TY - JOUR A1 - Perring, Michael P. A1 - Bernhardt-Roemermann, Markus A1 - Baeten, Lander A1 - Midolo, Gabriele A1 - Blondeel, Haben A1 - Depauw, Leen A1 - Landuyt, Dries A1 - Maes, Sybryn L. A1 - De Lombaerde, Emiel A1 - Caron, Maria Mercedes A1 - Vellend, Mark A1 - Brunet, Joerg A1 - Chudomelova, Marketa A1 - Decocq, Guillaume A1 - Diekmann, Martin A1 - Dirnboeck, Thomas A1 - Doerfler, Inken A1 - Durak, Tomasz A1 - De Frenne, Pieter A1 - Gilliam, Frank S. A1 - Hedl, Radim A1 - Heinken, Thilo A1 - Hommel, Patrick A1 - Jaroszewicz, Bogdan A1 - Kirby, Keith J. A1 - Kopecky, Martin A1 - Lenoir, Jonathan A1 - Li, Daijiang A1 - Malis, Frantisek A1 - Mitchell, Fraser J. G. A1 - Naaf, Tobias A1 - Newman, Miles A1 - Petrik, Petr A1 - Reczynska, Kamila A1 - Schmidt, Wolfgang A1 - Standovar, Tibor A1 - Swierkosz, Krzysztof A1 - Van Calster, Hans A1 - Vild, Ondrej A1 - Wagner, Eva Rosa A1 - Wulf, Monika A1 - Verheyen, Kris T1 - Global environmental change effects on plant community composition trajectories depend upon management legacies JF - Global change biology N2 - The contemporary state of functional traits and species richness in plant communities depends on legacy effects of past disturbances. Whether temporal responses of community properties to current environmental changes are altered by such legacies is, however, unknown. We expect global environmental changes to interact with land-use legacies given different community trajectories initiated by prior management, and subsequent responses to altered resources and conditions. We tested this expectation for species richness and functional traits using 1814 survey-resurvey plot pairs of understorey communities from 40 European temperate forest datasets, syntheses of management transitions since the year 1800, and a trait database. We also examined how plant community indicators of resources and conditions changed in response to management legacies and environmental change. Community trajectories were clearly influenced by interactions between management legacies from over 200 years ago and environmental change. Importantly, higher rates of nitrogen deposition led to increased species richness and plant height in forests managed less intensively in 1800 (i.e., high forests), and to decreases in forests with a more intensive historical management in 1800 (i.e., coppiced forests). There was evidence that these declines in community variables in formerly coppiced forests were ameliorated by increased rates of temperature change between surveys. Responses were generally apparent regardless of sites’ contemporary management classifications, although sometimes the management transition itself, rather than historic or contemporary management types, better explained understorey responses. Main effects of environmental change were rare, although higher rates of precipitation change increased plant height, accompanied by increases in fertility indicator values. Analysis of indicator values suggested the importance of directly characterising resources and conditions to better understand legacy and environmental change effects. Accounting for legacies of past disturbance can reconcile contradictory literature results and appears crucial to anticipating future responses to global environmental change. KW - biodiversity change KW - climate change KW - disturbance regime KW - forestREplot KW - herbaceous layer KW - management intensity KW - nitrogen deposition KW - plant functional traits KW - time lag KW - vegetation resurvey Y1 - 2017 U6 - https://doi.org/10.1111/gcb.14030 SN - 1354-1013 SN - 1365-2486 VL - 24 IS - 4 SP - 1722 EP - 1740 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - De Frenne, Pieter A1 - Rodriguez-Sanchez, Francisco A1 - Coomes, David Anthony A1 - Bäten, Lander A1 - Versträten, Gorik A1 - Vellend, Mark A1 - Bernhardt-Römermann, Markus A1 - Brown, Carissa D. A1 - Brunet, Jörg A1 - Cornelis, Johnny A1 - Decocq, Guillaume M. A1 - Dierschke, Hartmut A1 - Eriksson, Ove A1 - Gilliam, Frank S. A1 - Hedl, Radim A1 - Heinken, Thilo A1 - Hermy, Martin A1 - Hommel, Patrick A1 - Jenkins, Michael A. A1 - Kelly, Daniel L. A1 - Kirby, Keith J. A1 - Mitchell, Fraser J. G. A1 - Naaf, Tobias A1 - Newman, Miles A1 - Peterken, George A1 - Petrik, Petr A1 - Schultz, Jan A1 - Sonnier, Gregory A1 - Van Calster, Hans A1 - Waller, Donald M. A1 - Walther, Gian-Reto A1 - White, Peter S. A1 - Woods, Kerry D. A1 - Wulf, Monika A1 - Graae, Bente Jessen A1 - Verheyen, Kris T1 - Microclimate moderates plant responses to macroclimate warming JF - Proceedings of the National Academy of Sciences of the United States of America N2 - Recent global warming is acting across marine, freshwater, and terrestrial ecosystems to favor species adapted to warmer conditions and/or reduce the abundance of cold-adapted organisms (i.e., "thermophilization" of communities). Lack of community responses to increased temperature, however, has also been reported for several taxa and regions, suggesting that "climatic lags" may be frequent. Here we show that microclimatic effects brought about by forest canopy closure can buffer biotic responses to macroclimate warming, thus explaining an apparent climatic lag. Using data from 1,409 vegetation plots in European and North American temperate forests, each surveyed at least twice over an interval of 12-67 y, we document significant thermophilization of ground-layer plant communities. These changes reflect concurrent declines in species adapted to cooler conditions and increases in species adapted to warmer conditions. However, thermophilization, particularly the increase of warm-adapted species, is attenuated in forests whose canopies have become denser, probably reflecting cooler growing-season ground temperatures via increased shading. As standing stocks of trees have increased in many temperate forests in recent decades, local microclimatic effects may commonly be moderating the impacts of macroclimate warming on forest understories. Conversely, increases in harvesting woody biomass-e.g., for bioenergy-may open forest canopies and accelerate thermophilization of temperate forest biodiversity. KW - climate change KW - forest management KW - understory KW - climatic debt KW - range shifts Y1 - 2013 U6 - https://doi.org/10.1073/pnas.1311190110 SN - 0027-8424 VL - 110 IS - 46 SP - 18561 EP - 18565 PB - National Acad. of Sciences CY - Washington 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 - Baeten, Lander A1 - Warton, David I. A1 - Van Calster, Hans A1 - De Frenne, Pieter A1 - Verstraeten, Gorik A1 - Bonte, Dries A1 - Bernhardt-Römermann, Markus A1 - Cornelis, Johnny A1 - Decocq, Guillaume A1 - Eriksson, Ove A1 - Hedl, Radim A1 - Heinken, Thilo A1 - Hermy, Martin A1 - Hommel, Patrick A1 - Kirby, Keith J. A1 - Naaf, Tobias A1 - Petrik, Petr A1 - Walther, Gian-Reto A1 - Wulf, Monica A1 - Verheyen, Kris T1 - A model-based approach to studying changes in compositional heterogeneity JF - Methods in ecology and evolution : an official journal of the British Ecological Society Y1 - 2014 SN - 2041-210X SN - 2041-2096 VL - 5 IS - 2 SP - 156 EP - 164 PB - Wiley-Blackwell CY - Hoboken 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 -