Articles | Volume 11, issue 2
https://doi.org/10.5194/soil-11-991-2025
https://doi.org/10.5194/soil-11-991-2025
Original research article
 | 
28 Nov 2025
Original research article |  | 28 Nov 2025

Availability of labile carbon controls the temperature-dependent response of soil organic matter decomposition in alpine soils

Dario Püntener, Tatjana C. Speckert, Yves-Alain Brügger, and Guido L. B. Wiesenberg

Viewed

Total article views: 4,267 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,555 592 120 4,267 72 152 201
  • HTML: 3,555
  • PDF: 592
  • XML: 120
  • Total: 4,267
  • Supplement: 72
  • BibTeX: 152
  • EndNote: 201
Views and downloads (calculated since 29 Apr 2025)
Cumulative views and downloads (calculated since 29 Apr 2025)

Viewed (geographical distribution)

Total article views: 4,267 (including HTML, PDF, and XML) Thereof 4,203 with geography defined and 64 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 14 Jun 2026
Download
Short summary
Alpine soils store much carbon but warming and changes in vegetation could reverse this by turning them into carbon sources. In a one-year laboratory study, we examined alpine forest and pasture soils and added fresh grass litter marked with a carbon tracer to track decomposition under different temperatures. Our findings reveal that fresh plant material drives soil breakdown more than temperature alone, offering new insights into how climate change may affect carbon storage in mountain regions.
Share