Increased Belowground Carbon Allocation Reduces Soil Carbon Losses Under Long-Term Warming

Verfasst von

Andreas Schindlbacher, Steve Kwatcho Kengdo, Jakob Heinzle, Ye Tian, Mathias Mayer, Josef Gadermaier, Chupei Shi, Caro Urbina Malo, Xiaofei Liu, Erich Inselsbacher, Robert Jandl, Carlos A. Sierra, Wolfgang Wanek, Werner Borken

Abstract

The response of the carbon cycle in forests to global warming could lead to a positive climate feedback if warming accelerates the mineralization of soil organic carbon (SOC), thereby causing net emissions of CO₂ into the atmosphere. In Europe, carbon-rich alpine forest soils could be particularly affected by global warming, as a greater rise in temperature is expected in this region than the global average. Here we show that nearly two decades of experimental soil warming (+4°C during the snow-free seasons) in a mountain forest in the Northern Limestone Alps significantly (~13% per 1°C warming) and persistently (no change in response over 18 years) increased soil CO₂ effluxes. The SOC stocks in the warmed plots decreased compared to controls, yet non-significantly, and quantitatively much less than the surplus carbon outflux from warmed soil suggests. We attribute the increase in soil CO₂ efflux primarily to stimulation of root respiration, which was most sensitive to long-term warming. Furthermore, increased root production, faster fine root turnover, and increased root exudation likely not only facilitated autotrophic respiration but also replenished the SOC pool. The radiocarbon age of SOC indicates a rejuvenation of SOC likely by increased input of root carbon into the lower topsoil. Overall, our findings suggest that increased C allocation into the rhizosphere can at least partially compensate for the C loss through increased SOC mineralization with rising temperatures over many years.

Details

Organisationseinheit(en): Institut für Erdsystemwissenschaften
Externe Organisation(en): Bundesforschungs- und Ausbildungszentrum für Wald, Naturgefahren und Landschaft (BFW)
Universität Bayreuth
Lawrence Berkeley National Laboratory (LBNL)
Universität Wien
Swedish University of Agricultural Sciences
Universität für Bodenkultur Wien (BOKU)
Eidg. Forschungsanstalt für Wald, Schnee und Landschaft (WSL)
Institute for Biodiversity and Ecosystem Dynamics - Amsterdam
Fujian Normal University
Max-Planck-Institut für Biogeochemie
Typ: Artikel
Journal: Global change biology
Band: 31
ISSN: 1354-1013
Publikationsdatum: 16.10.2025
Publikationsstatus: Veröffentlicht
Peer-reviewed: Ja
ASJC Scopus Sachgebiete: Globaler Wandel, Umweltchemie, Ökologie, Allgemeine Umweltwissenschaft
Ziele für nachhaltige Entwicklung: SDG 13 - Klimaschutzmaßnahmen
Elektronische Version(en): https://doi.org/10.1111/gcb.70561 (Zugang: Offen )