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  -