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(Table 1) Stable isotope ratios of foraminifera from sediment core W8402A-14
In the publication, d13C and d18O were erroneously exchanged. This is the corrected version. -
(Table 1) Sedimentology of core W8709A-8
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(Table 1) Sedimentology of core W8709A-8TC
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(Table 1) Sedimentology of core W8709A-1
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(Table 1) Sedimentology of core W8709A-13
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(Table 1) Sedimentology of core W8709A-13TC
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(Table 2) Age determinations on sediment core W8709A-8
Depths include the addition of 140 cm, to splice with the trigger core -
(Table 2) Age determinations on sediment core W8709A-8TC
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(Table 2) Age determinations on sediment core W8709A-13
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(Table 3) Stable isotope ratios measured on Uvigerina sp. from sediment core ...
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(Table 3) Stable isotope ratios measured on Uvigerina sp. from sediment core ...
This dataset has no description
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(Table 3) Stable isotope ratios measured on Uvigerina sp. from sediment core ...
This dataset has no description
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(Table 3) Stable isotope ratios measured on Uvigerina sp. from sediment core ...
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(Table 2a) Sea surface temperature reconstructed from Alkenones in sediment c...
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(Table 1a) Sea surface temperature reconstructed from Alkenones in sediment c...
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Age determination of sediment core W8709A-13
Northeast Pacific benthic foraminiferal d18O and d13 reveal repeated millennial-scale events of strong deep-sea ventilation (associated with nutrient depletion and/or high gas... -
Sea surface temperature reconstruction of sediment profile W8709A-8
Assessment of changes in surface ocean conditions, in particular, sea-surface temperature (SST), is essential to understand long-term changes in climate especially in regions... -
Sedimentology and stable isotope ratios of the northwest Pacific
The Multitracers Experiment studied a transect of water column, sediment trap, and sediment data taken across the California Current to develop quantitative methods for... -
(Appendix 1) Compilation of calcium carbonate concentrations from deep sea se...
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(Appendix 1) Compilation of calcium carbonate concentrations from deep sea se...
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