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(Table 2) Properties of relict ice and sand wedges from six sites near Rio Ga...
Relict sand wedges are ubiquitous in southern Patagonia. At six sites we conducted detailed investigations of stratigraphy, soils, and wedge frequency and characteristics. Some... -
Tab.2: Soil properties in Nunavut and Northwest Territories, Canada
Soils of Arctic Canada were sampled during the Tundra Northwest Expedition 1999 (TNW-99) at 17 sites that cover the ecological regions of the High, Mid and Low Arctic zones.... -
Results from controlled decomposizion of gas hydrates from ODP Leg 112 (Table 1)
Gas hydrates were recovered during coring by Ocean Drilling Program (ODP) Leg 112 at Sites 685 and 688 on the Peruvian outer continental margin at latitudes of 9° and 11.5°S,... -
Plant water isotopes from West Africa (Benin and Senegal)
Observed and predicted triple oxygen isotope composition of water extracted from leaf, stem and wood samples collected at Belefoungou (BE, Benin), Nalohou (NA, Benin) and Dahra... -
Lipid metabolism in Decapods: morphometric data and total lipid content
For lipid analysis see 113-119 of Postel et a. (2000). -
Fatty acid distribution in ancient permafrost deposits at the Batagay Megaslu...
This dataset presents the fatty acid concentrations (range: n-C12 to n-C34) from 9 sediment samples which are given in µg/g sediment. Different fatty acid compounds were found:... -
Incubation data from sediment cores from the North Pacific CDisK-IV expedition
Duplicate cores from each station were incubated in a cold room (2°C) for 6-14 days to provide constraints on elemental fluxes to and from the seafloor. An incubation cap was... -
(U-Th)/He ages from zircons collected from the upper Marsyangdi valley of cen...
This dataset contains the results of three individual (U-Th)/He analyses using Zircons extracted from bedrock samples. The bedrock samples were collected from medium-high grade... -
Organic matter biogeochemistry using lipid biomarker analysis of a rapidly er...
Organic carbon (OC) stored in Arctic permafrost represents one of Earth’s largest and most vulnerable terrestrial carbon pools. Amplified climate warming across the Arctic... -
Biogenic silica, lithology and elemental composition of piston sediment core ...
Dataset includes depth and ¹⁴C based age-depth model of core from Lake 850 taken in March 2019. Biogenic silica, density, total organic carbon (TOC), total nitrogen content (%N)... -
Grain-size statistics of surface sediments off Helgoland
This dataset has no description
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Mineral composition of sediment core EN18208 from Lake Ilirney, Chukotka, far...
This dataset has no description
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Biomarker of sediment core LV53-19-1
This dataset has no description
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Total benthic foraminiferal denitrification from the Peruvian OMZ from sedime...
This dataset has no description
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(U-Th)/He ages from Zircons collected in the central Nepal Himalaya: raw data
This dataset has no description
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Response of the microbial food web to gradients of organic matter and grazing...
Zooplankton treatment: HZ: zooplankton added, LZ: Zooplankton removedCarbon treatment: 0C: No glucose addition, 0.5: 0.5 x Redfield. 1: 1xRedfield, 2: 2xRedfield, 3: 3XRedfield -
Response of the microbial food web to gradients of organic matter and grazing...
Zooplankton treatment: HZ: zooplankton added, LZ: Zooplankton removedCarbon treatment: 0C: No glucose addition, 0.5: 0.5 x Redfield. 1: 1xRedfield, 2: 2xRedfield, 3: 3XRedfield -
Fission track age for apatite sample MS_146_1 from the western Greater Caucasus
Each graticule square has an area of 0.000001386 cm2. Number of graticule squares is used with the track count to determine track densities. -
Fission track age for apatite sample MS_098_1 from the western Greater Caucasus
Each graticule square has an area of 0.000001386 cm2. Number of graticule squares is used with the track count to determine track densities. -
Fission track age for apatite sample MS_093_1 from the western Greater Caucasus
Each graticule square has an area of 0.000001386 cm2. Number of graticule squares is used with the track count to determine track densities.
