MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA
<p>Relics of the paleosol of Mesoarchean age (3000–2930 Ma) developed on tuffs and lavas of komatiites from Koikary Area (Central Karelia) were studied. Microscopic tubular and spherical structures morphologically similar to fossilized remnants of microorganisms were found in the preserved par...
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Karelian Research Centre of the Russian Academy of Sciences
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doaj-2fd1e5f99b8a4b5b84572b1301859fec2020-11-25T02:51:28ZengKarelian Research Centre of the Russian Academy of SciencesTransactions of the Karelian Research Centre of the Russian Academy of Sciences1997-32172312-45042017-11-01011789010.17076/geo683493MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIAСветлана Юрьевна Чаженгина0Александра Владимировна Бакаева1Зоя Павловна Рыбникова2Павел Владимирович Медведев3Сергей Анатольевич Светов4Svetlana ChazhenginaAlexandra Bakaeva5Zoya Rybnikova6Pavel Medvedev7Sergey Svetov8Институт геологии Карельского Научного Центра РАН, ПетрозаводскИнститут геологии Карельского Научного Центра РАН, ПетрозаводскИнститут геологии Карельского Научного Центра РАН, ПетрозаводскИнститут геологии Карельского Научного Центра РАН, ПетрозаводскИнститут геологии Карельского Научного Центра РАН, ПетрозаводскInstitute of Geology, Karelian Research Centre, Russian Academy of Sciences 11 Pushkinskaya St., 185910 Petrozavodsk, Karelia, RussiaInstitute of Geology, Karelian Research Centre, Russian Academy of Sciences 11 Pushkinskaya St., 185910 Petrozavodsk, Karelia, RussiaInstitute of Geology, Karelian Research Centre, Russian Academy of Sciences 11 Pushkinskaya St., 185910 Petrozavodsk, Karelia, RussiaInstitute of Geology, Karelian Research Centre, Russian Academy of Sciences 11 Pushkinskaya St., 185910 Petrozavodsk, Karelia, Russia<p>Relics of the paleosol of Mesoarchean age (3000–2930 Ma) developed on tuffs and lavas of komatiites from Koikary Area (Central Karelia) were studied. Microscopic tubular and spherical structures morphologically similar to fossilized remnants of microorganisms were found in the preserved part of the crust profile, represented by a layer of chloritite. The nature of these micro structures and the possibility of their interpretation as acidophilic bacteria inhabiting the land in the zone of chemical weathering of volcanic rocks are discussed.</p>http://journals.krc.karelia.ru/index.php/precambrian/article/view/683микрофоссилии, мезоархей, кора выветривания, коматииты, фенноскандинавский щит |
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DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Светлана Юрьевна Чаженгина Александра Владимировна Бакаева Зоя Павловна Рыбникова Павел Владимирович Медведев Сергей Анатольевич Светов Svetlana Chazhengina Alexandra Bakaeva Zoya Rybnikova Pavel Medvedev Sergey Svetov |
spellingShingle |
Светлана Юрьевна Чаженгина Александра Владимировна Бакаева Зоя Павловна Рыбникова Павел Владимирович Медведев Сергей Анатольевич Светов Svetlana Chazhengina Alexandra Bakaeva Zoya Rybnikova Pavel Medvedev Sergey Svetov MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA Transactions of the Karelian Research Centre of the Russian Academy of Sciences микрофоссилии, мезоархей, кора выветривания, коматииты, фенноскандинавский щит |
author_facet |
Светлана Юрьевна Чаженгина Александра Владимировна Бакаева Зоя Павловна Рыбникова Павел Владимирович Медведев Сергей Анатольевич Светов Svetlana Chazhengina Alexandra Bakaeva Zoya Rybnikova Pavel Medvedev Sergey Svetov |
author_sort |
Светлана Юрьевна Чаженгина |
title |
MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA |
title_short |
MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA |
title_full |
MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA |
title_fullStr |
MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA |
title_full_unstemmed |
MICROFOSSILS FROM RELICT MESOARCHEAN PALEOSOL DEVELOPED ON KOMATIITES FROM KOIKARY AREA, CENTRAL KARELIA |
title_sort |
microfossils from relict mesoarchean paleosol developed on komatiites from koikary area, central karelia |
publisher |
Karelian Research Centre of the Russian Academy of Sciences |
series |
Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
issn |
1997-3217 2312-4504 |
publishDate |
2017-11-01 |
description |
<p>Relics of the paleosol of Mesoarchean age (3000–2930 Ma) developed on tuffs and lavas of komatiites from Koikary Area (Central Karelia) were studied. Microscopic tubular and spherical structures morphologically similar to fossilized remnants of microorganisms were found in the preserved part of the crust profile, represented by a layer of chloritite. The nature of these micro structures and the possibility of their interpretation as acidophilic bacteria inhabiting the land in the zone of chemical weathering of volcanic rocks are discussed.</p> |
topic |
микрофоссилии, мезоархей, кора выветривания, коматииты, фенноскандинавский щит |
url |
http://journals.krc.karelia.ru/index.php/precambrian/article/view/683 |
work_keys_str_mv |
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