Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom

The detailed researches established that the columnar structures of the ferromanganese stromatolites - are the bacterial mats, formed by the interchanging of the fossilized bacterial layers, aggregates of trichomes of thread bacteria, glycocalyx layers. Oncolites appeared in a result of active integ...

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Main Authors: V. V. Avdonin, E. A. Zhegallo, N. E. Sergeeva
Format: Article
Language:Russian
Published: Sergo Ordzhonikidze Russian State University for Geological Prospecting 2016-04-01
Series:Известия высших учебных заведений: Геология и разведка
Subjects:
Online Access:https://www.geology-mgri.ru/jour/article/view/119
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author V. V. Avdonin
E. A. Zhegallo
N. E. Sergeeva
author_facet V. V. Avdonin
E. A. Zhegallo
N. E. Sergeeva
author_sort V. V. Avdonin
collection DOAJ
description The detailed researches established that the columnar structures of the ferromanganese stromatolites - are the bacterial mats, formed by the interchanging of the fossilized bacterial layers, aggregates of trichomes of thread bacteria, glycocalyx layers. Oncolites appeared in a result of active integration of the bacterial layers with the sediment (precipitate) and assimilation of the petrogenic components.
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series Известия высших учебных заведений: Геология и разведка
spelling doaj.art-335efb6913514ca7bcfa6d70018772d72025-03-11T08:42:07ZrusSergo Ordzhonikidze Russian State University for Geological ProspectingИзвестия высших учебных заведений: Геология и разведка0016-77622618-87082016-04-0102273210.32454/0016-7762-2016-2-27-32119Microstructure of ferromanganese stromatolites and oncolites of the ocean bottomV. V. Avdonin0E. A. Zhegallo1N. E. Sergeeva2Lomonosov Moscow State UniversityBorissiak Paleontological Institute of the Russian Academy of SciencesLomonosov Moscow State UniversityThe detailed researches established that the columnar structures of the ferromanganese stromatolites - are the bacterial mats, formed by the interchanging of the fossilized bacterial layers, aggregates of trichomes of thread bacteria, glycocalyx layers. Oncolites appeared in a result of active integration of the bacterial layers with the sediment (precipitate) and assimilation of the petrogenic components.https://www.geology-mgri.ru/jour/article/view/119ferromanganese stromatolitesoncolitesbacterial matsbacterial layers
spellingShingle V. V. Avdonin
E. A. Zhegallo
N. E. Sergeeva
Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
Известия высших учебных заведений: Геология и разведка
ferromanganese stromatolites
oncolites
bacterial mats
bacterial layers
title Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
title_full Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
title_fullStr Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
title_full_unstemmed Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
title_short Microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
title_sort microstructure of ferromanganese stromatolites and oncolites of the ocean bottom
topic ferromanganese stromatolites
oncolites
bacterial mats
bacterial layers
url https://www.geology-mgri.ru/jour/article/view/119
work_keys_str_mv AT vvavdonin microstructureofferromanganesestromatolitesandoncolitesoftheoceanbottom
AT eazhegallo microstructureofferromanganesestromatolitesandoncolitesoftheoceanbottom
AT nesergeeva microstructureofferromanganesestromatolitesandoncolitesoftheoceanbottom