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Fig. 4 in Distribution and habitat suitability of two neighboring Lycian salamanders

Fig. 4. Variables with the highest contributions to the potential distributions of L. flavimembris (a) and L. fazilae (b) according to MaxEnt, with the standard errors in shown blue. In each graph, the y-axis indicates the probability of presence and the x-axis shows the contribution of each variable. See Table 1 for definitions of the environmental variables.

Fig. 6 in Distribution and habitat suitability of two neighboring Lycian salamanders

Fig. 6. Frequencies of Bedrock types on the different presence points of L. flavimembris and L. fazilae. Bedrock type abbreviations: Alluvion [All], Breccias [Brec], Pebble Stone-Sandstone-Mudstone [PS-SS-MS], Chert [Cher], Cherty Limestone [Cher LS], Dolomite [Dol], Limestone [LS], Melange [Mel], Peridotite [Per], Spilite-Basalt-Tuff [SBT], Sandstone-Mudstone [SS-MS], Sandstone-Mudstone-Limestone [SS-MS-LS], Volcanite-Sedimentary Rock [V-SR], and all unknown rock types [Unknown].

Fig. 3 in Distribution and habitat suitability of two neighboring Lycian salamanders

Fig. 3. Results of the Jackknife test for evaluating the relative importance of environmental variables for L. flavimembris (a) and L. fazilae (b). See Table 1 for definitions of the environmental variables.

Fig. 2 in Distribution and habitat suitability of two neighboring Lycian salamanders

Fig. 2. The receiver operating characteristic (ROC) curves for L. flavimembris (a) and L. fazilae (b).

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Lycian rock cut tombs of Dalyan

Lycia was a geopolitical region in Anatolia in what are now the provinces of Antalya and Muğla on the southern coast of Turkey, bordering the Mediterranean Sea, and Burdur Province inland. Known to history since the records of ancient Egypt and the Hittite Empire in the Late Bronze Age, it was populated by speakers of the Luwian language group. Written records began to be inscribed in stone in the Lycian language after Lycia's involuntary incorporation into the Achaemenid Empire in the Iron Age. At that time (546 BC) the Luwian speakers were decimated, and Lycia received an influx of Persian speakers. Ancient sources seem to indicate that an older name of the region was Alope . Source: Objaverse 1.0 / Sketchfab

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Fig. 5. MaxEnt habitat suitability maps for L in Distribution and habitat suitability of two neighboring Lycian salamanders

Fig. 5. MaxEnt habitat suitability maps for L. flavimembris (a) and L. fazilae (b).

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Fig. 1 in Distribution and habitat suitability of two neighboring Lycian salamanders

Fig. 1. Study area and distributions of presence data for L. flavimembris and L. fazilae.

Fig. 7 in A novel method to calculate climatic niche similarity among species with restricted ranges-the case of terrestrial Lycian salamanders

Fig. 7 Mean of 100 Maxent SDMs computed with pooled species records of all Lyciasalamandra species omitting L. fazilae (a), L. flavimembris (b), and L. luschani (c). Areas climatically suitable for salamanders and suitable due to the presence of carstic limestone formations are indicated (dark greyMaxent values above the minimum training presence, black values above the minimum 10% training omission threshold). Areas climatically unsuitable to Lycian salamanders are indicated in light grey where carstic limestone formations are present and white where they are not

Fig. 5 in A novel method to calculate climatic niche similarity among species with restricted ranges-the case of terrestrial Lycian salamanders

Fig. 5 Relative position of species records in environmental niche space. Note the decreasing number of species records with decreasing temperature and precipitation. This pattern corroborates well field observations by Klewen (1991) and Steinfartz and Mutz (1998)

Fig. 2 Conceptual differences among proposed niche overlap analyses. Imagine a in A novel method to calculate climatic niche similarity among species with restricted ranges-the case of terrestrial Lycian salamanders

Fig. 2 Conceptual differences among proposed niche overlap analyses. Imagine a set of three species with different preferences along an environmental gradient. Using SDM projections, it is possible to derive for each species a probability distribution across the gradient. Comparing two species as proposed by Warren et al. (2008), the overlap (grey area in the middle panel) of their respective probability distributions in geographic space is computed (pair-wise niche overlap). In our jackknife approach, a probability distribution derived from all species records is compared to a probability distribution derived from all minus one species. The 1−the resulting overlap value reflects the relative contribution of the omitted species to the entire probability distribution (grey area in the lower panel) and can be used as measure to rank all species when omitting them iteratively. Note that these specific indices are comparable only across each method but not among the different approaches

Fig. 1 a in A novel method to calculate climatic niche similarity among species with restricted ranges-the case of terrestrial Lycian salamanders

Fig. 1 a Presence of carstic limestone formations (light grey) and species records used for species distribution modelling (SDM). White dots Lyciasalamandra antalyana, black dots L. atifi, black squares L. billae, grey squares L. fazilae, black triangles L. flavimembris, white triangles L. helverseni, grey triangles L. luschani. b Mean of 100 Maxent SDMs computed with pooled species records of all Lyciasalamandra species. c Maxent SDMs trained with all pooled records omitting L. helverseni. Areas climatically suitable for salamanders and also suitable due to the presence of carstic limestone formations are indicated. Dark grey Maxent values above the minimum training presence, black values above the minimum 10% training omission threshold. Areas climatically unsuitable to Lycian salamanders are indicated in light grey where carstic limestone formations are present and white where they are not

Fig. 6 in A novel method to calculate climatic niche similarity among species with restricted ranges-the case of terrestrial Lycian salamanders

Fig. 6 Mean of 100 Maxent SDMs computed with pooled species records of all Lyciasalamandra species omitting L. antalyana (a), L. atifi (b), and L. billae (c). Areas climatically suitable for salamanders and suitable due to the presence of carstic limestone formations are indicated (dark grey Maxent values above the minimum training presence, black values above the minimum 10% training omission threshold). Areas climatically unsuitable to Lycian Salamanders are indicated in light grey where carstic limestone formations are present and white where they are not