-
Late Miocene and Pliocene dinoflagellate cysts, acritarchs and terrestrial pa...
The globally warm climate of the early Pliocene gradually cooled from 4 million years ago, synchronous with decreasing atmospheric CO2 concentrations. In contrast,... -
Stratigraphic occurrence of selected marine palynomorph species recorder in t...
Dinoflagellate cysts were recovered throughout the Paleogene succession of Hole 647A, which contains an almost complete deep-water record of early Eocene through early late... -
Dinoflagellate abundance of Hole 94-611C
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Dinoflagellate abundance of Hole 94-607A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Dinoflagellate abundance of Hole 94-607
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Palynological counts (dinoflagellate cysts) and foraminiferal geochemistry (δ...
This dataset has no description
-
(Figure 3) Range chart of dinocysts of ODP Hole 104-643A
Species abundance: A = abundant (>25%), C = common (2-25%), R = rare (<2%), - = not present
