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(Table T5) Cretaceous calcareous nannofossil abundance of ODP Hole 173-1069A
Sediment depth is given in mbsf. Abundance estimates as follows: Abundance: A = abundant, C = common, F = few, R = rare, 1 = single, B = barren, - = not found. -
(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... -
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 3) Distribution of late Cretaceous nannofossils in DSDP Hole 77-538A
Species abundances: V = very abundant (> 10 specimens per field of view at 1560 X), A = abundant (1 to 10 specimens per field), C, common (1 specimen per 2-10 fields), F =... -
(Table 4) Distribution of Cretaceous calcareous nannofossils in ODP Hole 114-...
Species abundances: VA = very abundant (>5 specimens/field of view), A = abundant (>1 specimen/field), C = common (>1 specimen/8 fields), F = few (>1 specimen/10... -
(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... -
Distribution of calcareous nannofossils in Cretaceous to Paleogene sediments ...
Site 1262 in the South Atlantic Ocean has provided a stratigraphically continuous deep Cretaceous/Paleogene boundary sequence. High resolution calcareous nannofossil...