Reduced advection into Atlantic Ocean deep eastern basins during last glaciation maximum
- 1 December 1983
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 306 (5943) , 577-580
- https://doi.org/10.1038/306577a0
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Carbon Isotopic Changes in Benthic Foraminifera from the Western South Atlantic: Reconstruction of Glacial Abyssal Circulation PatternsPublished by Cambridge University Press (CUP) ,2017
- Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical EvidenceScience, 1982
- Glacial to interglacial changes in ocean chemistryProgress in Oceanography, 1982
- Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminiferaMarine Micropaleontology, 1981
- Core-top evaluation of benthic foraminiferal isotopic ratios for paleo-oceanographic interpretationsPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Paleocirculation of the Deep North Atlantic: 150,000-Year Record of Benthic Foraminifera and Oxygen-18Science, 1979
- The deep waters of the western North Atlantic during the past 24,000 years, and the re-initiation of the Western Boundary UndercurrentMarine Micropaleontology, 1979
- Carbon-13 in Uvigerina: Tropical Rainforest History and the Equatorial Pacific Carbonate Dissolution CyclesPublished by Springer Nature ,1977
- Upper Pleistocene Ethmodiscus rex Oozes from the Eastern Equatorial AtlanticMicropaleontology, 1975
- Pleistocene Climates and Chronology in Deep-Sea SedimentsScience, 1968