Dataset - B2FIND

Chemistry of ice core AUF87 from the Russian Arctic

This dataset has no description

(Table 3) Geochemistry of borehole fluids of ODP Hole 137-504B

Circulation of seawater through basaltic basement for several million years after crustal emplacement has been inferred from studies of surface heat flow, and may play a...

Pore water and peat geochemistry measured close to Rostock (Germany) in 2015

In natural coastal wetlands, high supplies of marine sulfate suppress methanogenesis. Coastal wetlands are, however, often subject to disturbance by dyking and drainage for...

Geochemistry and mineralogy of sediment core PG1238

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GRIP Ion Concentrations

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GISP2 Ions: Deep (D) Core

Ion data set produced by the Glacier Research Group for the GISP2 D core, from 2 - 3040 m. 2 to 96 m is B core data. The remainder of data is from D core. D core samples were...

GISP2 Ions: B core (0-200 meters)

This is the ion data set produced by the Glacier Research Group for the GISP2 B core drilled at the GISP2 site during the summer of 1989. The data is bi-yearly, a combination of...

GISP2 Ions: Shallow (B) Core (Detailed)

GISP2 major ion concentrations in parts per billion (ppb) by mass. Blanks in the H2O2 data indicate samples that were not analyzed. Blanks in other chemical species represent...

GISP2 Ions: Deep (D) Core (Detailed)

GISP2 major ion concentrations in parts per billion (ppb) by mass. Blanks in chemical species represent samples below detection limits. Firn samples were cleaned in the freezer...

Inorganic ion concentrations in bodyfluids of marine invertebrates exposed to...

Laboratory experiments were conducted in the climate chambers at GEOMAR Helmholtz Centre for Ocean Research Kiel in the time between March and November 2018. Experiments were...

Inorganic ions in size-resolved aerosol particles sampled from the Arctic in ...

Size-resolved atmospheric particles were collected in the Arctic during the PS 106 campaign (2017). For the collection of the aerosol particles, a five-stage low-pressure BERNER...

(Table 1) Ion concentrations in the haemolymph of Apherusa glacialis after in...

Amphipods living at the underside of Arctic sea ice are exposed to varying salinities due to freezing and melting, and have to cope with the resulting osmotic stress....

Ion concentration, salinity and total dissolved solids (TDS) in Holocene mult...

Holocene massive ground ice near the Sabettayakha River mouth, on the coast of the Gulf of Ob, Yamal Peninsula, northwest Siberia is studied. Three boreholes (Nr 12, 17 and 42)...