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

Saved in:
Authors:Duplessy, Jean-Claude; Shackleton, Nicholas J.
Author Affiliations:Primary:
CNRS-CEA, Cent. Fribles Radioact., Gif-sur-Yvette, France
Other:
Univ. Cambridge, United Kingdom
Volume Title:Nature (London)
Source:Nature (London), 316(6028), p.500-507. Publisher: Macmillan Journals, London, United Kingdom. ISSN: 0028-0836
Publication Date:1985
Note:In English. 45 refs.; illus. incl. 1 table, sketch maps
Summary:The 13C analyses of benthic foraminifera from the major ocean basins show that circulation of the world ocean deep water is very sensitive to climate, and changes drastically during climatic transitions. [R.K.H.]
Subjects:Benthic taxa; Bottom currents; C-13/C-12; Carbon; Cenozoic; Climate effects; Climate-induced circulation; Currents; Deep-sea environment; Deglaciation; Foraminifera; Geochemical indicators; Glacial environment; Global; Interglacial environment; Isotopes; Marine environment; Microfossils; O-18/O-16; Ocean circulation; Oxygen; Paleo-oceanography; Paleocirculation; Paleoclimatology; Paleoecology; Pleistocene; Quaternary; Stable isotopes; Stratigraphy; Upper Pleistocene; World ocean; Changes; Evolution; Invertebrata; Protista
Abstract Numbers:86M/2086
Record ID:1985082671
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
Tags: Add Tag
No Tags, Be the first to tag this record!
Be the first to leave a comment!
You must be logged in first