Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6441492 | Marine Geology | 2015 | 12 Pages |
Abstract
The near absence of reworked pollen grains in core JPC32 contrasts with the high quantity of reworked material in nearby but deeper located marine sites, suggesting that the JPC32 record was not affected by the Deep Western Boundary Current (DWBC) since the end of the Younger Dryas and should be considered a key site for studying past climate changes in the western North Atlantic.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
F. Naughton, L. Keigwin, D. Peteet, S. Costas, S. Desprat, D. Oliveira, A. de Vernal, A. Voelker, F. Abrantes,