Carbon 13 in Pacific Deep and Intermediate Waters, 0-370 ka: Implications for Ocean Circulation and Pleistocene CO2
نویسندگان
چکیده
منابع مشابه
North Atlantic surface-ocean control of Pleistocene deep-ocean circulation
Deep basins of the North Atlantic were occupied by a cold 13 C-depleted (nutrient-rich) water mass during glaciations, and a warmer 13C-enriched (nutrient-poor) water mass (modern NADW) during interglaciations. This mode of deep-water variability is related directly to migration of the North Atlantic Polar Front. Down-core stable isotope records from the Atlantic and Antarctic suggest that 13C ...
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a Department of Applied Mathematics, School of Mathematics and Statistics, University of New South Wales, Sydney, NSW 2052, Australia b Department of Geography/Earth Research Institute, University of California, Santa Barbara, CA 93106-4060, USA c Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, CA 90095-1565, USA d Lamont-Doherty Earth Observatory, Columbi...
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ژورنال
عنوان ژورنال: Paleoceanography
سال: 1991
ISSN: 0883-8305
DOI: 10.1029/90pa02303