Was deep water formed in the North Pacific during the Late Quaternary? Cadmium evidence from the Northwest Pacific
- 30 June 1994
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 124 (1-4) , 185-194
- https://doi.org/10.1016/0012-821x(94)00082-4
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- An Oceanographic Explanation for the Apparent Carbon Isotope‐Cadmium Discordancy in the Glacial Antarctic?Paleoceanography and Paleoclimatology, 1993
- The influence of air and sea exchange on the carbon isotope distribution in the seaGlobal Biogeochemical Cycles, 1992
- Paleoenvironmental Change of the Kuroshio Region since the Last Glacial Age.The Quaternary Research (Daiyonki-Kenkyu), 1992
- Water Mass Conversion in the Glacial Subarctic Pacific (54°N, 148°W): Physical Constraints and the Benthic‐Planktonic Stable Isotope RecordPaleoceanography and Paleoclimatology, 1991
- Changes in redox conditions in deep-sea sediments of the subarctic North Pacific Ocean: Possible evidence for the presence of North Pacific Deep WaterPaleoceanography and Paleoclimatology, 1989
- Cadmium: Chemical tracer of deepwater paleoceanographyPaleoceanography and Paleoclimatology, 1988
- Changes in the distribution of δ13C of deep water ΣCO2 between the Last Glaciation and the HolocenePaleoceanography and Paleoclimatology, 1988
- Variability in the deep and intermediate water circulation of the Atlantic Ocean during the past 25,000 years: Northern Hemisphere modulation of the Southern OceanEarth and Planetary Science Letters, 1987
- Why is no deep water formed in the North Pacific?Journal of Marine Research, 1983
- Water chemistry control of cadmium content in Recent benthic foraminiferaNature, 1982