Dataset - B2FIND

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,...

Stable isotope ratios on bolboforma from Hole 104-642C

Specimens picked by Dorothee Spiegler. Isotope data measured by Kyaw Winn in 1986-1988 with the CARBO KIEL Massenspectrometer Finnigan MAT 251, Christian-Albrechts-University,...

(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

(Table 5) Pleistocene ostracodes from ODP Hole 104-644A

X = present, - = absent

(Table 4) Pleistocene to Miocene ostracodes from ODP Hole 104-643A

X = present, - = absent

(Table 3) Pliocene/Pleistocene ostracodes from ODP Hole 104-642C

X = present, - = absent

(Table 2) Pleistocene to Miocene ostracodes from ODP Hole 104-642B

X = present, - = absent

(Table 2) Distribution of ice-rafted fossils in ODP Hole 104-643A

Abundance: C = common, R = rare, VR = very rare, - = not present

(Table 1) Distribution of ice-rafted fossils in ODP Hole 104-642B

Abundance: A = abundant, C = common, R = rare, VR = very rare, - = not present

(Table 3) Stratigraphic distribution of silicoflaggelates, ebridians and acti...

Sample 104-644A-1H-1,68-69 to 104-644A-10H-1,63-64, 104-644A-11H-2,67-68, 104-644A-13H-3,53-54, 104-644A-19H-3,66-67, 104-644A-22H-4,66-67, 104-644A-25H-3,48-49,...

(Table 1) Stratigraphic distribution of silicoflagellates in lower Miocene to...

Samples 104-642C-1H-1,80-81 to 104-642C-8H-3,30-31 (Quatenary to Pliocene), 104-642C-10H-2,71-72 (Lower Pliocene) and 104-642D-11x-2,55-56 barren. Species abundance: *1 = P (=...