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Assessing the Duration of the Paleocene‐Eocene Thermal Maximum
GEOPHYSICAL RESEARCH LETTERS
01 april 2025
Victor Piedrahita, David Heslop, Andrew P. Roberts...
The Paleocene‐Eocene Thermal Maximum (PETM) was a climate/carbon cycle perturbation recognized in stable carbon isotope (δ13C) records w...
The evolution of the tropical Indian Ocean since the last glacial maximum
ADVANCED UNDERSTANDING OF TROPICAL-SUBTROPICAL HYDROCLIMATE CHANGES DURING THE PLEISTOCENE, HOLOCENE, AND ANTHROPOCENE II ORAL
paleoceanography and paleoclimatology | 10 december 2024
Gianluca Marino, Jimin Yu, Laura Rodríguez-Sanz, N...
The tropical Indian Ocean features a warm pool that covers a large fraction of its surface, controls regional atmospheric circulation and convection, ...
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What is the paleoenvironmental significance of biogenic magnetite? Insights from early Eocene records
ENVIRONMENTAL MAGNETISM I ORAL
geomagnetism, paleomagnetism and electromagnetism | 10 december 2024
Victor Piedrahita, Elcho Rohling, David Heslop, An...
Early Eocene sedimentary archives contain records of a series of short-lived (>200 kyr) carbon cycle perturbations that were associated with massiv...
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Reconciling the Apparent Discrepancy Between Cenozoic Deep‐Sea Temperatures From Proxies and From Benthic Oxygen Isotope Deconvolution
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
01 november 2024
Elcho Rohling, Thomas Gernon, David Heslop, Gert-J...
Understanding past deep‐sea temperature and sea‐water oxygen isotope ratios is fundamental to environmental Earth science. For example,...
Bayesian Errors‐in‐Variables Estimation of Specific Climate Sensitivity
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
30 september 2024
David Heslop, Elcho Rohling, Gavin Foster, Jimin Y...
Estimation of climate sensitivity is fundamental to assessing how global climate will warm as atmospheric CO2 ${\mathrm{C}\mathrm{O}}_{2}$ concentr...
Orbital‐Scale Global Ocean Sea Surface Temperatures Coupling With Cryosphere‐Carbon Cycle Changes Over the Past 4 Million Years
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
25 july 2024
Ze Zhang, Elcho Rohling, David Kemp, Zhixiang Wang...
Changes in the thermal conditions of the ocean surface, the interface for air‐sea exchange, are critical for understanding global climate and...
Glacial terminations and rates of sea-level rise
ADVANCES IN UNDERSTANDING THE CAUSES, MECHANISMS, AND IMPACTS OF QUATERNARY ABRUPT CLIMATE CHANGES AND THEIR IMPLICATIONS FOR THE FUTURE II POSTER
paleoceanography and paleoclimatology | 14 december 2023
Hsun-Ming Hu, Gianluca Marino, Maria Fernanda Sanc...
Glacial terminations in the late Pleistocene are notable for their high rates of sea-level rise. Occurring ~340 thousand years before the present (kyr...
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Estimating Plio‐Pleistocene North African Monsoon Runoff Into the Mediterranean Sea and Temperature Impacts
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
04 november 2023
David Heslop, Udara Amarathunga, Elcho Rohling
Sapropels are dark, organic‐rich layers found in Mediterranean sediments that formed during periods of bottom water anoxia. While various mec...