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Changes in Atmospheric Convection Over the Indo‐Pacific Warm Pool and Coupled IOD and ENSO Patterns During the Last Glacial Maximum
GEOPHYSICAL RESEARCH LETTERS
17 march 2025
Xinquan Zhou, Stéphanie Duchamp-Alphonse, Xiaoxu S...
This study investigates how the convection over the Indo‐Pacific Warm Pool responds to the Last Glacial Maximum conditions. Paleoproductivity...
A Late Quaternary Spatiotemporal Reconstruction of Pacific Deoxygenation
OXYGENATION DYNAMICS IN PAST OCEANS II ORAL
paleoceanography and paleoclimatology | 10 december 2024
Martin Tetard, Alexander Pohl, Yusuke Okazaki, And...
Oxygen minimum zones (OMZs) are subsurface regions of the ocean that are severely depleted in dissolved oxygen (<0.5 mL L-1). Nowadays they extend ...
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A New Method for the Detection of Siliceous Microfossils on Sediment Microscope Slides Using Convolutional Neural Networks
JOURNAL OF GEOPHYSICAL RESEARCH: BIOGEOSCIENCES
01 september 2024
Camille Godbillot, Ross Marchant, Luc Beaufort, Ka...
Diatom communities preserved in sediment samples are valuable indicators for understanding the past and present dynamics of phytoplankton communiti...
Controls on Alkenone Carbon Isotope Fractionation in the Modern Ocean
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
23 december 2021
Samuel Phelps, Heather M. Stoll, Clara T. Bolton, ...
Carbon isotope records from alkenone biomarkers (εp37:2) produced by haptophyte algae are frequently used for atmospheric CO2 paleobarometry, ...
Harmonizing Miocene alkenone- and boron-based carbonate chemistry reconstructions
EXPLORING THE EVOLUTION OF THE EARTH SYSTEM DURING THE MIOCENE I
paleoceanography and paleoclimatology | 07 december 2020
Samuel R. Phelps, Heather M. Stoll, Clara T. Bolto...
The carbon isotopic composition of phytoplankton organic matter and the boron isotopic composition of planktic foraminifera are two key archives for r...
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Importance of Coccolithophores in the Ocean Deep Biomass
CONSTRAINING GREENHOUSE GAS EXCHANGE PROCESSES USING REMOTE SENSING AND IN SITU OBSERVATIONS II POSTERS
atmospheric sciences | 13 december 2019
Amos Winter, Manfredi Manizza, Josue Millan, Diana...
The Deep Biomass (DB), located in the lowest part of the euphotic zone (approx. 80 m to 300 m) primarily in the subtropical gyres is an unexplored par...
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Carbon trading in a low CO2 world: understanding carbon isotopic fractionation in coccolithophores over glacial-interglacial cycles
FALL MEETING 2018
12 december 2018
Clara T. Bolton, Luc Beaufort, Emmeline Gray, Samu...
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Paleoceanographic Evolution of the Equatorial Indian Ocean during the Late Miocene
FALL MEETING 2018
12 december 2018
Clara T. Bolton, Nils Andersen, Luc Beaufort, Mart...
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