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气候和坡向对智利沿海山脉成土过程中土壤细菌群落组成的影响

Impact of Climate and Slope Aspects on the Composition of Soil Bacterial Communities Involved in Pedogenetic Processes along the Chilean Coastal Cordillera.

作者信息

Rodriguez Victoria, Moskwa Lisa-Marie, Oses Rómulo, Kühn Peter, Riveras-Muñoz Nicolás, Seguel Oscar, Scholten Thomas, Wagner Dirk

机构信息

GFZ German Research Centre for Geosciences, Section Geomicrobiology, 14473 Potsdam, Germany.

Centro Regional de Investigación y Desarrollo Sustentable de Atacama, Universidad de Atacama (CRIDESAT UDA), Copayapu 484, Copiapó 1530000, Chile.

出版信息

Microorganisms. 2022 Apr 20;10(5):847. doi: 10.3390/microorganisms10050847.

Abstract

Soil bacteria play a fundamental role in pedogenesis. However, knowledge about both the impact of climate and slope aspects on microbial communities and the consequences of these items in pedogenesis is lacking. Therefore, soil-bacterial communities from four sites and two different aspects along the climate gradient of the Chilean Coastal Cordillera were investigated. Using a combination of microbiological and physicochemical methods, soils that developed in arid, semi-arid, mediterranean, and humid climates were analyzed. , , , , and were found to increase in abundance from arid to humid climates, while and decreased along the transect. Bacterial-community structure varied with climate and aspect and was influenced by pH, bulk density, plant-available phosphorus, clay, and total organic-matter content. Higher bacterial specialization was found in arid and humid climates and on the south-facing slope and was likely promoted by stable microclimatic conditions. The presence of specialists was associated with ecosystem-functional traits, which shifted from pioneers that accumulated organic matter in arid climates to organic decomposers in humid climates. These findings provide new perspectives on how climate and slope aspects influence the composition and functional capabilities of bacteria, with most of these capabilities being involved in pedogenetic processes.

摘要

土壤细菌在土壤发生过程中起着基础性作用。然而,关于气候和坡面朝向对微生物群落的影响以及这些因素在土壤发生过程中的后果,目前仍缺乏相关知识。因此,对智利海岸山脉气候梯度上四个地点和两个不同坡面的土壤细菌群落进行了调查。采用微生物学和物理化学方法相结合的方式,对在干旱、半干旱、地中海和湿润气候条件下发育的土壤进行了分析。结果发现,[具体物种1]、[具体物种2]、[具体物种3]、[具体物种4]和[具体物种5]的丰度从干旱气候到湿润气候逐渐增加,而[具体物种6]和[具体物种7]则沿样带减少。细菌群落结构随气候和坡面朝向而变化,并受到pH值、容重、植物有效磷、黏土和总有机质含量的影响。在干旱和湿润气候以及朝南的坡面上发现了更高的细菌特异性,这可能是由稳定的微气候条件促进的。特有物种的存在与生态系统功能特征相关,这些特征从干旱气候下积累有机质的先锋物种转变为湿润气候下的有机分解者。这些发现为气候和坡面朝向如何影响细菌的组成和功能能力提供了新的视角,其中大多数能力都参与了土壤发生过程。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/46db/9143490/f76cf714b33e/microorganisms-10-00847-g001.jpg

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