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Chemical and isotopic compositions of pore and botom waters at Sites ARA06C-J...
Cl- and alkalinity were determined by visual titration with 0.1 M AgNO~3~ and 0.02 M HCl, respectively. NH~4~+ and PO~4~3 were measured spectrophotometrically (UV-2450, Shimazu)... -
δ¹¹B, Mg/Ca, and input variables for calculated pH and CO₂ during the late Pl...
This dataset has no description
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(Table 1) Boron contents and boron, carbon, and oxygen isotope data for ODP S...
Note that in the manuscript text the values of the d11B shift due to variable pH have been not reported correctly. The shifts are +13.7 per mil at pH=7 and +15.3 per mil at... -
(Table 1) Boron contents and boron, carbon, and oxygen isotope data for ODP S...
Note that in the manuscript text the values of the d11B shift due to variable pH have been not reported correctly. The shifts are +13.7 per mil at pH=7 and +15.3 per mil at... -
(Table 1) Stable isotope ratios of pore water from ODP Hole 127-797B
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(Table 1) Stable isotope ratios of pore water from ODP Site 127-796
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(Table 1) Stable isotope ratios of pore water from ODP Site 127-795
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(Table 1) Stable isotope ratios of pore water from ODP Site 127-794
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(Table 1) Boron contents and B, C, and O isotope signatures from the authigen...
This dataset has no description
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(Table 1) Boron contents and B, C, and O isotope signatures from the authigen...
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(Table 1) Cl, Sr, and B concentrations and 87Sr/86Sr and d11B values from por...
This dataset has no description
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(Table 1) Cl, Sr, and B concentrations and 87Sr/86Sr and d11B values from por...
This dataset has no description
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(Table 1) Cl, Sr, and B concentrations and 87Sr/86Sr and d11B values from por...
This dataset has no description
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(Table 1) Cl, Sr, and B concentrations and 87Sr/86Sr and d11B values from por...
This dataset has no description
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(Table 1) Cl, Sr, and B concentrations and 87Sr/86Sr and d11B values from por...
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Chemical and isotopic compositions of altered MORB from ODP Hole 187-1154A
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Chemical and isotopic compositions of altered MORB from ODP Hole 187-1155B
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Chemical and isotopic compositions of altered MORB from ODP Hole 187-1160B
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(Table 1) Results of pore water analyses, including boron content and boron i...
Drilling a transect of holes across the Costa Rica forearc during ODP Leg 170 demonstrated the margin wedge to be of continental, non accretionary origin, which is intersected... -
B- and O-isotope and Mg/Ca ratios of planktonic foraminifera and estimates of...
The dominant period of Pleistocene glacial cycles changed during the mid-Pleistocene from 40,000 years to 100,000 years, for as yet unknown reasons. Here we present a...