Catalytic power of enzymes decreases with temperature: New insights for understanding soil C cycling and microbial ecology under warming. (16th May 2018)

• Record Type: Journal Article
• Authors: Alvarez, Gaël; Shahzad, Tanvir; Andanson, Laurence; Bahn, Michael; Wallenstein, Matthew D.; Fontaine, Sébastien
• Is Part Of: Global change biology. Volume 24:Number 9(2018)
• Page Start: 4238
• Page End: 4250
• Publication Date: 2018-05-16
• Subjects: enzymatic activity -- enzyme denaturation -- enzyme trait -- SOC decomposition under warming -- temperature sensitivity; Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.14281
• Languages: English
• ISSNs: 1354-1013

Abstract

Abstract: Most current models of soil C dynamics predict that climate warming will accelerate soil C mineralization, resulting in a long‐term CO2 release and positive feedback to global warming. However, ecosystem warming experiments show that CO2 loss from warmed soils declines to control levels within a few years. Here, we explore the temperature dependence of enzymatic conversion of polymerized soil organic C (SOC) into assimilable compounds, which is presumed the rate‐limiting step of SOC mineralization. Combining literature review, modelling and enzyme assays, we studied the effect of temperature on activity of enzymes considering their thermal inactivation and catalytic activity. We defined the catalytic power of enzymes ( E power ) as the cumulative amount of degraded substrate by one unit of enzyme until its complete inactivation. We show a universal pattern of enzyme's thermodynamic properties: activation energy of catalytic activity ( EA cat ) < activation energy of thermal inactivation ( EA inact ). By investing in stable enzymes (high EA inact ) having high catalytic activity (low EA cat ), microorganisms may maximize the E power of their enzymes. The counterpart of such EAs' hierarchical pattern is the higher relative temperature sensitivity of enzyme inactivation than catalysis, resulting in a reduction in E power under warming. Our findings could explain the decrease with temperature in soil enzyme pools, microbial biomass (MB) and carbon use efficiency (CUE) reported in some warming experiments and studies monitoring the seasonal variation in soil enzymes. They also suggest that a decrease in soil enzyme pools due to their faster inactivation under warming contributes to the observed attenuation of warming effect on soil C mineralization. This testable theory predicts that the ultimate response of SOC degradation to warming can be positive or negative depending on the relative temperature response of E power and microbial production of enzymes. Abstract : While most current models of soil C dynamics predict that climate warming will accelerate soil CO2 release, ecosystem warming experiments show that soil CO2 loss declines to control levels within a few years. We re‐analysed the temperature dependence of biological processes (e.g. soil C degradation) by focusing on an overlooked process, the thermal inactivation of enzymes. We show a universal pattern of enzyme's thermodynamic properties leading to decrease in enzymes catalytic power with temperature. Our findings can explain the attenuation with time of warming effect on soil respiration and provide new insights for understanding organism's response to their thermal environment.