Bacterial mats of the oxide ores in the world ocean
Bacterial mats, formed by successively accumulating biofilms, are the main constructive component of the oxide ferromanganese ores on the oceanic floor. The coordinated behavior of the bacterial colonies in the biofilms controlled the growth of the stromatolites and onkolites structures. Biofilms of...
Main Authors: | , , |
---|---|
Format: | Article |
Language: | Russian |
Published: |
Sergo Ordzhonikidze Russian State University for Geological Prospecting
2017-08-01
|
Series: | Известия высших учебных заведений: Геология и разведка |
Subjects: | |
Online Access: | https://geology.mgri-rggru.ru/jour/article/view/244 |
id |
doaj-74de5c0602a5450fbe01303d1ab52fd2 |
---|---|
record_format |
Article |
spelling |
doaj-74de5c0602a5450fbe01303d1ab52fd22021-01-12T06:04:23ZrusSergo Ordzhonikidze Russian State University for Geological ProspectingИзвестия высших учебных заведений: Геология и разведка0016-77622618-87082017-08-0104454910.32454/0016-7762-2017-4-45-49244Bacterial mats of the oxide ores in the world oceanV. V. Avdonin0E. A. Zhegallo1N. E. Sergeeva2Lomonosov Moscow State UniversityBorissiak Paleontological Institute of the Russian Academy of SciencesLomonosov Moscow State UniversityBacterial mats, formed by successively accumulating biofilms, are the main constructive component of the oxide ferromanganese ores on the oceanic floor. The coordinated behavior of the bacterial colonies in the biofilms controlled the growth of the stromatolites and onkolites structures. Biofilms of the stromatolite bacterial mats represent the microbial community, with the thread bacteria forming a poiygonal network that determines a piliar structure of the crusts. Bacterial mats in nodules are festoon-shaped. Biofilms in festoons intensely interact with the environment, assimilating petrogenic components and consuming the sedimentary material.https://geology.mgri-rggru.ru/jour/article/view/244oxide oresbacterial matsbiofilmsthread bacteria |
collection |
DOAJ |
language |
Russian |
format |
Article |
sources |
DOAJ |
author |
V. V. Avdonin E. A. Zhegallo N. E. Sergeeva |
spellingShingle |
V. V. Avdonin E. A. Zhegallo N. E. Sergeeva Bacterial mats of the oxide ores in the world ocean Известия высших учебных заведений: Геология и разведка oxide ores bacterial mats biofilms thread bacteria |
author_facet |
V. V. Avdonin E. A. Zhegallo N. E. Sergeeva |
author_sort |
V. V. Avdonin |
title |
Bacterial mats of the oxide ores in the world ocean |
title_short |
Bacterial mats of the oxide ores in the world ocean |
title_full |
Bacterial mats of the oxide ores in the world ocean |
title_fullStr |
Bacterial mats of the oxide ores in the world ocean |
title_full_unstemmed |
Bacterial mats of the oxide ores in the world ocean |
title_sort |
bacterial mats of the oxide ores in the world ocean |
publisher |
Sergo Ordzhonikidze Russian State University for Geological Prospecting |
series |
Известия высших учебных заведений: Геология и разведка |
issn |
0016-7762 2618-8708 |
publishDate |
2017-08-01 |
description |
Bacterial mats, formed by successively accumulating biofilms, are the main constructive component of the oxide ferromanganese ores on the oceanic floor. The coordinated behavior of the bacterial colonies in the biofilms controlled the growth of the stromatolites and onkolites structures. Biofilms of the stromatolite bacterial mats represent the microbial community, with the thread bacteria forming a poiygonal network that determines a piliar structure of the crusts. Bacterial mats in nodules are festoon-shaped. Biofilms in festoons intensely interact with the environment, assimilating petrogenic components and consuming the sedimentary material. |
topic |
oxide ores bacterial mats biofilms thread bacteria |
url |
https://geology.mgri-rggru.ru/jour/article/view/244 |
work_keys_str_mv |
AT vvavdonin bacterialmatsoftheoxideoresintheworldocean AT eazhegallo bacterialmatsoftheoxideoresintheworldocean AT nesergeeva bacterialmatsoftheoxideoresintheworldocean |
_version_ |
1724340671210323968 |