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Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia). / Ponomarchuk, V. A.; Dobretsov, N. L.; Lazareva, E. V. et al.

In: Doklady Earth Sciences, Vol. 490, No. 2, 01.02.2020, p. 76-80.

Research output: Contribution to journal › Article › peer-review

Harvard

Ponomarchuk, VA, Dobretsov, NL, Lazareva, EV, Zhmodik, SM, Karmanov, NS, Tolstov, AV & Pyryaev, AN 2020, 'Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia)', Doklady Earth Sciences, vol. 490, no. 2, pp. 76-80. https://doi.org/10.1134/S1028334X20020117

APA

Ponomarchuk, V. A., Dobretsov, N. L., Lazareva, E. V., Zhmodik, S. M., Karmanov, N. S., Tolstov, A. V., & Pyryaev, A. N. (2020). Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia). Doklady Earth Sciences, 490(2), 76-80. https://doi.org/10.1134/S1028334X20020117

Vancouver

Ponomarchuk VA, Dobretsov NL, Lazareva EV, Zhmodik SM, Karmanov NS, Tolstov AV et al. Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia). Doklady Earth Sciences. 2020 Feb 1;490(2):76-80. doi: 10.1134/S1028334X20020117

Author

Ponomarchuk, V. A. ; Dobretsov, N. L. ; Lazareva, E. V. et al. / Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia). In: Doklady Earth Sciences. 2020 ; Vol. 490, No. 2. pp. 76-80.

BibTeX

@article{303d0b564a91465b8925d71bf7bb31a6,
title = "Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia)",
abstract = "Carbonates of the Tomtor complex of ultramafic alkaline rocks and carbonatites (the northern part of the Republic of Sakha Yakutia) are distinguished by a wide range of carbon isotopic composition δ13C from +2 to –59.9‰. The geological position, localization patterns, mineral and chemical compositions and the relationship with REE mineralization of samples with values of δ13C carbonates from –25 to –59‰ are characterized. The formation of abnormally low δ13C in carbonates is determined by the biogenic oxidation of methane from δ13Cmet to –70‰.",
keywords = "biogenic processes, carbon isotopes, REE deposits, the Tomtor carbonatite complex, weathering crust of carbonatites, MASSIF, ORIGIN, AGE",
author = "Ponomarchuk, {V. A.} and Dobretsov, {N. L.} and Lazareva, {E. V.} and Zhmodik, {S. M.} and Karmanov, {N. S.} and Tolstov, {A. V.} and Pyryaev, {A. N.}",
year = "2020",
month = feb,
day = "1",
doi = "10.1134/S1028334X20020117",
language = "English",
volume = "490",
pages = "76--80",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Evidence of Microbial-Induced Mineralization in Rocks of the Tomtor Carbonatite Complex (Arctic Siberia)

AU - Ponomarchuk, V. A.

AU - Dobretsov, N. L.

AU - Lazareva, E. V.

AU - Zhmodik, S. M.

AU - Karmanov, N. S.

AU - Tolstov, A. V.

AU - Pyryaev, A. N.

PY - 2020/2/1

Y1 - 2020/2/1

N2 - Carbonates of the Tomtor complex of ultramafic alkaline rocks and carbonatites (the northern part of the Republic of Sakha Yakutia) are distinguished by a wide range of carbon isotopic composition δ13C from +2 to –59.9‰. The geological position, localization patterns, mineral and chemical compositions and the relationship with REE mineralization of samples with values of δ13C carbonates from –25 to –59‰ are characterized. The formation of abnormally low δ13C in carbonates is determined by the biogenic oxidation of methane from δ13Cmet to –70‰.

AB - Carbonates of the Tomtor complex of ultramafic alkaline rocks and carbonatites (the northern part of the Republic of Sakha Yakutia) are distinguished by a wide range of carbon isotopic composition δ13C from +2 to –59.9‰. The geological position, localization patterns, mineral and chemical compositions and the relationship with REE mineralization of samples with values of δ13C carbonates from –25 to –59‰ are characterized. The formation of abnormally low δ13C in carbonates is determined by the biogenic oxidation of methane from δ13Cmet to –70‰.

KW - biogenic processes

KW - carbon isotopes

KW - REE deposits

KW - the Tomtor carbonatite complex

KW - weathering crust of carbonatites

KW - MASSIF

KW - ORIGIN

KW - AGE

UR - http://www.scopus.com/inward/record.url?scp=85084917670&partnerID=8YFLogxK

U2 - 10.1134/S1028334X20020117

DO - 10.1134/S1028334X20020117

M3 - Article

AN - SCOPUS:85084917670

VL - 490

SP - 76

EP - 80

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 24330350