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(Table T5) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table T4) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table T3) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table T2) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table T1) Occurrence of Lower Cretaceous planktonic foraminifera in ODP Hole...
Sediment depth is given in mbsf. Abundance estimates as follows: - = not found, R = rare, F = few, C = common, A = abundant. -
(Table 6) Relative abundance of pollen grains and spores at ODP Hole 103-641A
This dataset has no description
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(Appendix A) Trace metal content of sediments around the CTBE at ODP Hole 103...
This dataset has no description
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(Table 2) Compilation of biostratigraphy and organic geochemistry studies at ...
This dataset has no description
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(Table 1) Description of CTBE samples from ODP Hole 103-641A and DSDP Hole 43...
Clay minerals are numbered according to their relative abundance in the clay fraction; higher numbers indicate decreasing amounts; smectite, the dominant clay mineral in all... -
(Table 4) Stratigraphic distribution of spores and pollen grains in the trans...
X = present, - = absent -
(Table 3) Distribution of dinoflagellate cysts in ODP Hole 103-641A
X = present, - = absent -
(Figure 5) Distribution of Upper Cretaceous agglutinated benthic foraminifers...
Species abundance: r = very rare, R = rare (1-3 specimens), F = few (+/-5), C = common (>10), A = abundant (>50) -
(Figure 3) Distribution of Upper Cretaceous agglutinated benthic foraminifers...
Species abundance: r = very rare, R = rare (1-3 specimens), F = few (+/-5), C = common (>10), A = abundant (>50) -
Texture description and distribution of components in ODP Hole 103-639D (Figu...
A detailed analysis of the texture, matrix, and elements of the microfacies from the carbonate sequence recovered in ODP Hole 639D resulted in a typological classification of 10... -
Distribution of Upper Cretaceous deep water agglutinated foraminifera in sedi...
The stratigraphic and biogeographic distribution of more than 170 species of deep-water agglutinated benthic foraminifers (DWAF) from the North Atlantic and adjacent marginal... -
The Cenomanian/Turronian Boundary Event at ODP Hole 103-641A
Drilling at ODP Site 641 (on the western margin of Galicia Bank, off northwestern Spain) revealed a thin, but pronounced, interval of black shale and gray-green claystone. Our... -
Agglutinated benthic foraminifera of the Upper Cretaceous
A reexamination of the agglutinated benthic foraminiferal microfaunas found in the Upper Cretaceous red and brown clays of DSDP Hole 603B and ODP Holes 640A and 641A allows us... -
Lower Cretaceous planktonic foraminifer stratigraphy of sediments from ODP Le...
During Ocean Drilling Program Leg 171B, an Aptian to Turonian sedimentary succession yielding exceptionally well-preserved planktonic foraminiferal faunas was recovered at Sites... -
Occurrence of some well known benthonic foraminiferal species in samples from...
The basal beds on the Shatsky Rise cored during Leg 6 of the Deep Sea Drilling Project are the oldest sediments recovered to date in the Pacific Ocean. Based on benthonic... -
(Figure 4) Stratigraphic distribution of planktonic foraminifera in DSDP Hole...
During Deep Sea Drilling Project Leg 93, upper Miocene through Quaternary sediments were continuously cored in Hole 604, located on the upper continental rise of the New Jersey...
