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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; ? =... -
Width analysis of 50 specimen from Eiffellithus coccolith from ODP Core 207-1...
The evolution of the calcareous nannofossil E. turriseiffelii - E. eximius lineage in the Turonian from the western tropical Atlantic and Indian Ocean indicates identical... -
Length analysis of 50 specimen from Eiffellithus coccolith from ODP Core 207-...
The evolution of the calcareous nannofossil E. turriseiffelii - E. eximius lineage in the Turonian from the western tropical Atlantic and Indian Ocean indicates identical... -
Cross bar angle analysis of 50 specimen from Eiffellithus coccolith from ODP ...
The evolution of the calcareous nannofossil E. turriseiffelii - E. eximius lineage in the Turonian from the western tropical Atlantic and Indian Ocean indicates identical... -
Bar length analysis of 50 specimen from Eiffellithus coccolith from ODP Core ...
The evolution of the calcareous nannofossil E. turriseiffelii - E. eximius lineage in the Turonian from the western tropical Atlantic and Indian Ocean indicates identical... -
(Table 4) Distribution of Albian-Cenomanian nannofossils in DSDP Hole 77-540
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 2) Distribution of Aptian-Albian nannofossils in DSDP Holes 77-538A an...
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 =... -
(Figure 3) Distribution of Maastrichtian calcareous nannofossils in ODP Hole ...
Sediment depth is given in mbsf. Species abundance: A = abundant (more than 1 specimen per field of view; 1250 X); C = common (at least 1 specimen in 10 fields of view); F =... -
(Figure 1) Calcareous nannofossil abundances in ODP Hole 150-905A
Species abundance: - = not present; r = very rare, R = rare, F = few, C = common, A = abundant, W = very abundant, and ( ) = redeposited. Nannofossil abundance is the number of... -
Range table from nannofossils in ODP Hole 150-905A
This dataset has no description
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Range table from nannofossils in ODP Hole 144-878A
This dataset has no description
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Late Albian Col de Palluel (SE France, Niveau Breistroffer): range chart in p...
values with <1 = rare occurence, not counted -
Lower Albian LArboudeysse (Niveau Paquier) range chart in percentages of nann...
Method see Geisen et al, 1999, Micropaleontology. Volume: 1000 ml, high: 5 cm, field of view: 0.000227 cm**2 -
Lower Albian Mazagan Plateau (Oceanic Anoxic station 1b) range chart, DSDP Si...
Volume: 1000 ml, high: 5 cm, field of view: 0.000227 cm**2 -
Upper Aptian Pré-Guittard (Niveau Kilian) range chart in percentages of nanno...
Method see Geisen et al, 1999, Micropaleontology. Volume: 1000 ml, high: 5 cm, field of view: 0.000227 cm**2 -
Lower Albian, Niveau Paquier range chart of nannofossils in SE France
C=common (>1 specimen/field view); F=frequent (1 specimen/2-10 fields of view); R=rare (1 speciemen/>11 fields of view) -
Upper Aptian Niveau Kilian range chart of nannofossils in SE France
C=common (>1 specimen/field view); F=frequent (1 specimen/2-10 fields of view); R=rare (1 speciemen/>11 fields of view) -
(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...
