Amino acids in the Karelian shungites
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 f...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Shanina, S. N. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2010 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2010 |
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| Übergeordnetes Werk: |
Enthalten in: Geochemistry international - SP MAIK Nauka/Interperiodica, 1964, 48(2010), 9 vom: Sept., Seite 917-931 |
|---|---|
| Übergeordnetes Werk: |
volume:48 ; year:2010 ; number:9 ; month:09 ; pages:917-931 |
| Links: |
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| DOI / URN: |
10.1134/S0016702910090053 |
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OLC2062979649 |
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| 520 | |a 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. | ||
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10.1134/S0016702910090053 doi (DE-627)OLC2062979649 (DE-He213)S0016702910090053-p DE-627 ger DE-627 rakwb eng 550 VZ Shanina, S. N. verfasserin aut Amino acids in the Karelian shungites 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 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. Kerogen Geochemistry International Origin Life Original Amino Acid Shungite Rock Golubev, E. A. aut Enthalten in Geochemistry international SP MAIK Nauka/Interperiodica, 1964 48(2010), 9 vom: Sept., Seite 917-931 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:48 year:2010 number:9 month:09 pages:917-931 https://doi.org/10.1134/S0016702910090053 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 AR 48 2010 9 09 917-931 |
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10.1134/S0016702910090053 doi (DE-627)OLC2062979649 (DE-He213)S0016702910090053-p DE-627 ger DE-627 rakwb eng 550 VZ Shanina, S. N. verfasserin aut Amino acids in the Karelian shungites 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 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. Kerogen Geochemistry International Origin Life Original Amino Acid Shungite Rock Golubev, E. A. aut Enthalten in Geochemistry international SP MAIK Nauka/Interperiodica, 1964 48(2010), 9 vom: Sept., Seite 917-931 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:48 year:2010 number:9 month:09 pages:917-931 https://doi.org/10.1134/S0016702910090053 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 AR 48 2010 9 09 917-931 |
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10.1134/S0016702910090053 doi (DE-627)OLC2062979649 (DE-He213)S0016702910090053-p DE-627 ger DE-627 rakwb eng 550 VZ Shanina, S. N. verfasserin aut Amino acids in the Karelian shungites 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 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. Kerogen Geochemistry International Origin Life Original Amino Acid Shungite Rock Golubev, E. A. aut Enthalten in Geochemistry international SP MAIK Nauka/Interperiodica, 1964 48(2010), 9 vom: Sept., Seite 917-931 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:48 year:2010 number:9 month:09 pages:917-931 https://doi.org/10.1134/S0016702910090053 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 AR 48 2010 9 09 917-931 |
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10.1134/S0016702910090053 doi (DE-627)OLC2062979649 (DE-He213)S0016702910090053-p DE-627 ger DE-627 rakwb eng 550 VZ Shanina, S. N. verfasserin aut Amino acids in the Karelian shungites 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 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. Kerogen Geochemistry International Origin Life Original Amino Acid Shungite Rock Golubev, E. A. aut Enthalten in Geochemistry international SP MAIK Nauka/Interperiodica, 1964 48(2010), 9 vom: Sept., Seite 917-931 (DE-627)12960321X (DE-600)241677-3 (DE-576)01509703X 0016-7029 nnns volume:48 year:2010 number:9 month:09 pages:917-931 https://doi.org/10.1134/S0016702910090053 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 AR 48 2010 9 09 917-931 |
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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. © Pleiades Publishing, Ltd. 2010 |
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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. © Pleiades Publishing, Ltd. 2010 |
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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. © Pleiades Publishing, Ltd. 2010 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2062979649</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401080015.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2010 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S0016702910090053</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062979649</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)S0016702910090053-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Shanina, S. N.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Amino acids in the Karelian shungites</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Pleiades Publishing, Ltd. 2010</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Kerogen</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geochemistry International</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Origin Life</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Original Amino Acid</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Shungite Rock</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Golubev, E. A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Geochemistry international</subfield><subfield code="d">SP MAIK Nauka/Interperiodica, 1964</subfield><subfield code="g">48(2010), 9 vom: Sept., Seite 917-931</subfield><subfield code="w">(DE-627)12960321X</subfield><subfield code="w">(DE-600)241677-3</subfield><subfield code="w">(DE-576)01509703X</subfield><subfield code="x">0016-7029</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:48</subfield><subfield code="g">year:2010</subfield><subfield code="g">number:9</subfield><subfield code="g">month:09</subfield><subfield code="g">pages:917-931</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1134/S0016702910090053</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">48</subfield><subfield code="j">2010</subfield><subfield code="e">9</subfield><subfield code="c">09</subfield><subfield code="h">917-931</subfield></datafield></record></collection>
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