Abstract
AbstractViruses are abundant, ubiquitous members of soil communities that kill microbial cells, but how they respond to perturbation of soil ecosystems is essentially unknown. Here, we investigated lineage-specific virus-host dynamics in grassland soil following “wet-up”, when resident microbes are both resuscitated and lysed after a prolonged dry period. Quantitative isotope tracing, time-resolved metagenomics and viromic analyses indicated that dry soil held a diverse but low biomass reservoir of virions, of which only a subset thrived following wet-up. Viral richness decreased by 50% within 24 h post wet-up, while viral biomass increased four-fold within one week. Counter to recent hypotheses suggesting temperate viruses predominate in soil, our evidence indicates that wet-up is dominated by viruses in lytic cycles. We estimate that viruses drive a measurable and continuous rate of cell lysis, with up to 46% of microbial death driven by viral lysis one week following wet-up. Thus, viruses contribute to turnover of soil microbial biomass and the widely reported CO2efflux following wet-up of seasonally dry soils.
Publisher
Cold Spring Harbor Laboratory
Cited by
3 articles.
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