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      High-throughput Fluorometric Measurement of Potential Soil Extracellular Enzyme Activities

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          Abstract

          Microbes in soils and other environments produce extracellular enzymes to depolymerize and hydrolyze organic macromolecules so that they can be assimilated for energy and nutrients. Measuring soil microbial enzyme activity is crucial in understanding soil ecosystem functional dynamics. The general concept of the fluorescence enzyme assay is that synthetic C-, N-, or P-rich substrates bound with a fluorescent dye are added to soil samples. When intact, the labeled substrates do not fluoresce. Enzyme activity is measured as the increase in fluorescence as the fluorescent dyes are cleaved from their substrates, which allows them to fluoresce. Enzyme measurements can be expressed in units of molarity or activity. To perform this assay, soil slurries are prepared by combining soil with a pH buffer. The pH buffer (typically a 50 mM sodium acetate or 50 mM Tris buffer), is chosen for the buffer's particular acid dissociation constant (pKa) to best match the soil sample pH. The soil slurries are inoculated with a nonlimiting amount of fluorescently labeled ( i.e. C-, N-, or P-rich) substrate. Using soil slurries in the assay serves to minimize limitations on enzyme and substrate diffusion. Therefore, this assay controls for differences in substrate limitation, diffusion rates, and soil pH conditions; thus detecting potential enzyme activity rates as a function of the difference in enzyme concentrations (per sample).

          Fluorescence enzyme assays are typically more sensitive than spectrophotometric ( i.e. colorimetric) assays, but can suffer from interference caused by impurities and the instability of many fluorescent compounds when exposed to light; so caution is required when handling fluorescent substrates. Likewise, this method only assesses potential enzyme activities under laboratory conditions when substrates are not limiting. Caution should be used when interpreting the data representing cross-site comparisons with differing temperatures or soil types, as in situ soil type and temperature can influence enzyme kinetics.

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          Most cited references48

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          Stoichiometry of soil enzyme activity at global scale.

          Extracellular enzymes are the proximate agents of organic matter decomposition and measures of these activities can be used as indicators of microbial nutrient demand. We conducted a global-scale meta-analysis of the seven-most widely measured soil enzyme activities, using data from 40 ecosystems. The activities of beta-1,4-glucosidase, cellobiohydrolase, beta-1,4-N-acetylglucosaminidase and phosphatase g(-1) soil increased with organic matter concentration; leucine aminopeptidase, phenol oxidase and peroxidase activities showed no relationship. All activities were significantly related to soil pH. Specific activities, i.e. activity g(-1) soil organic matter, also varied in relation to soil pH for all enzymes. Relationships with mean annual temperature (MAT) and precipitation (MAP) were generally weak. For hydrolases, ratios of specific C, N and P acquisition activities converged on 1 : 1 : 1 but across ecosystems, the ratio of C : P acquisition was inversely related to MAP and MAT while the ratio of C : N acquisition increased with MAP. Oxidative activities were more variable than hydrolytic activities and increased with soil pH. Our analyses indicate that the enzymatic potential for hydrolyzing the labile components of soil organic matter is tied to substrate availability, soil pH and the stoichiometry of microbial nutrient demand. The enzymatic potential for oxidizing the recalcitrant fractions of soil organic material, which is a proximate control on soil organic matter accumulation, is most strongly related to soil pH. These trends provide insight into the biogeochemical processes that create global patterns in ecological stoichiometry and organic matter storage.
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            Ecoenzymatic stoichiometry of microbial organic nutrient acquisition in soil and sediment.

            Biota can be described in terms of elemental composition, expressed as an atomic ratio of carbon:nitrogen:phosphorus (refs 1-3). The elemental stoichiometry of microoorganisms is fundamental for understanding the production dynamics and biogeochemical cycles of ecosystems because microbial biomass is the trophic base of detrital food webs. Here we show that heterotrophic microbial communities of diverse composition from terrestrial soils and freshwater sediments share a common functional stoichiometry in relation to organic nutrient acquisition. The activities of four enzymes that catalyse the hydrolysis of assimilable products from the principal environmental sources of C, N and P show similar scaling relationships over several orders of magnitude, with a mean ratio for C:N:P activities near 1:1:1 in all habitats. We suggest that these ecoenzymatic ratios reflect the equilibria between the elemental composition of microbial biomass and detrital organic matter and the efficiencies of microbial nutrient assimilation and growth. Because ecoenzymatic activities intersect the stoichiometric and metabolic theories of ecology, they provide a functional measure of the threshold at which control of community metabolism shifts from nutrient to energy flow.
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              Optimization of hydrolytic and oxidative enzyme methods for ecosystem studies

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                Author and article information

                Journal
                J Vis Exp
                J Vis Exp
                JoVE
                Journal of Visualized Experiments : JoVE
                MyJove Corporation
                1940-087X
                2013
                15 November 2013
                15 November 2013
                : 81
                : 50961
                Affiliations
                1Natural Resource Ecology Laboratory, Colorado State University
                2Biosciences Division, Oak Ridge National Laboratory
                3Department of Bioengineering, University of Colorado
                Author notes

                Correspondence to: Matthew D. Wallenstein at matthew.wallenstein@ 123456colostate.edu

                Article
                50961
                10.3791/50961
                3991303
                24299913
                8e50763b-69b9-4191-bc9b-0442f0e75907
                Copyright © 2013, Journal of Visualized Experiments

                This is an open-access article distributed under the terms of the Creative Commons Attribution-NonCommercial License, which permits non-commercial use, distribution, and reproduction, provided the original work is properly cited.

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                Categories
                Environmental Sciences

                Uncategorized
                environmental sciences,issue 81,ecological and environmental phenomena,environment,biochemistry,environmental microbiology,soil microbiology,ecology,eukaryota,archaea,bacteria,soil extracellular enzyme activities (eeas),fluorometric enzyme assays,substrate degradation,4-methylumbelliferone (mub),7-amino-4-methylcoumarin (muc),enzyme temperature kinetics,soil

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