Near-field sea-level variability in northwest Europe and ice sheet stability during the last interglacial
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- 作者：A.J. Longa ; a.j.long@durham.ac.uk" class="auth_mail" title="E-mail the corresponding author ; N.L.M. Barlowa ; n.l.m.barlow@durham.ac.uk" class="auth_mail" title="E-mail the corresponding author ; F.S. Busschersb ; freek.busschers@tno.nl" class="auth_mail" title="E-mail the corresponding author ; K.M. Cohenc ; K.M.Cohen@uu.nl" class="auth_mail" title="E-mail the corresponding author ; W.R. Gehrelsd ; roland.gehrels@york.ac.uk" class="auth_mail" title="E-mail the corresponding author ; L.M. Wakee ; leanne.wake@northumbria.ac.uk" class="auth_mail" title="E-mail the corresponding author
- 关键词：Sea level ; Interglacial ; Ice-sheet collapse ; Eemian ; MIS 5e ; Glacio-isostatic adjustment
- 刊名：Quaternary Science Reviews
- 出版年：2015
- 出版时间：15 October 2015
- 年：2015
- 卷：126
- 期：Complete
- 页码：26-40
- 全文大小：2495 K
文摘
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Last Interglacial (LIG) highstand coral reefs record meter-scale sea-level jumps.
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We test for such jumps in nearfield, temperate coastal settings of Northwest Europe.
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There is no coherent, regional-scale evidence for large sea-level jumps.
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There is no strong evidence for LIG ice sheet collapse/regrowth during the highstand.
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Caution is needed when inferring ice sheet collapse from LIG highstand sea-level data.