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,...

(Table T1) Dinoflagellate cyst abundance in ODP Hole 171B-1053A sediments

Site 1053 is located at the top of an escarpment cut into the upper part of Blake Nose (29°59.5385'N, 76°31.4135'W). The total core recovery was 189.5 m of upper middle to upper...

Dinocyst occurrences and zonations from IODP Hole 313-M0029A

Sediment depth is given in mbsf. Ph = phytoclasts, flin = foraminifer lining, AOM = amorphous organic matter.

Dinocyst occurrences and zonations from IODP Hole 313-M0028A

Sediment depth is given in mbsf. AOM = amorphous organic matter, flin = phytoclasts.

Dinocyst occurrences and zonations from IODP Hole 313-M0027A

Sediment depth is given in mbsf.DN = zones from de Verteuil and Norris (1996), NSO = zone from Van Simaeys et al. (2005), Ph = phytoclasts, AOM = amorphous organic matter, flin...

Dinoflagellate abundance of Hole 81-555

Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)

(Fig. 3) Raw counts and stratigraphic ranges of selected dinoflagellate cyst ...

Sediment depth is given in mbsf. Cells with "" (replaced by "<1") indicates species only encountered outside regular counts, () replaced by "#1", (n) replaced by #n indicates...