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(Table 4) Stratigraphic distribution of calcareous nannofossil taxa from ODP ...
Species abundance: P = present (1 specimen per 201-500 fields of view), R = rare (1 specimen per 51-200 fields), F = few (1 specimen per 11-50 fields), C = common (1 specimen... -
(Table 3) Stratigraphic distribution of calcareous nannofossil taxa from ODP ...
Species abundance: P = present (1 specimen per 201-500 fields of view), R = rare (1 specimen per 51-200 fields), F = few (1 specimen per 11-50 fields), C = common (1 specimen... -
(Table 2) Stratigraphic distribution of calcareous nannofossil taxa from ODP ...
Species abundance: P = present (1 specimen per 201-500 fields of view), R = rare (1 specimen per 51-200 fields), F = few (1 specimen per 11-50 fields), C = common (1 specimen... -
(Appendix A) Campanian-Maastrichtian calcareous nannofossils in DSDP Hole 44-...
The latest Cretaceous (Campanian–Maastrichtian) is characterized by several global cooling and intermittent warming events. These climatic changes influenced the... -
(Figure 10) Occurrence of coccoliths in two carbonate cycles at DSDP Hole 71-511
P = present, - = not present. -
(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...