-
(Figure 6) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Figure 4) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Figure 3) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Fig. 13) Distribution of dinoflagellate cysts in Early Cretaceous sediments ...
Species abundance: F = 1-5 %, C = 6-15 %, A = >15 %, - = not present -
Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(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... -
(Figure 2) Foraminifera in lower to middle Albian sediments of DSDP Hole 80-549
The Early Cretaceous series of Site 549 have been analyzed from both an ecological and a chronostratigraphical viewpoint. Lithology and microfaunal assemblages allow the... -
(Appendix) Late Cretaceous calcareous nannofossils of DSDP Holes 80-549 and 8...
he early late Cretaceous (Cenomanian–early Turonian) is thought to have been one of the warmest periods of the Phanerozoic. This period was characterised by tropical sea surface... -
Nannofossil abundance of Hole 80-549A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 80-548
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 80-548
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Benthic foraminifera abundance of Hole 80-548
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Benthic foraminifera abundance of Hole 80-549A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and...
Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major... -
(Figure 5) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Figure 2) Occurrence of planktonic foraminifers and other selected constitue...
Species abundance: A = abundant, C = common, F = few, R = rare, ? = questionable occurrence, - = absent. -
(Table 8) Benthic foraminifera genera assemblage at DSDP Section 80-548A-28
This dataset has no description
-
(Table 7) Benthic foraminifera genera assemblage at DSDP Section 80-548A-22
This dataset has no description
-
(Table 6) Benthic foraminifera genera assemblage at DSDP Section 80-548A-16-3
This dataset has no description
