Abstract
The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could be established (Zone 2, below 380 m: high Pinus, Quercus, and Carya values; Zone 1, above 380 m; high Pinus, and Sphagnum values). The marine pollen record was found to reflect the history of the vegetation of the eastern United States, the flora from Zone 2 indicating a warmer climate than that from Zone 1, which depicts a climatic cooling trend. The onset of Western Boundary Undercurrent deposition had no noticeable effect on the pollen distribution in the marine sediment. -Author
Cite
CITATION STYLE
Van Der Kaars, W. A. (1987). Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic. Initial Reports DSDP, Leg 93, Norfolk, Virginia to Norfolk, Virginia Part 2, 783–788. https://doi.org/10.2973/dsdp.proc.93.124.1987
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