Topical IssueSoils as a source and sink for CO2– Mechanisms and regulation of organic matter stabilisation in soils (editors: I. Kögel-Knabner and E. Matzner). Synthesis of the DFG Priority Program SPP 1090 (German Research Foundation—“Deutsche Forschungsgemeinschaft”)
Soil-carbon preservation through habitat constraints and biological limitations on decomposer activity†
Article first published online: 31 JAN 2008
Copyright © 2008 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim
Journal of Plant Nutrition and Soil Science
Volume 171, Issue 1, pages 27–35, February, 2008
How to Cite
Ekschmitt, K., Kandeler, E., Poll, C., Brune, A., Buscot, F., Friedrich, M., Gleixner, G., Hartmann, A., Kästner, M., Marhan, S., Miltner, A., Scheu, S. and Wolters, V. (2008), Soil-carbon preservation through habitat constraints and biological limitations on decomposer activity. Z. Pflanzenernähr. Bodenk., 171: 27–35. doi: 10.1002/jpln.200700051
- Issue published online: 31 JAN 2008
- Article first published online: 31 JAN 2008
- Manuscript Accepted: 9 JUL 2007
- soil microflora;
- soil fauna;
- carbon turnover;
We review recent experimental results on the role of soil biota in stabilizing or destabilizing soil organic matter (SOM). Specifically, we analyze how the differential substrate utilization of the various decomposer organisms contributes to a decorrelation of chemical stability, residence time, and carbon (C) age of organic substrates.
Along soil depth profiles, a mismatch of C allocation and abundance of decomposer organisms is consistently observed, revealing that a relevant proportion of soil C is not subjected to efficient decomposition. Results from recent field and laboratory experiments suggest that (1) bacterial utilization of labile carbon compounds is limited by short-distance transport processes and, therefore, can take place deep in the soil under conditions of effective local diffusion or convection. In contrast, (2) fungal utilization of phenolic substrates, including lignin, appears to be restricted to the upper soil layer due to the requirement for oxygen of the enzymatic reaction involved. (3) Carbon of any age is utilized by soil microorganisms, and microbial C is recycled in the microbial food web. Due to stoichiometric requirements of their metabolism, (4) soil animals tend to reduce the C concentration of SOM disproportionally, until it reaches a threshold level.
The reviewed investigations provide new and quantitative evidence that different soil C pools underlie divergent biological constraints of decomposition. The specialization of decomposers towards different substrates and microhabitats leads to a relatively longer persistence of virtually all kinds of organic substrates in the nonpreferred soil spaces. We therefore propose to direct future research explicitly towards such biologically nonpreferred areas where decomposition rates are slow, or where decomposition is frequently interrupted, in order to assess the potential for long-term preservation of C in the soil.