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| Titel |
Increased belowground C release during initial plant development of Populus deltoides x nigra grown under light and C reserve limited conditions |
| VerfasserIn |
Mirjam S. Studer, Rolf T. W. Siegwolf, Michael W. I. Schmidt, Samuel Abiven |
| Konferenz |
EGU General Assembly 2014
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 16 (2014) |
| Datensatznummer |
250091323
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| Publikation (Nr.) |
 EGU/EGU2014-5609.pdf |
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| Zusammenfassung |
| Plants might be a key factor for the long-term stabilisation of carbon (C) in the soil, e.g. through enhanced physical protection of root-derived C against microbial decomposition in soil aggregates. On the other hand C released by the plants into the soil might promote the decomposition of native soil organic matter (SOM) through the stimulation of microbial activity.
We measured the C budget of developing plant-soil systems (Populus deltoides x nigra, Cambisol soil) in the laboratory under controlled environmental conditions. In order to distinguish plant-derived from native C in the SOM and the soil CO2 efflux, we labelled the poplar shoots continuously with 13C-CO2 from first emergence of leaves (sprouting from stem cuttings). Throughout the experiment the CO2 fluxes (photosynthetic assimilation, dark respiratory loss, soil CO2 efflux) were measured frequently (every 30 min) and the 13C was traced in the soil CO2 efflux (1-2 times a week). After 10 weeks the plant-soil systems were destructively harvested and the distribution of the 13C distribution was analysed.
The plants developed slowly (compared to previous experiments), most likely due to limitation in C reserves (long term cutting storage) and C supply (low light intensities). The amount of 13C recovered in the roots, microbial biomass and soil CO2 efflux was directly correlated with the leaf area of the different plant individuals. After 3-4 weeks of plant development we observed a high peak in the total soil CO2 efflux. During this time the relative belowground C release was increased massively over the basal rate of 17 % of net C assimilated, whereby the variability between the plant individuals was large. The smallest plants, i.e. the plants that were most resource limited, obtained the highest belowground C release accounting at the peak time for up to 57 % of net assimilated C. We hypothesize that the plants released specific compounds, which either directly (enzymatically) or indirectly (priming) enhanced the decomposition of native SOM as a survival mechanisms (e.g. mine for nutrients).
The results of this study confirm linear correlations between aboveground plant traits (leaf area) and belowground C allocation into roots, microbial biomass and plant-derived respiration. However it also highlights that plant-soil systems are not permanently in a steady state. C allocation patterns can change massively when the plant is under stress, which affects other fluxes within the terrestrial C cycle, such as the microbial decomposition of SOM. |
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