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Chemical composition of hydrothermal fluids at station MSM04/3-275-ROV-5
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-271-ROV-11
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-259-ROV-25
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-3
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-17
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-13
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-257-ROV-12
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-253-ROV-9
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-253-ROV-10
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Chemical composition of hydrothermal fluids at station MSM04/3-244-ROV-7
Inductively Coupled Plasma Mass Spectrometry: dilution factor = 25; Matrix = 0.5M HNO3. Inductively Coupled Plasma Optical Emission Spectrometry: dilution factor = 10; Matrix =... -
Concentrations of trace elements measured in soils (0 - 2 cm) at Lhù'ààn Mân'...
This dataset has no description
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Concentrations of trace elements measured in lichens at Lhù'ààn Mân' (Kluane ...
This dataset has no description
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Field gas measurements from wells in Van Phuc village, Hanoi, Vietnam
Arsenic groundwater contamination is threatening the health of millions of people worldwide, particularly in river deltas in South and Southeast Asia where geogenic arsenic is... -
(Table S3) B/Ca ratios Cibicidoides wuellerstorfi from Holocene sediments
Size fraction of benthic foraminifera = 150-250 µm. -
(Table S1) B/Ca ratios and stable isotope record of Nuttallides umbonifera fr...
Size fraction of benthic foraminifera = 150-250 µm. -
Summary of boron isotope and Mg/Ca data
Biological productivity and carbon export in the equatorial Atlantic are thought to have been dramatically higher during the last glacial period than during the Holocene. Here... -
Trace element composition of concretions, ICP–MS measurements
In order to get a complete geochemical signature, 14 P-rich concretions, chosen among the different cores, were acid digested (Table 3a and Table 3b). In a clean laboratory, 1.7... -
Geochemical data on otoliths of chaetodon speculum from New Caledonia
Coral reefs are one of the most diverse ecosystems on Earth. They are currently exposed to increasing levels of anthropogenic perturbations. Several recent reviews point to the... -
(Table 2) Trace metal concentrations in ODP Hole 169-1033B
We measured the concentrations of redox-sensitive trace metals (Mn, V, Mo, U, Cd and Re) in sediments from ODP Leg 169S Hole 1033B in Saanich Inlet, British Columbia, to... -
(Table 1) Boron analyses from ODP Sites 186-1150 and 186-1151
Interstitial pore waters from Ocean Drilling Program (ODP) Sites 1150 and 1151, both penetrating ca. 1200 m of sub-seafloor sediment from the upper Japan Trench forearc, were...
