Sporadic shutdown of North Atlantic deep water production during the Glacial–Holocene transition?
- 1 November 1986
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 324 (6092) , 53-55
- https://doi.org/10.1038/324053a0
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- Abyssal characteristics of the World Ocean watersPublished by Elsevier ,2003
- Biological fractionation of oxygen and carbon isotopes by recent benthic foraminiferaPublished by Elsevier ,2003
- Deep-sea carbonates: Reading the carbon-isotope signalInternational Journal of Earth Sciences, 1986
- Does the ocean–atmosphere system have more than one stable mode of operation?Nature, 1985
- Ocean circulation in the Norwegian sea during the last deglaciation: Isotopic evidencePalaeogeography, Palaeoclimatology, Palaeoecology, 1985
- Two-Step Deglaciation: 14C-Dated High-Resolution δ18O Records from the Tropical Atlantic OceanQuaternary Research, 1985
- Box cores from the equatorial Pacific: 14C sedimentation rates and benthic mixingMarine Geology, 1982
- Stable isotopes in benthic foraminifera from ontong-java plateau, box cores ERDC 112 and 123Palaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Stable isotope composition of benthic foraminifera from the equatorial PacificNature, 1981
- Evidence of climatic changes in North Atlantic deep-sea cores, with remarks on isotopic paleotemperature analysisProgress in Oceanography, 1965