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Pliocene-Pleistocene distribution of benthic foraminifers from ODP Hole 110-6...
Site 672 is located on the Atlantic abyssal plain to the east of the Lesser Antilles forearc region. It serves as a stratigraphic reference section for sediments entering the... -
Benthic foraminifera abundance of Hole 42-372
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Benthic foraminifera abundance of Hole 76-533
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Appendix Table 4) Distribution of dead benthic foraminifera in surface sedim...
Samples SO136-004MUC, SO136-043BX, SO136-147BX investigated by Nabulis. The data of B. aculeata and B. elongata may be inverted, the author's species description mention one... -
(Appendix Table 3) Distribution of live benthic foraminifera in surface sedim...
Samples SO136-004MUC, SO136-043BX, SO136-147BX investigated by Nabulsi. The data of B. aculeata and B. elongata may be inverted, the author's species description mention one... -
(Supplement S3) Absolute abundances of benthic foraminifers from Alvin dive A...
This dataset has no description
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(Supplement S2) Absolute abundances of benthic foraminifers from Alvin dive A...
This dataset has no description
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(Supplement S1) Absolute abundances of benthic foraminifers from Alvin dive A...
This dataset has no description
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(Table 6) Benthic foraminiferal community at DSDP Hole 94-611C
This dataset has no description
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(Table 5) Benthic foraminiferal community at DSDP Site 94-610
This dataset has no description
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(Table 4) Benthic foraminiferal community at DSDP Hole 94-609B
This dataset has no description
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Pliocene benthic foraminiferal abundances of ODP Hole 105-646B from north Atl...
Our benthic foraminiferal data clearly indicate eight layers of deep-water turbidites during the Messinian (MTL 1-8) and one in the early Pliocene (PTL 1) in Ocean Drilling...
