Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.5194/bg-16-1133-2019 |
The origin and role of biological rock crusts in rocky desert weathering | |
Wieler, Nimrod1; Ginat, Hanan2; Gillor, Osnat1; Angel, Roey3,4 | |
通讯作者 | Gillor, Osnat ; Angel, Roey |
来源期刊 | BIOGEOSCIENCES
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ISSN | 1726-4170 |
EISSN | 1726-4189 |
出版年 | 2019 |
卷号 | 16期号:6页码:1133-1145 |
英文摘要 | In drylands, microbes that colonize rock surfaces have been linked to erosion because water scarcity excludes traditional weathering mechanisms. We studied the origin and role of rock biofilms in geomorphic processes of hard lime and dolomitic rocks that feature comparable weathering morphologies, although these two rock types originate from arid and hyperarid environments, respectively. We hypothesized that weathering patterns are fashioned by salt erosion and mediated by the rock biofilms that originate from the adjacent soil and dust. We used a combination of microbial and geological techniques to characterize rock morphologies and the origin and diversity of their biofilms. Amplicon sequencing of the SSU rRNA gene suggested that bacterial diversity is low and dominated by Proteobacteria and Actinobacteria. These phyla only formed laminar biofilms on rock surfaces that were exposed to the atmosphere and burrowed up to 6 mm beneath the surface, protected by sedimentary deposits. Unexpectedly, the microbial composition of the biofilms differed between the two rock types and was also distinct from the communities identified in the adjacent soil and settled dust, showing a habitat-specific filtering effect. Moreover, the rock bacterial communities were shown to secrete extracellular polymeric substances (EPSs) that form an evaporation barrier, reducing water loss rates by 65 %75 %. The reduced water transport rates through the rock also limit salt transport and its crystallization in surface pores, which is thought to be the main force for weathering. Concomitantly, the biofilm layer stabilizes the rock surface via coating and protects the weathered front. Our hypothesis contradicts common models, which typically consider biofilms to be agents that promote weathering. In contrast, we propose that the microbial colonization of mineral surfaces acts to mitigate geomorphic processes in hot, arid environments. |
类型 | Article |
语种 | 英语 |
国家 | Israel ; Czech Republic |
开放获取类型 | Green Submitted, gold |
收录类别 | SCI-E |
WOS记录号 | WOS:000461618700003 |
WOS关键词 | LABORATORY SIMULATION ; MICROBIAL COLONIZATION ; NAMIB DESERT ; BACTERIAL ; CRYSTALLIZATION ; SURFACES ; DESICCATION ; SANDSTONE ; NEGEV ; LIFE |
WOS类目 | Ecology ; Geosciences, Multidisciplinary |
WOS研究方向 | Environmental Sciences & Ecology ; Geology |
来源机构 | Ben-Gurion University of the Negev |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/214606 |
作者单位 | 1.Ben Gurion Univ Negev, Blaustein Inst Desert Res, Zuckerberg Inst Water Res, Sede Boqer Campus, Beer Sheva, Israel; 2.Dead Sea & Arava Sci Ctr, Dead Sea, Israel; 3.Biol Ctr CAS, Soil & Water Res Infrastruct, Prague, Czech Republic; 4.Biol Ctr CAS, Inst Soil Biol, Prague, Czech Republic |
推荐引用方式 GB/T 7714 | Wieler, Nimrod,Ginat, Hanan,Gillor, Osnat,et al. The origin and role of biological rock crusts in rocky desert weathering[J]. Ben-Gurion University of the Negev,2019,16(6):1133-1145. |
APA | Wieler, Nimrod,Ginat, Hanan,Gillor, Osnat,&Angel, Roey.(2019).The origin and role of biological rock crusts in rocky desert weathering.BIOGEOSCIENCES,16(6),1133-1145. |
MLA | Wieler, Nimrod,et al."The origin and role of biological rock crusts in rocky desert weathering".BIOGEOSCIENCES 16.6(2019):1133-1145. |
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