Soil bacteria are essential to reduce climate change and promote sustainability. These microbes have a significant role in improving soil health, cycling nutrients, and sequestering carbon, all of which lower greenhouse gas emissions. Soil bacteria help in carbon storage and atmospheric CO2 reduction by encouraging plant development and aiding in the breakdown of organic materials. Additionally, they strengthen the soil’s resistance to severe weather, which stabilizes ecosystems. Climate change mitigation can be greatly enhanced by utilizing the potential of soil bacteria through sustainable agricultural methods like biofertilizers and bioremediation. This concluding chapter emphasizes the necessity for more research to maximize the function of soil microbial communities in climate change methods and emphasizes the need to comprehend and utilize these communities to achieve long-term environmental sustainability.

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Soil Microbiota as Key Players in Mitigating Climate Change and Achieving a Sustainable Environment: A Conclusion

  • Rajnanda Thaosen,
  • Dona Mazumder,
  • Nandita Das,
  • Piyush Pandey

摘要

Soil bacteria are essential to reduce climate change and promote sustainability. These microbes have a significant role in improving soil health, cycling nutrients, and sequestering carbon, all of which lower greenhouse gas emissions. Soil bacteria help in carbon storage and atmospheric CO2 reduction by encouraging plant development and aiding in the breakdown of organic materials. Additionally, they strengthen the soil’s resistance to severe weather, which stabilizes ecosystems. Climate change mitigation can be greatly enhanced by utilizing the potential of soil bacteria through sustainable agricultural methods like biofertilizers and bioremediation. This concluding chapter emphasizes the necessity for more research to maximize the function of soil microbial communities in climate change methods and emphasizes the need to comprehend and utilize these communities to achieve long-term environmental sustainability.