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Pollen and spore abundance of Hole 42-374
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
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Microfossil abundance of Hole 42-378
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 42-375
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 42-374
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 42-372
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 42-371
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
(Table 2) Mass spectra of highly dealkylated metallo-(Cu,Ni)-etioporphyrins i...
Calculated from average mass spectrum of mixed (CUE, NiE, NiD) isolates. Low-voltage (14 eV) mass spectra isotopically-corrected and series-normalized. -
(Table 3) Survey of Atlantic Ocean DSDP sites for hiatuses PH and NH 1 throug...
This dataset has no description
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(Table 1) Distribution of copper porphyrins and other pigments in deep-sea se...
Copper porphyrins have been isolated from deep-sea sediments collected during six legs of the Deep Sea Drilling Project-International Program of Ocean Drilling. These pigments... -
Highly dealkylated copper and nickel etioporpyfrins in marine sediments
Copper porphyrins have been recognized as natural constituents of marine sediments only within the past 5 years (Palmer and Baker, 1978, Science201, 49–51). In that report it... -
Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes
Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of... -
(Table 7) Uranium contents in DSDP Leg 42 Black Sea bottom sediments before a...
This dataset has no description
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(Table 3) Uranium contents in Black Sea bottom sediments from DSDP Leg 42 holes
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 42-373A
This dataset has no description
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(Table 2) Fractionation of bitumen from DSDP sediment samples
This dataset has no description
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(Table 1) Sediment description and TOC content of DSDP samples
This dataset has no description
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(Table 2) Composition of aliphatic-naphthenic fraction of hydrocarbons from B...
Zero values mean traces. -
(Table 1) Composition of paraffinic hydrocarbons in aliphatic-naphthenic frac...
Zero values mean traces.