Non‐Native Earthworms Alter Carbon Sequestration in Arctic Tundra Ecosystems

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Abstract Earthworms, as detritivores, play a significant role in breaking down soil organic carbon (SOC). The introduction of non‐native earthworms to arctic ecosystems has, therefore, raised concerns about the potential impact they may have on one of the world's largest SOC reservoirs. Earthworms could also have considerable effects on plant productivity, and the lack of experimental studies quantifying their impact on carbon (C) reservoirs in both soil and plants makes it difficult to predict the effect of earthworms on ecosystem C storage. Here we experimentally tested how earthworms known to be non‐native to arctic ecosystems (Aporrectodea spp. and Lumbricus spp.) affect C reservoirs in soil and plants (above and belowground separately) in two common tundra vegetation types (heath and meadow). Earthworms lowered the mean SOC pool and substantially altered SOC quality in meadow soils by increasing the proportion of aromatic‐C compounds. Simultaneously, earthworms increased the C pool stored in plant biomass, which counteracted earthworm‐induced SOC losses in meadow ecosystems. A positive earthworm effect on belowground biomass in heath soil facilitated a net ecosystem uptake of ∼0.84 kg C m−2 over the 4‐year study period. The higher C uptake into plant biomass in the heath resulted in a notable increase of SOC but lower δ13C values, likely because of recently captured C being sourced from roots or litter. Our observations of vegetation‐specific feedbacks between plants, earthworms, and soils advance our understanding of non‐native earthworms' impact on SOC dynamics and C budgets in high‐latitude ecosystems.