Cs enrichment controlled by microbial community: Evidence from sinters along a temperature gradient of the Daggyai Major Geyser, Tibet
Author:
Affiliation:
1. State Key Laboratory of Biogeology and Environmental Geology China University of Geosciences Wuhan China
2. Department of Earth and Atmospheric Sciences University of Alberta Edmonton Canada
Funder
National Natural Science Foundation of China
State Key Laboratory of Biogeology and Environmental Geology
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12600
Reference28 articles.
1. The influence of microbial mats on travertine precipitation in active hydrothermal systems (Central Italy)
2. The hot spring and geyser sinters of El Tatio, Northern Chile
3. Magmatic fluid input explaining the geochemical anomaly of very high arsenic in some southern Tibetan geothermal waters
4. Microbial biofacies in hot-spring sinters; a model based on Ohaaki Pool, North Island, New Zealand
5. Silicified Microbes in a Geyser Mound: The Enigma of Low-Temperature Cyanobacteria in a High-Temperature Setting
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