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This article in SSSAJ

  1. Vol. 61 No. 2, p. 475-481
     
    Received: Nov 15, 1995
    Published: Mar, 1997


    * Corresponding author(s): zogg@umich.edu
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doi:10.2136/sssaj1997.03615995006100020015x

Compositional and Functional Shifts in Microbial Communities Due to Soil Warming

  1. Gregory P. Zogg ,
  2. Donald R. Zak,
  3. David B. Ringelberg,
  4. David C. White,
  5. Neil W. MacDonald and
  6. Kurt S. Pregitzer
  1. School of Natural Resources and Environment, Univ. of Michigan, Ann Arbor, MI 48109-1115
    Center for Environmental Biotechnology, Univ. of Tennessee, Knoxville, TN 37932-2575
    Biology Dep., Grand Valley State Univ., Allendale, MI 49401-9403
    School of Forestry, Michigan Technological Univ., Houghton, MI 49931

Abstract

Abstract

Microbial decomposition processes are typically described using first-order kinetics, and the effect of elevated temperature is modeled as an increase in the rate constant. However, there is experimental data to suggest that temperature increases the pool size of substrate C available for microbial respiration with little effect on first-order rate constants. We reasoned that changes in soil temperature alter the composition of microbial communities, wherein dominant populations at higher temperatures have the ability to metabolize substrates that are not used by members of the microbial community at lower temperatures. To gain insight into changes in microbial community composition and function following soil warming, we used molecular techniques of phospholipid fatty acid (PLFA) and lipopolysaccharide fatty acid (LPS-OHFA) analysis and compared the kinetics of microbial respiration for soils incubated from 5 to 25°C. Substrate pools for microbial respiration and the abundance of PLFA and LPS-OHFA biomarkers for Gram-positive and Gram-negative bacteria differed significantly among temperature treatments, providing evidence for a shift in the function and composition of microbial communities related to soil warming. We suggest that shifts in microbial community composition following either large seasonal variation in soil temperature or smaller annual increases associated with global climate change have the potential to alter patterns of soil organic matter decomposition by a mechanism that is not considered by current simulation models.

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