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(Table III) Occurrence of selected diatom taxa in DSDP Hole 18-173, Californi...
Taxa abundance: A = abundant, C = common, F = few, R = rare * = reworked, - = not present -
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... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
Nannofossil abundance of Hole 18-173
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 18-172
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Foraminifera abundance of Hole 18-176
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Microfossil abundance of Hole 18-173
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 18-172
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geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated.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... -
Planktic foraminifera abundance of Hole 18-177A
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 18-177
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 18-174A
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 18-173
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Supplement S3) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
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(Table 1) Major and trace element composition of marine sediments of the worl...
Sediment depth is given in mbsf. All concentrations reported relative to dry weight (110°C). -
(Table 1) Hf-Nd isotope ratios of marine sediments of the world's major subdu...
This dataset has no description
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(Table 1) Composition of sediments of Aleutian DSDP sites
Point counting analysis -
(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
This dataset has no description
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(Table 1) Electron microprobe analyses of volcanic glass of some tephra layer...
Values are recalculated to 100% on a fluide-free basis. Original oxide totals before recalculation are given to indicate approximate degree of hydration of volcanic glass. -
(Table 3) Petrological parameters of sands and sandstones from DSDP and ODP h...
Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline...
