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Stratigraphic occurrence of selected marine palynomorph species recorder in t...
Dinoflagellate cysts were recovered throughout the Paleogene succession of Hole 647A, which contains an almost complete deep-water record of early Eocene through early late... -
Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 14...
This dataset has no description
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Range table from dinoflagellates, acritarchs and prasinophytes in ODP Hole 14...
This dataset has no description
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Neogene palynomorpha from site 93-603, part 2
This dataset has no description
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Neogene palynomorpha from site 81-552
This dataset has no description
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Dinoflagellate abundance of Hole 38-338
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Dinoflagellate abundance of Hole 81-552
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table T3) Abundance of dinoflagellates and other palynomorphs in Maastrichti...
Sediment depth is given in median mbsf. -
(Appendix B) Dinoflagellate cysts occurrence in DSDP Hole 38-338
This dataset has no description
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Distribution of dinoflagellate cysts in Eocene-Oligocene sediments of ODP Hol...
Species abundance: A = abundant, P = present, - = absent. -
(Table 3) Dinocyst ranges in ODP Hole 104-642D
X = present, - = not present -
(Figure 1) Dinoflagellate cyst stratigraphy of DSDP Hole 80-548A
Cyst assemblages from Sites 548, 549, and 550 were examined and gave evidence of early Eocene to late Miocene age. These assemblages were compared with other North Atlantic... -
(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... -
Dinoflagellates and pollen of the Brito-Arctic Igneous Province flora, ODP Ho...
Palynological studies of the intrabasaltic sediment layers in the lower volcanic series from ODP Leg 104 outer Voring Plateau Hole 642E Cores 102 through 109 indicated abundant... -
Results of palynological analysis of Hole 302-M0004A
Abundance: A = abundant, P = poor, B = barren. Preservation: M = moderate. Depth = provisional. Numerical values are abundance in counts. -
Results of palynological analysis of Hole 302-M0002A
Abundance: A = abundant, C = common, F = few, R = rare, B = barren. Preservation: M = moderate. Numerical values are abundance in counts.
