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Berlin Brandenburg


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  • 1
    Language: English
    In: Plant and Soil, 2013, Vol.370(1), pp.497-509
    Description: 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 super(-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 super(-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).
    Keywords: Aboveground biomass ; Belowground biomass ; Carbon distribution ; Carbon sequestration ; Dike ; Ecosystem services ; Floodplain forest
    ISSN: 0032-079X
    E-ISSN: 1573-5036
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  • 2
    Language: English
    In: Science of the Total Environment, 01 January 2017, Vol.574, pp.1261-1275
    Description: Aboveground carbon (C) sequestration in trees is important in global C dynamics, but reliable techniques for its modeling in highly productive and heterogeneous ecosystems are limited. We applied an extended dendrochronological approach to disentangle the functioning of drivers from the atmosphere (temperature, precipitation), the lithosphere (sedimentation rate), the hydrosphere (groundwater table, river water level fluctuation), the biosphere (tree characteristics), and the anthroposphere (dike construction). Carbon sequestration in aboveground biomass of riparian L. and L. was modeled (1) over time using boosted regression tree analysis (BRT) on cross-datable trees characterized by equal annual growth ring patterns and (2) across space using a subsequent classification and regression tree analysis (CART) on cross-datable and not cross-datable trees. While C sequestration of cross-datable responded to precipitation and temperature, cross-datable also responded to a low Danube river water level. However, CART revealed that C sequestration over time is governed by tree height and parameters that vary over space (magnitude of fluctuation in the groundwater table, vertical distance to mean river water level, and longitudinal distance to upstream end of the study area). Thus, a uniform response to climatic drivers of aboveground C sequestration in was only detectable in trees of an intermediate height class and in taller trees (〉 21.8 m) on sites where the groundwater table fluctuated little (≤ 0.9 m). The detection of climatic drivers and the river water level in depended on sites at lower altitudes above the mean river water level (≤ 2.7 m) and along a less dynamic downstream section of the study area. Our approach indicates unexploited opportunities of understanding the interplay of different environmental drivers in aboveground C sequestration. Results may support species-specific and locally adapted forest management plans to increase carbon dioxide sequestration from the atmosphere in trees.
    Keywords: Boosted Regression Tree ; Carbon Sequestration ; Classification and Regression Tree ; Climate ; Danube River ; Dendrochronology ; Environmental Sciences ; Biology ; Public Health
    ISSN: 0048-9697
    E-ISSN: 1879-1026
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  • 3
    Language: English
    In: Geomorphology, 01 June 2014, Vol.214, pp.157-167
    Description: Sediment trapping and organic carbon (OC) accretion in soil are crucial ecosystem services of floodplain forests. However, interactions between the two processes have scarcely been analyzed at the ecosystem level. This study aimed at quantifying OC accretion parameters (CAP, including sedimentation rate, OC concentration, OC accretion) over roughly the last 50 years on both sides of a dike in a Danubian floodplain forest in Austria. Additionally, we determined soil OC stocks (0–100 cm in depth) and modeled both CAP and OC stocks in relation to environmental parameters. Overall, mean sedimentation rate and OC accretion of the riparian forest were 0.8 cm y and 3.3 t OC ha y and significantly higher in flooded riparian forest (FRF; 1.0 cm y and 4.1 t OC ha y ) than in diked riparian forest (DRF; 0.3 cm y and 1.5 t OC ha y ). In contrast, mean OC concentration (0.05 t OC m ) and OC stocks (238 t OC ha ) were significantly higher in the DRF than in FRF (0.05 vs. 0.04 t OC m and 286 vs. 201 t OC ha ). Modeling revealed tree species, fluctuation of groundwater table, and the distance to the river as valuable indicators for OC accretion rate. The OC concentration and distance to the river were positively and sedimentation negatively correlated with OC stock. The dike was consistently ruled out as a significant predictor variable. Consequently, differences among FRF and DRF seem to be related rather to longer term processes during the last centuries than directly to the dike. Our findings highlight the relevance of sediment quality (i.e., OC concentration) for building up long-term soil OC stocks, whereas sediment quantity is the main driver of recent OC accretion rates.
    Keywords: Carbon Accretion Rate ; Carbon Stock ; Dendrogeomorphology ; Dike ; Floodplain Forest ; Sedimentation Rate ; Geography ; Geology
    ISSN: 0169-555X
    E-ISSN: 1872-695X
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  • 4
    Description: Riparian forests are expected to play a crucial role in the global carbon (C) cycle but the complex mechanisms of C sequestration in forests remain poorly understood. This study used a comprehensive approach to analyze C sequestration that included the main C compartments in forests, i.e., litterfall, fine roots, and aboveground woody biomass. We aimed at modeling each of them in response to an array of environmental drivers to untangle the functioning of C sequestration by compartment. The study was conducted in a Central European riparian forest that is part of the Donau-Auen National Park in Austria. Carbon sequestration by compartment was correlated with environmental parameters (climate, stream flow, hydrological, spatial, and forest stand parameters) using generalized linear mixed models (GLMM), and the correlations were prioritized by hierarchical partitioning. Our results suggest divergent responses of C sequestration in different ecosystem compartments under dry and wet soil conditions. In particular, dry conditions led to significantly higher C sequestration in aboveground woody biomass (larger distance to the low groundwater table), whereas wetter conditions fostered C sequestration in fine-root (smaller magnitude of fluctuation in the groundwater table) and leaf biomass (smaller distance to the low groundwater table). Fine roots and litterfall responded to...
    Keywords: Biowissenschaften; Biologie ; Climate ; Danube River ; Fine Roots ; Flooding ; Fraxinus Excelsior ; Generalized Linear Mixed Model ; Hydrology ; Litterfall ; Populus Alba ; Quercus Robur ; Salix Alba ; Stem Production
    ISSN: 2150-8925
    Source: DataCite
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