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Figure 4 in Seasonal community structure of the molluscan macrofauna at the marine-lagoonal environmental transition at Kalloni solar saltworks (Lesvos Island, NE Aegean Sea, Greece)

Figure 4. Cluster analysis dendrogram and nMDS ordination plot of the sampling sites (1, gulf; 2, channel; 3, pond1; 4, pond2) in each season (WI, winter; SP, spring; SU, summer; AU, autumn).

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Figure 2 in Seasonal community structure of the molluscan macrofauna at the marine-lagoonal environmental transition at Kalloni solar saltworks (Lesvos Island, NE Aegean Sea, Greece)

Figure 2. Spatial and seasonal variations of the proportions of the trophic types of the dominant molluscan species. HER, herbivorous; DS, surface deposit feeders; SU, suspension feeders.

FIGURES 9–10 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURES 9–10. PAE for the Transmexican Volcanic Belt (TVB). 9, consensus cladogram. Bracket shows the clade that defines an area of endemism. 10, areas and microareas of endemism.

FIGURES 7–8 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURES 7–8. PAE for the Sierra Madre Oriental (SMOR). 7, consensus cladogram. Brackets show the clade that defines an area of endemism. 8, areas and microareas of endemism.

FIGURES 5–6 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURES 5–6. PAE for the Sierra Madre Occidental (SMOC). 5, consensus cladogram. Bracket shows the clade that defines an area of endemism. 6, areas and microareas of endemism.

FIGURES 13–14 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURES 13–14. PAE for the Chiapas Highlands (CHIS). 13, consensus cladogram. Bracket shows the clade that defines an area of endemism. 14, areas and microareas of endemism.

FIGURES 11–12 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURES 11–12. PAE for the Sierra Madre del Sur (SMS). 11, consensus cladogram. 12, microareas of endemism.

FIGURES 1–4 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURES 1–4. Areas and microareas of endemism for the MTZ defined using PAE. 1, areas of endemism for the whole MTZ. 2, microareas of endemism for the whole MTZ. 3, areas of endemism for each province of the MTZ. 4, microareas of endemism for each province of the MTZ. SMOC, Sierra Madre Occidental; SMOR, Sierra Madre Oriental; TVB, Transmexican Volcanic Belt; SMS, Sierra Madre del Sur; CHIS, Chiapas Highlands.

FIGURE 15 in Testing the biogeographical regionalization of the Mexican Transition Zone based on the distribution of Curculionidae (Insecta: Coleoptera)

FIGURE 15. Consensus cladogram of PAE for the provinces of the MTZ. CHIS, Chiapas Highlands; SMS, Sierra Madre del Sur; SMOR, Sierra Madre Oriental; TVB, Transmexican Volcanic Belt; SMOC, Sierra Madre Occidental.

Figure 4. Mismatch distributions for 11 in Phylogeography of the Poecilimon luschani species group (Orthoptera, Tettigoniidae): a radiation strictly correlated with climatic transitions in the Pleistocene

Figure 4. Mismatch distributions for 11 populations of the Poecilimon luschani species group for cytochrome c oxidase subunit I (COI) sequences. The continuous and interrupted (connecting circles) lines indicate the expected (Exp) and observed (Obs) distributions of pairwise differences obtained by fitting a model of sudden population expansion. A, İzmir (P. ledereri); B, Aydın (P. tuncayi); C, Kütahya (P. egrigozi); D, Balıkesir (P. helleri); E- Es¸en2 (P. l. chobanovi); F, Es¸en3 (P. l. chobanovi); G, Demre (P. l. luschani); H, Kalkan (P. l. luschani); I, Patara (P. l. luschani); J, Olympos (P. l. birandi); K, Bakırlıdag (P. l. birandi).

Figure 2 in Phylogeography of the Poecilimon luschani species group (Orthoptera, Tettigoniidae): a radiation strictly correlated with climatic transitions in the Pleistocene

Figure 2. BEAST chronogram based on concatenated sequences of cytochrome c oxidase subunit I + 16S rDNA for the Poecilimon luschani species group. Divergence times inferred according to Bayesian inference with an uncorrelated lognormal relaxed clock in BEAST (MPT, Mid-Pleistocene Transition; IIGP, initiation of intense glaciation periods; for details of populations see Table 1 and for the haplotype codes see Tables S1, S2).

Figure 5 in Phylogeography of the Poecilimon luschani species group (Orthoptera, Tettigoniidae): a radiation strictly correlated with climatic transitions in the Pleistocene

Figure 5. Climatic cycles during the Mid and Late Pleistocene and time to the most recent common ancestor of the main nodes in the Poecilimon luschani species group. The median estimates are shown by a dashed line; the 95% highest posterior density (HPD) limits are shown by the pale blue horizontal bars. Node numbers, median estimates, and HPD are shown in Table 4 (time chart for climatic cycles modified from Cohen et al., 2012). (Colour version of figure available online.)

Figure 1 in Phylogeography of the Poecilimon luschani species group (Orthoptera, Tettigoniidae): a radiation strictly correlated with climatic transitions in the Pleistocene

Figure 1. Populations sampled for specimens used in the study (for details of the localities see Table 1).

Figure 3. Gaussian Markov random field skyride plots for 11 in Phylogeography of the Poecilimon luschani species group (Orthoptera, Tettigoniidae): a radiation strictly correlated with climatic transitions in the Pleistocene

Figure 3. Gaussian Markov random field skyride plots for 11 populations of the Poecilimon luschani species group. The median estimates are shown as a thick solid line, and the 95% highest posterior density limits are shown by the grey area. The background grey graphs show fluctuations in temperature during the respective periods of the Pleistocene. The upper and lower margins show the time in kiloyears (Kyr), the left margin shows the log of the effective population size (Nef), and the right margin the departure in temperature (ΔT in °C). Names of the glacial periods are indicated in the boxes at the bottom of the graphs. The background graph shows the temperature reconstruction of Vostok; modified from http://agwobserver.wordpress.com. A, İzmir (P. ledereri); B, Aydın (P. tuncayi); C, Kütahya (P. egrigozi); D, Balıkesir (P. helleri); E- Es¸en2 (P. l. chobanovi); F, Es¸en3 (P. l. chobanovi); G, Demre (P. l. luschani); H, Kalkan (P. l. luschani); I, Patara (P. l. luschani); J, Olympos (P. l. birandi); K, Bakırlıdag (P. l. birandi).

Figure 6 in Phylogeography of the Poecilimon luschani species group (Orthoptera, Tettigoniidae): a radiation strictly correlated with climatic transitions in the Pleistocene

Figure 6. Evolution in ecological preferences of the species, subspecies, and populations of the Poecilimon luschani group. Solid lines indicate lowland habitats and dotted lines highland habitats. Polymorphic branches are shown by both lines. Locations of the taxa are indicated on the map given on the right (L, low altitudes; H, high altitudes; polymorphic species indicated by both).

Figure 34 in A new genus and species of eomysticetid (Cetacea: Mysticeti) and a reinterpretation of 'Mauicetus' lophocephalus Marples, 1956: Transitional baleen whales from the upper Oligocene of New Zealand

Figure 34. Life restoration of Tokarahia kauaeroa gen. et sp. nov. Artwork by Christopher Gaskin, ©Geology Museum, University of Otago.

Figure 32 in A new genus and species of eomysticetid (Cetacea: Mysticeti) and a reinterpretation of 'Mauicetus' lophocephalus Marples, 1956: Transitional baleen whales from the upper Oligocene of New Zealand

Figure 32. Interpretive reconstructions of crania of described eomysticetids, drawn to scale, with missing parts indicated by dashed lines and preserved portions symmetrically flipped. Reconstruction of Tokarahia lophocephalus based on published photograph from Marples (1956).

Figure 30 in A new genus and species of eomysticetid (Cetacea: Mysticeti) and a reinterpretation of 'Mauicetus' lophocephalus Marples, 1956: Transitional baleen whales from the upper Oligocene of New Zealand

Figure 30. Vertebrae of Tokarahia sp., cf. Tokarahia lophocephalus (OU 22081): A, atlas in posterior view; B, atlas in dorsal view; C, axis in anterior view; D, axis in dorsal view; E, cervical vertebra in anterior view; F, posterior view; G, partial cervical vertebra in anterior view; H, posterior view; I, sternum in dorsal view; J, ventral view.

Figure 29 in A new genus and species of eomysticetid (Cetacea: Mysticeti) and a reinterpretation of 'Mauicetus' lophocephalus Marples, 1956: Transitional baleen whales from the upper Oligocene of New Zealand

Figure 29. Isolated tooth of Tokarahia sp., cf. Tokarahia lophocephalus (OU 22081): A, tooth in mesial view; B, lingual or labial view; C, distal view; D, lingual or labial view; E, photograph of broken cross section.

Figure 27 in A new genus and species of eomysticetid (Cetacea: Mysticeti) and a reinterpretation of 'Mauicetus' lophocephalus Marples, 1956: Transitional baleen whales from the upper Oligocene of New Zealand

Figure 27. Articulated left tympanoperiotic of Tokarahia sp., cf. Tokarahia lophocephalus (OU 22081), whitened with ammonium chloride. Articulated periotic and posterior process of bulla in medial (A) and ventral (B) view. Articulated tympanoperiotic in: dorsal view (C, relative to bulla); posterior view (D); medial view (E, relative to bulla); and lateral view (F, relative to bulla).