This R scripts generate the figures of the manuscript published by De Vleeschouwer et al. (2023) North Atlantic Drift Sediments Constrain Eocene Tidal Dissipation and the Evolution of the Earth-Moon System. Paleoceanography and Paleoclimatolog
The warming trend that started in the latest Paleocene and culminated in the Early Eocene Climatic O...
The middle Eocene is a transitional period from the greenhouse early Eocene to the ice-house Eocene-...
The Atlantic meridional overturning circulation (AMOC) is a key component of the modern global ocean...
Cyclostratigraphy and astrochronology are now at the forefront of geologic timekeeping. While this t...
International audienceThe theoretical prediction of Earth-Moon dynamics in deep geologic time is ham...
Here we show that the onset of deep water overflow from the Norwegian-Greenland Sea into the North A...
Here we show that the onset of deep water overflow from the Norwegian-Greenland Sea into the North A...
Ocean circulation plays a critical role in the Earth’s climate system through the storage and transf...
This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Depar...
The tidally driven vertical diffusivity in the abyssal ocean during the early Eocene (55 Ma) is inve...
North Atlantic Deep Water (NADW) currently redistributes heat and salt between Earth’s ocean basins,...
Here we publish simulated early-middle Eocene annual mean ocean temperature, salinity, density, mixe...
Milankovitch band variations of past climate, inferred from the rock record, have been used to astro...
The differential effects of climate change, sea level, and water mass circulation on deposition/eros...
Earth’s continents in the present day are the dispersed fragments of the former supercontinent Pange...
The warming trend that started in the latest Paleocene and culminated in the Early Eocene Climatic O...
The middle Eocene is a transitional period from the greenhouse early Eocene to the ice-house Eocene-...
The Atlantic meridional overturning circulation (AMOC) is a key component of the modern global ocean...
Cyclostratigraphy and astrochronology are now at the forefront of geologic timekeeping. While this t...
International audienceThe theoretical prediction of Earth-Moon dynamics in deep geologic time is ham...
Here we show that the onset of deep water overflow from the Norwegian-Greenland Sea into the North A...
Here we show that the onset of deep water overflow from the Norwegian-Greenland Sea into the North A...
Ocean circulation plays a critical role in the Earth’s climate system through the storage and transf...
This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Depar...
The tidally driven vertical diffusivity in the abyssal ocean during the early Eocene (55 Ma) is inve...
North Atlantic Deep Water (NADW) currently redistributes heat and salt between Earth’s ocean basins,...
Here we publish simulated early-middle Eocene annual mean ocean temperature, salinity, density, mixe...
Milankovitch band variations of past climate, inferred from the rock record, have been used to astro...
The differential effects of climate change, sea level, and water mass circulation on deposition/eros...
Earth’s continents in the present day are the dispersed fragments of the former supercontinent Pange...
The warming trend that started in the latest Paleocene and culminated in the Early Eocene Climatic O...
The middle Eocene is a transitional period from the greenhouse early Eocene to the ice-house Eocene-...
The Atlantic meridional overturning circulation (AMOC) is a key component of the modern global ocean...
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