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Four Climate Cycles of Recurring Deep and Surface Water Destabilizations on the Iberian Margin

Martrat, Belen, Grimalt, Joan O., Shackleton, Nicholas J., de Abreu, Lucia, Hutterli, Manuel A., Stocker, Thomas F.·2007·Science

Abstract

Centennial climate variability over the last ice age exhibits clear bipolar behavior. High-resolution analyses of marine sediment cores from the Iberian margin trace a number of associated changes simultaneously. Proxies of sea surface temperature and water mass distribution, as well as relative biomarker content, demonstrate that this typical north-south coupling was pervasive for the cold phases of climate during the past 420,000 years. Cold episodes after relatively warm and largely ice-free periods occurred when the predominance of deep water formation changed from northern to southern sources. These results reinforce the connection between rapid climate changes at Mediterranean latitudes and century-to-millennial variability in northern and southern polar regions.

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Metadata

Authors
Martrat, B., Grimalt, J. O., Shackleton, N. J., de Abreu, L., Hutterli, M. A., & Stocker, T. F.
Venue
Science
Published
2007-07-27
Volume
317
Issue
5837
Pages
502-507
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1978347718
Cited by
723
References
0
FWCI
16.66
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Four Climate Cycles of Recurring Deep and Surface Water Destabilizations on the Iberian Margin. https://app.cochat.ai/papers/10.1126/science.1139994
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Martrat, B., Grimalt, J. O., Shackleton, N. J., de Abreu, L., Hutterli, M. A., & Stocker, T. F. (2007). Four Climate Cycles of Recurring Deep and Surface Water Destabilizations on the Iberian Margin. Science. https://doi.org/10.1126/science.1139994

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Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.