Radiocarbon sediment ages and sedimentation rates in the Red Sea

DOI

Results of radiocarbon dating of 23 cores (81 determinations) collected in the Red Sea rift zone at 8°N are presented. All of the main tectonic structures were dated: the upper and lower tectonic benches, the salt scarp, and the axial zone. Sediments in the upper tectonic bench exhibit normal sedimentation, while all other structures, which have highly dissected relief, show extensive re-deposition or non-accumulation of sediments. Sedimentation rate in Holocene was from two to three times lower than in Late Würm.

Supplement to: Kuptsov, Vladimir M; Palkina, Alla M (1986): Radiocarbon dating of bottom sediments of the Red Sea. Oceanology, 26(3), 341-345

Identifier
DOI https://doi.org/10.1594/PANGAEA.756434
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.756434
Provenance
Creator Kuptsov, Vladimir M; Palkina, Alla M
Publisher PANGAEA
Publication Year 1986
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 (39.500W, 17.500S, 40.282E, 18.197N); Red Sea