Journal
PLOS ONE
Volume 8, Issue 5, Pages -Publisher
PUBLIC LIBRARY SCIENCE
DOI: 10.1371/journal.pone.0062901
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Funding
- National Natural Science Foundation grants of China [41030211, 41002123, 40972211]
- Key Project of International Cooperation of China Ministry of Science & Technology (MOST) [2013DFA31980]
- Scientific Research Funds for the 1000 Talents'' Program Plan from China University of Geosciences-Beijing
- Tongji University
- National Science Foundation [OISE-0968421, DBI REU 1005223, ETBC-1024614]
- Program for New Century Excellent Talents in University [NCET-12-0954]
- Directorate For Geosciences
- Division Of Earth Sciences [1024614] Funding Source: National Science Foundation
- Office Of The Director
- Office Of Internatl Science &Engineering [968421] Funding Source: National Science Foundation
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The Tibetan Plateau in Northwest China hosts a number of hot springs that represent a biodiversity hotspot for thermophiles, yet their diversity and relationship to environmental conditions are poorly explored in these habitats. In this study we investigated microbial diversity and community composition in 13 Tibetan hot springs with a wide range of temperatures (22.1-75 degrees C) and other geochemical conditions by using the 16S rRNA gene pyrosequencing approach. Bacteria (10(8)-10(11) copy/g; 42 bacterial phyla) in Tibetan hot springs were more abundant and far more diverse than Archaea (10(7)-10(10) copy/g; 5 archaeal phyla). The dominant bacterial phyla systematically varied with temperature. Moderate temperatures (75-66 degrees C) favored Aquificae, GAL35, and novel Bacteria, whereas low temperatures (60-22.1 degrees C) selected for Deinococcus-Thermus, Cyanobacteria, and Chloroflexi. The relative abundance of Aquificae was correlated positively with temperature, but the abundances of Deinococcus-Thermus, Cyanobacteria, and Chloroflexi were negatively correlated with temperature. Cyanobacteria and Chloroflexi were abundant in Tibetan hot springs and their abundances were positively correlated at low temperatures (55-43 degrees C) but negatively correlated at moderate temperatures (75-55 degrees C). These correlation patterns suggest a complex physiological relationship between these two phyla. Most archaeal sequences were related to Crenarchaeota with only a few related to Euryarchaeota and Thaumarchaeota. Despite the fact that microbial composition in Tibetan hot springs was strongly shaped by temperature, microbial diversity (richness, evenness and Shannon diversity) was not significantly correlated with temperature change. The results of this study expand our current understanding of microbial ecology in Tibetan hot springs and provide a basis for a global comparison.
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