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Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia). / Dobretsov, N. L.; Zhmodik, S. M.; Lazareva, E. V. и др.

в: Doklady Earth Sciences, Том 496, № 2, 02.2021, стр. 135-138.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Dobretsov, NL, Zhmodik, SM, Lazareva, EV, Bryanskaya, AV, Ponomarchuk, VA, Saryg-ool, BY, Kirichenko, IS, Tolstov, AV & Karmanov, NS 2021, 'Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia)', Doklady Earth Sciences, Том. 496, № 2, стр. 135-138. https://doi.org/10.1134/S1028334X21020057

APA

Dobretsov, N. L., Zhmodik, S. M., Lazareva, E. V., Bryanskaya, A. V., Ponomarchuk, V. A., Saryg-ool, B. Y., Kirichenko, I. S., Tolstov, A. V., & Karmanov, N. S. (2021). Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia). Doklady Earth Sciences, 496(2), 135-138. https://doi.org/10.1134/S1028334X21020057

Vancouver

Dobretsov NL, Zhmodik SM, Lazareva EV, Bryanskaya AV, Ponomarchuk VA, Saryg-ool BY и др. Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia). Doklady Earth Sciences. 2021 февр.;496(2):135-138. doi: 10.1134/S1028334X21020057

Author

Dobretsov, N. L. ; Zhmodik, S. M. ; Lazareva, E. V. и др. / Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia). в: Doklady Earth Sciences. 2021 ; Том 496, № 2. стр. 135-138.

BibTeX

@article{e2c2ce6f98f0471d9ba642a6b27eee58,
title = "Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia)",
abstract = "Data indicating the important role of microorganisms in the redistribution of REEs in the weathering crust and the decisive role in the concentration of REEs during the formation of ores in the upper ore horizon of the Tomtor field are obtained. The uptake of REEs was carried out by the community of microorganisms, such as phototrophs, methanogens, methanotrophs, and proteobacteria, which form the basis of the microbiocenosis for this paleoecosystem. The isotopic composition of C carbonates in all samples studied with fossilized microorganisms corresponds to the biogenic one, and the isotopic composition δ18ОSMOW (from 7 to 20‰) indicates the endogenous (hydrothermal) and, to a lesser extent, exogenous nature of the solutions. The low (87Sr/86Sr)I values of carbonates (~0.7036–0.7042) exclude the participation of seawater.",
keywords = "carbonatites, microorganisms, Tomtor Nb–REE field, weathering crust",
author = "Dobretsov, {N. L.} and Zhmodik, {S. M.} and Lazareva, {E. V.} and Bryanskaya, {A. V.} and Ponomarchuk, {V. A.} and Saryg-ool, {B. Yu} and Kirichenko, {I. S.} and Tolstov, {A. V.} and Karmanov, {N. S.}",
note = "Funding Information: This work was supported by the Russian Science Foundation, project no. 18-17-00120, and in part by the Ministry of Science and Higher Education of the Russian Federation, project no. 0259-2021-0010 (diagnostics of microorganisms). The analytical works were performed at the Center for Collective Use for Multielement and Isotopic Studies, Siberian Branch, Russian Academy of Sciences. Publisher Copyright: {\textcopyright} 2021, Pleiades Publishing, Ltd. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.",
year = "2021",
month = feb,
doi = "10.1134/S1028334X21020057",
language = "English",
volume = "496",
pages = "135--138",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Structural and Morphological Features of the Participation of Microorganisms in the Formation of Nb–REE–Rich Ores of the Tomtor Field (Russia)

AU - Dobretsov, N. L.

AU - Zhmodik, S. M.

AU - Lazareva, E. V.

AU - Bryanskaya, A. V.

AU - Ponomarchuk, V. A.

AU - Saryg-ool, B. Yu

AU - Kirichenko, I. S.

AU - Tolstov, A. V.

AU - Karmanov, N. S.

N1 - Funding Information: This work was supported by the Russian Science Foundation, project no. 18-17-00120, and in part by the Ministry of Science and Higher Education of the Russian Federation, project no. 0259-2021-0010 (diagnostics of microorganisms). The analytical works were performed at the Center for Collective Use for Multielement and Isotopic Studies, Siberian Branch, Russian Academy of Sciences. Publisher Copyright: © 2021, Pleiades Publishing, Ltd. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.

PY - 2021/2

Y1 - 2021/2

N2 - Data indicating the important role of microorganisms in the redistribution of REEs in the weathering crust and the decisive role in the concentration of REEs during the formation of ores in the upper ore horizon of the Tomtor field are obtained. The uptake of REEs was carried out by the community of microorganisms, such as phototrophs, methanogens, methanotrophs, and proteobacteria, which form the basis of the microbiocenosis for this paleoecosystem. The isotopic composition of C carbonates in all samples studied with fossilized microorganisms corresponds to the biogenic one, and the isotopic composition δ18ОSMOW (from 7 to 20‰) indicates the endogenous (hydrothermal) and, to a lesser extent, exogenous nature of the solutions. The low (87Sr/86Sr)I values of carbonates (~0.7036–0.7042) exclude the participation of seawater.

AB - Data indicating the important role of microorganisms in the redistribution of REEs in the weathering crust and the decisive role in the concentration of REEs during the formation of ores in the upper ore horizon of the Tomtor field are obtained. The uptake of REEs was carried out by the community of microorganisms, such as phototrophs, methanogens, methanotrophs, and proteobacteria, which form the basis of the microbiocenosis for this paleoecosystem. The isotopic composition of C carbonates in all samples studied with fossilized microorganisms corresponds to the biogenic one, and the isotopic composition δ18ОSMOW (from 7 to 20‰) indicates the endogenous (hydrothermal) and, to a lesser extent, exogenous nature of the solutions. The low (87Sr/86Sr)I values of carbonates (~0.7036–0.7042) exclude the participation of seawater.

KW - carbonatites

KW - microorganisms

KW - Tomtor Nb–REE field

KW - weathering crust

UR - http://www.scopus.com/inward/record.url?scp=85102505991&partnerID=8YFLogxK

U2 - 10.1134/S1028334X21020057

DO - 10.1134/S1028334X21020057

M3 - Article

AN - SCOPUS:85102505991

VL - 496

SP - 135

EP - 138

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 28257227