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Speleothem evidence for MIS 5c and 5a sea level above modern level at Bermuda

Abstract:

The history of sea level in regions impacted by glacio-isostasy provides constraints on past ice-sheet distribution and on the characteristics of deformation of the planet in response to loading. The Western North Atlantic–Caribbean region, and Bermuda in particular, is strongly affected by the glacial forebulge that forms as a result of the Laurentide ice-sheet present during glacial periods. The timing of growth of speleothems, at elevations close to sea level can provide records of minimum...

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Publication status:
Published
Peer review status:
Peer reviewed

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
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Name:
Natural Environment Research Council
Grant:
NE/1008861/1
NE/I008365/1
Publisher:
Elsevier
Journal:
Earth and Planetary Science Letters More from this journal
Volume:
457
Pages:
325-334
Publication date:
2016-11-02
Acceptance date:
2016-10-07
DOI:
EISSN:
1385-013X
ISSN:
0012-821X
Keywords:
Pubs id:
pubs:656433
UUID:
uuid:fb3ac99c-39a4-4ffb-a698-c2f5ba923199
Local pid:
pubs:656433
Source identifiers:
656433
Deposit date:
2016-11-01

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