Soil organic matter interactions along the elevation gradient of the James Ross Island (Antarctica)
Around half of the Earth’s soil organic carbon (SOC) is presently stored in the Northern permafrost region. In polar permafrost regions, low temperatures particularly inhibit both the production and biodegradation of organic matter. In such conditions, abiotic factors such as mesoclimate,...
Main Authors: | , , , , , , , , , , , |
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Format: | Text |
Language: | English |
Published: |
2024
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Subjects: | |
Online Access: | https://doi.org/10.5194/egusphere-2024-607 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-607/ |