Shanina, Svetlana N; Golubev, E A (2010): Organic carbon and amino acid concentration of Karelian shungite rocks from the lake Onego area, Russia [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.792625, Supplement to: Shanina, SN; Golubev, EA (2010): Amino acids in the Karelian shungites. Geochemistry International, 48(9), 917-931, https://doi.org/10.1134/S0016702910090053
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Abstract:
The study of amino acids in the Precambrian shungite rocks of Karelia showed that their contents vary within 25-89 µg/g depending on proportions between shungite and mineral components. It was established that the amino acids exhibit an excess of L-enantiomers. In the shungite rocks, they form organomineral complexes with silica and aluminosilicates, being built in the globular structure of shungite matter. There are several sources of amino acids in shungites: secondary synthesis, microbial pollution, and original amino acids of organic matter in shungite rocks.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 62.363720 * Median Longitude: 34.768560 * South-bound Latitude: 62.222000 * West-bound Longitude: 34.303000 * North-bound Latitude: 62.594000 * East-bound Longitude: 35.364000
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets
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Datasets listed in this publication series
- Shanina, SN; Golubev, EA (2010): (Table 2) Amino acid concentrations in Karelian shungite samples from the Onego lake area. https://doi.org/10.1594/PANGAEA.792624
- Shanina, SN; Golubev, EA (2010): (Table 1) Description and organic carbon content of shungite samples from the Onego lake area. https://doi.org/10.1594/PANGAEA.792622