2011 - Fellow of the American Association for the Advancement of Science (AAAS)
2001 - Fellow of American Geophysical Union (AGU)
His primary scientific interests are in Oceanography, Foraminifera, North Atlantic Deep Water, Thermohaline circulation and Glacial period. His work on Oceanography is being expanded to include thematically relevant topics such as Paleontology. His Foraminifera research is multidisciplinary, relying on both Bottom water, δ18O and Radiocarbon dating.
His North Atlantic Deep Water research is multidisciplinary, incorporating elements of Younger Dryas, Climate change, Abrupt climate change and Atlantic multidecadal oscillation. His Glacial period study combines topics from a wide range of disciplines, such as Ice core, Holocene and Ice sheet. His Paleoclimatology study incorporates themes from Quaternary and Terrigenous sediment.
His primary areas of investigation include Oceanography, Foraminifera, Table, Paleontology and Glacial period. All of his Oceanography and Holocene, Deglaciation, North Atlantic Deep Water, Deep sea and Last Glacial Maximum investigations are sub-components of the entire Oceanography study. He interconnects Younger Dryas and Radiocarbon dating in the investigation of issues within Deglaciation.
His studies in North Atlantic Deep Water integrate themes in fields like Atlantic multidecadal oscillation, Climate change and Gulf Stream. In his study, which falls under the umbrella issue of Foraminifera, Geomorphology is strongly linked to Geochemistry. His Glacial period research includes themes of Paleoclimatology and Ice sheet.
His primary areas of study are Oceanography, Last Glacial Maximum, Holocene, Glacial period and Deglaciation. The concepts of his Oceanography study are interwoven with issues in Sediment, Climatology and Radiocarbon dating. His Last Glacial Maximum research is multidisciplinary, relying on both Abyssal zone, Water mass, Atlantic water and Deep sea.
His research in the fields of Stadial overlaps with other disciplines such as Vegetation. His Glacial period study deals with North Atlantic Deep Water intersecting with Abrupt climate change. His work deals with themes such as Younger Dryas, Physical geography, Quaternary science and Paleoclimatology, which intersect with Deglaciation.
Lloyd D Keigwin mostly deals with Oceanography, Glacial period, Last Glacial Maximum, Deep sea and Deglaciation. His Oceanography and Foraminifera, Younger Dryas, Sea ice, Ocean current and Ice sheet investigations all form part of his Oceanography research activities. The various areas that Lloyd D Keigwin examines in his Glacial period study include North Atlantic Deep Water and Climate change.
His Last Glacial Maximum study also includes fields such as
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Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes
J. F. McManus;R. Francois;J.-M. Gherardi;L. D. Keigwin.
Nature (2004)
North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature
Edward A. Boyle;Lloyd Keigwin.
Nature (1987)
Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years : changes in deep ocean circulation and chemical inventories
E.A. Boyle;L.D. Keigwin.
Earth and Planetary Science Letters (1985)
Sudden changes in North Atlantic circulation during the last deglaciation
Scott J. Lehman;Lloyd D. Keigwin.
Nature (1992)
The Little Ice Age and Medieval warm period in the Sargasso Sea
Lloyd D. Keigwin.
Science (1996)
Formation of the Isthmus of Panama
Aaron O’Dea;Harilaos A. Lessios;Anthony G. Coates;Ron I. Eytan.
Science Advances (2016)
Isotopic Paleoceanography of the Caribbean and East Pacific: Role of Panama Uplift in Late Neogene Time
Lloyd Keigwin.
Science (1982)
Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence
Edward A. Boyle;Lloyd D. Keigwin.
Science (1982)
The influence of microhabitats on the carbon isotopic composition of deep-sea benthic foraminifera
Daniel C. McCorkle;Lloyd D. Keigwin;Bruce H. Corliss;Steven R. Emerson.
Paleoceanography (1990)
Pliocene closing of the Isthmus of Panama, based on biostratigraphic evidence from nearby Pacific Ocean and Caribbean Sea cores
Lloyd D. Keigwin.
Geology (1978)
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