- Abstract:
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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...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 1.4mb)
-
- Publisher copy:
- 10.1016/j.epsl.2016.10.005
-
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Earth and Planetary Science Letters Journal website
- Volume:
- 457
- Pages:
- 325-334
- Publication date:
- 2016-11-02
- Acceptance date:
- 2016-10-07
- DOI:
- EISSN:
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1385-013X
- ISSN:
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0012-821X
- Pubs id:
-
pubs:656433
- URN:
-
uri:fb3ac99c-39a4-4ffb-a698-c2f5ba923199
- UUID:
-
uuid:fb3ac99c-39a4-4ffb-a698-c2f5ba923199
- Local pid:
- pubs:656433
- Copyright holder:
- Elsevier B.V.
- Copyright date:
- 2016
- Notes:
-
Copyright © 2016 Elsevier B.V. This is the accepted manuscript version of the article. The final version is available online from Elsevier at: https://doi.org/10.1016/j.epsl.2016.10.005
Journal article
Speleothem evidence for MIS 5c and 5a sea level above modern level at Bermuda
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