Fine root and aboveground carbon stocks in riparian forests: the roles of diking and environmental gradients

Fine root and aboveground carbon stocks in riparian forests: the roles of diking and environmental gradients

Aims We analysed current carbon (C) stocks in fine root and aboveground biomass of riparian forests and influential environmental parameters on either side of a dike in the Donau-Auen National Park, Austria. Methods On both sides of the dike, carbon (C) stock of fine roots (CFR) under four dominant...

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Veröffentlicht in:Plant and Soil. - Springer Science + Business Media. - 370(2013), 1/2, Seite 497-509
1. Verfasser: Rieger, Isaak (VerfasserIn)
Weitere Verfasser: Lang, Friederike, Kleinschmit, Birgit, Kowarik, Ingo, Cierjacks, Arne
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2013
Zugriff auf das übergeordnete Werk:Plant and Soil
Schlagworte:Biological sciences Physical sciences
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520 |a Aims We analysed current carbon (C) stocks in fine root and aboveground biomass of riparian forests and influential environmental parameters on either side of a dike in the Donau-Auen National Park, Austria. Methods On both sides of the dike, carbon (C) stock of fine roots (CFR) under four dominant tree species and of aboveground biomass (CAB) were assessed by topsoil cores (0-30 cm) and angle count sampling method respectively (n=48). C stocks were modeled, performing boosted regression trees (BRT). Results Overall CFR was 2.8 t ha⁻¹, with significantly higher C stocks in diked (DRF) compared to flooded riparian forests (FRF). In contrast to CFR, mean CAB was 123 t ha⁻¹ and lower in DRF compared to FRF. However, dike construction was consistently ruled out as a predictor variable in BRT. CFR was influenced by the distance to the Danube River and the dominant tree species. CAB was mainly influenced by the magnitude of fluctuations in the groundwater table and the distances to the river and the low groundwater table. Conclusions Despite pronounced differences in FRF and DRF, we conclude that there is only weak support that dikes directly influence C allocation in floodplain forests within the time scale considered (110 years). 
540 |a © 2013 Springer 
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650 4 |a Biological sciences  |x Ecology  |x Population ecology  |x Synecology  |x Biocenosis  |x Plant communities  |x Forests  |x Riparian forests 
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650 4 |a Biological sciences  |x Agriculture  |x Agricultural sciences  |x Agronomy  |x Soil science  |x Soils  |x Riparian soils 
650 4 |a Physical sciences  |x Earth sciences  |x Hydrology  |x Water tables 
650 4 |a Biological sciences  |x Biology  |x Botany  |x Plant ecology  |x Forest ecology  |x Forest ecosystems 
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650 4 |a Physical sciences  |x Earth sciences  |x Geography  |x Geomorphology  |x Landforms  |x Fluvial landforms  |x Alluvial landforms  |x Alluvial plains  |x Floodplains 
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700 1 |a Kleinschmit, Birgit  |e verfasserin  |4 aut 
700 1 |a Kowarik, Ingo  |e verfasserin  |4 aut 
700 1 |a Cierjacks, Arne  |e verfasserin  |4 aut 
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