Инд. авторы: Terleev A.A., Simonov V.A., Kanygin A.V., Tokarev D.A., Stupakov S.I., Kotlyarov A.V.
Заглавие: Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl-Tashtyg ore field (Eastern Tuva)
Библ. ссылка: Terleev A.A., Simonov V.A., Kanygin A.V., Tokarev D.A., Stupakov S.I., Kotlyarov A.V. Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl-Tashtyg ore field (Eastern Tuva) // Russian Geology and Geophysics. - 2014. - Vol.55. - Iss. 1. - P.54-61. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы: DOI: 10.1016/j.rgg.2013.12.004; РИНЦ: 21863503; SCOPUS: 2-s2.0-84892985089; WoS: 000330218200005;
Реферат: eng: Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl-Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal systems similar in characteristics to present-day 'black smokers' at ocean bottoms. Along with archaeocyaths and Cyanophyta from the host sedimentary rocks and microfossils from basalt amygdules, various cyanobacteria, monocyatheans, and sponge spicules have been found in ferrosiliceous deposits and metasedimentary rocks. Scanning electron microscopic, mineralogical, and thermobarogeochemical studies helped to reconstruct their hydrothermal environment. © 2013 V.S. Sobolev IGM, Siberian Branch of the RAS.
Ключевые слова: Cyanobacteria; Archaeocyatha; algae; Tuva; Russian Federation; sedimentary rock; scanning electron microscopy; pyrite; ore deposit; mineralogy; microfossil; hydrothermal deposit; host rock; cyanobacterium; Cambrian; biota; reconstruction;
Издано: 2014
Физ. характеристика: с.54-61