-
(Table 6) Distribution of Miocene-Pleistocene calcareous nannofossils in ODP ...
Species abundances: V = very abundant (>10 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 2-10 fields of view), F =... -
(Table 4) Distribution of Miocene-Pleistocene calcareous nannofossils in ODP ...
Species abundances: V = very abundant (>10 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 2-10 fields of view), F =... -
(Table 1) Distribution of Oligocene-Pleistocene calcareous nannofossils in OD...
Species abundances: V = very abundant (>10 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 2-10 fields of view), F =... -
(Table 2) Distribution of benthic foraminifera in ODP Hole 120-748A
1 indicate presence and >10 indicates dominance in samples where specimen numbers were too small for statistically significant percentages to be calculated -
(Table 1) Distribution of benthic foraminifera in ODP Site 120-747
X = present, - = absent -
(Table 3) Distribution of middle Eoecen-lowest Miocene calcareous nannofossil...
V = very abundand, A = abundant, C = common, F = few, R = rare, r = rare reworked specimens, F = few reworked specimens, - = absent. The high-latitude zonation of Wei and Wise... -
(Table 2) Relative abundances of calcareous nannofossils in ODP Hole 120-748A
This dataset has no description
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Census of calcareous nannofossil taxa expressed as percent of total number of...
This dataset has no description
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Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
Abundances of siliceous sponge spicules in ODP Site 120-748 (Table 1)
Siliceous sponge spicules are present and often diverse in sediments drilled by Ocean Drilling Program Leg 120. The sponge spicule assemblages are tabulated for Holes 748A and... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
(Appendix A) Stable carbon and oxygen isotope ratios of foraminifera of ODP H...
Sediment depth is given in rescaled mbsf. -
(Table 2) Stable carbon and oxygen isotope record of planktonic foraminifera ...
Sediment depth is given in mbsf. No adjustments have been applied and no outliers are excluded. -
(Table 2) Stable carbon and oxygen isotope record of benthic foraminifera fro...
Sediment depth is given in mbsf. No adjustments have been applied and no outliers are excluded. -
(Table 2) Neogene benthic foraminifers of ODP Hole 120-748B
This dataset has no description
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(Table 1) Benthic foraminifer and ostracode stable carbon and oxygen isotope ...
Size fraction >150 µm. -
(Table 14) Miocene diatom biostratigraphy of ODP Hole 120-751A
R = rare ( one specimen of a particular species encountered in 5-20 fields of view using a 40X objective and 10X ocular), F = frequent (one specimen in every 5 fields), C =... -
(Appendix C) Stratigraphic range and relative abundance of Neogene planktonic...
Species abundance: A = abundant (>25%), C = common (16-24%), F = frequent (6-15%), R = rare (1-5%), - = absent, based on a random sample of 200-400 specimens from the >63... -
(Appendix B) Stratigraphic range and relative abundance of Neogene planktonic...
Species abundance: A = abundant (>25%), C = common (16-24%), F = frequent (6-15%), R = rare (1-5%), - = absent, based on a random sample of 200-400 specimens from the >63... -
(Appendix A) Stratigraphic range and relative abundance of Neogene planktonic...
Species abundance: A = abundant (>25%), C = common (16-24%), F = frequent (6-15%), R = rare (1-5%), - = absent, based on a random sample of 200-400 specimens from the >63...
