TY - JOUR A1 - Heinken, Thilo A1 - Weber, Ewald T1 - Consequences of habitat fragmentation for plant species do we know enough? JF - Perspectives in plant ecology, evolution and systematics N2 - Habitat fragmentation is one of the most important causes for the decline of plant species. However, plants differing in phylogeny, habitat requirements and biology are likely to respond differently to habitat fragmentation. We ask whether case studies on the effects of habitat fragmentation conducted so far allow generalizations about its effects on the fitness and genetic diversity of populations of endangered plant species. We compared the characteristics of plant species endangered in Germany whose sensitivity to habitat fragmentation had been studied with those of the endangered species that had not been studied. We found strong discrepancies between the two groups with regard to their taxonomy and traits relevant to their sensitivity to habitat fragmentation. Monocots, graminoids, clonal, abiotically pollinated and self compatible species were underrepresented among the studied species, and most study species were from a few habitat types, in particular grasslands. We conclude that our current knowledge of the effects of habitat fragmentation on plant populations is not sufficient to provide widely applicable guidelines for species management. The selection of species studied so far has been biased toward species from certain habitats and species exhibiting traits that probably make them vulnerable to habitat fragmentation. Future studies should include community-wide approaches in different habitats, e.g. re-visitation studies in which the species pool is assessed at different time intervals, and population-biological studies of species from a wide range of habitats, and of different life forms and growth strategies. A more representative picture of the effects of habitat fragmentation would allow a better assessment of threats and more specific recommendations for optimally managing populations of endangered plants. KW - CSR-strategies KW - Naturally rare species KW - Plant conservation KW - Recently rare species KW - Species traits KW - Taxonomic position Y1 - 2013 U6 - https://doi.org/10.1016/j.ppees.2013.05.003 SN - 1433-8319 VL - 15 IS - 4 SP - 205 EP - 216 PB - Elsevier CY - Jena 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 - Schwarzer, Christian A1 - Heinken, Thilo A1 - Luthardt, Vera A1 - Joshi, Jasmin Radha T1 - Latitudinal shifts in species interactions interfere with resistance of southern but not of northern bog-plant communities to experimental climate change JF - The journal of ecology N2 - The persistence of species under changed climatic conditions depends on adaptations and plastic responses to these conditions and on interactions with their local plant community resulting in direct and indirect effects of changed climatic conditions. Populations at species' range margins may be especially crucial in containing a gene pool comprising adaptations to extreme climatic conditions. Many species of northern European bog ecosystems reach their southern lowland range limit in central Europe. In a common-garden experiment, we experimentally assessed the impact of projected climatic changes on five bog-plant species (including peat moss Sphagnum magellanicum) sampled along a latitudinal gradient of 1400km from Scandinavia to the marginal lowland populations in Germany. Populations were cultivated in monocultures and in experimental communities composed of all five species from their local community, and exposed to five combinations of three climate treatments (warming, fluctuating water-tables, fertilization) in a southern common garden. Whereas most monocultures showed a decreasing biomass production from southern to northern origins under southern environmental conditions, in the experimental mixed-species communities, an increasing biomass production towards northern communities was observed together with a shift in interspecific interactions along the latitudinal gradient. While negative dominance effects prevailed in southern communities, higher net biodiversity effects were observed in northern subarctic communities. The combined effects of climate treatments increased biomass production in monocultures of most origins. In communities, however, overall the treatments did not result in significantly changed biomass production. Among individual treatments, water-table fluctuations caused a significant decrease in biomass production, but only in southern communities, indicating higher vulnerability to changed climatic conditions. Here, negative effects of climate treatments on graminoids were not compensated by the slightly increased growth of peat moss that benefited from interspecific interactions only in northern communities.Synthesis. We conclude that shifting interactions within multispecies communities caused pronounced responses to changed climatic conditions in wetland communities of temperate southern marginal, but not of northern subarctic origin. Therefore, future models investigating the impacts of climate change on plant communities should consider geographical variation in species interactions an important factor influencing community responses to changed climatic conditions. KW - additive partitioning of biodiversity effects KW - biodiversity KW - ecosystem services KW - ecosystem stability KW - intraspecific divergence KW - multifactorial environmental change KW - nitrogen deposition KW - northern peatlands KW - Sphagnum magellanicum KW - wetland ecosystems Y1 - 2013 U6 - https://doi.org/10.1111/1365-2745.12158 SN - 0022-0477 SN - 1365-2745 VL - 101 IS - 6 SP - 1484 EP - 1497 PB - Wiley-Blackwell 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 - Liang, Wei A1 - Heinrich, Ingo A1 - Simard, Sonia A1 - Helle, Gerhard A1 - Linan, Isabel Dorado A1 - Heinken, Thilo T1 - Climate signals derived from cell anatomy of Scots pine in NE Germany JF - Tree physiology N2 - Tree-ring chronologies of Pinus sylvestris L. from latitudinal and altitudinal limits of the species distribution have been widely used for climate reconstructions, but there are many sites within the temperate climate zone, as is the case in northeastern Germany, at which there is little evidence of a clear climate signal in the chronologies. In this study, we developed long chronologies of several cell structure variables (e. g., average lumen area and cell wall thickness) from P. sylvestris growing in northeastern Germany and investigated the influence of climate on ring widths and cell structure variables. We found significant correlations between cell structure variables and temperature, and between tree-ring width and relative humidity and vapor pressure, respectively, enabling the development of robust reconstructions from temperate sites that have not yet been realized. Moreover, it has been shown that it may not be necessary to detrend chronologies of cell structure variables and thus low-frequency climate signals may be retrieved from longer cell structure chronologies. The relatively extensive resource of archaeological material of P. sylvestris covering approximately the last millennium may now be useful for climate reconstructions in northeastern Germany and other sites in the temperate climate zone. KW - cell structure KW - dendroclimatology KW - Pinus sylvestris KW - quantitative wood anatomy KW - tree rings Y1 - 2013 U6 - https://doi.org/10.1093/treephys/tpt059 SN - 0829-318X SN - 1758-4469 VL - 33 IS - 8 SP - 833 EP - 844 PB - Oxford Univ. Press CY - Oxford ER - TY - JOUR A1 - Liang, Wei A1 - Heinrich, Ingo A1 - Helle, Gerhard A1 - Linan, Isabel Dorado A1 - Heinken, Thilo T1 - Applying CLSM to increment core surfaces for histometric analyses a novel advance in quantitative wood anatomy JF - Dendrochronologia : an interdisciplinary journal of tree-ring science N2 - A novel procedure has been developed to conduct cell structure measurements on increment core samples of conifers. The procedure combines readily available hardware and software equipment. The essential part of the procedure is the application of a confocal laser scanning microscope (CLSM) which captures images directly from increment cores surfaced with the advanced WSL core-microtome. Cell wall and lumen are displayed with a strong contrast due to the monochrome black and green nature of the images. Consecutive images are merged into long images representing entire increment cores which are then analysed for cell structures in suitable software. KW - Wood anatomy KW - Cell structures KW - Confocal laser scanning microscopy KW - CLSM KW - Dendrochronology KW - Surface preparation Y1 - 2013 U6 - https://doi.org/10.1016/j.dendro.2012.09.002 SN - 1125-7865 VL - 31 IS - 2 SP - 140 EP - 145 PB - Elsevier CY - Jena ER -