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Maureen Raymo

Maureen E. Raymo (born 1959) is an American paleoclimatologist and marine geologist. She is the Co-Founding Dean Emerita of the Columbia Climate School and the G. Unger Vetlesen Professor of Earth & Environmental Sciences at Columbia University. From 2011 to 2022, she was also the Director of Lamont-Doherty Earth Observatory's (LDEO) Core Repository and…

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Alma mater
Brown University (Sc.B) · Columbia University (M.A., M.Phil., Ph.D.)
Born
(1959-12-27) December 27, 1959 (age 66) Los Angeles
Fields
Climate Scientist and Marine Geologist
Workplaces
Lamont–Doherty Earth Observatory · Columbia University · Columbia Climate School

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Maureen Raymo

Nodes52
Edges51
Triples16
Avg. degree1.96
Density0.038462
Components1

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Maureen Raymo

Top relations

related to External links · 5
Maureen Raymo → Columbia University, Doherty Earth Observatory, Lamont, Maureen RaymoCurrent, Personal Website
Workplaces · 3
Maureen Raymo → Columbia Climate School, Columbia University, Lamont–Doherty Earth Observatory
Alma mater · 2
Maureen Raymo → Brown University (Sc.B), Columbia University (M.A., M.Phil., Ph.D.)
Born · 1
Maureen Raymo → (1959-12-27) December 27, 1959 (age 66) Los Angeles
Fields · 1
Maureen Raymo → Climate Scientist and Marine Geologist

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Important terminology

raymo sea level pliocene also earth ice climate university columbia hypothesis work marine science years shorelines sciences past first change

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
Maureen RaymoAlma materBrown University (Sc.B)1.00infobox
Maureen RaymoAlma materColumbia University (M.A., M.Phil., Ph.D.)1.00infobox
Maureen RaymoBorn(1959-12-27) December 27, 1959 (age 66) Los Angeles1.00infobox
Maureen RaymoFieldsClimate Scientist and Marine Geologist1.00infobox
Maureen RaymoWorkplacesLamont–Doherty Earth Observatory1.00infobox
Maureen RaymoWorkplacesColumbia University1.00infobox
Maureen RaymoWorkplacesColumbia Climate School1.00infobox
the Himalayasinstance oftectonic uplift of areas0.80text
Tibetan Plateau over the last 40 million years enhanced the chemical weathering of mineralsinstance oftectonic uplift of areas0.80text
which removed carbon dioxide from the atmosphereinstance oftectonic uplift of areas0.80text
resulted in cooling that spurred the growth of large ice sheetsinstance oftectonic uplift of areas0.80text
Maureen Raymorelated to External linksLamont0.60section

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