HOW ROOTS CONTROL THE FLUX OF CARBON TO THE RHIZOSPHERE

By J. Farrar, M. Hawes, Davey L. Jones, S. Lindow. 2003

437 citations recorded by the source corpus.

Subfields: Molecular Biology, Plant Science

View Paper: https://www.semanticscholar.org/paper/6fcb481a9e7a4a90f4bdd85aca82e49747cd9909

How researchers see this paper

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

In Molecular Biology

1. Y. Kuzyakov
2. P. Nannipieri
3. C. Nguyen
4. I. Dodd
5. Davey L. Jones
6. P. Hirsch
7. Johan Six
8. David L. Jones

In Plant Science

1. Y. Kuzyakov
2. Davey L. Jones
3. David L. Jones
4. M. Bonkowski
5. Richard P Phillips
6. C. Nguyen
7. R. Finlay
8. L. Carvalhais

Citations in the corpus

• Glucose uptake by maize roots and its transformation in the rhizosphere (2006, background): “glutamate, glycine) and organic acids (e.g. citrate, lactate; Farrar et al., 2003).”
• Revisiting the hypothesis that fungal-to-bacterial dominance characterizes turnover of soil organic matter and nutrients (2015, background): “The plant influence is provided both from aboveground sources such as litter input (Hieber and Gessner 2002, Romani et al. 2006, Sayer et al. 2011, Rousk et al. 2013), and from belowground sources, such as root exudates and deposition (Farrar et al. 2003).”
• Rhizosphere: its structure, bacterial diversity and significance (2014, background): “…components like water soluble compounds including simple carbohydrates, amino acids, organic acids, plant hormones, vitamins, phenolics, sugar phosphate esters, ions and many other carbon-containing secondary metabolites (Uren 2001; Farrar et al. 2003; Bais et al. 2006; Cheng and Gershenson 2007).”
• Linking 3D Soil Structure and Plant-Microbe-Soil Carbon Transfer in the Rhizosphere (2018, background): “…the flow of recently fixed C (McCully and Canny, 1985) from the stele toward the cortex Frontiers in Environmental Science | www.frontiersin.org 7 February 2018 | Volume 6 | Article 9 via the apoplastic pathway, i.e., along cell walls (Farrar et al., 2003; Jones et al., 2009; Kaiser et al., 2015).”
• Root exudate components change litter decomposition in a simulated rhizosphere depending on temperature (2006, background): “Current evidence suggests that root exudation is maximal at root tips although this is clearly solute and plant species specific (Jaeger et al. 1999; Farrar et al. 2003).”
• Plant-driven selection of microbes (2009, background): “1 (Farrar et al. 2003; Moore et al. 2007).”
• Intercropping with legume for agroecological cropping systems: Complementarity and facilitation processes and the importance of soil microorganisms. A review (2017, background): “This intensified root activity, and consequently the increase in rhizodeposits, improves soil carbon content and has a positive impact on nutrient storage and on the soil exchange capacity (Balesdent et al., 2011; Farrar et al., 2003; Oelbermann and Echarte, 2011).”
• Stoichiometry constrains microbial response to root exudation- insights from a model and a field experiment in a temperate forest (2012, background): “…ATP-ase H + pumps to create a negative membrane potential that aids in cation uptake; this membrane potential also drives negatively charged compounds out of root cells, including many organic acids such as citrate −3 , malate −2 , and oxalate −2 (Farrar et al., 2003; Jones et al., 2004).”
• MOLECULAR SIGNALS AND RECEPTORS: CONTROLLING RHIZOSPHERE INTERACTIONS BETWEEN PLANTS AND OTHER ORGANISMS (2003, background): “The use of bacterial reporter gene-fusions as molecular sensors to track the release of nutrients and signal molecules in the rhizosphere is an important tool for future work in field ecology (Farrar et al. 2003).”
• Rhizosphere biology and crop productivity—a review (2006, background): “The net carbon (since, importantly, roots can take up rhizosphere carbon) released from roots ranges from 5 to 10% of net carbon fixed by the plant (reviewed in Farrar et al. 2003).”
• Rhizobacteria that produce auxins and contain 1-amino-cyclopropane-1-carboxylic acid deaminase decrease amino acid concentrations in the rhizosphere and improve growth and yield of well-watered and water-limited potato (Solanum tuberosum) (2015, background): “, 2013; Moe, 2013), and there is increasing evidence of plant uptake of amino acids from the rhizosphere (Jones & Darrah, 1994; Farrar et al., 2003; Sauheitl et al., 2009).”