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Herbert, T. D. et al. (2001): Collapse of the California Current during glacial maxima linked to climate change on land
Leg/Site/Hole:
Related Expeditions:
ODP 146
ODP 167
ODP 167 1012
ODP 167 1020
ODP 146 893
Identifier:
ID:
2001-055492
Type:
georefid
Creator:
Name:
Herbert, T. D.
Affiliation:
Brown University, Department of Geological Sciences, Providence, RI, United States
Role:
author
Name:
Schuffert, J. D.
Affiliation:
University of California at Santa Cruz, United States
Role:
author
Name:
Andreasen, D.
Affiliation:
Lamont-Doherty Earth Observatory, United States
Role:
author
Name:
Heusser, L.
Affiliation:
Boise State University, United States
Role:
author
Name:
Lyle, M.
Affiliation:
Oregon State University, United States
Role:
author
Name:
Mix, A.
Affiliation:
University of Southern California, United States
Role:
author
Name:
Ravelo, A. C.
Affiliation:
Centro de Investigacion Cientifica y de Educacion Superior de Ensenada, Mexico
Role:
author
Name:
Stott, L. D.
Affiliation:
Role:
author
Name:
Herguera, J. C.
Affiliation:
Role:
author
Identification:
Title:
Collapse of the California Current during glacial maxima linked to climate change on land
Year:
2001
Source:
Science
Publisher:
American Association for the Advancement of Science, Washington, DC, United States
Volume:
293
Issue:
5527
Pages:
71-76
Abstract:
Language:
English
Genre:
Serial
Rights:
URL:
Coverage:
Geographic coordinates:
North:41.0003
West:-126.2604
East: -116.2500
South:32.1658
Keywords:
Quaternary geology; California; California Current; Cenozoic; climate change; continental margin; currents; Devils Hole; East Pacific; glacial environment; glacial geology; ice sheets; isotope ratios; isotopes; Leg 146; Leg 167; Nevada; North Pacific; Northeast Pacific; Nye County Nevada; O-18/O-16; ocean currents; Ocean Drilling Program; ODP Site 1012; ODP Site 1020; ODP Site 893; oxygen; Pacific Ocean; paleo-oceanography; paleoclimatology; paleotemperature; Quaternary; sea-surface temperature; stable isotopes; temperature; United States; upper Quaternary;
.
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