Southernmost evidence of large European Ice Sheet-derived freshwater discharges during the Heinrich Stadials of the Last Glacial Period (Galician Interior Basin, Northwest Iberian Continental Margin)
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- 作者：M. Plaza-Morlotea ; D. Reya ; danirey@uvigo.es" class="auth_mail" title="E-mail the corresponding author ; J.F. Santosb ; S. Ribeirob ; D. Heslopc ; A. Bernabeua ; K.J. Mohameda ; B. Rubioa ; V. Martí ; nsd ; b
- 关键词：neodymium and strontium isotopes ; magnetic properties ; Heinrich Stadials ; ice rafted detritus ; meltwater ; Last Glacial Period
- 刊名：Earth and Planetary Science Letters
- 出版年：2017
- 出版时间：1 January 2017
- 年：2017
- 卷：457
- 期：Complete
- 页码：213-226
- 全文大小：3463 K
文摘
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HS identification and delimitation at Iberian Margin by non-nutrient based proxies.
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Isotopic and FORC provenance of the last six HSs in a distal area.
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Laurentide IRD are preceded in time by European meltwater (Channel River) discharges.
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EIS fluvial inputs can intensify AMOC weakening and accelerate LIS–EIS collapses.