Diagram representing the impacts of viruses on aqueous sediment geochemistry. Organic matter (OM) sinks to the sediments, which is cycled in the microbial community, as well as increasing abundance, diversity, activity, and degradation of OM. From this “microbial loop” recalcitrant dissolved organic matter (RDOM) and dissolved inorganic carbon (DIC) are stored in sediments. Carbon is also released into the atmosphere from the sediment, and viral infection transfers genes between hosts or releases exogenous DNA to be used by bacteria, potentially aiding in metabolic activity. Created in BioRender. Williams, J. (2026) https://BioRender.com/b4wqimp.
#MicrobiologyMonday: Marine sediments store vast amounts of carbon. By infecting and lysing microbes, viruses shape biogeochemical cycling from coastal zones to the deep sea and influence long-term carbon storage. Get the story in #AppEnvMicro: asm.social/2Qv