Geochemistry on sediment core Co1014 from Rauer Group, Antarctica

DOI

The history of glacial advances and retreats of the East Antarctic ice sheet during the Holocene is not well-known, due to limited field evidence in both the marine and terrestrial realm. A 257-cm-long sediment core was recovered from a marine inlet in the Rauer Group, East Antarctica, 1.8 km in front of the present ice-sheet margin. Radiocarbon dating and lithological characteristics reveal that the core comprises a complete marine record since 4500 yr. A significant ice-sheet expansion beyond present ice margins therefore did not occur during this period.

Supplement to: Berg, Sonja; Wagner, Bernd; White, Duanne A; Melles, Martin (2010): No significant ice-sheet expansion beyond present ice margins during the past 4500 yr at Rauer Group, East Antarctica. Quaternary Research, 74, 23-25

Identifier
DOI https://doi.org/10.1594/PANGAEA.745308
Related Identifier https://doi.org/10.1016/j.yqres.2010.04.004
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.745308
Provenance
Creator Berg, Sonja ORCID logo; Wagner, Bernd ORCID logo; White, Duanne A ORCID logo; Melles, Martin ORCID logo
Publisher PANGAEA
Publication Year 2010
Funding Reference German Research Foundation https://doi.org/10.13039/501100001659 Crossref Funder ID 5472008 https://gepris.dfg.de/gepris/projekt/5472008 Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 2 datasets
Discipline Earth System Research
Spatial Coverage (77.926 LON, -68.833 LAT); Shcherbinina Island