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Ostracode relative abundances and geochemistry in surface sediments from Lake...
Understanding the ecology of bioindicators such as ostracods is essential in order to reconstruct past environmental and climate change from analysis of fossil assemblages... -
(Table T1) Pore-water strontium content, and Sr isotope composition and ages ...
Strontium concentrations and 87Sr/86Sr values were measured on pore-water and sedimentary carbonate samples from sediments recovered at Sites 1049-1053 on the Blake Spur during... -
Dissolved elemental and dissolved ion concentrations of Lena River water from...
We collected water samples from the river surface in the center of the Olenekskaya Channel near Samoylov Island using a pre-rinsed HDPE 1 L bottle. During the open water period... -
Temperature, electrical conductivity, DOC, CDOM, stable water isotopes and ma...
A number of studies expect an increase of carbon export by rivers to the Arctic Ocean due to rapidly changing climate in the ArcticOne possible reason for the increase of carbon... -
Electrical Conductivity, DOC, CDOM, stable water isotopes and major ions of t...
Current warming, shifting hydrological regimes and accelerated permafrost thaw in the catchment of the Arctic rivers will affect their water biogeochemistry and the ice that... -
(Table 2b) Concentrations of dissolved trace chemical elements in river water...
This dataset has no description
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Sedimentology and hydrochemistry in thawing permafrost of Herschel Island
This dataset has no description
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Hydrochemistry of a small Low Arctic watershed on Herschel Island in 2016
This dataset has no description
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Pore-water analyses of permafrost deposits from Byk_98_Mkh (Bykovsky Peninsul...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Byk_98_Mkh-6.2 (Bykovsky Peni...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Byk_98_Mkh-1.6.1 (Bykovsky Pe...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Byk_98_MB-6.3 (Bykovsky Penin...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Pore-water analyses of permafrost deposits from Byk_98_BH2 (Bykovsky Peninsul...
In order to get information about the pore-water characteristics from the dry samples, the water-soluble elements in the sediments were determined by shaking the samples with a... -
Porewater geochemisty of sediment core Iv-99 (Ivashkina Lagoon, Bykovsky Peni...
This dataset has no description
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Hydrochemistry at site PG1975
This dataset has no description
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Pore water geochemistry of sediment core BK-8
This dataset has no description
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Geochemistry of Holocene sediments at Yedoma cliff
This dataset has no description
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(Tab 1) Biogeochemistry of groundwater during acetate and bicarbonate amendme...
Sampling port depths are for the depths are in meters below ground surface (BGS) and are for discrete multichannel sampling ports. If no depth is given, wells are typically... -
Characterization of freshwater, seawater and submarine groundwater discharge ...
This dataset has no description
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A 1.3.3. Data of the batch experiments with the sandy fraction of harbour sed...
This dataset has no description
