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MICROHEAT: Heat dissipation and matter turnover in the course of microbial succession constrained by substrate and oxygen availability

Subject Area Soil Sciences
Microbial Ecology and Applied Microbiology
Term since 2021
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 465122443
 
Current challenge to increase sequestration of soil carbon (C) - the largest and most important terrestrial C stock - requires understanding the processes of carbon losses during microbial decomposition of diverse organic compounds, which serve as a substrate to obtain C, energy and nutrients for microbial metabolism. A tense competition between microbial groups for available soil organics results in a trade off between fast but less efficient or slow but more efficient metabolism of substrate. The mechanism of such a trade off is a basic ecological subject and their consequences are of a great importance for C retention in soils and C losses into the atmosphere. The proposed project Microheat considers that transformation of organic substrates in soil occurs in the course of multi-stage microbial succession through a sequence of decomposition stages. The duration, amplitude and dominating taxa of each successional stage as well as an efficiency of carbon utilization are dependent on substrate quality and amount and are restricted by contrasting oxygen availability in soil microhabitats resulting in simultaneous occurrence of aerobic and anaerobic decomposition depending on the local oxygen concentrations. The methodological novelty and challenge of Microheat, therefore, is in estimation of the anaerobic soil volume fraction via application of X-ray CT to study the effect of oxygen diffusion constraints on C and energy use efficiency (CUE and EUE). The peculiarity of Microheat is in its conceptual view linking matter (CO2) and energy (heat) losses to microbial growth and to the range of enzyme-mediated reactions related to various stages of substrate decomposition. The Microheat project aims to relate an efficiency of microbial metabolism with heat and C losses in course of microbial succession during decomposition of organic compounds in soil. This will be done by a combination of kinetic approaches to relate matter and energy losses with 1) changes in dominating microbial populations in soil, 2) microbial functional traits, and 3) turnover time of carbon sources. The project will test applicability of specific heat dissipation as indicator of thermodynamic efficiency of the soil microbiome. As a result, a variable CUE as a function of independently determined microbial traits will be suggested for carbon models considering dynamically changing fraction of anaerobic soil volume. The Microheat project will make a promising contribution to elucidating regulatory mechanisms of energy and matter turnover based on the microbial trade-offs between rate and efficiency of organic compounds decomposition in soil.
DFG Programme Priority Programmes
 
 

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