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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 (2 - 10 cm) at Lhù'ààn Mân...
This dataset has no description
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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. -
Concentrations of trace elements measured in soils (0 - 10 cm) at Lhù'ààn Mân...
This dataset has no description
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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... -
(Table 1) Radiolarian accumulation rates and geochemistry of ODP Site 184-1143
Late Miocene–Recent micropaleontological and geochemical records from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea (SCS) indicate that increase and... -
Geochemical analyses from different surface sediment samples of Lake Towuti, ...
For granulometric, geochemical and mineralogical analyses, approximately 25 ml of each surface sample was frozen for 24 hours and subsequently lyophilized using a Christ BETA... -
Diel cycling of Arsenic and Antimony in the Macleay River in October 2016
Diel sampling was conducted in a small pool in Bakers Creek (Macleay River), immediately upstream from the confluence with the main Macleay River trunk channel during October... -
Seasonal mobility of Arsenic and Antimony in the Macleay River 2016-2019
Water samples from the Macleay River were collected from Bellbrook bridge (30°49'10.58"S; 152°30'20.33"E) over a 35 month period (August 2016 to July 2019) at approximately 0.5...
