Changes in enzyme activities and soil microbial community composition along carbon and nutrient gradients at the Franz Josef chronosequence, New Zealand
By V. Allison, L. Condron, D. Peltzer, Sarah J. Richardson, Benjamin L Turner. 2007
333 citations recorded by the source corpus.
Subfields: Ecology, Soil Science
View Paper: https://www.semanticscholar.org/paper/86af5f557d0de2c956ae8a7b03249feea34c14ef
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- R. Sinsabaugh
- J. F. Follstad Shah
- M. Weintraub
- S. Allison
- M. Wallenstein
- Zhenghu Zhou
- Chuankuan Wang
- Mark P. Waldrop
In Soil Science
- R. Sinsabaugh
- J. F. Follstad Shah
- M. Weintraub
- S. Allison
- Yiqi Luo
- M. Wallenstein
- Zhenghu Zhou
- Chuankuan Wang
Citations in the corpus
- The Role of Microbial Communities in the Formation and Decomposition of Soil Organic Matter (2010, background): “The lipid content of soil organic matter ranges from 2% to 20% (Allison et al. 2007b).”
- Nitrogen inputs accelerate phosphorus cycling rates across a wide variety of terrestrial ecosystems. (2012, neutral): “Other studies have looked at phosphatase activity across gradients of P availability, and generally show a trend of increasing phosphatase activity with decreasing P availability (Wright & Reddy, 2001; Allison et al., 2007b; Wang et al., 2010a; Turner, 2010).”
- Ecoenzymatic stoichiometry of stream sediments with comparison to terrestrial soils (2011, methodology): “3 across a New Zealand soil chronosequence (Allison et al. 2007).”
- Trends in soil microbial communities during secondary succession (2017, methodology): “Extracellular enzymatic efficiency was calculated as extracellular enzyme activity normalized to per unit microbial biomass C (Allison et al., 2007), i.”
- Plant nitrogen uptake drives rhizosphere bacterial community assembly during plant growth (2015, background): “…reduction in soil nutrient availability increases C:N stoichiometry within the rhizosphere, which can initiate microbial extracellular enzyme production to oxidize or hydrolyze soil organic matter to release otherwise unavailable nutrients (Allison et al., 2007; Kuzyakov, 2010; Drake et al., 2013).”
- Evolutionary-Economic Principles as Regulators of Soil Enzyme Production and Ecosystem Function (2010, background): “Extracellular enzymes target nearly every macromolecule on earth, including proteins (proteases), carbohydrates (amylases, cellulases), amino sugar polymers (chitinases), organic phosphates (phosphatases), and lignins (oxidases, peroxidases) (Burns 1978; Allison et al. 2007a).”
- Soil microbial diversity and activity linked to crop yield and quality in a dryland organic wheat production system (2016, background): “Extracellular enzyme production depends on bacterial and fungal biomass, physiological state, and species composition of the community, as well as a variety of environmental factors (Allison et al., 2007).”
- Microbial and Enzyme Activities of Saline and Sodic Soils (2016, background): “Moreover, phosphatase activity has been shown to be inversely related to inorganic P availability in the soil system, especially in salt-affected soils (Allison et al., 2007; Allison et al., com/journa Copyright © 2015 John Wiley & Sons, Ltd. 2011).”