Элементный состав матов минеральных источников Байкальской рифтовой зоны
| Parent link: | Геохимия живого вещества: международная молодежная школа-семинар, посвященная 150-летию со дня рождения В. И. Вернадского (1863-2013), Томск, 2-5 июня 2013 г./ Национальный исследовательский Томский политехнический университет (ТПУ) ; Российская академия наук (РАН), Институт геохимии и аналитической химии (ГЕОХИ) ; Российское геологическое общество (РосГео), Томское региональное отделение. [С. 169-172].— , 2013 |
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| Summary: | Заглавие с титульного листа The Baikal rift area is characterized by a rich variety of mineral springs. The research of microbial communities has been started quite recently, but there is a lot of information showing the important role of microbial communities of hot springs in the evolution of life in the Precambrian [1]. The complex studies in thermal springs have shown that severe environmental conditions (high temperature, alkaline pH and high sulfide content) contribute to the development of specific microbial communities, having significant biodiversity and high intensity of biogeochemical processes, comparable to the microbial communities of neutral thermal spring. The main feature of these communities is the formation of microbial mats. The mats are biocoenosis composed of prokaryotes and located at the bottom of ponds or in the shore area. The shape of mats is the most similar to films of mould. The ancient bacterial mats were the only biocoenosis on the Earth. Currently, bacterial mats are the most common in hot springs |
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2013
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| Online Access: | http://www.lib.tpu.ru/fulltext/c/2013/C32/034.pdf |
| Format: | Electronic Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=242271 |