-
Planktic foraminiferal biostratigraphy of ODP Hole 171-1052E (Table S3)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1050C (TAble S2)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1049C (Table S1)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
(Table S3) Relative abundance of planktic foraminifera species in the >150 mi...
DEPTH, sediment/rock [m] gives the depth below the Cretaceous-Paleogene boundary. -
(Table S1) Relative abundance of planktic foraminifera species in the >150 mi...
DEPTH, sediment/rock [m] gives the depth below the Cretaceous-Paleogene boundary. <1 = present. -
(Figure 11) 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. -
(Figure 9) Distribution of Maaestrichtian planktonic foraminifera 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 3) Distribution of planktonic foraminifers in the Upper Cretaceous of...
Species abundance: C = common, F = few, R = rare,VR = very rare, - = not observed. -
(Table 1) Distribution of planktonic foraminifera shells of different species...
This dataset has no description
-
(Figure 2) Distribution chart of creatceous planktonic foraminifera of ODP Ho...
species abundance: A = abundant, C = common, F = few, R = rare, P = present, - = absent -
(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...
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... -
(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... -
(Table Ia) Planktic foraminifera abundances in the latest Cretaceous sample i...
This dataset has no description
-
(Appendix B) Relative abundances of larger size planktonic foraminifera in la...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron -
(Appendix A) Relative abundances of smaller size planktonic foraminifera in l...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron -
(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...
