Soil and rhizosphere microorganisms have the same Q10 for respiration in a model system

By E. Bååth, H. Wallander. 2003

87 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Plant Science, Soil Science

View Paper: https://www.semanticscholar.org/paper/64a94739c1e4a5387b0bb043690d49b3a01644f8

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

In Plant Science

In Soil Science

Citations in the corpus

Rhizospheric and heterotrophic respiration of a warm-temperate oak chronosequence in China (2011, methodology): “Few models can be used to estimate these two components separately (Bååth and Wallander, 2003), due to our limited understanding of the factors controlling each component (Davidson et al.”
Does the temperature sensitivity of decomposition of soil organic matter depend upon water content, soil horizon, or incubation time? (2005, result): “This problem has most recently been shown by Baath & Wallander (2003) who demonstrated that the results by Boone et al. (1998) – a higher temperature sensitivity of root compared the soil microbial respiration – were partly caused by interaction with vegetation activity.”
On the variability of respiration in terrestrial ecosystems: moving beyond Q10 (2006, background): “Bååth & Wallander (2003) grew pine seedling roots, mycorrhizae, and soil microorganisms in separate experimental compartments of growth chambers that were exposed to the same varying temperature regimes over time periods sufficiently short to preclude significant tissue growth.”
Acclimation to temperature and temperature sensitivity of metabolism by ectomycorrhizal fungi (2008, methodology): “…among ECM fungal species in their ability to acclimate indicates that the response of the ectomycorrhizal fungal community as a whole, which contributes significantly to soil respiration (Rygiewicz & Andersen, 1994; Bååth & Wallander, 2003), will be determined by the structure of that community.”
Forest soil CO2 flux: uncovering the contribution and environmental responses of ectomycorrhizas (2007, background): “…flux component The lack of an EM fungal respiration temperature response is in direct conflict with the short-term (1–3 days) laboratory study of Bååth & Wallander (2003), which noted that the temperature sensitivities of rhizosphere (including EM fungi) vs. soil heterotrophic respiration do…”