| Literature DB >> 34248371 |
João C Campos1, Sara Rodrigues1, Teresa Freitas2, João A Santos2, João P Honrado1, Adrián Regos3.
Abstract
BACKGROUND: Climate change has been widely accepted as one of the major threats for global biodiversity and understanding its potential effects on species distribution is crucial to optimise conservation planning in future scenarios under global change. Integrating detailed climatic data across spatial and temporal scales into species distribution modelling can help to predict potential changes in biodiversity. Consequently, this type of data can be useful for developing efficient biodiversity management and conservation planning. The provision of such data becomes even more important in highly biodiverse regions, currently suffering from climatic and landscape changes. The Transboundary Biosphere Reserve of Meseta Ibérica (BRMI; Portugal-Spain) is one of the most relevant reserves for wildlife in Europe. This highly diverse region is of great ecological and socio-economical interest, suffering from synergistic processes of rural land abandonment and climatic instabilities that currently threaten local biodiversity.Aiming to optimise conservation planning in the Reserve, we provide a complete dataset of historical and future climate models (1 x 1 km) for the BRMI, used to build a series of distribution models for 207 vertebrate species. These models are projected for 2050 under two climate change scenarios. The climatic suitability of 52% and 57% of the species are predicted to decrease under the intermediate and extreme climatic scenarios, respectively. These models constitute framework data for improving local conservation planning in the Reserve, which should be further supported by implementing climate and land-use change factors to increase the accuracy of future predictions of species distributions in the study area. NEW INFORMATION: Herein, we provide a complete dataset of state-of-the-art historical and future climate model simulations, generated by global-regional climate model chains, with climatic variables resolved at a high spatial resolution (1 × 1 km) over the Transboundary Biosphere Reserve of Meseta Ibérica. Additionally, a complete series of distribution models for 207 species (168 birds, 24 reptiles and 15 amphibians) under future (2050) climate change scenarios is delivered, which constitute framework data for improving local conservation planning in the reserve. João C. Campos, Sara Rodrigues, Teresa Freitas, João A. Santos, João P. Honrado, Adrián Regos.Entities:
Keywords: Iberian Peninsula; biodiversity; climate change; climate models; conservation; species distribution models.
Year: 2021 PMID: 34248371 PMCID: PMC8249360 DOI: 10.3897/BDJ.9.e66509
Source DB: PubMed Journal: Biodivers Data J ISSN: 1314-2828
Figure 1.Geographic location of the study areas: the Iberian Peninsula (climate variables and biodiversity data provided at 10 × 10 km resolution) and the Transboundary Biosphere Reserve of Meseta Ibérica (data provided at 1 × 1 km resolution).
Species information: taxonomic group, scientific name, species code and number of presences used for modelling (N). The quality threshold (area under the curve - AUC) used for model selection (to be included on ensemble modelling) are indicated. The accuracy metrics of ensemble species distribution models (SDMs), measured by the AUC and True Skill Statistics (TSS), are also mentioned. Ten model replicates were conducted for each species.
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| ACI | 1253 | 0.8 | 0.96 | 0.795 |
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| AOB | 2336 | 0.8 | 0.927 | 0.681 |
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| BSP | 4471 | 0.7 | 0.915 | 0.654 |
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| DGA | 1930 | 0.7 | 0.993 | 0.924 |
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| ECA | 3973 | 0.7 | 0.949 | 0.757 |
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| HMO | 1502 | 0.8 | 0.957 | 0.759 |
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| LBO | 1695 | 0.8 | 0.948 | 0.76 |
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| LHE | 701 | 0.8 | 0.971 | 0.833 |
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| PCU | 2221 | 0.8 | 0.968 | 0.786 |
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| PPE | 5587 | 0.8 | 0.989 | 0.932 |
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| PPU | 1765 | 0.7 | 0.95 | 0.776 |
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| PWA | 1897 | 0.8 | 0.918 | 0.659 |
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| RIB | 953 | 0.8 | 0.984 | 0.871 |
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| SSA | 2422 | 0.8 | 0.928 | 0.706 | |
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| TMA | 2485 | 0.7 | 0.924 | 0.673 | |
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| ACCGENT | 2266 | 0.7 | 0.991 | 0.895 |
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| ACCNISU | 2565 | 0.7 | 0.984 | 0.88 |
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| ACRARUN | 1348 | 0.8 | 0.99 | 0.908 |
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| ACRSCIR | 1581 | 0.7 | 0.991 | 0.912 |
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| AEGCAUD | 4157 | 0.7 | 0.888 | 0.599 |
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| ALAARVE | 2999 | 0.8 | 0.896 | 0.62 |
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| ALCATTH | 2285 | 0.7 | 0.861 | 0.542 |
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| ALERUFA | 5050 | 0.7 | 0.946 | 0.803 |
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| ANACLYP | 141 | 0.8 | 0.987 | 0.945 |
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| ANAPLAT | 3354 | 0.7 | 0.871 | 0.56 |
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| ANASTRE | 305 | 0.8 | 0.981 | 0.913 |
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| ANTCAMP | 2248 | 0.8 | 0.896 | 0.614 |
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| ANTSPIN | 439 | 0.8 | 0.987 | 0.908 |
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| ANTTRIV | 1163 | 0.8 | 0.97 | 0.846 |
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| APUMELB | 1047 | 0.7 | 0.975 | 0.849 |
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| APUPALL | 847 | 0.8 | 0.945 | 0.75 |
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| AQUCHRY | 700 | 0.7 | 0.968 | 0.835 |
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| ARDCINE | 543 | 0.7 | 0.994 | 0.944 |
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| ARDPURP | 259 | 0.8 | 0.977 | 0.872 |
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| ASIFLAM | 77 | 0.8 | 0.991 | 0.973 |
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| ASIOTUS | 1362 | 0.7 | 0.893 | 0.597 |
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| ATHNOCT | 4424 | 0.7 | 0.962 | 0.793 |
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| AYTFERI | 195 | 0.8 | 0.987 | 0.94 |
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| BUBBUBO | 2141 | 0.7 | 0.88 | 0.601 |
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| BUBIBIS | 287 | 0.8 | 0.964 | 0.827 |
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| BUROEDI | 2264 | 0.8 | 0.975 | 0.836 |
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| BUTBUTE | 4504 | 0.7 | 0.867 | 0.546 |
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| CALBRAC | 2245 | 0.8 | 0.992 | 0.909 |
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| CALRUFE | 246 | 0.8 | 0.985 | 0.903 |
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| CAPEURO | 1979 | 0.8 | 0.899 | 0.618 |
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| CAPRUFI | 1781 | 0.8 | 0.916 | 0.656 |
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| CARSPIN | 84 | 0.8 | 0.99 | 0.963 |
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| CECDAUR | 1253 | 0.8 | 0.992 | 0.952 |
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| CERBRAC | 2336 | 0.7 | 0.868 | 0.56 |
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| CETCETT | 4471 | 0.7 | 0.927 | 0.674 |
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| CHADUBI | 1930 | 0.7 | 0.989 | 0.896 |
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| CHEDUPO | 3973 | 0.8 | 0.98 | 0.907 |
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| CHLHYBR | 1502 | 0.8 | 0.991 | 0.959 |
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| CICCICO | 1695 | 0.8 | 0.927 | 0.705 |
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| CICNIGR | 701 | 0.8 | 0.964 | 0.838 |
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| CINCINC | 2221 | 0.8 | 0.937 | 0.728 |
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| CIRAERU | 5587 | 0.8 | 0.979 | 0.891 |
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| CIRCYAN | 1765 | 0.8 | 0.963 | 0.832 |
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| CIRGALL | 1897 | 0.7 | 0.944 | 0.728 |
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| CIRPYGA | 953 | 0.7 | 0.992 | 0.913 |
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| CISJUNC | 2422 | 0.8 | 0.97 | 0.814 |
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| CLAGLAN | 2485 | 0.7 | 0.994 | 0.925 |
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| COCCOCC | 2266 | 0.8 | 0.965 | 0.818 |
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| COLLIVI | 2565 | 0.7 | 0.945 | 0.787 |
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| COLOENA | 1348 | 0.8 | 0.917 | 0.68 |
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| COLPALU | 1581 | 0.7 | 0.947 | 0.793 |
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| CORCORO | 4157 | 0.8 | 0.936 | 0.701 |
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| CORGARR | 2999 | 0.8 | 0.927 | 0.705 |
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| CORMONE | 2285 | 0.7 | 0.992 | 0.902 |
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| COTCOTU | 5050 | 0.7 | 0.934 | 0.717 |
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| CUCCANO | 141 | 0.7 | 0.98 | 0.856 |
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| CYACYAN | 3354 | 0.8 | 0.954 | 0.765 |
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| DENMAJO | 305 | 0.8 | 0.974 | 0.814 |
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| DENMINO | 2248 | 0.8 | 0.95 | 0.751 |
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| EGRGARZ | 439 | 0.8 | 0.976 | 0.878 |
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| ELACAER | 1163 | 0.8 | 0.943 | 0.734 |
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| EMBCALA | 1047 | 0.7 | 0.908 | 0.695 |
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| EMBCIA | 847 | 0.8 | 0.94 | 0.681 |
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| EMBCIRL | 700 | 0.7 | 0.991 | 0.901 |
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| EMBCITR | 543 | 0.8 | 0.983 | 0.898 |
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| EMBHORT | 259 | 0.8 | 0.947 | 0.755 |
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| ERIRUBE | 77 | 0.8 | 0.905 | 0.619 |
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| FALNAUM | 1362 | 0.8 | 0.93 | 0.723 |
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| FALPERE | 4424 | 0.8 | 0.99 | 0.892 |
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| FALSUBB | 195 | 0.7 | 0.975 | 0.819 |
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| FICHYPO | 2141 | 0.8 | 0.975 | 0.899 |
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| FRICOEL | 287 | 0.7 | 0.901 | 0.644 |
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| FULATRA | 2264 | 0.8 | 0.927 | 0.688 |
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| GALCHLO | 4504 | 0.7 | 0.874 | 0.593 |
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| GALCRIS | 2245 | 0.8 | 0.934 | 0.701 |
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| GALTHEK | 246 | 0.8 | 0.943 | 0.710 |
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| GARGLAN | 1979 | 0.8 | 0.945 | 0.717 |
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| GYPFULV | 1781 | 0.7 | 0.999 | 0.98 |
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| HIEFASC | 84 | 0.8 | 0.997 | 0.956 |
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| HIEPENN | 1253 | 0.7 | 0.99 | 0.889 |
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| HIMHIMA | 2336 | 0.8 | 0.921 | 0.668 |
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| IXOMINU | 4471 | 0.8 | 0.991 | 0.944 |
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| JYNTORQ | 1930 | 0.7 | 0.989 | 0.891 |
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| LANCOLL | 3973 | 0.8 | 0.971 | 0.855 |
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| LANEXCU | 1502 | 0.7 | 0.885 | 0.611 |
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| LANSENA | 1695 | 0.8 | 0.947 | 0.761 |
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| LARRIDI | 701 | 0.8 | 0.994 | 0.968 |
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| LOXCURV | 2221 | 0.8 | 0.931 | 0.733 |
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| LULARBO | 5587 | 0.7 | 0.99 | 0.897 |
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| LUSMEGA | 1765 | 0.7 | 0.992 | 0.923 |
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| LUSSVEC | 1897 | 0.8 | 0.995 | 0.969 |
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| MELCALA | 953 | 0.8 | 0.918 | 0.681 |
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| MERAPIA | 2422 | 0.8 | 0.938 | 0.717 |
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| MILMIGR | 2485 | 0.7 | 0.976 | 0.835 |
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| MILMILV | 2266 | 0.8 | 0.938 | 0.727 |
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| MONSAXA | 2565 | 0.8 | 0.941 | 0.751 |
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| MONSOLI | 1348 | 0.8 | 0.992 | 0.908 |
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| MOTALBA | 1581 | 0.7 | 0.971 | 0.864 |
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| MOTCINE | 4157 | 0.8 | 0.94 | 0.7 |
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| MOTFLAV | 2999 | 0.8 | 0.97 | 0.836 |
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| MUSSTRI | 2285 | 0.7 | 0.977 | 0.835 |
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| NEOPERC | 5050 | 0.7 | 0.97 | 0.876 |
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| NYCNYCT | 141 | 0.8 | 0.995 | 0.974 |
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| OENHISP | 3354 | 0.8 | 0.909 | 0.686 |
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| OENLEUC | 305 | 0.8 | 0.945 | 0.754 |
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| OENOENA | 2248 | 0.8 | 0.923 | 0.674 |
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| ORIORIO | 439 | 0.7 | 0.91 | 0.666 |
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| OTITARD | 1163 | 0.8 | 0.961 | 0.797 |
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| OTUSCOP | 1047 | 0.7 | 0.925 | 0.695 |
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| PARATER | 847 | 0.8 | 0.92 | 0.669 |
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| PARCAER | 700 | 0.7 | 0.884 | 0.599 |
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| PARCRIS | 543 | 0.8 | 0.985 | 0.863 |
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| PARMAJO | 259 | 0.7 | 0.935 | 0.745 |
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| PASHISP | 77 | 0.8 | 0.942 | 0.736 |
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| PASMONT | 1362 | 0.7 | 0.869 | 0.541 |
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| PERAPIV | 4424 | 0.8 | 0.937 | 0.736 |
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| PERPERD | 195 | 0.8 | 0.993 | 0.954 |
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| PETPETR | 2141 | 0.8 | 0.905 | 0.63 |
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| PHACOLC | 287 | 0.8 | 0.997 | 0.985 |
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| PHOOCHR | 2264 | 0.8 | 0.91 | 0.632 |
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| PHOPHOE | 4504 | 0.8 | 0.949 | 0.77 |
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| PHYBONE | 2245 | 0.8 | 0.906 | 0.626 |
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| PHYCOLL | 246 | 0.8 | 0.922 | 0.678 |
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| PHYIBER | 1979 | 0.8 | 0.935 | 0.729 |
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| PICPICA | 1781 | 0.7 | 0.86 | 0.536 |
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| PICVIRI | 84 | 0.7 | 0.868 | 0.551 |
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| PODCRIS | 1253 | 0.8 | 0.978 | 0.889 |
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| PODNIGR | 2336 | 0.8 | 0.993 | 0.962 |
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| PRUCOLL | 4471 | 0.8 | 0.994 | 0.957 |
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| PRUMODU | 1930 | 0.8 | 0.976 | 0.844 |
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| PTEALCH | 3973 | 0.8 | 0.974 | 0.877 |
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| PTEORIE | 1502 | 0.8 | 0.968 | 0.84 |
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| PTYRUPE | 1695 | 0.8 | 0.992 | 0.902 |
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| PYRGRAC | 701 | 0.8 | 0.992 | 0.947 |
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| PYRPYRR | 2221 | 0.8 | 0.917 | 0.681 |
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| RALAQUA | 5587 | 0.7 | 0.995 | 0.948 |
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| RECAVOS | 1765 | 0.8 | 0.99 | 0.945 |
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| REGIGNI | 1897 | 0.8 | 0.928 | 0.693 |
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| REGREGU | 953 | 0.8 | 0.928 | 0.899 |
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| REMPEND | 2422 | 0.8 | 0.966 | 0.824 |
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| RIPRIPA | 2485 | 0.7 | 0.993 | 0.932 |
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| SAXRUBE | 2266 | 0.8 | 0.978 | 0.888 |
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| SAXTORQ | 2565 | 0.7 | 0.898 | 0.622 |
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| SERCITR | 1348 | 0.8 | 0.984 | 0.904 |
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| SITEURO | 1581 | 0.8 | 0.949 | 0.736 |
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| STENILO | 4157 | 0.8 | 0.996 | 0.981 |
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| STRALUC | 2999 | 0.7 | 0.991 | 0.896 |
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| STRDECA | 2285 | 0.7 | 0.898 | 0.651 |
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| STRTURT | 5050 | 0.7 | 0.927 | 0.697 |
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| STUUNIC | 141 | 0.7 | 0.923 | 0.71 |
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| SYLATRI | 3354 | 0.7 | 0.991 | 0.902 |
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| SYLBORI | 305 | 0.8 | 0.931 | 0.712 |
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| SYLCANT | 2248 | 0.8 | 0.896 | 0.602 |
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| SYLCOMM | 439 | 0.7 | 0.899 | 0.606 |
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| SYLCONS | 1163 | 0.8 | 0.947 | 0.747 |
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| SYLHORT | 1047 | 0.7 | 0.983 | 0.881 |
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| SYLMELA | 847 | 0.8 | 0.926 | 0.663 |
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| SYLUNDA | 700 | 0.7 | 0.906 | 0.643 |
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| TACRUFI | 543 | 0.7 | 0.967 | 0.817 |
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| TETTETR | 259 | 0.8 | 0.988 | 0.913 |
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| TICMURA | 77 | 0.8 | 0.997 | 0.975 |
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| TRITOTA | 1362 | 0.8 | 0.994 | 0.98 |
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| TROTROG | 4424 | 0.8 | 0.931 | 0.667 |
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| TURPHIL | 195 | 0.8 | 0.936 | 0.704 |
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| TURVISC | 2141 | 0.7 | 0.896 | 0.637 |
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| TYTALBA | 287 | 0.7 | 0.947 | 0.749 |
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| UPUEPOP | 2264 | 0.7 | 0.904 | 0.66 |
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| VANVANE | 4504 | 0.8 | 0.979 | 0.927 |
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| AER | 2245 | 0.7 | 0.932 | 0.73 |
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| AFR | 246 | 0.8 | 0.957 | 0.781 |
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| BCI | 1979 | 0.8 | 0.914 | 0.655 |
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| CAU | 1781 | 0.8 | 0.954 | 0.787 |
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| CBE | 84 | 0.7 | 0.993 | 0.943 |
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| CGI | 1253 | 0.7 | 0.932 | 0.715 |
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| CST | 2336 | 0.7 | 0.993 | 0.924 |
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| EOR | 4471 | 0.8 | 0.996 | 0.954 | |
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| HHI | 1930 | 0.8 | 0.918 | 0.692 |
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| IMO | 3973 | 0.8 | 0.995 | 0.965 | |
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| LSC | 1502 | 0.8 | 0.971 | 0.831 |
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| MBR | 1695 | 0.8 | 0.943 | 0.732 | |
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| MLE | 701 | 0.8 | 0.918 | 0.661 |
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| MMO | 2221 | 0.7 | 0.973 | 0.868 |
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| NAS | 5587 | 0.7 | 0.866 | 0.543 |
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| NMA | 1765 | 0.7 | 0.966 | 0.809 |
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| PAL | 1897 | 0.8 | 0.916 | 0.677 |
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| PBO | 953 | 0.8 | 0.994 | 0.95 |
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| PGU | 2422 | 0.7 | 0.984 | 0.885 |
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| TLE | 2485 | 0.7 | 0.944 | 0.746 | |
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| TMR | 2266 | 0.8 | 0.914 | 0.674 |
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| VLA | 2565 | 0.7 | 0.994 | 0.931 |
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| VSE | 1348 | 0.8 | 0.986 | 0.93 |
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| ZSC | 1581 | 0.7 | 0.866 | 0.574 |
Description of the bioclimatic variables used in species distribution models. The code, name, units and the regional (Iberian Peninsula) and local (Biosphere Reserve of Meseta Ibérica) ranges are indicated for each variable.
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| BIO3 | Isothermality | Coefficient | 25 – 43 | 33 - 40 |
| BIO4 | Temperature Seasonality | Coefficient | 387 - 870 | 666 - 813 |
| BIO10 | Mean Temperature of Warmest Quarter | ºC | 11.2 – 28.4 | 15.2 – 26.8 |
| BIO11 | Mean Temperature of Coldest Quarter | ºC | -7.8 – 12.9 | -3.1 – 6.7 |
| BIO15 | Precipitation Seasonality | Coefficient | 23 – 94 | 47 - 76 |
| BIO16 | Precipitation of Wettest Quarter | mm | 200 - 2200 | 510 - 1110 |
| BIO17 | Precipitation of Driest Quarter | mm | 0 - 470 | 0 - 130 |
| BIO19 | Precipitation of Coldest Quarter | mm | 30 - 1130 | 120 - 470 |
Figure 2.Example of the historical climate (1989-2005) model projections obtained for the Iberian Peninsula (I.P.; 10 × 10 km) and the Transboundary Biosphere Reserve of Meseta Ibérica (M.I.; 1 × 1 km). The models present the ensemble suitability values for the Tree pipit (; code: ANTRRIV).
Figure 3.Example of future climate model projections for 2050 obtained for the Transboundary Biosphere Reserve of Meseta Ibérica (M.I.; 1 × 1 km). The models present the ensemble suitability values for the Tree pipit (; code: ANTRRIV), according to each climate model (CNRM, IPSL, ICHEC and MPI; Jacob et al. 2020) and each Representative Concentration Pathways scenarios (RCP 4.5; RCP 8.5).
| Column label | Column description |
|---|---|
| Files of the historic period - AREA_EOBS_H_ALT_VAR_1 | Code description - AREA refers to the Iberian Peninsula (PI) or Meseta Ibérica (MI), EOBS to the historic climatic dataset of reference (E-OBS), H to the historical period (H), ALT to the altitudinal-based correction of climate variables, VAR to the three provided variables (RR - daily preciptation; TMAX - Maximum temperature; TMIN - Minimum temperature) and 1 to the spatial resolution (1 km). |
| Files of the future period - MI_MODEL_RCP_MR_ALT_VAR_1 | Code description - MI refers to the Meseta Ibérica, MODEL to the climate model used (CNRM-CERFACS-CNRM-CM5 - CNRM; ICHEC-EC-EARTH - ICHEC; IPSL-IPSL-CM5A-MR - IPSL; MPI-M-MPI-ESM-LR - MPI), RCP to the Representative Concentration Pathway (RCP 4.5 - 45; RCP 8.5 - 85), MR to the future period, ALT to the altitudinal-based correction of climate variables, VAR to the three provided variables (RR - daily preciptation; TMAX - Maximum temperature; TMIN - Minimum temperature) and 1 to the spatial resolution (1 km). |
| Column label | Column description |
|---|---|
| Climate models | Species distribution models of 207 vertebrates for 2005 and 2050 |