate high-fidelity age model is required. The …
reoccurring hyperthermal events, an accurate high-fidelity age model is required. The …