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No depth-dependence of fine root litter decomposition in temperate beech forest soils

Solly, Emily ; Schöning, Ingo ; Herold, Nadine ; Trumbore, Susan ; Schrumpf, Marion

In: Plant and Soil, 2015, vol. 393, no. 1-2, p. 273-282

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    Titel
    • No depth-dependence of fine root litter decomposition in temperate beech forest soils
    Autor
    • Solly, Emily. Max Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, 07745, Jena, Germany
    • Schöning, Ingo. Max Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, 07745, Jena, Germany
    • Herold, Nadine. Max Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, 07745, Jena, Germany
    • Trumbore, Susan. Max Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, 07745, Jena, Germany
    • Schrumpf, Marion. Max Planck Institute for Biogeochemistry, Hans-Knöll-Str. 10, 07745, Jena, Germany
    Dokumententyp
    • Postprint
    Sprache
    • Englisch
    Veröffentlicht in
    • Plant and Soil, 2015, vol. 393, no. 1-2, p. 273-282. Springer International Publishing
    Andere elektronische Ausgabe
    OAI-PMH-ID
    • oai:doc.rero.ch:332617
    Summary
    Aims: Subsoil organic carbon (OC) tends to be older and is presumed to be more stable than topsoil OC, but the reasons for this are not yet resolved. One hypothesis is that decomposition rates decrease with increasing soil depth. We tested whether decomposition rates of beech fine root litter varied with depth for a range of soils using a litterbag experiment in German beech forest plots. Methods: In three study regions (Schorfheide-Chorin, Hainich-Dün and Schwäbische-Alb), we buried 432 litterbags containing 0.5g of standardized beech root material (fine roots with a similar chemical composition collected from 2year old Fagus sylvatica L. saplings, root diameter < 2mm) at three different soil depths (5, 20 and 35cm). The decomposition rates as well as the changes in the carbon (C) and nitrogen (N) concentrations of the decomposing fine root litter were determined at a 6months interval during a 2years field experiment. Results: The amount of root litter remaining after 2years of field incubation differed between the study regions (76 ± 2% in Schorfheide-Chorin, 85 ± 2% in Schwäbische-Alb, and 88 ± 2% in Hainich-Dün) but did not vary with soil depth. Conclusions: Our results indicate that the initial fine root decomposition rates are more influenced by regional scale differences in environmental conditions including climate and soil parent material, than by changes in microbial activities with soil depth. Moreover, they suggest that a similar potential to decompose new resources in the form of root litter exists in both surface and deep soils.