| Literature DB >> 25389444 |
Antton Alberdi1, Ostaizka Aizpurua1, Joxerra Aihartza1, Inazio Garin1.
Abstract
Several alpine vertebrates share a distribution pattern that extends across the South-western Palearctic but is limited to the main mountain massifs. Although they are usually regarded as cold-adapted species, the range of many alpine vertebrates also includes relatively warm areas, suggesting that factors beyond climatic conditions may be driving their distribution. In this work we first recognize the species belonging to the mentioned biogeographic group and, based on the environmental niche analysis of Plecotus macrobullaris, we identify and characterize the environmental factors constraining their ranges. Distribution overlap analysis of 504 European vertebrates was done using the Sorensen Similarity Index, and we identified four birds and one mammal that share the distribution with P. macrobullaris. We generated 135 environmental niche models including different variable combinations and regularization values for P. macrobullaris at two different scales and resolutions. After selecting the best models, we observed that topographic variables outperformed climatic predictors, and the abruptness of the landscape showed better predictive ability than elevation. The best explanatory climatic variable was mean summer temperature, which showed that P. macrobullaris is able to cope with mean temperature ranges spanning up to 16°C. The models showed that the distribution of P. macrobullaris is mainly shaped by topographic factors that provide rock-abundant and open-space habitats rather than climatic determinants, and that the species is not a cold-adapted, but rather a cold-tolerant eurithermic organism. P. macrobullaris shares its distribution pattern as well as several ecological features with five other alpine vertebrates, suggesting that the conclusions obtained from this study might be extensible to them. We concluded that rock-dwelling and open-space foraging vertebrates with broad temperature tolerance are the best candidates to show wide alpine distribution in the Western Palearctic.Entities:
Keywords: Alpine distribution; Alpine long-eared bat; Biogeography; Chiroptera; Distribution; Modelling; Mountain long-eared bat; Zoogeography
Year: 2014 PMID: 25389444 PMCID: PMC4226887 DOI: 10.1186/s12983-014-0077-6
Source DB: PubMed Journal: Front Zool ISSN: 1742-9994 Impact factor: 3.172
Figure 1Geographic overlap between the distribution of and the distributions of analysed European vertebrates. Blue bars indicate birds, yellow bars indicate non-chiropteran mammals and red bars indicate bats. The names of the five species with the highest distribution resemblance, and the positions of P. auritus and P. austriacus are shown. Note that the species with cSSI values equal to 0 (distributions not-overlapped) are not shown and the list of species of birds and non-chiropteran mammals is limited to 100 species.
Composition, evaluation scores (AUCtest, AICc and MPA) and variable contribution ranks of the best models
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| Climatic | B8, B10, B12, B17 | 1 | 0.881 | 2688.1285 | 0.3383 | B10 (45.3) > B12 > B8 > B17 |
| B4, B10, B12, B15, B17 | 1 | 0.880 | 2619.7250 | 0.2972 | B10 (43.7) > B12 > B17 > B15 > B4 | |
| Topographic | ABR, ELEV | 1 | 0.873 | 2434.7099 | 0.365 | ABR (84.4) > ELEV |
| ABR, ELEV | 2 | 0.866 | 2478.7364 | 0.343 | ABR (86.1) > ELEV | |
| Climatic + Topographic | B4, B8, B10, B12, B15, B17, ELEV, ABR | 1 | 0.905 | 2542.8793 | 0.201 | ABR (71.7) > ELEV > B10 > B17 > B12 > B15 > B4 > B8 |
| B4, B8, B10, B12, B15, B17, ABR | 2 | 0.911 | 2409.3266 | 0.237 | ABR (79.9) > B10 > B12 > B15 > B17 > B4 > B8 | |
| Climatic + Habitat | B4, B8, B10, B12, B15, B17, LAND | 1 | 0.899 | 2426.4305 | 0.271 | B10 (32.7) > B12 > LAND > B8 > B17 > B15 > B4 |
| B4, B10, B12, B15, B17, LAND | 1 | 0.889 | 2472.1983 | 0.237 | B10 (37.0) > B12 > LAND > B17 > B15 > B4 | |
| Topographic + Habitat | ELEV, ABR, LAND | 1 | 0.873 | 2333.0673 | 0.321 | ABR (86.7) > ELEV > LAND |
| ABR, LAND | 2 | 0.876 | 2379.0112 | 0.321 | ABR (96.6) > LAND | |
| Climatic + Topographic + Habitat | B4, B8, B10, B12, B15, B17, ABR, LAND | 1 | 0.903 | 2334.3659 | 0.178 | ABR (70.6) > B10 > B17 > LAND > B15 > B12 > B8 > B4 |
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| Topographic | ELEV, SLOP, ORI | 1 | 0.9294 | 1087.2041 | 0.1381 | ELEV (56.3) > SLO > ORI |
| ELEV, SLOP | 1 | 0.9298 | 1108.6065 | 0.1574 | ELEV (54.9) > SLO | |
| Habitat | DIS-URBAN, DIS-FOREST, DIS-ROCK | 1 | 0.8968 | 1161.1387 | 0.2449 | dis-rock (74.3) > dis-urban > dis-forest |
| DIS-URBAN, DIS-ROCK | 1 | 0.8943 | 1321.0146 | 0.2471 | dis-rock (89.3) > dis-urban | |
| Topographic + Habitat | ELEV, SLOP, ORI, DIS-URBAN, DIS-FOREST, DIS-ROCK | 1 | 0.9429 | 1289.9253 | 0.0871 | dis-rock (32.0) > SLO > ELEV > dis-urban > dis-forest > ORI |
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Only the two models that obtained the best values in each variable-type combination are shown. The rest of the models can be found in Tables S1 and S2 in the Additional file 1. The contribution percentage of the best-ranked variable in each model is indicated in brackets. The selected models are marked in bold.
Figure 2Distribution model for presented on a greyscale elevation map. Only suitable areas (SV >0.2886) are shown in a colour gradient from light yellow (low suitability) to brown (high suitability). Presence location records used for modelling are represented by black dots and the darkened region is the area used for calibrating the model.
Different metrics on the contribution of variables to the best models
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| Broad-scale modeling | ||||
| ABR | 75.10 | 45.45 | 1.05 | 1.05 |
| B10 | 9.01 | 28.17 | 0.64 | 1.25 |
| B12 | 3.86 | 7.34 | 0.59 | 1.34 |
| B17 | 4.63 | 6.45 | 0.41 | 1.34 |
| B15 | 2.34 | 2.28 | 0.09 | 1.34 |
| LAND | 3.70 | 1.57 | 0.20 | 1.33 |
| B4 | 1.33 | 8.71 | 0.11 | 1.34 |
| Fine-scale modeling | ||||
| DIS-ROCK | 34.36 | 42.86 | 0.97 | 1.71 |
| SLOPE | 31.68 | 14.36 | 1.16 | 1.53 |
| ELEV | 25.50 | 28.49 | 1.02 | 1.68 |
| DIS-URBAN | 8.44 | 14.27 | 0.30 | 1.73 |
All values are averages of the 50 replicates of the best models. The relative contribution is obtained from the increase of the regularized gain when each variable is added to the model. The permutation importance is obtained by randomly permuting the values of that variable among the training points and measuring the decrease in training AUC produced by the permutation. The Jackknife training gain with only variable is the training gain that the model achieves when using only that variable, and the Jackknife training gain without this variable is the training gain that the model achieves when using the rest of variables except that one. Consequently, in the first three metrics larger values indicate higher contribution of variables to the model, while in the last one, the lower values indicate greater importance of variables to the model.
Figure 3Response curves of variables with the highest predictive ability. (A) Abruptness and (B) mean temperature of the warmest quarter, as estimated by the broad-scale modelling; (C) slope, (D) elevation and (E) distance to rocks (DIS-ROCK), as estimated by the fine-scale modelling.
Figure 4Geographical distributions of six vertebrate species with palealpine distribution. (A) Alpine long-eared bat Plecotus macrobullaris, (B) white-winged snowfinch Montifringilla nivalis, (C) alpine chough Pyrrhocorax graculus, (D) wallcreeper Tichodroma muraria (breeding areas), (E) snow vole Chionomys nivalis and (F) alpine accentor Prunella collaris (breeding areas). Map A was generated from data published by Alberdi et al. [14], and maps B-F were obtained from IUCN Red List of Threatened Species [69].
Figure 5Relationship between suitability and elevation in six mountain massifs. Vertical red lines indicate the lower suitability boundary. Horizontal dotted lines indicate the maximum elevation of the mountain range.
Characteristics of the variables used in the two modelling scales
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| Abruptness | Topographic | 30 arc-sec | Generated from elevation data |
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| Elevation | Topographic | 30 arc-sec | Wordclim SRTM |
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| Temperature seasonality | Climatic | 30 arc-sec | Worldclim Bioclim 4 |
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| Mean temperature of the wettest quarter | Climatic | 30 arc-sec | Worldclim Bioclim 8 |
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| Mean temperature of the warmest quarter | Climatic | 30 arc-sec | Worldclim Bioclim 10 |
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| Annual precipitation | Climatic | 30 arc-sec | Worldclim Bioclim 12 |
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| Precipitation seasonality | Climatic | 30 arc-sec | Worldclim Bioclim 15 |
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| Precipitation of the Driest Quarter | Climatic | 30 arc-sec | Worldclim Bioclim 17 |
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| Land cover | Habitat | 30 arc-sec | GLCNMO |
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| Elevation | Topographic | 100 m | SRTM 90 m DEM (CGIAR-CSI) |
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| Slope | Topographic | 100 m | Generated from elevation data |
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| Orientation | Topographic | 100 m | Generated from elevation data |
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| Distance to rock areas | Habitat | 100 m | Obtained from Corine LandCover 2006 |
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| Distance to forest areas | Habitat | 100 m | Obtained from Corine LandCover 2006 |
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| Distance to urban areas | Habitat | 100 m | Obtained from Corine LandCover 2006 |