Physics – Geophysics
Scientist
Physics
Geophysics
Scientist
Lamont-Doherty Earth Observatory and Department of Earth and Environmental Sciences, Columbia University, Palisades, New York, USA
Institute for Isotope Geology and Mineral Resources, Department of Earth Sciences, ETH-Zentrum, Sonneggstrasse 5, CH-8092 Zürich, Switzerland for Isotope Geology and Mineral Resources, Department of Earth Sciences, ETH-Zentrum, NO C61, Sonneggstrasse 5, CH-8092, Zürich, Switzerland
Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY 10964, USA; Institute for Isotope Geology and Mineral Resources, ETH-Zentrum, Sonneggstrasse 5, CH-8092 Zürich, Switzerland
Lamont-Doherty Earth Observatory of Columbia University, New York, USA
Lamont-Doherty Earth Observatory, 61 Route 9W, Palisades, NY 10964, USA; Department of Earth and Environmental Sciences, Columbia University, 61 Route 9W, Palisades, NY 10964, USA
Lamont-Doherty Earth Observatory and Department of Earth and Environmental Sciences, Columbia University, New York 10964, USA
Department of Earth Sciences, Institute for Isotope Geology and Mineral Resources, ETH-Zentrum, NO C61, Sonneggstrasse 5, CH-8092, Zürich, Switzerland
Department of Earth and Environmental Sciences, Columbia University, 16 Rt. 9W, Palisades, NY 10964, USA; Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK
Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY 10964, USA; Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027, USA
Lamont-Doherty Earth Observatory of Columbia University; Palisades, New York, USA
Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
ETH-Zürich, Institute for Isotope Geology and Mineral Resources, ETH-Zentrum, NO C61, Sonneggstr. 5, Zürich, 8092 Switzerland of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory, Earth Institute at Colu
Ar-Ar ages of glacially transported hornblende, Wilkes Land, Antarctica
Atlantic Ocean water mass distribution over the past 32,000 yrs from Nd isotopes in deep-sea corals
Deep and bottom water export from the Southern Ocean to the Pacific over the past 38 million years
Deep-sea coral aragonite as a recorder for the neodymium isotopic composition of seawater
Enhanced Atlantic Merdional Overturning Circulation during pronounced interstadials
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