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GISP2 Oxygen Isotope Ratios

Stuiver, Minze, Grootes, Pieter M.·2000·Quaternary Research

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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Metadata

Authors
Stuiver, M., & Grootes, P. M.
Venue
Quaternary Research
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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CoChat. (2026). Citation check: GISP2 Oxygen Isotope Ratios. https://app.cochat.ai/papers/10.1006/qres.2000.2127
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Stuiver, M., & Grootes, P. M. (2000). GISP2 Oxygen Isotope Ratios. Quaternary Research. https://doi.org/10.1006/qres.2000.2127

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