Marine Isotope Stage 3 sea level fluctuations: data synthesis and new outlook
Marine Isotope Stage 3 sea level fluctuations: data synthesis and new outlook
To develop a better understanding of the abrupt Dansgaard-Oeschger mode of climate change, it is essential that we establish whether the ice sheets are actively involved, as trigger or amplifier, or whether they merely respond in a passive manner. This requires careful assessment of the fundamental issues of magnitude and phasing of global ice volume fluctuations within marine isotope stage 3 (MIS 3), which to date remain enigmatic. We review recent advances in observational studies pertaining to these key issues and discuss the implications for modeling studies. Our aim is to construct a robust stratigraphic framework for the MIS 3 period regarding sea level variability, using the most up-to-date arguments available by combining insights from both modeling and observational approaches.
RG4003
Siddall, M.
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Rohling, E.J.
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Thompson, W.G.
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Waelbroeck, C.
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5 November 2008
Siddall, M.
9c045dd5-498b-488b-9c67-23e24d90ebcc
Rohling, E.J.
a2a27ef2-fcce-4c71-907b-e692b5ecc685
Thompson, W.G.
cadba642-3fa0-4989-8dbb-88ec1be0b238
Waelbroeck, C.
af7f17f5-9cd7-4e07-9b8b-21ed778971f2
Siddall, M., Rohling, E.J., Thompson, W.G. and Waelbroeck, C.
(2008)
Marine Isotope Stage 3 sea level fluctuations: data synthesis and new outlook.
Reviews of Geophysics, 46, .
(doi:10.1029/2007RG000226).
Abstract
To develop a better understanding of the abrupt Dansgaard-Oeschger mode of climate change, it is essential that we establish whether the ice sheets are actively involved, as trigger or amplifier, or whether they merely respond in a passive manner. This requires careful assessment of the fundamental issues of magnitude and phasing of global ice volume fluctuations within marine isotope stage 3 (MIS 3), which to date remain enigmatic. We review recent advances in observational studies pertaining to these key issues and discuss the implications for modeling studies. Our aim is to construct a robust stratigraphic framework for the MIS 3 period regarding sea level variability, using the most up-to-date arguments available by combining insights from both modeling and observational approaches.
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Published date: 5 November 2008
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Local EPrints ID: 50919
URI: http://eprints.soton.ac.uk/id/eprint/50919
PURE UUID: 98e2e894-607d-44e5-982b-d1074c17133a
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Date deposited: 16 Apr 2008
Last modified: 16 Mar 2024 02:46
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Author:
M. Siddall
Author:
W.G. Thompson
Author:
C. Waelbroeck
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