2023 - Research.com Earth Science in United States Leader Award
His primary scientific interests are in Oceanography, Paleontology, Glacial period, Cenozoic and Quaternary. His Oceanography study is mostly concerned with Foraminifera, Deep sea, Paleoclimatology, Climate change and Ice sheet. The study incorporates disciplines such as Ocean current and Thermohaline circulation in addition to Paleoclimatology.
His study in Ice sheet is interdisciplinary in nature, drawing from both Meltwater and Younger Dryas. His Neogene and Late Miocene study, which is part of a larger body of work in Paleontology, is frequently linked to Surface, bridging the gap between disciplines. His work deals with themes such as Volcanism, Water column, Eocene Thermal Maximum 2 and Cretaceous, which intersect with Cenozoic.
Oceanography, Paleontology, Foraminifera, Benthic zone and Younger Dryas are his primary areas of study. His research integrates issues of Glacial period and Quaternary in his study of Oceanography. The concepts of his Glacial period study are interwoven with issues in Holocene and Ice sheet.
His research investigates the link between Foraminifera and topics such as Sediment that cross with problems in Structural basin. In Benthic zone, James P. Kennett works on issues like Table, which are connected to Mineralogy. James P. Kennett has included themes like Megafauna, Radiocarbon dating and Physical geography in his Younger Dryas study.
His scientific interests lie mostly in Oceanography, Paleontology, Younger Dryas, Foraminifera and Quaternary. His Oceanography study combines topics in areas such as Structural basin, Sediment and Continental margin. His Paleontology study incorporates themes from Isotopes of oxygen and Plankton.
His work on Younger Dryas impact hypothesis as part of general Younger Dryas study is frequently linked to COSMIC cancer database, bridging the gap between disciplines. The various areas that he examines in his Foraminifera study include Glacial period, Deglaciation, Stadial and Oxygen minimum zone. His study explores the link between Quaternary and topics such as Methane that cross with problems in Geomorphology, Earth science and Environmental chemistry.
The scientist’s investigation covers issues in Younger Dryas, Paleontology, Oceanography, Glacial period and Younger Dryas impact hypothesis. His Younger Dryas research incorporates elements of Glacier, Greenland Ice Sheet Project, Northern Hemisphere and Impact winter. His study involves Foraminifera, Ocean current and Climate change, a branch of Oceanography.
His studies in Foraminifera integrate themes in fields like Deglaciation and Holocene. His Younger Dryas impact hypothesis study also includes fields such as
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Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene
J. P. Kennett;L. D. Stott.
Cenozoic evolution of Antarctic glaciation the Circum-Antarctic Ocean and their impact on global paleoceanography
James P. Kennett.
Journal of Geophysical Research (1977)
The middle Miocene climatic transition: East Antarctic ice sheet development, deep ocean circulation and global carbon cycling
Benjamin P. Flower;James P. Kennett.
Palaeogeography, Palaeoclimatology, Palaeoecology (1994)
Neogene planktonic foraminifera: A phylogenetic atlas
James P. Kennett;M. S. Srinivasan.
Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode
Wallace S. Broecker;James P. Kennett;Benjamin P. Flower;James T. Teller.
Brief interstadial events in the Santa Barbara basin, NE Pacific, during the past 60 kyr
Richard J. Behl;Richard J. Behl;James P. Kennett.
Carbon isotopic evidence for methane hydrate instability during quaternary interstadials
James P. Kennett;Kevin G. Cannariato;Ingrid L. Hendy;Richard J. Behl.
Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling
R. B. Firestone;A. West;J. P. Kennett;L. Becker.
Proceedings of the National Academy of Sciences of the United States of America (2007)
Middle Miocene Southern Ocean cooling and Antarctic cryosphere expansion.
Amelia E. Shevenell;James P. Kennett;David W. Lea.
The chronology of the last deglaciation: implications to the cause of the Younger Dryas event
W. S. Broecker;M. Andree;W. Wolfli;H. Oeschger.
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