Paired benthic foraminiferal Cd/Ca and Zn/Ca evidence for a greatly increased presence of Southern Ocean Water in the glacial North Atlantic
- 15 August 2002
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 17 (3) , 10-1-10-18
- https://doi.org/10.1029/2000pa000598
Abstract
No abstract availableKeywords
This publication has 65 references indexed in Scilit:
- Glacial-to-Holocene Redistribution of Carbonate Ion in the Deep SeaScience, 2001
- Chemical Hydrography of the South Atlantic During the Last Glacial Maximum: Cd vs. δ13CPublished by Springer Nature ,1996
- Deep thermohaline circulation in the low‐latitude Atlantic during the Last GlacialPaleoceanography and Paleoclimatology, 1995
- Cadmium/calcium and carbon isotope reconstructions of the glacial northeast Atlantic OceanPaleoceanography and Paleoclimatology, 1995
- North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperatureNature, 1987
- Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: changes in deep ocean circulation and chemical inventoriesEarth and Planetary Science Letters, 1985
- Does the ocean–atmosphere system have more than one stable mode of operation?Nature, 1985
- Hydrography of the central Atlantic—IV. Intermediate waters of antarctic originDeep Sea Research Part A. Oceanographic Research Papers, 1981
- Cadmium, zinc, copper, and barium in foraminifera testsEarth and Planetary Science Letters, 1981
- Oceanographic distributions of cadmium, zinc, nickel, and copper in the North PacificEarth and Planetary Science Letters, 1980