"Knowing the composition and turnover of viral communities across space and time is necessary to begin unraveling what constrains host-virus interactions in soil," said LLNL scientist and co-author Jennifer Pett-Ridge. "We found that the soil 'virosphere' is highly diverse, dynamic, active and spatially structured; it also appears to be capable of rapid responses to changing environmental conditions, particularly the amount of rainfall."
Soils are physically, chemically and biologically heterogeneous. The intricate network of aggregates and pore spaces that constitute the soil matrix not only sustains a varying landscape of properties but also restricts the movement of microorganisms.
Through infection and mortality of other microbiota, viruses have countless effects on host metabolism, evolution and Earth's biogeochemical cycles. The sheer abundance of soil viruses hints at their likely importance in terrestrial ecosystems.
Previous rainfall manipulation experiments have shown that reduced precipitation can reshape soil bacterial community composition. Until recently, it was not known whether these shifts might be coupled to changes in the soil virosphere, although recent observations suggest that water availability could be a major driver of soil viral community assembly.
In the new research, the team found that viruses adapt more rapidly than their microbial hosts when exposed to climate changes such as drought. As soil moisture decreased, the viral community composition shifted and types of viruses that are predicted to infect drought-adapted actinobacteria became more dominant.
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