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(Appendix A) Nannofossil stratigraphic range chart for the late Maastrichtian...
The response of calcareous nannofossils to the end-Cretaceous warming is investigated in the Tropical Pacific DSDP Site 577A (Shatsky Rise) through the record of 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... -
(Table T11) Calcareous nannofossil stratigraphy of ODP Hole 198-1212B
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 T10) Calcareous nannofossil stratigraphy of ODP Hole 198-1212A
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 T9) Calcareous nannofossil stratigraphy of ODP Hole 198-1211C
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 T8) Calcareous nannofossil stratigraphy of ODP Hole 198-1211A
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 T7) Calcareous nannofossil stratigraphy of ODP Hole 198-1210B
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 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 T5) Calcareous nannofossil stratigraphy of ODP Hole 198-1209C
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 T4) Calcareous nannofossil stratigraphy of ODP Hole 198-1209A
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 T3) Calcareous nannofossil stratigraphy of ODP Hole 198-1208A
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... -
(Table T1) Calcareous nannofossil stratigraphy of ODP Hole 198-1207A
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 3) Late Maastrichtian calcareous nannofossils in ODP Hole 198-1212B
<1 denotes species encountered in traverses after the statistical count. -
(Table 1) Late Maastrichtian calcareous nannofossils in DSDP Hole 22-212
<1 denotes species encountered in traverses after the statistical count. -
(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...
