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Rock eval analysis of sediment core PS115/2_2
Sediment Core PS115/2-2 was recovered from the Amundsen Basin in 3600 m water depth at the eastern flank of the Gakkel Ridge during Polarstern Expedition PS115/2 in 2018 (Stein,... -
Organic geochemistry of sediment cores 9R and 10R at site PS104_20-2
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(Table 4) Organic geochemistry of sediment core PS72/350-2
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(Table 2) Characteristic of organic matter from Volgian sediments of the Ivki...
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Sedimentology and geochemistry of core PS2123-2
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Organic geochemistry on surface sediment samples from the Fram Strait and Yer...
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Organic geochemistry of sediment core PS2123-3
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Organic geochemistry of sediment core PS2122-1
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Analysis of organic material in sediment core PS2763-7
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Analysis of organic material in sediment core PS2761-10
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(Fig. 3) Analysis of organic material in sediment core PS2742-5
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(Fig. 3) Organic geochemistry of sediment core PS2476-4
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Figure 3. Geochemistry of sediment core PS2138-2
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Analysis of sediment samples from Arctic sea ice
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Sedimentology and geochemistry of core PS2122-2
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Observing soil organic carbon spatial and seasonal variability at the Golan H...
Soil organic matter (SOM) stores most of the terrestrial carbon, and changes in this storage can have a significant effect on the global carbon cycle. Various approaches have... -
(Table 1) Organic and inorganic geochemical analysis of Late Jurassic to Earl...
The Late Jurassic to Early Cretaceous (Volgian-Ryazanian) was a period of a second-order sea-level low stand, and it provided excellent conditions for the formation of shallow... -
Analysis of organic material on Site 177-1089 (Table A-10)
Depth, sediment = composite depth -
Analysis of organic material on Site 177-1093 (Table 17)
Depth, sediment = composite depth -
Analysis of organic material in surface sea ice samples from the Nordic Seas ...
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