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      Post‐glacial range formation of temperate forest understorey herbs – Insights from a spatio‐temporally explicit modelling approach

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          Abstract

          Aim

          Our knowledge of Pleistocene refugia and post‐glacial recolonization routes of forest understorey plants is still very limited. The geographical ranges of these species are often rather narrow and show highly idiosyncratic, often fragmented patterns indicating either narrow and species‐specific ecological tolerances or strong dispersal limitations. However, the relative roles of these factors are inherently difficult to disentangle.

          Location

          Central and south‐eastern Europe.

          Time period

          17,100 BP – present.

          Major taxa studied

          Five understorey herbs of European beech forests: Aposeris foetida, Cardamine trifolia, Euphorbia carniolica, Hacquetia epipactis and Helleborus niger.

          Methods

          We used spatio‐temporally explicit modelling to reconstruct the post‐glacial range dynamics of the five forest understorey herbs. We varied niche requirements, demographic rates and dispersal abilities across plausible ranges and simulated the spread of species from potential Pleistocene refugia identified by phylogeographical analyses. Then we identified the parameter settings allowing for the most accurate reconstruction of their current geographical ranges.

          Results

          We found a largely homogenous pattern of optimal parameter settings among species. Broad ecological niches had to be combined with very low but non‐zero rates of long‐distance dispersal via chance events and low rates of seed dispersal over moderate distances by standard dispersal vectors. However, long‐distance dispersal events, although rare, led to high variation among replicated simulation runs.

          Main conclusions

          Small and fragmented ranges of many forest understorey species are best explained by a combination of broad ecological niches and rare medium‐ and long‐distance dispersal events. Stochasticity is thus an important determinant of current species ranges, explaining the idiosyncratic distribution patterns of the study species despite strong similarities in refugia, ecological tolerances and dispersal abilities.

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          Most cited references61

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          Climatologies at high resolution for the earth’s land surface areas

          High-resolution information on climatic conditions is essential to many applications in environmental and ecological sciences. Here we present the CHELSA (Climatologies at high resolution for the earth’s land surface areas) data of downscaled model output temperature and precipitation estimates of the ERA-Interim climatic reanalysis to a high resolution of 30 arc sec. The temperature algorithm is based on statistical downscaling of atmospheric temperatures. The precipitation algorithm incorporates orographic predictors including wind fields, valley exposition, and boundary layer height, with a subsequent bias correction. The resulting data consist of a monthly temperature and precipitation climatology for the years 1979–2013. We compare the data derived from the CHELSA algorithm with other standard gridded products and station data from the Global Historical Climate Network. We compare the performance of the new climatologies in species distribution modelling and show that we can increase the accuracy of species range predictions. We further show that CHELSA climatological data has a similar accuracy as other products for temperature, but that its predictions of precipitation patterns are better.
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            Assessing the accuracy of species distribution models: prevalence, kappa and the true skill statistic (TSS)

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              The Phanerozoic record of global sea-level change.

              K. Miller (2005)
              We review Phanerozoic sea-level changes [543 million years ago (Ma) to the present] on various time scales and present a new sea-level record for the past 100 million years (My). Long-term sea level peaked at 100 +/- 50 meters during the Cretaceous, implying that ocean-crust production rates were much lower than previously inferred. Sea level mirrors oxygen isotope variations, reflecting ice-volume change on the 10(4)- to 10(6)-year scale, but a link between oxygen isotope and sea level on the 10(7)-year scale must be due to temperature changes that we attribute to tectonically controlled carbon dioxide variations. Sea-level change has influenced phytoplankton evolution, ocean chemistry, and the loci of carbonate, organic carbon, and siliciclastic sediment burial. Over the past 100 My, sea-level changes reflect global climate evolution from a time of ephemeral Antarctic ice sheets (100 to 33 Ma), through a time of large ice sheets primarily in Antarctica (33 to 2.5 Ma), to a world with large Antarctic and large, variable Northern Hemisphere ice sheets (2.5 Ma to the present).
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                Author and article information

                Contributors
                wolfgang.willner@univie.ac.at
                Journal
                Glob Ecol Biogeogr
                Glob Ecol Biogeogr
                10.1111/(ISSN)1466-8238
                GEB
                Global Ecology and Biogeography
                John Wiley and Sons Inc. (Hoboken )
                1466-822X
                1466-8238
                10 April 2023
                July 2023
                : 32
                : 7 ( doiID: 10.1111/geb.v32.7 )
                : 1046-1058
                Affiliations
                [ 1 ] Department of Botany and Biodiversity Research University of Vienna Rennweg 14 Vienna 1030 Austria
                [ 2 ] Vienna Doctoral School of Ecology and Evolution (VDSEE) University of Vienna Djerassiplatz 1 Vienna 1030 Austria
                [ 3 ] Department of Botany University of Innsbruck Sternwartestr. 15 Innsbruck 6020 Austria
                [ 4 ] Institute of Botany of the Czech Academy of Sciences Zámek 1 Průhonice 252 43 Czech Republic
                Author notes
                [*] [* ] Correspondence

                Wolfgang Willner, Department of Botany and Biodiversity Research, University of Vienna, Rennweg 14, Vienna 1030, Austria.

                Email: wolfgang.willner@ 123456univie.ac.at

                Author information
                https://orcid.org/0000-0003-1591-8386
                https://orcid.org/0000-0003-3919-0887
                Article
                GEB13677 GEB-2022-0147.R2
                10.1111/geb.13677
                10947399
                38504871
                f9036c15-7f8c-411d-9a71-d71216affa08
                © 2023 The Authors. Global Ecology and Biogeography published by John Wiley & Sons Ltd.

                This is an open access article under the terms of the http://creativecommons.org/licenses/by/4.0/ License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

                History
                : 03 February 2023
                : 09 March 2022
                : 22 February 2023
                Page count
                Figures: 5, Tables: 1, Pages: 13, Words: 9847
                Funding
                Funded by: Austrian Science Fund , doi 10.13039/501100002428;
                Award ID: P29413
                Categories
                Research Article
                Research Articles
                Custom metadata
                2.0
                July 2023
                Converter:WILEY_ML3GV2_TO_JATSPMC version:6.3.9 mode:remove_FC converted:18.03.2024

                dispersal limitation,europe,forest herbs,long‐distance dispersal,pleistocene refugia,post‐glacial recolonization,range filling,spatio‐temporally explicit modelling

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