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Soil microbial diversity significantly impacts carbon cycling and CO2 emissions. Reduced diversity accelerates the decomposition of easily degradable carbon sources, highlighting the importance of preserving soil biodiversity.

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Area of Science:

  • Soil Ecology
  • Microbial Ecology
  • Biogeochemistry

Background:

  • Functional redundancy in soil microbial communities challenges the direct link between microbial diversity and carbon transformations.
  • The relationship between microbial diversity and soil carbon cycling is not fully understood, particularly concerning different carbon source types.

Purpose of the Study:

  • To investigate how decreasing microbial diversity affects the decomposition of easily degradable (allochthonous) versus recalcitrant (autochthonous) carbon sources.
  • To test the hypothesis that functional redundancy decreases with increasing carbon source recalcitrance, altering the diversity-carbon cycling relationship.

Main Methods:

  • Manipulated microbial diversity in controlled laboratory experiments.
  • Assessed the decomposition rates of allochthonous and autochthonous carbon sources under varying diversity levels.
  • Measured global carbon dioxide (CO2) emissions as an indicator of decomposition.

Main Results:

  • A decrease in microbial diversity significantly affected the decomposition of both autochthonous and allochthonous carbon sources.
  • Reduced microbial diversity led to a decrease in overall CO2 emissions by up to 40%.
  • Lower diversity shifted CO2 emissions towards the preferential decomposition of more degradable carbon sources, with effects amplified by nutrient availability.

Conclusions:

  • Soil carbon cycling is more sensitive to microbial diversity changes than previously thought, especially in nutrient-rich environments.
  • Preserving soil microbial diversity is crucial for maintaining soil ecosystem services, including carbon storage, particularly under global change scenarios.
  • Findings underscore the importance of microbial diversity for organic matter decomposition and soil carbon dynamics.