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Raw U, Th, age model, and calculated authigenic uranium
This dataset has no description
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Oxygen and carbon stable isotopes of Globobulimina spp. and Cibicidoides wuel...
This dataset has no description
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Oxygen and carbon stable isotopes of Globobulimina spp. and Cibicidoides wuel...
This dataset has no description
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Flux of excess barium from ODP Site 202-1240
This dataset has no description
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Authigenic uranium from ODP Site 202-1240
This dataset has no description
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Authigenic uranium from ODP Site 138-846
This dataset has no description
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(Table 2) Age model of DSDP Hole 81-552A
This dataset has no description
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Calcium carbonate content of sediment core 85-574
This dataset has no description
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Calcium carbonate content of sediment core 85-573A
This dataset has no description
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Calcium carbonate content of sediment core 85-572C
This dataset has no description
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Calcium carbonate content of sediment core 85-572A
This dataset has no description
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Age model of sediment core 85-574
This dataset has no description
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Age model of sediment core 85-573A
This dataset has no description
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Age model of sediment core 85-574
This dataset has no description
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Age model of sediment core 85-573A
This dataset has no description
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Age model of Hole 86-580
This dataset has no description
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Calcium carbonate preservation in the equatorial Pacific
The Pliocene-Pleistocene history of CaCO3 preservation in the central equatorial Pacific is reconstructed from a suite of deep-sea cores and is compared to fluctuations in... -
Age models and stable isotope record of sediment cores from the Atlantic Ocean
The high-resolution delta18O and delta13C records of benthic foraminifera from a 150,000-year long core from the Caribbean Sea indicate that there was generally high delta13C... -
Stable isotope record of benthic foraminifera in late Pleistocene sediments
Variations in the contribution of North Atlantic Deep Water (NADW), relative to North Pacific Deep Water (NPDW), to the Southern Ocean, are assessed by comparing delta13C... -
(Table A7) CaCO3, opal, and stable isotope ratios of Cibicides spp. from sedi...
The ages have been derived through oxygen isotope stratigraphy with various supplemental control points from 14C and biostratigraphy and are given as calculated ages.
