Mechanisms of real and apparent priming effects and their dependence on soil microbial biomass and community structure: critical review

By Е. Blagodatskaya, Y. Kuzyakov. Biology and Fertility of Soils, 2008

1,458 citations recorded by the source corpus.

Subfields: Ecology, Environmental Engineering, Soil Science

View Paper: https://www.semanticscholar.org/paper/30e2f61c4124e4dee3d03b74ae34e58ba8639761

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Citations in the corpus

Root exudates increase N availability by stimulating microbial turnover of fast-cycling N pools (2017, positive): “…of SOM decomposition by root exudates is lower in soil with higher nutrient availability (nutrient mining theory; Fontaine et al., 2003, 2004, 2011; Blagodatskaya and Kuzyakov, 2008; Guenet et al., 2010; Paterson and Sim, 2013; Sullivan and Hart, 2013), but contrasting results have been found as…”
Stability and dynamics of enzyme activity patterns in the rice rhizosphere: Effects of plant growth and temperature (2017, background): “Such an increase is mainly connected to the production of this common enzyme by both plants and microorganisms (Blagodatskaya and Kuzyakov, 2008; Dick and Tabatabai, 1984; Nannipieri et al., 2011).”
Revisiting the hypothesis that fungal-to-bacterial dominance characterizes turnover of soil organic matter and nutrients (2015, neutral): “…has been thought to capture disparate life strategies for soil microbial decomposers, associating bacteria with an rselected strategy for C and nutrient use, and fungi with a K-selected strategy (Fontaine et al. 2003, Fontaine and Barot 2005, Blagodatskaya and Kuzyakov 2008, Fierer et al. 2009).”
Grass invasion of a hardwood forest is associated with declines in belowground carbon pools (2010, background): “Furthermore, when considering both Litton et al.'s (2008) study and ours there is support for the proposition that the strength of preferential substrate utilization vs. priming may be dependent on the relative increase in inputs (Blagodatskaya & Kuzyakov, 2008; Bradford et al., 2008c).”
Laccases: toward disentangling their diversity and functions in relation to soil organic matter cycling (2010, background): “1), which is associated with a succession of microbial communities: r-strategists (synonymous terms: opportunistic, zymogenic, or copiotrophic microbes) dominating the early stages and are later replaced by K-strategists (synonymous terms: persisting, autochthonous, or oligotrophic microbes) (Blagod”
Linking microbial community composition to C loss rates during wood decomposition (2017, background): “Because fungal and bacterial communities have very different C use efficiencies (Fontaine et al., 2003; Blagodatskaya and Kuzyakov, 2008) and environment condition requirements (Boddy, 2001; Kaiser et al., 2014), our finding could be critical for the development of models that explicitly consider…”
Erratum to The chemical and functional characterization of soil N and its biotic components (2009, background): “The observation that added substrates that decompose rapidly supply nutrients but usually do not build up SOM led Löhnis (1926) to suggest the priming phenomena that was (Broadbent and Bartholomew, 1948) and still is (Fontaine et al., 2004; Blagodatskaya and Kuzyakov, 2008) the subject of controvers”
Rhizosphere priming: a nutrient perspective (2013, background): “…effects under low nutrient availability may occur because priming also depends on soil properties such as total C content and texture (Zhang et al., 2013), mineralogy (Rasmussen et al., 2007), pH (Blagodatskaya and Kuzyakov, 2008; Luo et al., 2011), and heavy metal concentration (Ohm et al., 2011).”
Connecting the green and brown worlds . allometric and stoichiometric predictability of above- and below-ground networks (2013, background): “…have been suggested to be linked through priming effects that exemplify the interaction between the green and the brown world: the mineralisation of SOM is influenced (mostly enhanced, but sometimes reduced) by inputs of fresh organic compounds (Blagodatskaya and Kuzyakov, 2008; Kuzyakov, 2010).”
Carbon use efficiency of microbial communities: stoichiometry, methodology and modelling. (2013, background): “In contrast, carbon sources that are recalcitrant to decomposition, as the result of stochastic oxidation and condensation reactions in the environment, may reduce CUE by increasing the cost of extracellular and intracellular catabolism (Blagodatskaya & Kuzyakov 2008).”
Intercropping with legume for agroecological cropping systems: Complementarity and facilitation processes and the importance of soil microorganisms. A review (2017, background): “…matter (SOM) decomposition rates are increased by the addition of fresh organic matter from legumes, which stimulates the activities of soil bacteria communities involved in the mineralization of stable SOM (Bernard et al., 2007, 2009; Blagodatskaya and Kuzyakov, 2008; Fontaine et al., 2003).”
Priming and microbial nutrient limitation in lowland tropical forest soils of contrasting fertility (2012, background): “Priming due to co-metabolism of organic matter by nutrient-limited microorganisms can be identified by an increase in the microbial synthesis of extracellular enzymes to liberate nutrients from organic matter (Kuzyakov et al. 2000; Schimel and Weintraub 2003; Blagodatskaya and Kuzyakov 2008).”