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(Table 4) Planktic foraminiferal abundance in Oligocene to Early Miocene sedi...
Species abundance: S = scattered (1-3 specimens), R = rare (<10 %), F = few (3-15 %), C = common (15-30 %), A = abundant (30-50 %), D = dominant (>50 %), - = not present,... -
Planktonic foraminifera counts and their oxygen and carbon isotopes at the IO...
This dataset contains data from Integrated Ocean Drilling Program Site U1334, which is correlated in the depth domain to Site 1218 before ages were assigned. The dataset... -
Planktic foraminifera abundance of Hole 40-363
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 40-362A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 40-362
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 40-360
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table T1) Planktonic foraminiferal stratigraphy of ODP Hole 173-1065A sediments
Sediment depth is given in mbsf. Abundance estimate as follows: A = abundant, C = common, F = few, R = rare, B = barren, - = not found; rw = reworked. -
(Figure 5) Planktonic foraminifera distribution in ODP Hole 101-628A
Species abundance: F/C = few to common, R = rare, r = reworked, ? = questioably presente, - = not present. -
(Table 14) Distribution of planktonic foraminifera in the late Oligocene sect...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 13) Distribution of planktonic foraminifera in the latest Oligocene to...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 12) Distribution of planktonic foraminifera in the early Miocene secti...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 9) Distribution of planktonic foraminifera in the early Pliocene to Ho...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 8) Distribution of planktonic foraminifera in the late Cretaceous and ...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 6) Distribution of planktonic foraminifera in the late Oligocene to mi...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Table 2) Distribution of planktonic foraminifera in the latest Oligocene to ...
Species abundance: R = rare, F = few, C = common, A = abundant, ? = questionable, RW = reworked, - = not present. -
(Figure 6) Stratigraphic ranges of selected planktonic foraminifers at ODP Ho...
Species abundance: T = trace (one specimen), R = rare (<3%), F = few (3-15%), C = common (16-30%), A = abundant (>30%), P = present, samples with too few planktonic... -
(Figure 5) Stratigraphic ranges of selected planktonic foraminifers at ODP Ho...
Species abundance: T = trace (one specimen), R = rare (<3%), F = few (3-15%), C = common (16-30%), A = abundant (>30%), P = present, samples with too few planktonic... -
(Figure 4) Stratigraphic ranges of selected planktonic foraminifers at ODP Ho...
Species abundance: T = trace (one specimen), R = rare (<3%), F = few (3-15%), C = common (16-30%), A = abundant (>30%), P = present, samples with too few planktonic... -
(Table 2) Planktonic foraminifer species distribution, abundance, and preserv...
Species abundance: A = abundant; C = common; F = few; R = rare; + = present, but not subjectively quantified; - = absent, but looked for; blank = absent; ? = questionable... -
(Appendix) Stable carbon and oxygen isotopes, and Mg/Ca ratios of foraminifer...
To better understand the links between the carbon cycle and changes in past climate over tectonic timescales we need new geochemical proxy records of secular change in silicate...
