| Literature DB >> 10677463 |
Abstract
Throughout the last glacial cycle, reorganizations of deep ocean water masses were coincident with rapid millennial-scale changes in climate. Climate changes have been less severe during the present interglacial, but evidence for concurrent deep ocean circulation change is ambiguous.Entities:
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Year: 2000 PMID: 10677463 PMCID: PMC34300 DOI: 10.1073/pnas.97.4.1343
Source DB: PubMed Journal: Proc Natl Acad Sci U S A ISSN: 0027-8424 Impact factor: 11.205