TY - JOUR A1 - Verheyen, Kris A1 - Baeten, Lander A1 - De Frenne, Pieter A1 - Bernhardt-Römermann, Markus A1 - Brunet, Jorg A1 - Cornelis, Johnny A1 - Decocq, Guillaume A1 - Dierschke, Hartmut A1 - Eriksson, Ove A1 - Hedl, Radim A1 - Heinken, Thilo A1 - Hermy, Martin A1 - Hommel, Patrick A1 - Kirby, Keith J. A1 - Naaf, Tobias A1 - Peterken, George A1 - Petrik, Petr A1 - Pfadenhauer, Joerg A1 - Van Calster, Hans A1 - Walther, Gian-Reto A1 - Wulf, Monika A1 - Verstraeten, Gorik T1 - Driving factors behind the eutrophication signal in understorey plant communities of deciduous temperate forests JF - The journal of ecology N2 - 1. Atmospheric nitrogen (N) deposition is expected to change forest understorey plant community composition and diversity, but results of experimental addition studies and observational studies are not yet conclusive. A shortcoming of observational studies, which are generally based on resurveys or sampling along large deposition gradients, is the occurrence of temporal or spatial confounding factors. 2. We were able to assess the contribution of N deposition versus other ecological drivers on forest understorey plant communities by combining a temporal and spatial approach. Data from 1205 (semi-)permanent vegetation plots taken from 23 rigorously selected understorey resurvey studies along a large deposition gradient across deciduous temperate forest in Europe were compiled and related to various local and regional driving factors, including the rate of atmospheric N deposition, the change in large herbivore densities and the change in canopy cover and composition. 3. Although no directional change in species richness occurred, there was considerable floristic turnover in the understorey plant community and a shift in species composition towards more shade-tolerant and nutrient-demanding species. However, atmospheric N deposition was not important in explaining the observed eutrophication signal. This signal seemed mainly related to a shift towards a denser canopy cover and a changed canopy species composition with a higher share of species with more easily decomposed litter. 4. Synthesis. Our multi-site approach clearly demonstrates that one should be cautious when drawing conclusions about the impact of atmospheric N deposition based on the interpretation of plant community shifts in single sites or regions due to other, concurrent, ecological changes. Even though the effects of chronically increased N deposition on the forest plant communities are apparently obscured by the effects of canopy changes, the accumulated N might still have a significant impact. However, more research is needed to assess whether this N time bomb will indeed explode when canopies will open up again. KW - atmospheric deposition KW - determinants of plant community diversity and structure KW - Ellenberg indicator values KW - forest herbs KW - forest management KW - large herbivores KW - north-western Europe KW - resurveys KW - (semi-)permanent plots Y1 - 2012 U6 - https://doi.org/10.1111/j.1365-2745.2011.01928.x SN - 0022-0477 VL - 100 IS - 2 SP - 352 EP - 365 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Kaiser, Thomas A1 - Wehrhan, Marc A1 - Werner, Armin A1 - Sommer, Michael T1 - Regionalizing ecological moisture levels and groundwater levels in grassland areas using thermal remote sensing JF - Grassland science N2 - Site-specific soil moisture and groundwater levels are key input parameters for ecological modeling. Obtaining such information in a comprehensive manner is difficult for large regions. We studied a floodplain region in the Federal State of Brandenburg, Germany, to examine the degree to which the average depth of groundwater tables can be derived from surface temperatures obtained by the ASTER radiospectrometer (spatial resolution of 90 m per pixel). A floristic ecological indicator representing the site-specific moisture level was applied to develop a proxy between the thermal satellite data and groundwater table depth. The use of spring scenes (late April to early May) from 2 years proved to be well suited for minimizing the effects of weather and land use. Vegetation surveys along transects that were 2 m wide across the pixel diagonals allowed for the calculation of average ecological moisture values of pixel-sites by applying Ellenberg-numbers. These values were used to calibrate the satellite data locally. There was a close relationship between surface temperature and the average ecological moisture value (R2 = 0.73). Average ecological moisture values were highly indicative of the average groundwater levels during a 7-year measurement series (R2 = 0.93). Satellite-supported thermal data from spring were suitable for estimating the average groundwater levels of low-lying grasslands on a larger scale. Ecological moisture values from the transect surveys effectively allowed the incorporation of relief heterogeneity within the thermal grid and the establishment of the correlation between thermal data and average groundwater table depth. Regression functions were used to produce a map of groundwater levels at the study site. KW - Ellenberg indicator values KW - groundwater table KW - satellite data KW - soil moisture Y1 - 2012 U6 - https://doi.org/10.1111/j.1744-697X.2011.00240.x SN - 1744-6961 VL - 58 IS - 1 SP - 42 EP - 52 PB - Wiley-Blackwell CY - Malden ER -