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, pedogenic...

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Bibliographic Details
Main Authors: Vlcek, Vitezslav, Juřička, David, Valtera, Martin, Dvořáčková, Helena, Štulc, Vojtěch, Bednaříková, Michaela, Šimečková, Jana, Váczi, Peter, Pohanka, Miroslav, Kapler, Pavel, Barták, Miloš, Enev, Vojtěch
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-607
https://noa.gwlb.de/receive/cop_mods_00072274
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00070496/egusphere-2024-607.pdf
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-607/egusphere-2024-607.pdf