Microbial Diversity of Hypersaline Sediments from Lake Lucero Playa in White Sands National Monument, New Mexico, USA

被引:21
|
作者
Sirisena, Kosala Ayantha [1 ,2 ,3 ]
Ramirez, Steven [1 ]
Steele, Andrew [2 ]
Glamoclija, Mihaela [1 ]
机构
[1] Rutgers State Univ, Dept Earth & Environm Sci, Newark, NJ 07102 USA
[2] Carnegie Inst Sci, Geophys Lab, Washington, DC 20005 USA
[3] Univ Sri Jayewardenepura, Dept Zool, Nugegoda, Sri Lanka
关键词
Microbial diversity; Lake Lucero; Bacteria; Archaea; Eukaryotic microbes; Hypersaline sediment; Gypsiferous; EXTREMELY HALOPHILIC ARCHAEON; CYANOBACTERIUM EUHALOTHECE SP; SP NOV; GEN; NOV; HYDROTHERMAL SEDIMENTS; BACTERIAL DIVERSITY; MIKROCYTOS-MACKINI; MERIDIANI-PLANUM; ATACAMA DESERT; GYPSUM DUNES;
D O I
10.1007/s00248-018-1142-z
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Lake Lucero is a gypsum-rich, hypersaline, ephemeral playa located on the southern part of the Alkali Flat at the White Sands National Monument (WSNM), New Mexico, USA. This modern playa setting provides a dynamic extreme environment that changes from a freshwater lake to a hypersaline dry desert during the year. We investigated the microbial diversity (bacteria, archaea, and microbial eukaryotes) of the Lake Lucero sediments using 16S- and 18S-based amplicon sequencing approach and explored the diversity patterns in different geochemical microenvironments. Our results indicated that similar microbial communities, in particular bacterial communities colonized, were remarkably consistent across our depth profiles. Therefore, these communities show a first-order relevance on the environmental conditions (moisture content, oxygen content, and mineral composition). We found that Proteobacteria, Actinobacteria, Bacteroidetes, Firmicutes, and Gemmatimonadetes were the major bacterial phyla, while Cyanobacteria were present in relatively low abundances and appeared only at the surface. Genus level assessment reflected that Truepera, Delftia, and Pseudomonas were the predominant bacterial genera across all samples. Euryarchaeota was the major archaeal phylum in all the samples, while Candidatus Halobonum and Candidatus Nitrososphaera were the main genera. Diatoms were the dominant eukaryotic group in surface samples and Fungi, Ciliophora, Metazoa, and Nematodes were the other major groups. As expected, metabolic inference indicated that aerobic microbial communities were near surface colonizers, with anaerobic communities dominating with increasing depth. We demonstrated that these microbial communities could be used to characterize unique geochemical microenvironments enabling us to extrapolate these results into other terrestrial and possibly extraterrestrial environments with comparable geochemical characteristics.
引用
收藏
页码:404 / 418
页数:15
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