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Seawater carbonate chemistry and calcification in the Bahama Bank, 1964-1965
Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm... -
Interstitial water chemistry of Hole 81-555
Details given in volume 81, chapter 34 -
Interstitial water chemistry of Hole 81-554A
Details given in volume 81, chapter 34 -
Interstitial water chemistry of Hole 81-554
Details given in volume 81, chapter 34 -
Interstitial water chemistry of Hole 81-553A
Details given in volume 81, chapter 34 -
Interstitial water chemistry of Hole 81-553
Details given in volume 81, chapter 34 -
Interstitial water chemistry of Hole 81-552A
Details given in volume 81, chapter 34 -
Interstitial water chemistry of Hole 81-552
Details given in volume 81, chapter 34 -
Composition of water extracts from Barents Sea sediments of the drill core BA...
This dataset has no description
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Sediment pore water chemistry and geophysical measurements of Site PG1227
This dataset has no description
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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... -
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... -
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... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Pore water chemistry, grain sizes and sediment temperature of sediment core C...
Methods: Temperature measurements were made using thermistors and infra-red sensors. Pore water was extracted from thawed sediment using Rhizons™ (0.15 µm pore diameter).... -
Sedimentology and hydrochemistry in thawing permafrost of Herschel Island
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...
