K
K. McIntyre
Researcher at California Institute of Technology
Publications - 4
Citations - 1202
K. McIntyre is an academic researcher from California Institute of Technology. The author has contributed to research in topics: North Atlantic Deep Water & Glacial period. The author has an hindex of 3, co-authored 4 publications receiving 1122 citations. Previous affiliations of K. McIntyre include University of California, Santa Cruz.
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Journal ArticleDOI
The Salinity, Temperature, and δ18O of the Glacial Deep Ocean
TL;DR: In this paper, pore fluid measurements of the chloride concentration and the oxygen isotopic composition from Ocean Drilling Program cores were used to reconstruct salinity and temperature of the deep ocean during the last glacial maximum (LGM).
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The oxygen isotopic composition of seawater during the Last Glacial Maximum
Daniel P. Schrag,Jess F. Adkins,K. McIntyre,Jane Alexander,David A. Hodell,Christopher D. Charles,Jerry F. McManus +6 more
TL;DR: In this paper, high-resolution oxygen and hydrogen isotope measurements were made on pore fluids from deep-sea sediments from sites in the North and South Atlantic to provide direct measurements of changes in the isotopic composition of bottom waters during the Last Glacial Maximum (LGM).
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Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene
Maureen E. Raymo,Delia W Oppo,Benjamin P. Flower,David A. Hodell,Jerry F. McManus,Kathryn A Venz,K. F. Kleiven,K. McIntyre +7 more
TL;DR: In this article, a compilation of data suggests that, unlike today (an extreme interglaciation), the two primary sources of northern deep water, Norwegian-Greenland Sea and Labrador Sea/subpolar North Atlantic, had different characteristic δ13C values over most of the Pleistocene.
Journal ArticleDOI
Ground truthing the Cd/Ca-carbon isotope relationship in foraminifera of the Greenland-Iceland-Norwegian Seas
K. McIntyre,Ana Christina Ravelo,Margaret Lois Delaney,Linda Davis Anderson,Truls Johannessen +4 more
TL;DR: In this article, the authors examined whether the paleoceanographic nutrient proxies, δ13C and cadmium/calcium in foraminiferal calcite, are well coupled to nutrients in the region of North Atlantic Deep Water formation, and presented data from two transects of the Greenland-Iceland-Norwegian Seas.