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(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 12) Distribution of planktonic foraminifera shells with different pres...
This dataset has no description
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(Table 2) Distribution of planktonic foraminifera shells of different species...
This dataset has no description
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(Table 1) Distribution of planktonic foraminifera shells of different species...
This dataset has no description
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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... -
Species counts of planktic foraminifera (<106µm) from ODP Site 208-1262
Core samples were washed over a 38µm sieve and dried in an oven at 40°C. Planktic foraminifera species and genera abundance counts were made on 49 samples. -
(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. -
(Table T2) Planktonic foraminifera stratigraphy of ODP Hole 198-1211C sediments
Sediment depth is given in mbsf. Abundance estimates as follows: AA = very abundant (>50%), A = abundant (30%-50%), C = common (10%-30%), F = few (5%-10%), R = rare (1%-5%),... -
(Table T1) Planktonic foraminifera stratigraphy of ODP Hole 198-1209C sediments
Sediment depth is given in mbsf. Abundance estimates as follows: AA = very abundant (>50%), A = abundant (30%-50%), C = common (10%-30%), F = few (5%-10%), R = rare (1%-5%),... -
(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 =... -
(Table 2) Occurrence of Late Cretaceous foraminifers and radiolarians in ODP ...
Species abundance: X = present, cf = confer, - = absent. -
(Figure 3) Distribution chart of creatceous planktonic foraminifera of ODP Ho...
species abundance: A = abundant, C = common, F = few, R = rare, P = present, - = absent, ? = questionable -
(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
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(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...
