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(Table 5) Diatom biostratigraphy of ODP Hole 167-1011B sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 13) Diatom biostratigraphy of ODP Site 167-1022 sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 12) Diatom biostratigraphy of ODP Hole 167-1021B sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 11) Diatom biostratigraphy of ODP Hole 167-1020C sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and - = not found. -
(Table 10) Diatom biostratigraphy of ODP Hole 167-1020B sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 9) Diatom biostratigraphy of ODP Hole 167-1019C sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 8) Diatom biostratigraphy of ODP Hole 167-1018A sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 7) Diatom biostratigraphy of ODP Hole 167-1016A sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and B = barren, - = not found. -
(Table 6) Diatom biostratigraphy of ODP Hole 167-1014A sediments
DEPTH, sediment is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, T = trace, and - = not found. -
(Table 7) Relative abundances of stratigraphically useful planktonic foramini...
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, B = barren, - = not found. -
(Table 6) Relative abundances of stratigraphically useful planktonic foramini...
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, B = barren, - = not found. -
(Table 5) Relative abundances of stratigraphically useful planktonic foramini...
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, B = barren, - = not found. -
(Table 4) Relative abundances of stratigraphically useful planktonic foramini...
Sediment depth is given in mbsf. Abundance estimates as follows: A = abundant, C = common, F = few, R = rare, B = barren, - = not found. -
(Table 1) Trace element and Tl isotope composition of Late Neogene pyrites
This dataset has no description
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(Appendix G) Benthic foraminifera accumulation rates of ODP Site 167-10121
Sediment depth is given in mbsf. Age interpolated after Lisiecki and Raymo timescale (2005, doi:10.1029/2004PA001071) -
(Appendix G) Benthic foraminifera extinction group species in ODP Hole 167-1012B
Sediment depth is given in mbsf. Age interpolated after Lisiecki and Raymo timescale (2005, doi:10.1029/2004PA001071) -
δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...
The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are... -
CLAM age model and pollen profile of sediment core 167-1019
This dataset has no description
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(Table 1) Abundance of selected diatom taxa in the mid-Pliocene of ODP Hole 1...
Diatom assemblages from the middle part of the Pliocene (3.2-2.5 Ma) were investigated from Ocean Drilling Program Sites 1016, 1021, and 1022 in an effort to infer... -
Benthic foraminiferal assemblages in ODP Hole 167-1017E
A strong oxygen-minimum zone (OMZ) currently exists along the California margin because of a combination of high surface-water productivity and poor intermediate-water...
