Microbial Diversity in Water and Sediment of Lake Chaka, an Athalassohaline Lake in Northwestern China

• DOI: 10.1128/aem.02869-05
• Publication Date: 2006-06-02T20:36:26Z
• Authors: Hongchen Jiang; Hailiang Dong; Gengxin Zhang; Bingsong Yu; Leah R. Chapman; Matthew W. Fields
• Keywords: 0301 basic medicine; China; Geologic Sediments; 0303 health sciences; Base Sequence; Molecular Sequence Data; Magnesium Chloride; Temperature; Water; Hydrogen-Ion Concentration; Sodium Chloride; Gram-Positive Bacteria; 6. Clean water; 03 medical and health sciences; 13. Climate action; Bacteroides; Cloning, Molecular; Water Microbiology; Phylogeny; DNA Primers

ABSTRACTWe employed culture-dependent and -independent techniques to study microbial diversity in Lake Chaka, a unique hypersaline lake (32.5% salinity) in northwest China. It is situated at 3,214 m above sea level in a dry climate. The average water depth is 2 to 3 cm. Halophilic isolates were obtained from the lake water, and halotolerant isolates were obtained from the shallow sediment. The isolates exhibited resistance to UV and gamma radiation. Microbial abundance in the sediments ranged from 108cells/g at the water-sediment interface to 107cells/g at a sediment depth of 42 cm. A major change in the bacterial community composition was observed across the interface. In the lake water, clone sequences affiliated with theBacteroideteswere the most abundant, whereas in the sediments, sequences related to low G+C gram-positive bacteria were predominant. A similar change was also present in the archaeal community. While all archaeal clone sequences in the lake water belonged to theHalobacteriales, the majority of the sequences in the sediments were related to those previously obtained from methanogenic soils and sediments. The observed changes in the microbial community structure across the water-sediment interface were correlated with a decrease in salinity from the lake water (32.5%) to the sediments (approximately 4%). Across the interface, the redox state also changed from oxic to anoxic and may also have contributed to the observed shift in the microbial community.