SOIL MICROBIAL RESPONSES TO CLIMATE CHANGE
One of the major current challenges for ecologists is to predict how ecosystems will function under the predicted range of future climates. Typically, ecologists extrapolate the relationships of temperature and moisture with the rates of various processes that occur in the soil (e.g. decomposition, N cycling) to estimate the rates of these processes under climate change. This approach assumes that these relationships are constant through time. For this assumption to be true, the microbial communities whose activity drives these soil processes either will not change in response to changing climate, or are functionally redundant. This assumption is in contrast to the generally accepted paradigm that plant, animal, and pathogen communities will shift in community composition and function in response to climate change. Our research examines whether microbial communities acclimate or adapt to changing climate. If they do, do the relationships between abiotic drivers and soil process rates also change?
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Funding: DOE Office of Science, National Institute for Climate Change Research (NICCR), USDA National Research Initiative (NRI), NSF Ecosystems