Soil respiration responses to temperature are controlled more by roots than by decomposition in balsam fir ecosystems

By M. Lavigne, R. Boutin, R. J. Foster, G. Goodine, Pierre Y. Bernier, G. Robitaille. 2003

123 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Nature and Landscape Conservation, Soil Science

View Paper: https://www.semanticscholar.org/paper/cb8e58bc785cdffad73ccc86771d2479d38636ec

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

1. Werner L. Kutsch
2. F. Moyano
3. E. Schulze
4. Y. Kuzyakov
5. O. Gavrichkova

In Nature and Landscape Conservation

1. E. Schulze

In Soil Science

1. Werner L. Kutsch
2. F. Moyano
3. E. Schulze
4. O. Gavrichkova
5. Y. Kuzyakov

Citations in the corpus

• Soil and root respiration in mature Alaskan black spruce forests that vary in soil organic matter decomposition rates (2005, background): “This observation might reflect the temperature sensitivity of root respiration (Boone et al. 1998; Lavigne et al. 2003; O’Connell et al. 2003) or that microbes were becoming substrate limited in 2001.”
• Response of mycorrhizal, rhizosphere and soil basal respiration to temperature and photosynthesis in a barley field (2007, background): “Thus, it is not surprising that these relations frequently fail to explain a large percentage of soil respiration (Janssens and Pilegaard, 2003; Lavigne et al., 2003).”