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Dinoflagellate cysts abundances in IODP Site 307-U1318
This dataset has no description
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Dinoflagellate cyst concentrations from the Pliocene to earliest Quaternary o...
This dataset has no description
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Palynological counts (dinoflagellate cysts) and foraminiferal geochemistry (δ...
This dataset has no description
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(Table S2) Palynomorph counts of DSDP Hole 94-610A
DEPTH, sediment/rock [m] is given in mbsf. Samples were counted until more than 200, and often more than 300, dinoflagellate cysts had been enumerated. A <1 in the data set... -
(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 4) Stratigraphic distribution of dinocyst taxa in ODP Hole 150-904A
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. -
Relative abundances of dinoflagellate cysts in several IODP and DSDP holes
This dataset has no description
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Raw counts of dinoflagellate cysts in several IODP and DSDP holes
This dataset has no description
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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,... -
Palynological analyses of the sediments around the Miocene/Pliocene boundary ...
The late Neogene evolution of the Arctic to Subarctic region is poorly understood due to few available records and poor age control. At the margin of the Arctic Ocean, Yermak... -
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...
