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Response of global deep-water circulation to Earth's climatic change 135,000–107,000 years ago

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Response of global deep-water circulation to Earth's climatic change 135,000–107,000 years ago (English)

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Jean-Claude Duplessy

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Nicholas J. Shackleton

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2

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language of work or name

English

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publication date

August 1985

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published in

Nature

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volume

316

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issue

6028

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page(s)

500-507

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https://scigraph.springernature.com/pub.10.1038/316500a0

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Warmth of the subpolar north atlantic ocean during northern hemisphere ice-sheet growth

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Deep water formation in the North Atlantic Ocean during the last ice age

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Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11.

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Paleocirculation of the deep north atlantic: 150,000-year record of benthic foraminifera and oxygen-18

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Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence

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Degree of saturation of CaCO3 in the oceans

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Temperature Dependence of Carbon Isotope Composition in Marine Plankton and Sediments

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Ocean chemistry during glacial time

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Oxygen Isotope Analyses and Pleistocene Temperatures Re-assessed

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Differential isotopic fractionation in benthic foraminifera and paleotemperatures reassessed

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Oxygen Isotope and Palaeomagnetic Stratigraphy of Equatorial Pacific Core V28-238: Oxygen Isotope Temperatures and Ice Volumes on a 105 Year and 106 Year Scale

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Glacial and interglacial wind regimes over the eastern subtropical Atlantic and North-West Africa

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Geology of Coral Terraces, Huon Peninsula, New Guinea: A Study of Quaternary Tectonic Movements and Sea-Level Changes

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Climatic conditions deduced from a 150-kyr oxygen isotope–pollen record from the Arabian Sea

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Polar ice evidence that atmospheric CO2 20,000 yr BP was 50% of present

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Carbon isotope data in core V19-30 confirm reduced carbon dioxide concentration in the ice age atmosphere

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DOI

10.1038/316500A0

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1034728589

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(Q59061750)

Response of global deep-water circulation to Earth's climatic change 135,000–107,000 years ago

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