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(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... -
Nannofossil abundance of Hole 17-171
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 17-167
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Late Cretaceous calcareous nannofossils distribution of IODP Site 369-U1513
1 = present, 0 = absent -
(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 -
(Table T6) Calcareous nannofossil stratigraphy of ODP Hole 198-1210A
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(Table T2) Calcareous nannofossil stratigraphy of ODP Hole 198-1207B
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant (>10 specimens per field of view [FOV]); C = common (1 -10 specimens per FOV); F = few (1... -
(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...
