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(Table 82) Chemical composition of basalts from the Nauru Basin at DSDP Site ...
Analyses have been carried out by S.P. Batalova and L.V. Shkodyuk (samples marked by *) in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of... -
(Table 62) Chemical composition of alkali basalts from the Emperor Mount Chai...
Analyses have been carried out by T.V. Sverkunova and T.K. Babova in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences. Ag, Mo, and... -
(Table1) Experimental design. Copepod species, alternative food source, femal...
This dataset has no description
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(Table T33) Chemical composition of basalts from Holes 462 and 462A, Leg 61 (...
This dataset has no description
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(Table T30) Chemical composition of basalts from Hole 471, Leg 63 (Baja Calif...
This dataset has no description
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(Table 1) Analyses of coarse fraction of DSDP Hole 94-609
This dataset has no description
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(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Table 3) Stable oxygen and carbon isotope ratios of benthic foraminifera in ...
Depth from barrel sheets (mbsf, Shipboard Scientific Pary, 1988). Mass spectrometer VG Isogas 903 triple-collector, after October 1988 (samples A 88/2048 onward) VG Isogas SIRA... -
(Table 3) Stable carbon and oxygen isotope ratios of foraminifera from surfac...
sampling depth 0-2 cm -
(Table 2) Stable carbon and oxygen isotope ratios of Miocene to Recent forami...
This dataset has no description
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(Table 1) Stable carbon and oxygen isotope ratios of Miocene to Recent forami...
This dataset has no description
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Trace element chemistry of pyrobitumen from the Tau-Tona mine in South Africa
High-grade gold and uranium mineralization in the Witwatersrand basin is intimately associated with pyrobitumen, implying that hydrocarbons may have played a role in the genesis... -
Deep-Ocean dissolved organic matter in hydrothermal vents
Oceanic dissolved organic carbon (DOC) is an important carbon pool, similar in magnitude to atmospheric CO2, but the fate of its oldest forms is not well understood (Dittmar and...
