Traits of Biomorphic Structure Formation in Kamchatka Geyserites


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Microstructures of silicic rocks shaped by the activity of thermophilic bacterial communities in active volcanism areas of Kamchatka are described in the present article. The role of microorganisms as a special matrix that accelerates the formation of microlayered rocks of mixed chemogenic and biogenic origin is demonstrated. The authors suggest the term “biosilicites” for such rocks.

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E. Zhegallo

Borissiak Paleontological Institute, Russian Academy of Sciences

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Email: ezheg@paleo.ru
俄罗斯联邦, Moscow, 117647

L. Zaytseva

Borissiak Paleontological Institute, Russian Academy of Sciences

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Email: l.zaytseva@mail.ru
俄罗斯联邦, Moscow, 117647

V. Orleansky

Winogradsky Institute of Microbiology, Federal Research Center “Fundamentals of Biotechnology,”
Russian Academy of Sciences

Email: karpovga@kscnet.ru
俄罗斯联邦, Moscow, 119071

O. Samylina

Winogradsky Institute of Microbiology, Federal Research Center “Fundamentals of Biotechnology,”
Russian Academy of Sciences

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Email: olga.samylina@gmail.com
俄罗斯联邦, Moscow, 119071

G. Karpov

Institute of Volcanology and Seismology, Far East Branch, Russian Academy of Sciences

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Email: karpovga@kscnet.ru
俄罗斯联邦, Petropavlovsk-Kamchatskii, 683006

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