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Palynological processing of 19 samples from Site 364 yielded 11 good assemblages. The frequent spores and pollen provide better biostratigraphic data than the useful, but rare, dinoflagellates. Cores 42-46 are considered early Albian, Cores 38-40 middle Albian, Cores 29-32 late Albian, Core 27 Vraconian or Cenomanian, and Cores 23-25 late Turonian to Coniacian, with many reworked Cenomanian-Turonian elements. The site was located a considerable distance from shore during the Cretaceous, or lacked large runoff from major river systems, as most spores and pollen are windborne. The climate may have been tropical but semi-arid; the vegetation was certainly very different from that at Site 361. Although restricted, marine influence in the form of dinoflagellates existed from the south.

Albian to Senonian Palynology of Site 364, Angola Basin