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GISP2 Oxygen Isotope Ratios
Abstract
The GISP2 oxygen isotope record, with its high-resolution detail, yields crucial information on past climate change. The glacial δ 18 O oscillations of the GISP2 core, with their very fast onsets, are templates of a prototype oscillation of variable duration with an amplitude of 3.9‰. The halfway mark of the cold–warm transition is reached in 2 years; the top is reached in 50 years. The δ 18 O–time gradient of the leading front is about 7.8‰ per 100 yr. After reaching the top, δ 18 O slowly declines by −0.14‰ per 100 yr. The duration of δ 18 O decline varies from a couple of centuries for fast oscillations to about 4000 yr for slower ones. The subsequent δ 18 O downturn during the warm–cold transition has a δ 18 O–time gradient of −3.2‰ per 100 yr and lasts about 80 yr.
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Citations
Cited by
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Lambeck, K., & Chappell, J. (2001) · Science · doi:10.1126/science.1059549 · Cited by 1,619
Dust cycle: An emerging core theme in Earth system science
Shao, Y., Wyrwoll, K.-H., Chappell, A., Huang, J., Lin, Z., McTainsh, G. H., Mikami, M., Tanaka, T. Y., Wang, X., & Yoon, S. (2011) · Aeolian Research · doi:10.1016/j.aeolia.2011.02.001 · Cited by 1,085
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Peterson, L. C., Haug, G. H., Hughen, K. A., & Röhl, U. (2000) · Science · doi:10.1126/science.290.5498.1947 · Cited by 913
The Laurentide and Innuitian ice sheets during the Last Glacial Maximum
Dyke, A. S., Andrews, J. T., Clark, P. U., England, J. H., Miller, G. H., Shaw, J., & Veillette, J. J. (2002) · Quaternary Science Reviews · doi:10.1016/s0277-3791(01)00095-6 · Cited by 711
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Metadata
- Authors
- Stuiver, M., & Grootes, P. M.
- Venue
- Quaternary Research
- Publisher
- Cambridge University Press (CUP)
- Published
- 2000-05
- Volume
- 53
- Issue
- 3
- Pages
- 277-284
- ISSN
- 0033-5894 (ISSN-L)
- 1096-0287
- OpenAlex
- W2063409788
- Cited by
- 603
- References
- 0
- FWCI
- 18.66
- Type
- journal article
- Language
- en
- Open access
- closed
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