Abstract

The globally expanding colonization of grasslands by shrubs increases soil organic carbon and nitrogen, but the effects of shrubs on phosphorus (P) cycling have been rarely studied. We compared P contents in roots and soil fractions, phosphatase activity in the 1 m profile, and in situ net P mineralization between shrubby Potentilla fruticosa patches and grassy interspaces in grazed shrubby meadows at three representative sites on the eastern Tibetan Plateau. The P uptake of P. fruticosa exceeded 1 m soil depth, whereas grasses acquired P mainly within the upper 0.6 m. The P contents in shoots, aboveground litter and roots under P. fruticosa were greater than those under grasses. Litter P stock under the shrubs was 4–8 times higher than that under grasses and the root P stock doubled compared to that in grass areas. P. fruticosa generally increased the organic P (OP) content in the topsoil but decreased inorganic P (IP) in the subsoil. Phosphorus availability increased in the topsoil but decreased in the subsoil under the shrubs compared to grasses. Microbial biomass P (MBP), the activities of acid and alkaline phosphatases, and OP lability were all greater in the 1 m soil under P. fruticosa than grasses, leading to faster P mineralization and the P turnover under the shrubs. In the 1 m soil, P. fruticosa increased MBP and OP stocks but decreased IP and available P stocks. The larger and deeply distributed root system of P. fruticosa improved its P uptake ability especially from the subsoil. The subsequent greater organic matter input through litter fall and root turnover under P. fruticosa fed a larger microbial biomass that synthesized more microbial-derived OP in the topsoil. We concluded that shrubs increase the biological (plant and microbial) P transformation in the soil, the P uplift in the profile, and P cycling in shrubby grassland ecosystems. Such mechanisms structuring spatial heterogeneity of P content, transformation, turnover and fluxes are common in shrubby grasslands worldwide.

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