TY - JOUR A1 - Wulf, Monika A1 - Rujner, Hendrik T1 - A GIS-based method for the reconstruction of the late eighteenth century forest vegetation in the Prignitz region (NE Germany) JF - Landscape ecology N2 - Our goal was to reconstruct the late eighteenth century forest vegetation of the Prignitz region (NE Germany) at a scale of 1:50,000. We also wanted to relate the historical forest vegetation to the actual and potential natural vegetation. For these purposes, we selected 15 woody species and transferred relevant data found in historical records from various sources together with the recent localities of (very) old individuals belonging to these woody species into ArcView GIS. Following multi-step data processing including the generation of a point density layer using a moving window with kernel estimation and derivation of vegetation units applying Boolean algebra rules together with information on site conditions, we derived 17 forest communities corresponding to the potential natural vegetation. We were able to reconstruct the historical forest vegetation for 90% of the forest area ca. 1780. Only two of the 17 forest communities covered large parts of the forested area. The oak forest with Agrostis capillaris covered about 44% of the total forest area, and alder forests on fenland made up about 37%. Oak-hornbeam forests with Stellaria holostea comprised slightly less than 6% of the forest area, while all other forest communities comprised less than 1%. The historical forest vegetation is more similar to the potential forest vegetation and quite different from the actual forest vegetation because coniferous tree species currently cover approximately two-thirds of the actual forest area. The most beneficial result of this study is the map of high-resolution historical vegetation units that may serve as the basis for various further studies, e.g., modelling long-term changes in biodiversity at the landscape scale. KW - Boolean algebra KW - Historical ecology KW - Kernel estimation KW - Moving window KW - Point density KW - Potential natural vegetation KW - Schmettau map KW - Toponymy KW - Vegetation map Y1 - 2011 U6 - https://doi.org/10.1007/s10980-010-9555-1 SN - 0921-2973 VL - 26 IS - 2 SP - 153 EP - 168 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Plue, Jan A1 - De Frenne, Pieter A1 - Acharya, Kamal P. A1 - Brunet, Jorg A1 - Chabrerie, Olivier A1 - Decocq, Guillaume A1 - Diekmann, Martin A1 - Graae, Bente J. A1 - Heinken, Thilo A1 - Hermy, Martin A1 - Kolb, Annette A1 - Lemke, Isgard A1 - Liira, Jaan A1 - Naaf, Tobias A1 - Shevtsova, Anna A1 - Verheyen, Kris A1 - Wulf, Monika A1 - Cousins, Sara A. O. T1 - Climatic control of forest herb seed banks along a latitudinal gradient JF - Global ecology and biogeography : a journal of macroecology N2 - Aim Seed banks are central to the regeneration strategy of many plant species. Any factor altering seed bank density thus affects plant regeneration and population dynamics. Although seed banks are dynamic entities controlled by multiple environmental drivers, climatic factors are the most comprehensive, but still poorly understood. This study investigates how climatic variation structures seed production and resulting seed bank patterns. Location Temperate forests along a 1900km latitudinal gradient in north-western (NW) Europe. Methods Seed production and seed bank density were quantified in 153 plots along the gradient for four forest herbs with different seed longevity: Geum urbanum, Milium effusum, Poa nemoralis and Stachys sylvatica. We tested the importance of climatic and local environmental factors in shaping seed production and seed bank density. Results Seed production was determined by population size, and not by climatic factors. G.urbanum and M.effusum seed bank density declined with decreasing temperature (growing degree days) and/or increasing temperature range (maximum-minimum temperature). P.nemoralis and S.sylvatica seed bank density were limited by population size and not by climatic variables. Seed bank density was also influenced by other, local environmental factors such as soil pH or light availability. Different seed bank patterns emerged due to differential seed longevities. Species with long-lived seeds maintained constant seed bank densities by counteracting the reduced chance of regular years with high seed production at colder northern latitudes. Main conclusions Seed bank patterns show clear interspecific variation in response to climate across the distribution range. Not all seed banking species may be as well equipped to buffer climate change via their seed bank, notably in short-term persistent species. Since the buffering capacity of seed banks is key to species persistence, these results provide crucial information to advance climatic change predictions on range shifts, community and biodiversity responses. KW - Climate change KW - interspecific variation KW - plant-climate interaction KW - seed longevity KW - seed production KW - temperate deciduous forest KW - temperature Y1 - 2013 U6 - https://doi.org/10.1111/geb.12068 SN - 1466-822X SN - 1466-8238 VL - 22 IS - 10 SP - 1106 EP - 1117 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Caron, Maria Mercedes A1 - De Frenne, Pieter A1 - Brunet, Jörg A1 - Chabrerie, Olivier A1 - Cousins, Sara A. O. A1 - Decocq, Guillaume A1 - Diekmann, Martin A1 - Graae, Bente Jessen A1 - Heinken, Thilo A1 - Kolb, Annette A1 - Lenoir, Jonathan A1 - Naaf, Tobias A1 - Plue, Jan A1 - Selvi, Federico A1 - Wulf, Monika A1 - Verheyen, Kris T1 - Divergent regeneration responses of two closely related tree species to direct abiotic and indirect biotic effects of climate change JF - Forest ecology and management N2 - Changing temperature and precipitation can strongly influence plant reproduction. However, also biotic interactions might indirectly affect the reproduction and recruitment success of plants in the context of climate change. Information about the interactive effects of changes in abiotic and biotic factors is essential, but still largely lacking, to better understand the potential effects of a changing climate on plant populations. Here we analyze the regeneration from seeds of Acer platanoides and Acer pseudoplatanus, two currently secondary forest tree species from seven regions along a 2200 km-wide latitudinal gradient in Europe. We assessed the germination, seedling survival and growth during two years in a common garden experiment where temperature, precipitation and competition with the understory vegetation were manipulated. A. platanoides was more sensitive to changes in biotic conditions while A. pseudoplatanus was affected by both abiotic and biotic changes. In general, competition reduced (in A. platanoides) and warming enhanced (in A. pseudoplatanus) germination and survival, respectively. Reduced competition strongly increased the growth of A. platanoides seedlings. Seedling responses were independent of the conditions experienced by the mother tree during seed production and maturation. Our results indicate that, due to the negative effects of competition on the regeneration of A. platanoides, it is likely that under stronger competition (projected under future climatic conditions) this species will be negatively affected in terms of germination, survival and seedling biomass. Climate-change experiments including both abiotic and biotic factors constitute a key step forward to better understand the response of tree species' regeneration to climate change. (C) 2015 Elsevier B.V. All rights reserved. KW - Acer KW - Regeneration KW - Latitudinal gradient KW - Temperature KW - Precipitation KW - Competition Y1 - 2015 U6 - https://doi.org/10.1016/j.foreco.2015.01.003 SN - 0378-1127 SN - 1872-7042 VL - 342 SP - 21 EP - 29 PB - Elsevier CY - Amsterdam ER - TY - JOUR A1 - Naaf, Tobias A1 - Wulf, Monika T1 - Does taxonomic homogenization imply functional homogenization in temperate forest herb layer communities? JF - Plant ecology : an international journal N2 - Biotic homogenization, the decrease in beta diversity among formerly distinct species assemblages, has been recognized as an important form of biotic impoverishment for more than a decade. Although researchers have stressed the importance of the functional dimension to understand its potential ecological consequences, biotic homogenization has mostly been studied at a taxonomic level. Here, we explore the relationship between taxonomic and functional homogenization using data on temperate forest herb layer communities in NW Germany, for which taxonomic homogenization has recently been demonstrated. We quantified beta diversity by partitioning Rao's quadratic entropy. We found a general positive relationship between changes in taxonomic and functional beta diversity. This relationship was stronger if multiple functional traits were taken into account. Averaged across sites, however, taxonomic homogenization was not consistently accompanied by functional homogenization. Depending on the traits considered, taxonomic homogenization occurred also together with functional differentiation or no change in functional beta diversity. The species shifts responsible for changes in beta diversity differed substantially between taxonomic and functional beta diversity measures and also among functional beta diversity measures based on different traits. We discuss likely environmental drivers for species shifts. Our study demonstrates that functional homogenization must be explicitly studied as an independent phenomenon that cannot be inferred from taxonomic homogenization. KW - Beta diversity KW - Biotic differentiation KW - Diversity partitioning KW - Functional diversity KW - Rao's quadratic entropy KW - Resurvey Y1 - 2012 U6 - https://doi.org/10.1007/s11258-011-9990-3 SN - 1385-0237 VL - 213 IS - 3 SP - 431 EP - 443 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Bernhardt-Römermann, Markus A1 - Baeten, Lander A1 - Craven, Dylan A1 - De Frenne, Pieter A1 - Hedl, Radim A1 - Lenoir, Jonathan A1 - Bert, Didier A1 - Brunet, Jorg A1 - Chudomelova, Marketa A1 - Decocq, Guillaume A1 - Dierschke, Hartmut A1 - Dirnboeck, Thomas A1 - Dörfler, Inken A1 - Heinken, Thilo A1 - Hermy, Martin A1 - Hommel, Patrick A1 - Jaroszewicz, Bogdan A1 - Keczynski, Andrzej A1 - Kelly, Daniel L. A1 - Kirby, Keith J. A1 - Kopecky, Martin A1 - Macek, Martin A1 - Malis, Frantisek A1 - Mirtl, Michael A1 - Mitchell, Fraser J. G. A1 - Naaf, Tobias A1 - Newman, Miles A1 - Peterken, George A1 - Petrik, Petr A1 - Schmidt, Wolfgang A1 - Standovar, Tibor A1 - Toth, Zoltan A1 - Van Calster, Hans A1 - Verstraeten, Gorik A1 - Vladovic, Jozef A1 - Vild, Ondrej A1 - Wulf, Monika A1 - Verheyen, Kris T1 - Drivers of temporal changes in temperate forest plant diversity vary across spatial scales JF - Global change biology N2 - Global biodiversity is affected by numerous environmental drivers. Yet, the extent to which global environmental changes contribute to changes in local diversity is poorly understood. We investigated biodiversity changes in a meta-analysis of 39 resurvey studies in European temperate forests (3988 vegetation records in total, 17-75years between the two surveys) by assessing the importance of (i) coarse-resolution (i.e., among sites) vs. fine-resolution (i.e., within sites) environmental differences and (ii) changing environmental conditions between surveys. Our results clarify the mechanisms underlying the direction and magnitude of local-scale biodiversity changes. While not detecting any net local diversity loss, we observed considerable among-site variation, partly explained by temporal changes in light availability (a local driver) and density of large herbivores (a regional driver). Furthermore, strong evidence was found that presurvey levels of nitrogen deposition determined subsequent diversity changes. We conclude that models forecasting future biodiversity changes should consider coarse-resolution environmental changes, account for differences in baseline environmental conditions and for local changes in fine-resolution environmental conditions. KW - atmospheric nitrogen deposition KW - evenness KW - forestREplot KW - forest management KW - game browsing KW - Shannon diversity KW - spatiotemporal resurvey data KW - species richness Y1 - 2015 U6 - https://doi.org/10.1111/gcb.12993 SN - 1354-1013 SN - 1365-2486 VL - 21 IS - 10 SP - 3726 EP - 3737 PB - Wiley-Blackwell CY - Hoboken ER - 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 - Wasof, Safaa A1 - Lenoir, Jonathan A1 - Gallet-Moron, Emilie A1 - Jamoneau, Aurelien A1 - Brunet, Jörg A1 - Cousins, Sara A. O. A1 - De Frenne, Pieter A1 - Diekmann, Martin A1 - Hermy, Martin A1 - Kolb, Annette A1 - Liira, Jaan A1 - Verheyen, Kris A1 - Wulf, Monika A1 - Decocq, Guillaume T1 - Ecological niche shifts of understorey plants along a latitudinal gradient of temperate forests in north-western Europe JF - Global ecology and biogeography : a journal of macroecology N2 - Aim In response to environmental changes and to avoid extinction, species may either track suitable environmental conditions or adapt to the modified environment. However, whether and how species adapt to environmental changes remains unclear. By focusing on the realized niche (i.e. the actual space that a species inhabits and the resources it can access as a result of limiting biotic factors present in its habitat), we here examine shifts in the realized-niche width (i.e. ecological amplitude) and position (i.e. ecological optimum) of 26 common and widespread forest understorey plants across their distributional ranges. Location Temperate forests along a ca. 1800-km-long latitudinal gradient from northern France to central Sweden and Estonia. Methods We derived species' realized-niche width from a -diversity metric, which increases if the focal species co-occurs with more species. Based on the concept that species' scores in a detrended correspondence analysis (DCA) represent the locations of their realized-niche positions, we developed a novel approach to run species-specific DCAs allowing the focal species to shift its realized-niche position along the studied latitudinal gradient while the realized-niche positions of other species were held constant. Results None of the 26 species maintained both their realized-niche width and position along the latitudinal gradient. Few species (9 of 26: 35%) shifted their realized-niche width, but all shifted their realized-niche position. With increasing latitude, most species (22 of 26: 85%) shifted their realized-niche position for soil nutrients and pH towards nutrient-poorer and more acidic soils. Main conclusions Forest understorey plants shifted their realized niche along the latitudinal gradient, suggesting local adaptation and/or plasticity. This macroecological pattern casts doubt on the idea that the realized niche is stable in space and time, which is a key assumption of species distribution models used to predict the future of biodiversity, hence raising concern about predicted extinction rates. KW - Beta diversity KW - climate change KW - detrended correspondence analyses KW - Ellenberg indicator values KW - forest understorey plant species KW - niche optimum KW - niche width KW - plant community KW - realized niche Y1 - 2013 U6 - https://doi.org/10.1111/geb.12073 SN - 1466-822X VL - 22 IS - 10 SP - 1130 EP - 1140 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Maes, Sybryn L. A1 - Perring, Michael P. A1 - Vanhellemont, Margot A1 - Depauw, Leen A1 - Van den Bulcke, Jan A1 - Brumelis, Guntis A1 - Brunet, Jorg A1 - Decocq, Guillaume A1 - den Ouden, Jan A1 - Härdtle, Werner A1 - Hedl, Radim A1 - Heinken, Thilo A1 - Heinrichs, Steffi A1 - Jaroszewicz, Bogdan A1 - Kopecký, Martin A1 - Malis, Frantisek A1 - Wulf, Monika A1 - Verheyen, Kris T1 - Environmental drivers interactively affect individual tree growth across temperate European forests JF - Global change biology N2 - Forecasting the growth of tree species to future environmental changes requires abetter understanding of its determinants. Tree growth is known to respond to global‐change drivers such as climate change or atmospheric deposition, as well as to localland‐use drivers such as forest management. Yet, large geographical scale studiesexamining interactive growth responses to multiple global‐change drivers are relativelyscarce and rarely consider management effects. Here, we assessed the interactiveeffects of three global‐change drivers (temperature, precipitation and nitrogen deposi-tion) on individual tree growth of three study species (Quercus robur/petraea, Fagus syl-vatica and Fraxinus excelsior). We sampled trees along spatial environmental gradientsacross Europe and accounted for the effects of management for Quercus. We collectedincrement cores from 267 trees distributed over 151 plots in 19 forest regions andcharacterized their neighbouring environment to take into account potentially confounding factors such as tree size, competition, soil conditions and elevation. Wedemonstrate that growth responds interactively to global‐change drivers, with species ‐specific sensitivities to the combined factors. Simultaneously high levels of precipita-tion and deposition benefited Fraxinus, but negatively affected Quercus’ growth, high-lighting species‐specific interactive tree growth responses to combined drivers. ForFagus, a stronger growth response to higher temperatures was found when precipita-tion was also higher, illustrating the potential negative effects of drought stress underwarming for this species. Furthermore, we show that past forest management canmodulate the effects of changing temperatures on Quercus’ growth; individuals in plotswith a coppicing history showed stronger growth responses to higher temperatures.Overall, our findings highlight how tree growth can be interactively determined by glo-bal‐change drivers, and how these growth responses might be modulated by past for-est management. By showing future growth changes for scenarios of environmentalchange, we stress the importance of considering multiple drivers, including past man-agement and their interactions, when predicting tree growth. KW - basal area increment KW - climate change KW - Fagus KW - Fraxinus KW - historical ecology KW - nitrogen deposition KW - Quercus KW - tree-ring analysis Y1 - 2018 U6 - https://doi.org/10.1111/gcb.14493 SN - 1354-1013 SN - 1365-2486 VL - 25 IS - 1 SP - 201 EP - 217 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Leuschner, Christoph A1 - Wulf, Monika A1 - Baeuchler, Patricia A1 - Hertel, Dietrich T1 - Forest continuity as a key determinant of soil carbon and nutrient storage in beech forests on sandy soils in Northern Germany JF - Ecosystems N2 - Forest (or tree) age has been identified as an important determinant of the carbon (C) storage potential of forest soils. A large part of Central Europe's current forested area was affected by land use change with long periods of cultivation in past centuries suggesting that the organic C stocks in the soil (SOC) under recent forest may partly be legacies of the past and that stand age effects have to be distinguished from forest continuity effects (that is, the time since re-afforestation). We examined the influence of mean tree age and forest continuity on the SOC pool and the stores of total N and available P, Ca, Mg, and K in the soil (mineral soil and organic layer) across a sample of 14 beech (Fagus sylvatica) forests on sandy soil with variable tree age (23-189 years) and forest continuity (50-year-old afforestation to ancient ('permanent') forest, that is, > 230 years of proven continuity). Ancient beech forests (> 230 years of continuity) stored on average 47 and 44% more organic C and total N in the soil than recent beech afforestation (50-128 years of continuity). Contrary to expectation, we found large and significant C and N pool differences between the forest categories in the mineral soil but not in the organic layer indicating that decade- or century-long cultivation has reduced the subsoil C and nutrient stores while the organic layer element pools have approached a new equilibrium after only 50-128 years. PCA and correlation analyses suggest that forest continuity cannot be ignored when trying to understand the variation in soil C stocks between different stands. Forest clearing, subsequent cultivation, and eventual re-afforestation with beech resulted in similar relative stock reductions of C and N and, thus, no change in soil C/N ratio. We conclude that the continuity of forest cover, which may or may not be related to tree age, is a key determinant of the soil C and nutrient stores of beech forests in the old cultural landscape of Central Europe. KW - afforestation KW - ancient forests KW - available phosphorus KW - calcium KW - Fagus sylvatica KW - forest clear-cut KW - magnesium KW - nitrogen KW - potassium KW - sandy soil Y1 - 2014 U6 - https://doi.org/10.1007/s10021-013-9738-0 SN - 1432-9840 SN - 1435-0629 VL - 17 IS - 3 SP - 497 EP - 511 PB - Springer CY - New York ER - TY - JOUR A1 - Nitsch, Paula A1 - Kaupenjohann, Martin A1 - Wulf, Monika T1 - Forest continuity, soil depth and tree species are important parameters for SOC stocks in an old forest (Templiner Buchheide, northeast Germany) JF - Geoderma : an international journal of soil science N2 - Forest mineral soils have the potential to accumulate large amounts of carbon (C). Numerous factors, which have often been insufficiently studied, affect soil organic C (SOC) stocks. Detailed knowledge of variation in SOC storage is important to assess the C accumulation potential of forest soils. To examine the impacts of forest continuity, soil depth and tree species on SOC stocks, 15 ancient ( > 230 years of forest continuity) and 15 old ( > 100 but < 200 years of forest continuity) forest soils, topsoil and subsoil in the Templiner Buchheide (Brandenburg, NE Germany) were compared. The old forest sites were afforested on former grassland or wasteland. On all sites grew one of three dominant tree species: European beech (Fagus sylvatica), Scots pine (Pinus sylvestris) or oak (Quercus spec.). Pine forest sites had been underplanted with beech and were mixed-species stands. Soil samples were taken down to a mean depth of 55 cm. Total contents of SOC, nitrogen (N), phosphorus (P), sulphur (S), calcium (Ca), potassium (K) and magnesium (Mg); soil pH; and bulk densities were determined. The soils of ancient forest sites stored significantly more total SOC, N, P, S, K and Mg than did the old ones. Mean total SOC stocks in ancient forests of all three tree species were 12-17% larger compared with those in old forests. Significant differences in SOC stocks between the two forest continuity groups appeared only in subsoil and not in topsoil. Pine forest stored larger SOC stocks than did beech and oak forests. Significant differences were found between ancient pine and oak forests and between ancient beech and oak forests. Soils in ancient beech and pine forests at depths of between 29 and 55 cm contained, on average, even 50% larger SOC stocks than did soils at the same depths in ancient oak forests and in all old forests. Forest continuity significantly affected SOC stocks. These results support previous studies that old forests are still able to enrich SOC. Although soil samples were carried out to a mean depth of only 55 cm, the results indicate that differences in SOC stocks between ancient and old forest could also be found in deeper soil layers. It was suggested that beech and mixed-species stands of beech and pine and total soil P stocks had a positive effect on SOC stocks in subsoil. To understand SOC accumulation in forests, especially in subsoil, with a forest continuity of > 100 years, the role of different tree species and of total P cycling in forests, deeper sampling depths and repeated sampling would be required. KW - Ancient forest KW - C sequestration KW - Land-use history KW - Forest age KW - Total P KW - Subsoil Y1 - 2017 U6 - https://doi.org/10.1016/j.geoderma.2017.08.041 SN - 0016-7061 SN - 1872-6259 VL - 310 SP - 65 EP - 76 PB - Elsevier Science CY - Amsterdam ER -