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A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates
Abstract
Evidence from North Atlantic deep sea cores reveals that abrupt shifts punctuated what is conventionally thought to have been a relatively stable Holocene climate. During each of these episodes, cool, ice-bearing waters from north of Iceland were advected as far south as the latitude of Britain. At about the same times, the atmospheric circulation above Greenland changed abruptly. Pacings of the Holocene events and of abrupt climate shifts during the last glaciation are statistically the same; together, they make up a series of climate shifts with a cyclicity close to 1470 ± 500 years. The Holocene events, therefore, appear to be the most recent manifestation of a pervasive millennial-scale climate cycle operating independently of the glacial-interglacial climate state. Amplification of the cycle during the last glaciation may have been linked to the North Atlantic's thermohaline circulation.
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Climate oscillations since the end of the Wisconsinan glaciation, and especially in the Holocene, were much more regular and frequent than had been previously thought.
“Evidence from sediments in the North Atlantic shows that climate oscillations since the end of the Wisconsinan glaciation, and especially in the Holocene, were much more regular and frequent than had been previously thought (Bond et al., 1997).”
From Late-Quaternary history of the alpine flora of the New Hampshire White Mountains (2002) · cites this paper as Bond et al., 1997
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Walker, M. J. C., Berkelhammer, M., Björck, S., Cwynar, L. C., Fisher, D. A., Long, A. J., Lowe, J. J., Newnham, R. M., Rasmussen, S. O., & Weiss, H. (2012) · Journal of Quaternary Science · doi:10.1002/jqs.2565 · Cited by 919
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Wanner, H., Mercolli, L., Grosjean, M., & Ritz, S. P. (2015) · Journal of the Geological Society · doi:10.1144/jgs2013-101 · Cited by 218
The Pace of Cultural Evolution
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Late-Quaternary history of the alpine flora of the New Hampshire White Mountains
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Metadata
- Authors
- Bond, G., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., & Bonani, G.
- Affiliations
- G. Bond, M. Cheseby, R. Lotti, P. Almasi, P. deMenocal, P. Priore, and H. Cullen are at the Lamont-Doherty Earth Observatory of Columbia University, Route 9W, Palisades, NY 10964, USA. W. Showers is in the Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, 1125 Jordan Hall, Raleigh, NC 27695, USA. I. Hajdas and G. Bonani are in the AMS 14C Lab, ITP Eidgenössische Technische Hochschule (ETH) Honeggerberg, CH-8093 Zurich, Switzerland.
- Venue
- Science
- Published
- 1997-11-14
- Volume
- 278
- Issue
- 5341
- Pages
- 1257-1266
- ISSN
- 0036-8075
- 1095-9203
- Cited by
- 2,720
- References
- 1
- Language
- en
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