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ABSTRACT: Background
pH is frequently reported as the main driver for prokaryotic community structure in soils. However, pH changes are also linked to "spillover effects" on other chemical parameters (e.g., availability of Al, Fe, Mn, Zn, and Cu) and plant growth, but these indirect effects on the microbial communities are rarely investigated. Usually, pH also co-varies with some confounding factors, such as land use, soil management (e.g., tillage and chemical inputs), plant cover, and/or edapho-climatic conditions. So, a more comprehensive analysis of the direct and indirect effects of pH brings a better understanding of the mechanisms driving prokaryotic (archaeal and bacterial) community structures.Results
We evaluated an agricultural soil pH gradient (from 4 to 6, the typical ra
SUBMITTER: Lammel DR
PROVIDER: S-EPMC5996553 | biostudies-literature | 2018 Jun
REPOSITORIES: biostudies-literature