A regional 8200 cal. yr BP cooling event in northwest Europe, induced by final stages of the Laurentide ice‐sheet deglaciation?-Reference-Cited by-同舟云学术

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A regional 8200 cal. yr BP cooling event in northwest Europe, induced by final stages of the Laurentide ice‐sheet deglaciation?

Published:1998-03 Issue:2 Volume:13 Page:165-169
ISSN:0267-8179
Container-title:Journal of Quaternary Science
language:en
Short-container-title:J Quaternary Science

Author:

Klitgaard‐Kristensen Dorthe¹,Sejrup Hans Petter¹,Haflidason Haflidi¹,Johnsen Sigfus²,Spurk Marco³

Affiliation:

1. Department of Geology, University of Bergen, N‐5007 Bergen, Norway

2. The Niels Bohr Institute, Department of Geophysics, University of Copenhagen, Juliane Maries vej 30, DK‐2100 Copenhagen, Denmark

3. Botanical Institute, Garbenstr. 30, University of Hohenheim, D‐70593 Stuttgart, Germany

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/%28SICI%291099-1417%28199803/04%2913%3A2%3C165%3A%3AAID-JQS365%3E3.0.CO%3B2-%23

Reference31 articles.

1. Holocene climatic instability: A prominent, widespread event 8200 yr ago

2. Final stages in the collapse of the laurentide ice sheet, Hudson Strait, Canada, NWT: 14C AMS dates, seismics stratigraphy, and magnetic susceptibility logs

3. Synchronized Terrestrial Atmospheric Deglacial Records Around the North Atlantic

4. Reef drowning during the last deglaciation: Evidence for catastrophic sea-level rise and ice-sheet collapse

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