Ocean ventilation during the last 12,000 years: Hypothesis of counterpoint deep water production
- 30 November 1987
- journal article
- Published by Elsevier in Marine Geology
- Vol. 78 (1-2) , 1-10
- https://doi.org/10.1016/0025-3227(87)90064-8
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Limits on the ventilation rate for the deep ocean over the last 12000 yearsClimate Dynamics, 1986
- AMS Radiocarbon Dates on Foraminifera from Deep Sea SedimentsRadiocarbon, 1986
- On the time-scale of deglaciation: Atlantic deep-sea sediments and gulf of MexicoPalaeogeography, Palaeoclimatology, Palaeoecology, 1985
- 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
- 14C measurements on foraminifera of deep sea core V28-238 and their preliminary interpretationNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1984
- Radiocarbon measurements on coexisting benthic and planktic foraminifera shells: potential for reconstructing ocean ventilation times over the past 20 000 yearsNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1984
- Radiocarbon-dated evidence of worldwide early Holocene climate changeGeology, 1983
- Box cores from the equatorial Pacific: 14C sedimentation rates and benthic mixingMarine Geology, 1982
- ‘Unmixing’ of the deep-sea record and the deglacial meltwater spikeNature, 1977
- Glacial-Holocene Transition in Deep-Sea Carbonates: Selective Dissolution and the Stable Isotope SignalScience, 1977