Age determinations of sediments of the Sund Shelf

DOI

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).

According to natural changes in 14Catmos. some data can get more than one value of highest probability and more than one range of 1s probability during calibration. All samples measured at Leibniz-Labor, Kiel.

Supplement to: Hanebuth, Till J J; Stattegger, Karl; Grootes, Pieter Meiert (2000): Rapid flooding of the Sunda Shelf - a late-glacial sea-level record. Science, 288(5468), 1033-1035

Identifier
DOI https://doi.org/10.1594/PANGAEA.400944
Related Identifier https://doi.org/10.1126/science.288.5468.1033
Related Identifier https://doi.org/10.2312/reports-ifg.2000.12
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.400944
Provenance
Creator Hanebuth, Till J J ORCID logo
Publisher PANGAEA
Publication Year 2000
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 373 data points
Discipline Geosciences; Natural Sciences
Spatial Coverage (107.631W, 2.307S, 109.747E, 9.387N); Vietnam shelf; Sunda Shelf
Temporal Coverage Begin 1996-12-17T00:00:00Z
Temporal Coverage End 1997-01-08T00:00:00Z