Radionuclides and sedimentation rates of sediment cores from the eastern South Atlantic, supplement to: Frank, Martin; Gersonde, Rainer; Rutgers van der Loeff, Michiel M; Kuhn, Gerhard; Mangini, Augusto (1996): Late Quaternary sediment dating and quantification of lateral sediment redistribution applying 230Th-excess, a study of the eastern Atlantic sector of the Southern Ocean. Geologische Rundschau, 85(3), 554-566

High-resolution records of the natural radionuclide 230Th were measured in sediments from the eastern Atlantic sector of the Antarctic circumpolar current to obtain a detailed reconstruction of the sedimentation history of this key area for global climate change during the late Quaternary. High-reso...

Full description

Bibliographic Details
Main Authors: Frank, Martin, Gersonde, Rainer, Rutgers van der Loeff, Michiel M, Kuhn, Gerhard, Mangini, Augusto
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1996
Subjects:
Gravity corer Kiel type
Giant box corer
MultiCorer
ANT-VIII/3
ANT-IX/4
Polarstern
Marine Geochemistry @ AWI AWI_MarGeoChem
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Antarctic
Augusto
Southern Ocean
The Antarctic
Antarc*
Online Access:https://dx.doi.org/10.1594/pangaea.711823
https://doi.pangaea.de/10.1594/PANGAEA.711823
Description
Summary:High-resolution records of the natural radionuclide 230Th were measured in sediments from the eastern Atlantic sector of the Antarctic circumpolar current to obtain a detailed reconstruction of the sedimentation history of this key area for global climate change during the late Quaternary. High-resolution dating rests on the assumption that the 230Thex flux to the sediments is constant. Short periods of drastically increased sediment accumulation rates (up to a factor of 8) were determined in the sediments of the Antarctic zone during the climate optima at the beginning of the Holocene and the isotope stage 5e. By comparing expected and measured accumulation rate of 230Thex, lateral sediment redistribution was quantified and vertical particle rain rates originating from the surface water above were calculated. We show that lateral contributions locally were up to 6.5 times higher than the vertical particle rain rates. At other locations only 15% of the expected vertical particle rain rate were deposited.

Similar Items