Dataset - B2FIND

Sedimentological, micropaleontological and stable isotope investigation of th...

The recurrence of Braarudosphaera chalks in the lower Oligocene sequences of the subtropical South Atlantic has been a long-standing conundrum, with many hypotheses having been...

Stratigraphic distribution and the number of planktic foraminifera from IODP ...

Understanding planktic foraminiferal depth habitat along with consistent taxonomic concepts is key to accurate reconstruction of paleoceanographic records. The...

(Table 5) Oligocene planktonic foraminifera of DSDP Hole 29-277

Species abundance: A = abundant, C = common, F = few, R = rare, - = not observed.

(Table 4) Paleocene to Eocene planktonic foraminifera of DSDP Hole 29-277

Species abundance: A = abundant, C = common, F = few, R = rare, - = not observed.

(Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP...

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Planktic foraminifera abundance of Hole 29-282

Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)

Planktic foraminifera abundance of Hole 29-281

Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)

Planktic foraminifera abundance of Hole 29-277

Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)

Stable oxygen isotope ratios of foraminifera from late middle Eocene sediment...

High-resolution (~3 k.y.) delta18O records from middle Eocene mixed-layer dwelling planktonic foraminifera from the western North Atlantic show pronounced (>1‰) variability....