Below‐ground carbon flux and partitioning: global patterns and response to temperature

By C. Litton, C. Giardina. 2008

148 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Soil Science

View Paper: https://www.semanticscholar.org/paper/cf65e525358c119720f63ec4790b76c0276db03c

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. D. Metcalfe
2. Ram Oren
3. J. Bouillet
4. J. Gonçalves
5. D. Way
6. M. Stoll
7. Yann Nouvellon
8. H. Schultz

In Soil Science

1. Ram Oren
2. J. Bouillet
3. J. Gonçalves
4. Yann Nouvellon
5. Petr Baldrian
6. C. Plassard
7. R. Fisher
8. David A. Wardle

Citations in the corpus

• Evaluation of methods to estimate production, biomass and turnover of ectomycorrhizal mycelium in forests soils : A review (2013, background): “A better understanding of below ground carbon (C) flux is of fundamental importance to predict how changing climate will influence the C balance of forest (and other) ecosystems (Litton and Giardina, 2008).”
• Differential responses to changes in growth temperature between trees from different functional groups and biomes: a review and synthesis of data. (2010, background): “…forests, the fraction of gross primary productivity invested in belowground carbon flux is positively correlated with mean annual temperature (Litton and Giardina 2008), demonstrating that carbon allocation patterns can change with growing temperature and that trees from different biomes (or…”
• Partitioning of net primary production in Eucalyptus and Acacia stands and in mixed-species plantations: Two case-studies in contrasting tropical environments (2013, methodology): “Direct estimates of CUE for belowground production are lacking, severely constraining our ability to derive accurately BNPP from TBCF (Litton and Giardina, 2008).”
• Plant communities as drivers of soil respiration: pathways, mechanisms, and significance for global change (2011, background): “53 as mean annual site temperature rises from −5 to 30C (Litton and Giardina, 2008).”
• Some critical issues in environmental physiology of grapevines: future challenges and current limitations (2010, background): “additional effect on the turnover rate of organic matter in the soil, another possible source of CO2 during climate warming (Litton and Giardina 2008).”