Composition and Flux of Holocene Sediments on the Eastern Laptev Sea Shelf, Arctic Siberia

Bauch, Henning A., Kassens, Heidemarie, Naidina, Olga D., Kunz-Pirrung, Martina and Thiede, Jörn (2001) Composition and Flux of Holocene Sediments on the Eastern Laptev Sea Shelf, Arctic Siberia Quaternary Research, 55 (3). pp. 344-351. DOI 10.1006/qres.2000.2223.

[img] Text
2001_Bauch-etal-Composition_QuatRes-55.pdf - Published Version
Restricted to Registered users only

Download (212Kb) | Contact

Supplementary data:


A 467-cm-long core from the inner shelf of the eastern Laptev Sea provides a depositional history since 9400 cal yr. B.P. The history involves temporal changes in the fluvial runoff as well as postglacial sea-level rise and southward retreat of the coastline. Although the core contains marine fossils back to 8900 cal yr B.P., abundant pf ant debris in a sandy facies low in the core shows that a river influenced the study site until similar to 8100 cal yr B.P. As sea level rose and the distance to the coast increased, this riverine influence diminished gradually and the sediment type changed, by 7400 cal yr B.P., from sandy silt to clayey silt, Although total sediment input decreased in a step-like fashion from 7600 to 4000 cal yr B.P., this interval had the highest average sedimentation rates and the greatest fluxes in most sedimentary components, While this maximum probably resulted from middle Holocene climate warming, the low input of sand to the site after 7400 cal yr B.P. probably resulted from further southward retreat of the coastline and river mouth. Since about 4000 cat yr B.P., total sediment flux has remained rather constant in this part of the Laptev Sea shelf due to a gradual stabilization of the depositional regime after completion of the Holocene sea-level rise.

Document Type: Article
Additional Information: WOS:000168957000009
Keywords: Arctic Sea; Continental shelf; Sediments; Holocene; Siberia; Radiocarbon age calibration; Organic carbon; Marine samples; Lena River; Ice; Ocean; Quaternary; Nutrients; BP
Research affiliation: AWI
OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-P-OZ Paleo-Oceanography
Refereed: Yes
DOI etc.: 10.1006/qres.2000.2223
ISSN: 0033-5894
Date Deposited: 14 Jan 2015 09:10
Last Modified: 19 Sep 2016 12:15

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...