-
(Table 5) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-905A
X = present, - = absent, R = reworked, ? = questionable occurrence. -
(Table 3) Dinocyst ranges in ODP Hole 104-642D
X = present, - = not present -
(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 -
(Figure 10) Range chart of selected dinocysts and acritarchs of ODP Hole 104-...
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present -
(Figure 9) Range chart of selected dinocysts and acritarchs of ODP Hole 104-6...
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present -
(Figure 8) Range chart of selected dinocysts and acritarchs of ODP Hole 104-6...
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present -
(Figure 7) Range chart of selected dinocysts and acritarchs of ODP Hole 104-643A
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present -
(Figure 6) Range chart of selected dinocysts and acritarchs of ODP Hole 104-642C
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present -
(Figure 5) Range chart of selected dinocysts and acritarchs of ODP Hole 104-642A
Species abundance: A = abundant (>49%), C = common (10-49%), R = rare to frequent (1-9%), - = not present -
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,...
