Open AccessEnvironmental ScienceChemistryMedicine

M. Cotrufo, M. Wallenstein, C. Boot, K. Denef, E. Paul

2013.4.1GLOBAL CHANGE BIOLOGY

DOI: 10.1111/gcb.12113

tlooto Summary

It is proposed that labile plant constituents are the dominant source of microbial products, relative to input rates, because they are utilized more efficiently by microbes, and become the main precursors of stable SOM by promoting aggregation and through strong chemical bonding to the mineral soil matrix.

Abstract

The decomposition and transformation of above‐ and below‐ground plant detritus (litter) is the main process by which soil organic matter (SOM) is formed. Yet, research on litter decay and SOM formation has been largely uncoupled, failing to provide an effective nexus between these two fundamental processes for carbon (C) and nitrogen (N) cycling and storage. We present the current understanding of the importance of microbial substrate use efficiency and C and N allocation in controlling the proportion of plant‐derived C and N that is incorporated into SOM, and of soil matrix interactions in controlling SOM stabilization. We synthesize this understanding into the Microbial Efficiency‐Matrix Stabilization (MEMS) framework. This framework leads to the hypothesis that labile plant constituents are the dominant source of microbial products, relative to input rates, because they are utilized more efficiently by microbes. These microbial products of decomposition would thus become the main precursors of stable SOM by promoting aggregation and through strong chemical bonding to the mineral soil matrix.

Citation format

COTRUFO, M., et al. The microbial efficiency‐matrix stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: Do labile plant inputs form stable soil organic matter? GLOBAL CHANGE BIOLOGY, 2013, 19.