The apparent disparity in reaction to climate change will assuredly result in shifts in community composition. Water stress in warm seasons may favor C4 species, while increased CO2 availability may favor C3 species, and nitrogen-fixing plants and their associates may also fare better in increased CO2 conditions. Individualized responses to climate change will likely result in shifting ranges for most species, but does not guarantee the perpetuation of existing plant associations or community assemblages (Jones n.d.). I predict that the most dramatic changes in grassland ecosystems will occur in tropical, arid, and semi-arid regions which are slated to receive the double-whammy of increased temperatures and decreased precipitation. Many regions around the world are projected to receive less precipitation during critical growing periods with a concomitant increase in average temperatures. Despite the boost in photosynthetic capacity, increasing water stress as well as high temperatures which impair plant production may offset any increased vegetative production (Jones n.d.). The next few decades are likely to see southern grasslands shrink as deserts expand their boundaries while northern grasslands grow as temperature, drought, and insect pressures thin existing forests under the new climate regime.
Jones MB. n.d. The impacts of global climate change on grassland ecosystems. Climate Change: Implications and Role of Grasslands:181–188.
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