Temperature Sensitivity of Forest Soils and Greenhouse Gas Fluxes

A special issue of Forests (ISSN 1999-4907). This special issue belongs to the section "Forest Soil".

Deadline for manuscript submissions: 21 April 2025 | Viewed by 156

Special Issue Editor


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Guest Editor
Institute of Environmental Sciences, Faculty of Biology, Jagiellonian University, Gronostajowa 7, 30-387 Kraków, Poland
Interests: forestry; soil science; ecological engineering

Special Issue Information

Dear Colleagues,

Heterotrophic soil respiration (R) is the second largest carbon (C) flux in terrestrial ecosystems after primary producer respiration. The decomposition of soil organic matter (SOM), mainly by soil microorganisms, is highly temperature-dependent. The increased release of carbon dioxide (CO2) and other greenhouse gases (GHG) from the soil to the atmosphere due to climate warming may further accelerate global climate change, a phenomenon known as positive feedback. Despite the decline in global forest cover, forest ecosystems contribute significantly to global organic carbon stocks. The temperature sensitivity of forest soils remains one of the key uncertainties in global climate change research. Therefore, this Special Issue focuses on soil temperature sensitivity in forest ecosystems.

Potential topics include, but are not limited to, the following:

- temperature sensitivity of different SOM fractions;

- temperature sensitivity along climatic gradients;

- changes in soil microbial abundance and diversity under experimental warming;

- temperature sensitivity of forest soils under anthropogenic disturbances;

- limiting factors for the respiration rate of forest soils;

- temperature adaptation of soil microbial respiration.

Dr. Beata Klimek
Guest Editor

Manuscript Submission Information

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Keywords

  • global warming
  • soil C stock
  • temperate and boreal forests
  • soil microorganisms
  • soil respiration rate

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Published Papers

This special issue is now open for submission.
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