-
(Table 9) Distribution of selected diatoms in Miocene to Pleistocene sediment...
Species abundaces: D = dominant, A = abundant, C = common, F = few, R = rare, - = absent. -
(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 3) Distribution of diatoms in Pliocene sediments of DSDP Hole 86-580 i...
Ages follow the magnetostratigraphy of Bleil (1985) -
Diatom abundance of Hole 86-581
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 86-580
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 86-579A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 86-579
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 86-578
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 86-577
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table S2) Nannofossil abundances at DSDP Hole 86-577A
DEPTH, sediment is given in mbsf. Species abundances: A = abundant (>10 speciemens per field of view), C = common (5-10 specimens f/v), F = few (1-2 specimens f/v), R = rare... -
(Table S1) Nannofossil abundances at DSDP Hole 86-577
DEPTH, sediment is given in mbsf. Most data from Backman (1986). -
(Table 3) Accumulation rates and residence times of iridium, osmium and rheni...
Concentrations are given for dry sediments. -
Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
(Appendix A) Nannofossil stratigraphic range chart for the late Maastrichtian...
The response of calcareous nannofossils to the end-Cretaceous warming is investigated in the Tropical Pacific DSDP Site 577A (Shatsky Rise) through the record of species... -
Nannofossil abundance of Hole 86-577B
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 86-577A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 86-577
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
Concentrations and accumulation rates of platinum-group elements and rhenium ...
The nature of Re-platinum-group element (PGE; Pt, Pd, Ir, Os, Ru) transport in the marine environment was investigated by means of marine sediments at and across the... -
(Appendix 2-8) Distribution of planktonic foraminifera in late Neogene sedime...
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