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Dinoflagellate cysts abundances in IODP Site 307-U1318
This dataset has no description
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(Appendix B) Dinoflagellate cysts in ODP Site 170-1039 sediments
This dataset has no description
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(Appendix A) Raw counts and stratigraphic range of dinoflagellate cysts and a...
<1 = species recorded outside regular counts. -
(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... -
(Table T1) Abundance of dinoflagellates and other palynomorphs in ODP Hole 18...
Sediment depth is given in mbsf. Age model adopted from Stickley et al. (2004, doi:10.2973/odp.proc.sr.189.111.2004). -
(Table 5) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-905A
X = present, - = absent, R = reworked, ? = questionable occurrence. -
(Table 6) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-906A
X = present, - = absent. -
(Table 3) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-903C
X = present, - = absent. -
(Table 2) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-903A
X = present, - = absent. -
(Table 1) Stratigraphic distribution of dinocyst taxa in ODP Site 150-902
X = present, - = absent. -
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,... -
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...
