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Science 14 November 1997: Vol. 278. no. 5341, pp. 1257 - 1266 DOI: 10.1126/science.278.5341.1257
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Research Articles
A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates
Gerard Bond,
*
William Showers,
Maziet Cheseby,
Rusty Lotti,
Peter Almasi,
Peter deMenocal,
Paul Priore,
Heidi Cullen,
Irka Hajdas,
Georges Bonani
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.
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.
*
To whom correspondence should be addressed. E-mail:
gcb{at}lamont.ldgo.columbia.edu
Read the Full Text
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- Mire-development pathways and palaeoclimatic records from a full Holocene peat archive at Walton Moss, Cumbria, England.
- P. D. M. Hughes, P. D. M. Hughes, D. Mauquoy, K. E. Barber, and P. G. Langdon (2000)
The Holocene
10, 465-479
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- Evidence of 550-year and 1000-year cyclicities in North Atlantic circulation patterns during the Holocene.
- M. R. Chapman, M. R. Chapman, and N. J. Shackleton (2000)
The Holocene
10, 287-291
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- Drought and dust deposition in the West African Sahel: a 5500-year record from Kajemarum Oasis, northeastern Nigeria.
- F. A. Street-Perrott, F. A. Street-Perrott, J. A. Holmes, M. P. Waller, M. J. Allen, N. G. H. Barber, P. A. Fothergill, D. D. Harkness, M. Ivanovich, D. Kroon, et al. (2000)
The Holocene
10, 293-302
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- Was a change in thermohaline circulation responsible for the Little Ice Age?.
- W. S. Broecker (2000)
PNAS
97, 1339-1342
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- Detecting Holocene changes in thermohaline circulation.
- L. D. Keigwin and E. A. Boyle (2000)
PNAS
97, 1343-1346
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