-
(Table A1) Stable isotope ratios and paleotemperature calculation of selected...
Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world... -
(Figure 7) Distribution of Cretaceous planktonic foraminifers and associated ...
Species abundance: A = abundant, AF = frequent, C = common, F = few, R = rare, small case letters = reworked, cf. = confirm, ? = presence is questionable, - = absent. -
Distribution of foraminiferal fauna from ODP Hole 122-762C (Table 1)
Planktonic foraminiferal diversity, equitability and biostratigraphic analysis of samples from Ocean Drilling Program (ODP) Leg 122, Hole 762C show that in general, cool water... -
Range table from planktonic foraminifers in ODP Hole 192-1186A
This dataset has no description
-
Range table from planktonic foraminifers in ODP Hole 192-1183A
This dataset has no description
-
Range table from planktonic foraminifers in ODP Hole 171-1052E
This dataset has no description
-
Planktic foraminifera abundance of Hole 84-567A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Range table from planktonic foraminifers in ODP Hole 144-876A
This dataset has no description
-
(Table 1) Distribution of planktonic foraminifera in the Paleocene/Cretaceous...
Analysis of planktonic foraminifers from Section 605-66-1 established the Cretaceous/Tertiary (K/T) boundary between 68 and 73 cm. Comparison with the detailed zonation... -
Planktic foraminifera abundance of Hole 2-10
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 14-135
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 2) Planktic foraminiferal species and number of specimens present in 5...
Preservation is poor with strong dissolution in predominantly volcanic sediments. -
(Table 1b) Relative percent abundance of planktic foraminiferal species at DS...
This dataset has no description
-
(Table A1) Stable isotope ratios and paleotemperature calculation of selected...
Isotope data for sample 74-525A-40-2,104-106 of the following species: Abathomphalus mayaroensis, Globotruncana arca, Gublerina cuvillieri, Heterohelix globulosa, Heterohelix... -
(Appendix C) Stable isotope ratios and paleotemperature calculation of select...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron. Paleotemperature estimates were... -
(Appendix) Distribution of planktonic foraminifers at DSDP Hole 72-516F, Coni...
During Leg 72 in the western South Atlantic, Cretaceous sediments were recovered only at Hole 516F (Rio Grande Rise). Late Cretaceous planktonic foraminifers were found in Cores... -
(Table 2) Distribution of recurrent planktonic foraminifera at DSDP Hole 75-530A
Planktonic occurrences above Core 75 are too infrequent to justify plotting. A - abundant, C - common, R - rare, F - few, ? - questionable occurrence. -
(Figure 3) Distribution of planktonic foraminifers in the Upper Cretaceous of...
Species abundance: C = common, F = few, R = rare,VR = very rare, - = not observed.
