Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
10121297 | Physics of the Earth and Planetary Interiors | 2005 | 20 Pages |
Abstract
The reconstructed average sediment accumulation rates for the individual cores range from 0.6 to 19Â cm/ka and are compatible with their position within the WLB, with the lowest rates found close to the ridge of the sedimentary drifts. Moreover, the high-resolution age models obtained in this study provide original constraints to assess chronology, rates and amplitudes of the climatic and environmental processes affecting this key area of the peri-Antarctic margins during the Late Pleistocene.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geophysics
Authors
Patrizia Macrì, Leonardo Sagnotti, Jaume Dinarès-Turell, Andrea Caburlotto,