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FIGURES 14–15 in Lluciapomaresius nisae, a new species of Ephippigerini (Orthoptera: Tettigoniidae: Bradyporinae) from the northeast of the Iberian Peninsula

FIGURES 14–15. Ventral sclerites and subgenital plates of paratype of L. nisae (14) and L. panteli (15, redrawn according to Barat 2012).

FIGURES 10–13 in Lluciapomaresius nisae, a new species of Ephippigerini (Orthoptera: Tettigoniidae: Bradyporinae) from the northeast of the Iberian Peninsula

FIGURES 10–13. Titillators in dorsal and lateral view. Holotype of L. nisae (10,11), L. panteli from Albarca, Montsant (12,13).

FIGURES 2–9 in Lluciapomaresius nisae, a new species of Ephippigerini (Orthoptera: Tettigoniidae: Bradyporinae) from the northeast of the Iberian Peninsula

FIGURES 2–9. Dorsal view of Pronotum of males. Holotype of L. nisae (2) and male of L. panteli from Albarca, Montsant (3). Cerci of males in dorsal, in rear and in lateral view of holotype of L. nisae (4, 5, 6) and L. panteli from Albarca, Montsant (7, 8, 9).

FIGURE 1 in Lluciapomaresius nisae, a new species of Ephippigerini (Orthoptera: Tettigoniidae: Bradyporinae) from the northeast of the Iberian Peninsula

FIGURE 1. Map of the location of L. nisae with reference to the other species of the genera in Catalonia: L. ortegai and L. panteli.

FIGURE 13 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 13. Comparison of the expected outcomes of four major geographic models of evolution. M = I. monticola s. str.; G = I. galani; NML = Iberolacerta monticola astur ssp. nov. from the Northern Montes de León. The three main cladogenetic events dated by mitochondrial markers are indicated by the width of the lines separating the populations. Block arrows indicate direction of gene flow after the initial separation of I. m. astur ssp. nov. Arrowheads within text boxes under each model mark the expected tendency (upward or downward) of the corresponding indicators of nuclear genetic divergence. Reference values of divergence, obtained from the observed data, are shown at the bottom of the figure.

FIGURE 9 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 9. Specimens of I. monticola astur ssp. nov. from several localities across its distribution range: A.—Adult male in breeding period, with the typical green coloration. Note a typical disposition of scales in front of the masseteric plate. Salientes (Palacios del Sil, León)[loc. 2 in Fig. 1A]. B.—Ventral view of the same specimen of Fig.9 A. Throat and belly show greenish tinges, being in this later in a gradation from darker toward the sides to clearer in the middle. C.—A young male specimen of the vermiculated morph in breeding period. Greenish to brownish gray above. Salientes (Palacios del Sil, León) [loc. 2 in Fig. 1A]. D.—Ventral view of the same specimen as in C. E.—HOLOTYPUS (MNCN 44652). A brown colored male with eclipsed coloration in summer (probably also brown during the breeding period). Salientes (Palacios del Sil, León) [loc. 2 in Fig. 1A]. F.—Male from Sierra de las Tiendas (Murias de Paredes, León) [loc. 10 in Fig. 1A]. Eclipsed coloration still showing green coloration. G.—Male from Sierra de Villabandin (Murias de Paredes, León) [loc. 14 in Fig. 1A]. Summer (eclipsed) coloration. Moreover the animal is close to the molt and shows a very dark appearance due to the old skin. In this locality, NML-II haplotypes have been identified. However, these animals fall perfectly inside the morphological variability of the NML-I haplotype populations. H.—Hatchlings from Salientes (Palacios del Sil, León) [parents from loc. 2 in Fig. 1A]. Tail tips cut for genetic analysis.

FIGURE 1. A in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 1. A) General situation and localities of Iberolacerta monticola in the study area. Iberolacerta monticola s. str. occupies the main axis of the Cantabrian Range, north to the Luna and Sil rivers (inverted triangles), and I. m. astur ssp. nov. (round symbols) the Northern Montes de León, south to the abovementioned rivers. Localities of I. m. astur ssp. nov. are: 1.—Pico Nevadín and Braña de Peña Vendimia. 2.—La Poza del Puerto, Puerto del Portillin (=Alto de Vivero). 3.—Vivero. 4.—El Molar de Montrando, El Tambarón. 5.—Braña La Forcada, Pico de la Robeza, Peña Carnicera, Cerneya and Peñona de Brañalibrán. 6.—Peña de Valdiglesia. 7.—Alto de los Grillos. 8.—Catoute. 9.—Collado de Ocidiello and Pico Arcos del Agua (=Fernán Pérez). 10.—Sierra de las Tiendas. 11.—El Suspirón and Mortera de la Vieja. 12.—Los Bayos. 13.—Valdeloso Valley. 14.—Villabandin (Sierra de Villabandin, Southern Slopes) and 15.—Riolago de Babia (Sierra de Villabandin, northern slopes).

FIGURE 2 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 2. Principal Components Analysis. Males. Bidimensional plot of the specimens scores. Triangle: BABIA (Northern slopes of Sierra de Villabandín; NML-II haplotype). Inverted triangles: SALIENTES (Nevadin-Tambarón-Catoute populations; NML-I haplotype). Crosses: TIENDAS & SUSPIRON (Sierra de las Tiendas and Suspiron peak; NML-II haplotype). Blades: VILLABANDIN (Sierra de Villabandín or La Cañada; NML-II haplotype). Despite to be significant, the two first axes had a very poor discriminative power, with only a 33.8 % of variance explained (see text for details) and show a considerable overlap of the NML-I specimens that are distributed overlapping with the main part of the other samples. The second axis seems to have a geo-climatic interpretation, separating in the positive part the most northern (oceanic influenced) samples (BABIA) and in the negative part the ones inhabiting the more continental and harsh climate areas facing to the Spanish Northern Plateau (Meseta) (VILLABANDIN -Southern slopes of the same Sierra de Villabandin-), BAYOS, TIENDAS and SUSPIRON. Note that BABIA (triangle symbol) specimens are geographical neighbors (in the northern slopes) of VILLABANDIN (blades symbol) (in the southern slopes), but appear totally opposite in the PCA, in accord with this bioclimatic influence in the scalation. These more continental climate populations show the greater values for most scalation characteristics and the smaller ones for Tympanic plate size.

FIGURE 8 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 8. Three-dimensional representation of a Factorial Correspondence Analysis based on microsatellite genotypes of Iberolacerta monticola astur ssp. nov. individuals from the Northern Montes de León. The figure includes individuals of I. galani and I. monticola s. str. to be used as reference.

FIGURE 7 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 7. Summary plot of estimated membership coefficients for each individual, in each cluster (Q). Each individual is represented by a single vertical line broken into k colored segments, with lengths proportional to each of the k inferred clusters. The numbers (1–4) correspond to the predefined populations.

FIGURE 3 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 3. Principal Components Analysis. Females. Symbols as in Fig. 2. As in males, it is significant but also has a poor discrimination of the specimens into differentiated samples. The two axes together reach 32.3 % of variability explained (Fist axis: Eigenvalue of 2.91 and 17.14 % variance; Second axis 2.57 (15.14 % of variability), which is a very poor discriminative result. As in the male analysis, SALIENTES samples overlap with all the other ones, not allowing discriminating among groups or any geographic or climatic interpretation of the axes.

FIGURE 5 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 5. Canonical Discriminant Analysis. Females. First axis has two thirds of the total variability (Eigenvalue=1.3796; 69 % variance; Canonical Correlation 0.76) whereas the second one had the remaining one third (eigenvalue 0.6169, 31 % variance; Canonical Correlation 0.61). The female analysis presents less overlap among samples than the male analysis. The first axis separates I. galani in its positive part from I. monticola s. str. and I.m. astur ssp. nov. in its negative part. The second axis separates I.m. astur ssp. nov. in its positive part from the other two taxa. Discriminant axes obtained an 80.7 % of correct reclassification. Contrary to the male analysis, the I. m. astur ssp. nov. centroid is closer to the centroid of I. monticola than to the centroid of I. galani.

FIGURE 4 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 4. Canonical Discriminant Analysis. Males. Projection of the first two axes. First axis: Eigenvalue=0.958; 70.6 % variance explained; Canonical Correlation 0.70. Second axis: Eigenvalue=0.39; 29.4 % variance explained; Canonical Correlation 0.53. Both axes are significant and configure a bidimensional space with moderate overlap among the three taxa. The first axis separates I. monticola s. str. in its negative part from I. m. astur ssp. nov. and I. galani in the positive one. The second axis separates I. m. astur ssp. nov. from the other two taxa. These discriminant axes obtain a 78.3 % of correct reclassification. Iberolacerta galani and I. m. astur ssp. nov. centroids are the closest in the males bidimensional space, thus, their males are more similar in our analysis.

FIGURE 6 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 6. Phylogenetic tree of the mitochondrial haplotypes of Iberolacerta from the Northern Montes de León (NML), based on a strict-clock bayesian reconstruction. The tree is rooted using Lacerta agilis, and it includes representative sequences from the different Iberolacerta species. Statistical support values for the major clades, obtained by three different methods of analysis, are shown on each node; namely, from left to right, Bayes posterior probability (x100), ML metaGA best trees in consensus (%) and equally MP trees (%). A hyphen is inserted instead of a numerical value whenever a particular method did not support the Bayesian topology. Node bars indicate 95% credibility intervals (regions of highest posterior density) for the corresponding divergence time (in million years). Among brackets the localities of I. m. astur ssp. nov. referred in Fig. 1A.

FIGURE 11 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 11. Head of a male I. monticola astur ssp. nov. from Alto de la Poza del Puerto, Salientes, Palacios del Sil (León prov.) (Paratype NHMW39210 [ex-OA09081504]) showing the characteristic temporal disposition with a big masseteric and two enlarged scales ahead.

FIGURE 12 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 12. Variability (deviations from the most common disposition depicted in Fig. 11) in the temporal area of I. monticola astur ssp. nov. Left side (from top to bottom; oriented to the right): Puerto de los Portillinos; Alto de la Poza del Puerto; El Molar de Montrando; Alto de los Grillos (all four in Salientes, Palacios del Sil, León province); Sierra de Villabandín -Southern slopes-; and Mortera de la Vieja -El Suspirón—(the two in Murias de Paredes, León prov.). Rigth side (from top to bottom; oriented to the left): Pico Valdiglesias (Salientes, Palacios del Sil, León prov.); Los Bayos; El Campón de Posada; Sierra de las Tiendas (the three in Murias de Paredes, León prov.); and Riolago de Babia (two specimens) (San Emiliano de Babia, León prov.).

FIGURE 10 in A new mountain lizard from Montes de León (NW Iberian Peninsula): Iberolacerta monticola astur ssp. nov. (Squamata: Lacertidae)

FIGURE 10. Specimens of I. monticola astur ssp. nov. from several localities across its distribution range: A.—Adult female from Salientes (Palacios del Sil, León) [loc. 2 in Fig. 1A]. Note the more typical disposition of temporal scales in front the masseteric plate. B.—Young female from Los Bayos (Murias de Paredes, Leon) [loc. 12 in Fig. 1A]. In the foothills of the Sierra de Villabandin (where NML-II haplotype was identified) these specimens show NML-I haplotypes and are morphologically indistinguishable from all the other I. m. astur ssp. nov., including the Villabandin ones with NML-II haplotype. C.—An old female from El Tambarón, near Salientes (Palacios del Sil, León) [loc. 4 in Fig. 1A]. Very clear and contrasted pattern appears in these specimens living over quartzites instead of slates. This animal was the first NML-I specimen sequenced and identified. D.—The same specimen of Fig. 10K, in ventral view. E.—Female from El Molar de Montrando, near Salientes (Palacios del Sil, León) [loc. 4 in Fig. 1A]. Also clear colored and living over quartzites. F.—Young male from Sierra de Villabandin (Murias de Paredes, León) [loc. 14 in Fig. 1A]. Summer (eclipsed) coloration. See also fig. 9G. G.—Old female from Mortera de la Vieja, near El Supirón summit (Murias de Paredes, León) [loc. 11 in Fig. 1A]. This is the second area where NML-II haplotypes have been found. H.—Same specimen of Fig.10G in ventral view. Note the bluish tinge of the lateral ventral scale rows, found in other female specimens from this area and Sierra de las Tiendas.

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FIGURE 2 in An annotated check-list of lophogastrids (Crustacea: Lophogastrida) from the seas of the Iberian Peninsula

FIGURE 2. Cumulative number of the first record of species (N spp) and published reports of lophogastrids (N ms) over time in the Iberian Seas.

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FIGURE 5 in An annotated check-list of lophogastrids (Crustacea: Lophogastrida) from the seas of the Iberian Peninsula

FIGURE 5. Similarity of species distributions (nMDS/clustering) based on presence/absence of lophogastrid species in the 6 main geographic areas of the Iberian Seas (this study), the Mediterranean coasts of Italy (Wittmann & Ariani 2010) and Celtic, South Icelandic, South Greenlandic and North European Atlantic regions (Petryashov 2009).