North Atlantic Deepwater Temperature Change During Late Pliocene and Late Quaternary Climatic Cycles

Author:

Dwyer Gary S.1,Cronin Thomas M.2,Baker Paul A.1,Raymo Maureen E.3,Buzas Jeffrey S.4,Corrège Thierry5

Affiliation:

1. G. S. Dwyer and P. A. Baker, Department of Geology, Duke University, Durham, NC 27708, USA.

2. T. M. Cronin, U.S. Geological Survey, Branch of Paleontology and Stratigraphy, Mail Stop 970 National Center, Reston, VA 22092, USA.

3. M. E. Raymo, Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA.

4. J. S. Buzas, Department of Mathematics and Statistics, University of Vermont, Burlington, VT 05051, USA.

5. T. Corrège, Départment de Géologie et Océanographie, Université de Bordeaux I, Avenue des Facultés, Bordeaux, France.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference52 articles.

1. DIAGENESIS OF CARBONATES IN DEEP-SEA SEDIMENTS - EVIDENCE FROM SR/CA RATIOS AND INTERSTITIAL DISSOLVED SR2+ DATA;BAKER P.A.;JOURNAL OF SEDIMENTARY PETROLOGY,1982

2. COMPARISON OF ATLANTIC AND PACIFIC PALEOCHEMICAL RECORDS FOR THE LAST 215,000 YEARS - CHANGES IN DEEP OCEAN CIRCULATION AND CHEMICAL INVENTORIES;BOYLE E.A.;EARTH AND PLANETARY SCIENCE LETTERS,1985

3. BOYLE E.A., SCIENCE 249, 863 (1991).

4. DOES THE OCEAN-ATMOSPHERE SYSTEM HAVE MORE THAN ONE STABLE MODE OF OPERATION;BROECKER W.S.;NATURE,1985

5. BROECKER W.S., PALAEOCEANOGRAPHY 3, 1 (1988).

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