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(Table A1) Calcareous nannofossil of the Middle Cenomanian Event in ODP Site ...
Sediment depth is given in mcd. <1 = present outside count of 300 specimens. -
(Appendix A2) Calcareous nannofossil counts of ODP Site 207-1260
Sediment depth is given in mcd. Counts of 300 specimens on each slide, magnification of x1250. Two additional traverses, beyond the 300 count, were scanned for rare species.... -
(Appendix A1) Calcareous nannofossil counts of ODP Site 207-1258
Sediment depth is given in mcd. Counts of 300 specimens on each slide, magnification of x1250. Two additional traverses, beyond the 300 count, were scanned for rare species.... -
(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... -
Biostratigraphic distribution of calcareous nannofossils from ODP Hole 171-10...
Species Abundance: A, 1 specimen per field of view (FOV); C, 1 specimen per 10 FOV; F, 1 specimen per 50 FOV; R, 1 specimen per >50 FOV; rw = reworked specimen; ? =... -
Biostratigraphic distribution of calcareous nannofossils from ODP Hole 171-10...
Species Abundance: A, 1 specimen per field of view (FOV); C, 1 specimen per 10 FOV; F, 1 specimen per 50 FOV; R, 1 specimen per >50 FOV; rw = reworked specimen; ? =... -
Biostratigraphic distribution of calcareous nannofossils from ODP Hole 171-10...
Species Abundance: A, 1 specimen per field of view (FOV); C, 1 specimen per 10 FOV; F, 1 specimen per 50 FOV; R, 1 specimen per >50 FOV; rw = reworked specimen; ? =... -
Biostratigraphic distribution of calcareous nannofossils from ODP Hole 171-10...
This dataset has no description
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(Table S1) Calcareous nannofossil raw counting data of Kronsmoor Section 2
1 = species observered -
(Table S1) Calcareous nannofossil raw counting data of Kronsmoor Section 1
1 = species observered -
(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...
