Importance of rhizodeposition in the coupling of plant and microbial productivity

By E. Paterson. 2003

398 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/2b8db8ac045acdcb955d9b7446054e7fd010a352

How researchers see this paper

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

In Plant Science

In Soil Science

Citations in the corpus

Rhizosphere fauna: the functional and structural diversity of intimate interactions of soil fauna with plant roots (2009, positive): “Microorganisms in soil are generally limited by the availability of low-molecular weight carbon compounds and rhizodeposition plays a crucial role as energy source in the coupling of plant and microbial productivity (Paterson 2003).”
New approach for capturing soluble root exudates in forest soils (2008, neutral): “Because they occur in a narrow zone of soil around roots and are rapidly assimilated by soil microbes, root exudates are one of the most poorly quantified components of the belowground C cycle (Wardle 2002; Paterson 2003).”
Wetland plant decomposition under different nutrient conditions: what is more important, litter quality or site quality? (2006, background): “It also leads to shifts in composition of both plant and microbial communities ( Paterson 2003 ).”
Using functional traits to predict grassland ecosystem change: a mathematical test of the response‐and‐effect trait approach (2009, methodology): “, 2007a], presumably due to plant community dynamics (Paterson, 2003).”
Relative contributions of plant traits and soil microbial properties to mountain grassland ecosystem services (2013, background): “In turn, greater litter inputs to soil, and possibly greater root biomass, might stimulate microbial biomass N by providing more resources for microbes in the rhizosphere (Zak et al. 1994; Paterson 2003; Tscherko et al. 2004).”
Spatio‐temporal variations determine plant–microbe competition for inorganic nitrogen in an alpine meadow (2011, background): “Temporal frameworks are important to better understand relationships between above- and below-ground communities (Paterson 2003; Bardgett et al. 2005).”
Does accelerated soil organic matter decomposition in the presence of plants increase plant N availability (2009, neutral): “It has been suggested that the microbial decomposer community in the soil utilizes rhizodeposits as a C source and decompose SOM to acquire N (Kuzyakov et al., 2000; Paterson, 2003).”
Carbon flow in the rhizosphere: carbon trading at the soil–root interface (2009, background): “Knowledge of the partitioning of rhizosphere respiration into root, symbiont and rhizomicrobial components, however, is crucial if we are to gain a deeper understanding of rhizosphere C flow (Paterson 2003; Paterson et al. 2005).”
Plant-microbe-soil interactions in the rhizosphere: an evolutionary perspective (2009, background): “This stimulation of the mineralisation of soil organic matter following fresh organic matter inputs corresponds to the so-called ‘priming effect’ (Kuzyakov et al. 2000; Fontaine et al. 2003; Paterson 2003).”
FEEDBACK IN THE PLANT-SOIL SYSTEM (2005, background): “Feedback is explicitly incorporated into some models, for example those of Reference 47, which links differential litter decomposition rates different plant functional types, deﬁned by their relative growth rates and nutrient use efﬁciencies.”
Stoichiometry constrains microbial response to root exudation- insights from a model and a field experiment in a temperate forest (2012, background): “Microbes rapidly absorb exudates and use them for metabolism and exoenzyme production (Jones et al., 1996; Jones, 1998), which stimulates biogeochemical transformations in the rhizosphere relative to bulk soil (Dakora and Phillips, 2002; Paterson, 2003; Phillips et al., 2011).”
The Role of Soil Microorganisms in Plant Mineral Nutrition—Current Knowledge and Future Directions (2017, background): “So, even if the soil microbiota contains strains with genes encoding the aforementioned enzymes linked to soil health, soil conditions must be optimized for these microbial proteins to be expressed and active (Paterson, 2003).”