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@article{aa6cc57a7ce54b43b75f2e2d8732096f,
title = "Microbial biomineralization under extreme conditions: Case study of basaltic rocks, Tolbachik Volcano, Kamchatka, Russia",
abstract = "Microorganisms (bacteria, fungi and others) are considered to be the pioneers of the settlement under extreme conditions and take an active part in biomineralization and soil formation. We studied biofilms and for the firsttime identified the presence of microbial biomineralization in extreme conditions of Tolbachik Volcano area, Russia. Rock samples with lichen / cyanobacteria biofilms were studied by a complex of methods (optical and scanning electron microscopy, powder X-ray diffraction and energy-dispersive X-ray spectroscopy). We found that the acidic environment of biofilms favor oxalate biomineralization under the action of lichens and suppresses the carbonate biomineralization under the action of cyanobacteria. Calcium (whewellite, Ca(C2O4)⋅H2O, and weddellite, Ca(C2O4)⋅(2.5-x)H2O (0 ≤ x ≤ 0.25)) and copper oxalates (moolooite, Cu(C2O4)⋅nH2O) were found in lichen biofilms. Direct relationship between the age of lichen and intense of biomineralization was discovered. It was shown that the lichens not only extract calcium and heavy metals (Cu, Pb) from the basalticrock (both in situ and from weathered particles of the same rock brought by the wind) but increase their content in biofilm. The lichen species Psilolechia leprosa, Sarcogyne hypophaea, Rinodina cf. gennarii, and Ochrolechia subplicans subsp. subplicans can form oxalates. It was also found that (1) calcium and copper oxalates can be localized in the same lichen, (2) the species producing oxalic acid do not always produce oxalates and (3) the ratio of whewellite and weddellite formed by the same species lichen can vary significantly. Obtained resultsshow high abundancy of biomineralization in terrestrial environment, including extreme and provide some insights into mechanisms of microbial biomineralization.",
keywords = "Cyanobacteria, Heavy metals extraction, Lichen, Microbial biomineralization",
author = "Верещагин, {Олег Сергеевич} and Франк-Каменецкая, {Ольга Викторовна} and Власов, {Дмитрий Юрьевич} and Зеленская, {Марина Станиславовна} and Родина, {Оксана Андреевна} and Чернышова, {Ирина Александровна} and Гимельбрант, {Дмитрий Евгеньевич} and Степанчикова, {Ирина Сергеевна} and Бритвин, {Сергей Николаевич}",
year = "2023",
month = jun,
day = "1",
doi = "10.1016/j.catena.2023.107048",
language = "English",
volume = "226",
journal = "Catena",
issn = "0341-8162",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Microbial biomineralization under extreme conditions: Case study of basaltic rocks, Tolbachik Volcano, Kamchatka, Russia

AU - Верещагин, Олег Сергеевич

AU - Франк-Каменецкая, Ольга Викторовна

AU - Власов, Дмитрий Юрьевич

AU - Зеленская, Марина Станиславовна

AU - Родина, Оксана Андреевна

AU - Чернышова, Ирина Александровна

AU - Гимельбрант, Дмитрий Евгеньевич

AU - Степанчикова, Ирина Сергеевна

AU - Бритвин, Сергей Николаевич

PY - 2023/6/1

Y1 - 2023/6/1

N2 - Microorganisms (bacteria, fungi and others) are considered to be the pioneers of the settlement under extreme conditions and take an active part in biomineralization and soil formation. We studied biofilms and for the firsttime identified the presence of microbial biomineralization in extreme conditions of Tolbachik Volcano area, Russia. Rock samples with lichen / cyanobacteria biofilms were studied by a complex of methods (optical and scanning electron microscopy, powder X-ray diffraction and energy-dispersive X-ray spectroscopy). We found that the acidic environment of biofilms favor oxalate biomineralization under the action of lichens and suppresses the carbonate biomineralization under the action of cyanobacteria. Calcium (whewellite, Ca(C2O4)⋅H2O, and weddellite, Ca(C2O4)⋅(2.5-x)H2O (0 ≤ x ≤ 0.25)) and copper oxalates (moolooite, Cu(C2O4)⋅nH2O) were found in lichen biofilms. Direct relationship between the age of lichen and intense of biomineralization was discovered. It was shown that the lichens not only extract calcium and heavy metals (Cu, Pb) from the basalticrock (both in situ and from weathered particles of the same rock brought by the wind) but increase their content in biofilm. The lichen species Psilolechia leprosa, Sarcogyne hypophaea, Rinodina cf. gennarii, and Ochrolechia subplicans subsp. subplicans can form oxalates. It was also found that (1) calcium and copper oxalates can be localized in the same lichen, (2) the species producing oxalic acid do not always produce oxalates and (3) the ratio of whewellite and weddellite formed by the same species lichen can vary significantly. Obtained resultsshow high abundancy of biomineralization in terrestrial environment, including extreme and provide some insights into mechanisms of microbial biomineralization.

AB - Microorganisms (bacteria, fungi and others) are considered to be the pioneers of the settlement under extreme conditions and take an active part in biomineralization and soil formation. We studied biofilms and for the firsttime identified the presence of microbial biomineralization in extreme conditions of Tolbachik Volcano area, Russia. Rock samples with lichen / cyanobacteria biofilms were studied by a complex of methods (optical and scanning electron microscopy, powder X-ray diffraction and energy-dispersive X-ray spectroscopy). We found that the acidic environment of biofilms favor oxalate biomineralization under the action of lichens and suppresses the carbonate biomineralization under the action of cyanobacteria. Calcium (whewellite, Ca(C2O4)⋅H2O, and weddellite, Ca(C2O4)⋅(2.5-x)H2O (0 ≤ x ≤ 0.25)) and copper oxalates (moolooite, Cu(C2O4)⋅nH2O) were found in lichen biofilms. Direct relationship between the age of lichen and intense of biomineralization was discovered. It was shown that the lichens not only extract calcium and heavy metals (Cu, Pb) from the basalticrock (both in situ and from weathered particles of the same rock brought by the wind) but increase their content in biofilm. The lichen species Psilolechia leprosa, Sarcogyne hypophaea, Rinodina cf. gennarii, and Ochrolechia subplicans subsp. subplicans can form oxalates. It was also found that (1) calcium and copper oxalates can be localized in the same lichen, (2) the species producing oxalic acid do not always produce oxalates and (3) the ratio of whewellite and weddellite formed by the same species lichen can vary significantly. Obtained resultsshow high abundancy of biomineralization in terrestrial environment, including extreme and provide some insights into mechanisms of microbial biomineralization.

KW - Cyanobacteria

KW - Heavy metals extraction

KW - Lichen

KW - Microbial biomineralization

UR - https://www.mendeley.com/catalogue/b5ea60d7-8a84-30e6-a8f9-600d180d9c59/

U2 - 10.1016/j.catena.2023.107048

DO - 10.1016/j.catena.2023.107048

M3 - Article

VL - 226

JO - Catena

JF - Catena

SN - 0341-8162

M1 - 107048

ER -

ID: 103568045