Sulfur Cave (Romania), an extreme environment with microbial mats in a CO2-H2S/O2 gas chemocline dominated by mycobacteria

Autor: Casey Barr, Reka Incze, Nicu-Viorel Atudorei, Serban M. Sarbu, Calin Baciu, Rob J.M. van Spanning, Jean-François Flot, Emily J. Fleming, Sándor Sikó-Barabási, Radu Popa, Kenneth H. Nealson, Boglárka-Mercedesz Kis, Botond Hegyeli, Artur Ionescu, Zoltan Para, Ferenc L. Forray, Wilbert Bitter, Cristian Lascu, Joost W. Aerts
Přispěvatelé: Molecular Cell Physiology, AIMMS, Systems Bioinformatics, Molecular Microbiology, Medical Microbiology and Infection Prevention, AII - Infectious diseases
Jazyk: angličtina
Rok vydání: 2018
Předmět:
Zdroj: International Journal of Speleology, Vol 47, Iss 2, Pp 173-187 (2018)
Sarbu, S M, Aerts, J W, Flot, J-F, van Spanning, R J M, Baciu, C, Ionescu, A, Kis, B M, Incze, R, Siko-Barabasi, S, Para, Z, Hegyeli, B, Atudorei, N-V, Barr, C, Nealson, K H, Forray, F L, Lascu, C, Fleming, E J, Bitter, W & Popa, R 2018, ' Sulfur cave (Romania), an extreme environment with microbial mats in a Co2-H2S/O2 gas chemocline dominated by mycobacteria ', International Journal of Speleology, vol. 47, no. 2, pp. 173-187 . https://doi.org/10.5038/1827-806X.47.2.2164
International Journal of Speleology, 47(2), 173-187. Societa Speleologica Italiana
Sarbu, S M, Aerts, J W, Flot, J F, van Spanning, R J M, Baciu, C, Ionescu, A, Kis, B M, Incze, R, Siko-Barabasi, S, Para, Z, Hegyeli, B, Atudorei, N V, Barr, C, Nealson, K H, Forray, F L, Lascu, C, Fleming, E J, Bitter, W & Popa, R 2018, ' Sulfur cave (Romania), an extreme environment with microbial mats in a Co 2-H 2 S/O 2 gas chemocline dominated by mycobacteria ', International Journal of Speleology, vol. 47, no. 2, pp. 173-187 . https://doi.org/10.5038/1827-806X.47.2.2164
International Journal of Speleology, 47 (2
ISSN: 0392-6672
DOI: 10.5038/1827-806X.47.2.2164
Popis: Sulfur Cave (Puturosu Mountain, Romania) is an extreme environment, unique for displaying life in a gas chemocline. The lower part of the cave is filled with CO2, CH4, and H2S of mofettic origin, while the upper part contains air that floats above the heavier volcanic gasses. S° and H2SO4 (from sulfur-oxidation) cover the cave wall at and below the CO2-H2S:O2 gas/gas interface. On the cave wall, near the interface the pH is
SCOPUS: ar.j
info:eu-repo/semantics/published
Databáze: OpenAIRE