Archaeal Communities in a Heterogeneous Hypersaline-Alkaline Soil.

IF 4.6 Q2 MATERIALS SCIENCE, BIOMATERIALS ACS Applied Bio Materials Pub Date : 2015-05-13 eCollection Date: 2015-01-01 DOI:10.1155/2015/646820
Yendi E Navarro-Noya, César Valenzuela-Encinas, Alonso Sandoval-Yuriar, Norma G Jiménez-Bueno, Rodolfo Marsch, Luc Dendooven
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引用次数: 23

Abstract

In this study the archaeal communities in extreme saline-alkaline soils of the former lake Texcoco, Mexico, with electrolytic conductivities (EC) ranging from 0.7 to 157.2 dS/m and pH from 8.5 to 10.5 were explored. Archaeal communities in the 0.7 dS/m pH 8.5 soil had the lowest alpha diversity values and were dominated by a limited number of phylotypes belonging to the mesophilic Candidatus Nitrososphaera. Diversity and species richness were higher in the soils with EC between 9.0 and 157.2 dS/m. The majority of OTUs detected in the hypersaline soil were members of the Halobacteriaceae family. Novel phylogenetic branches in the Halobacteriales class were detected in the soil, and more abundantly in soil with the higher pH (10.5), indicating that unknown and uncharacterized Archaea can be found in this soil. Thirteen different genera of the Halobacteriaceae family were identified and were distributed differently between the soils. Halobiforma, Halostagnicola, Haloterrigena, and Natronomonas were found in all soil samples. Methanogenic archaea were found only in soil with pH between 10.0 and 10.3. Retrieved methanogenic archaea belonged to the Methanosarcinales and Methanomicrobiales orders. The comparison of the archaeal community structures considering phylogenetic information (UniFrac distances) clearly clustered the communities by pH.

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非均质高盐碱土壤中的古细菌群落。
本文对墨西哥原特克斯科科湖极盐碱土壤中电解电导率(EC)为0.7 ~ 157.2 dS/m、pH值为8.5 ~ 10.5的古细菌群落进行了研究。0.7 dS/m pH 8.5土壤中古细菌群落的α多样性值最低,并以属于中温性Candidatus Nitrososphaera的有限种型为主。EC值为9.0 ~ 157.2 dS/m的土壤多样性和物种丰富度较高。在高盐土壤中检测到的大部分OTUs是盐杆菌科的成员。在土壤中发现了新的系统发育分支,且在pH值较高(10.5)的土壤中更为丰富,表明该土壤中可能存在未知和未鉴定的古细菌。鉴定出盐杆菌科13个不同属,在土壤中分布不同。在所有土壤样品中均发现有盐生菌、盐生菌、盐生菌和钠单胞菌。产甲烷古菌仅存在于pH值为10.0 ~ 10.3的土壤中。检索到的产甲烷古生菌属于产甲烷亚目和产甲烷微生物亚目。考虑系统发育信息(UniFrac距离)的古细菌群落结构比较清楚地显示了pH对群落的聚集。
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来源期刊
ACS Applied Bio Materials
ACS Applied Bio Materials Chemistry-Chemistry (all)
CiteScore
9.40
自引率
2.10%
发文量
464
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