Shrub encroachment has emerged as a global phenomenon over the past century. Multiple drivers have been put forward to explain the increased shrub dominance in various ecosystems around the world. However, the potential role of phenology in regulating shrub encroachment is not well understood. We address this issue using 3-year continuous monitoring of the phenology of coexisting shrubs and grasses combined with observations of ecohydrological processes (water uptake) and soil conditions (root zone soil moisture, soil texture, and soil temperature) at four study sites in Inner Mongolia, China, with shrub coverage of Caragana microphylla ranging from 0%, to 6.8%, 26.8% and 34.2%. Along such an encroachment gradient, shrubs exhibited progressively earlier onsets and later ends of the growing season, with an overall extension in growing season length by 15 days to 22 days in the later stages of shrub encroachment. Conversely, the coexisting grasses showed earlier occurrences both in spring and autumn phenological phases, which resulted in a phenological gap between shrubs and grasses. Thus, a positive feedback could exist between these phenological changes and shrub encroachment. In shrub patches, soils were wetter, with finer texture, and with more suitable temperatures for plant survival and development, which favored the lengthening of growing season of shrubs. The longer growing seasons are associated with longer periods of water use and photosynthesis for shrubs, and better opportunities for water uptake, with the overall effect of facilitating shrub growth and further expansion.
Keywords: Caragana microphylla; Ecohydrology; Encroachment gradient; Soil moisture; Water uptake.
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