-
(Table 1) Isotopes δ¹⁸O and δ¹³C in Globigerina angiporoides and Oridorsalis ...
This dataset has no description
-
(Table 5) Oligocene planktonic foraminifera of DSDP Hole 29-277
Species abundance: A = abundant, C = common, F = few, R = rare, - = not observed. -
(Table 4) Paleocene to Eocene planktonic foraminifera of DSDP Hole 29-277
Species abundance: A = abundant, C = common, F = few, R = rare, - = not observed. -
Late Miocene-Early Pliocene oxygen and carbon isotopic measurements from DSDP...
This dataset has no description
-
(Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP...
This dataset has no description
-
(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
This dataset has no description
-
Noelaerhabdaceae coccolith length (mean, 5th percentile and 95th percentile) ...
This dataset contains the data plotted in Figure 5 of the review paper Coccoliths as Recorders of Paleoceanography and Paleoclimate over the Past 66 Million Years by Bolton... -
Occurrence of Globorotalia cavernula in the water column and sediments: globa...
Here, we present a global compilation of previously reported sightings of the rare planktic foraminifer Globorotalia cavernula Bé, 1967 as well as new observations of... -
(Data Set S1) Compiled benthic foraminiferal stable isotopic values
d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent. -
(Table 1) Stable oxygen isotope ratios of benthic foraminifera from Pacific O...
The thermal structure of the Pacific Ocean between water depths of about 1 and 4.5 kilometers is estimated from the oxygen isotopic ratio of benthonic foraminifera from... -
(Table 2) Stable carbon and oxygen isotope ratios of foraminifera of DSDP Hol...
Oxygen isotopic studies both of benthic formanifera (Emiliani, 1954, doi:10.1126/science.119.3103.853; Savin et al., 1975, doi:10.1130/0016-7606(1975)86<1499:TMP>2.0.CO;2;... -
Magnetic properties of the oceanic igneous rocks (Table 1)
Hysteresis measurements have been carried out on a suite of ocean-floor basalts with ages ranging from Quaternary to Cretaceous. Approximately linear, yet separate,... -
Stable isotope ratios of benthic foraminifera stable from Miocene Pacific sed...
Seven Miocene Pacific Ocean Deep Sea Drilling Project sites from four different water masses (planktonic foraminiferal biogeographic regions) have been correlated using 18... -
Bryozoan abundance of Hole 29-282
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Silicoflagellate abundance of Hole 29-278A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 29-281
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 29-280A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 29-278
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 29-275
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Microfossil abundance of Hole 29-283
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)
