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Abstract:
Soil microorganisms act as gatekeepers for soil–atmosphere carbon exchange by balancing
the accumulation and release of soil organic matter. However, poor understanding of the
mechanisms responsible hinders the development of effective land management strategies to
enhance soil carbon storage. Here we empirically test the link between microbial ecophysiological
traits and topsoil carbon content across geographically distributed soils and land
use contrasts. We discovered distinct pH controls on microbial mechanisms of carbon
accumulation. Land use intensification in low-pH soils that increased the pH above a
threshold (~6.2) leads to carbon loss through increased decomposition, following alleviation
of acid retardation of microbial growth. However, loss of carbon with intensification in nearneutral
pH soils was linked to decreased microbial biomass and reduced growth efficiency
that was, in turn, related to trade-offs with stress alleviation and resource acquisition. Thus,
less-intensive management practices in near-neutral pH soils have more potential for carbon
storage through increased microbial growth efficiency, whereas in acidic soils, microbial
growth is a bigger constraint on decomposition rates.
