Rapid flooding of the sunda shelf: A late-glacial sea-level record.

Hanebuth, T., Stattegger, K. and Grootes, P. M. (2000) Rapid flooding of the sunda shelf: A late-glacial sea-level record. Science, 288 (5468). pp. 1033-5. DOI 8284 [pii].

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Abstract

The increase in sea level from the last glacial maximum has been derived from a siliciclastic system on the tectonically stable Sunda Shelf in Southeast Asia. The time from 21 to 14 thousand calendar years before the present has been poorly covered in other records. The record generally confirms sea-level reconstructions from coral reefs. The rise of sea level during meltwater pulse 1A was as much as 16 meters within 300 years (14.6 to 14.3 thousand years ago).

Document Type: Article
Additional Information: Journal article United states Science (New York, N.Y.) Science. 2000 May 12;288(5468):1033-5.
Research affiliation: Kiel University
Refereed: Yes
Publisher: American Association for the Advancement of Science (AAAS)
Date Deposited: 02 Feb 2012 07:52
Last Modified: 28 Mar 2018 11:00
URI: https://oceanrep.geomar.de/id/eprint/16342

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