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FIGURE 6 in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 6. Photoplate of the Plášťovce and Hámor sections: A-C. Plášťovce section. A) lat. 48°9'23.53"N, lon. 18°57'26.67"E, fine grained tuffites. B) Lat. 48° 9'14.61", lon. 18°56'47.80", clast supported through-cross bedded gravels overlying fine grained tuffites. C) Lat. 48°9'28.24"N, lon. 18°57'28.60"E, main quarry wall exposing fine to coarse grained sand, clast supported massive gravels. D-G. Hámor section, lat. 48°12'51.66"N, lon. 19°31'35.74"E, D) Overall view of the outcropping sand. E-G) Alteration of through cross-bedded low-angle laminated sands and clast supported gravels with sandy matrix.

FIGURE 2 in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 2. Lithology of the studied sections with sedimentological logs and paleoflow orientation. For codes of lithofacies see Appendix 1.

FIGURE 1. Location map. A, A in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 1. Location map. A, A) Position of Novohrad-Nógrád Basin within the Pannonian Basin System. Modified from Rybár et al., 2016. B) Location map of studied sections. C) Lithostratigraphic scheme. Explanatory notes: FPB- Fiľakovo-Pétervására Basin; DB- Danube Basin; NNB-Novohrad-Nógrád Basin. Modified from Gradstein et al., 2012.

FIGURE 9 in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 9. Foraminifera and nannofossils – statistical results. A. Principal Component Analysis (PCA) of the nannofossil assemblages. B. Relative abundances of Reticulofenestra minuta and Coccolithus pelagicus in the main stratigraphic levels. C. Cluster diagram (Ward algorithm analysis) of the benthic foraminifera assemblages, D. Species diversity of benthic foraminifera showing relation to typical environment adopted from Murray (2006), E. Non-metric multidimensional scaling (nMDS) diagram of benthic foraminifera, F. Isotope analysis (δ18O, δ13C), G. Estimated paleodepths based on benthic foraminifera.

FIGURE 5 in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 5. Photoplate of the Stredné Plachtince and Horné Strháre sections: A-F. Stredné Plachtince section, lat. 48°13'20.69"N, lon. 19°18'18.54"E. A) Main quarry wall exposing Príbelce sand topped by pyroclastic breccias. B-C) Bioturbated grouped bidirectional planar cross-bedded sand. D) Sand with symmetrical ripples marked by arrow. E) Contact between bidirectional and unidirectional cross-beds marked by tuffite layer. F) Contact between unidirectional cross-beds and through cross-bedded gravels topped by pyroclastic breccias. G-K. Horné Strháre section, lat. 48°15'57.91"N, lon. 19°21'9.08"E. G) Overall view of the quarry. H) unidirectional planar sandy cross-beds. I) Trough cross-bedded sand with mud drapes. J) Contact between trough cross-bedded sand with mud drapes and clast supported through cross-bedded gravels. K) Contact between tuffites and pyroclastic breccias. L) Boulder-sized clast of the paraconglomerate facies. For codes of lithofacies marked in italic see Appendix 1.

FIGURE 4 in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 4. Photoplate of the Kosihovce and Príbelce sections: A-C. Kosihovce section, lat. 48°11'15.16"N, lon. 19°31'35.74"E. A) Fine-grained tuffites with faint lamination and symmetrical ripples. B) Detail of the sampling points. C) Fine-grained tuffite with faint lamination. For codes of lithofacies marked in italic see Appendix 1. D-J. Príbelce section, lat. 48°11'49.89"N, lon. 19°14'44.42"E. D) Type locality of the Príbelce Member, E) Fine to very coarse sand with grouped unidirectional cross-beds. F) Fine to very coarse sand with grouped bidirectional cross-beds, G) Detail of the symmetrical ripple composed of sand and tuffite. H) Grouped unidirectional trough cross-bedded sand. I) Pyroclastic breccia. J) Fossiliferous horizontally bedded clast supported gravels with sandy matrix. For codes of lithofacies marked in italic see Appendix 1.

FIGURE 3 in The Pannonian Basin System northern margin paleogeography, climate, and depositional environments in the time range during MMCT (Central Paratethys, Novohrad-Nógrád Basin, Slovakia)

FIGURE 3. Photoplate of the Čebovce and Trenč sections: A-C. Čebovce section, lat. 48°11'17.88"N, lon. 19°13'38.94"E, mud with faint lamination with slump bodies overlain by fine to coarse grained sand with pebbles. DG. Trenč section, lat. 48°13'20.47"N, lon. 19°14'44.42"E. D) Southern foot of the Strážna hora hill with oyster reefs outcropping at the forest boundary. E) Ostrea bed. F) Clast supported massive gravels. G) Fine-grained tuffite. For codes of lithofacies marked in italic see Appendix 1.

Fig. 9 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 9 Examples of the male calling song presented in a time frame of 500 ms with oscillograms (a, c, e, f, g, h) and spectrograms (b, d) of taxa currently considered subspecies of Poecilimon jonicus. a P. j. tessellatus, Greece, Peloponnesos, Kallithea, 22.4°C, daily recording, own data; b same; c P. j. lobulatus, mainland Greece, Amphilochia, 21°C, daily recording, own data; d same; e P. j. jonicus, Albania, Kolonje district,

Fig. 7 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 7 Land-sea configuration in the Aegean area in different periods of the Neogene based on reconstructions by Popov et al. (2004) (with details taken from Creutzburg 1963 and Dermitzakis 1990) with historical biogeography hypothesis for the Messinian. a Late Serravallian (12–11 Ma), a possible time for the origin and early divergence of Barbitistini; b late Tortonian (8.5–7 Ma), transgression of the Mid-Aegean area in Tortonian

Fig. 6 Timetrees for the P in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 6 Timetrees for the P. jonicus group based on different phylogenies and time calibrations with node labels referring to the time estimation in millions of years. a BEAST maximum clade credibility tree inferred from COI and ND2 partitions calibrated for the substitution rate of COI; b BEAST chronogram and RelTime timetree inferred from the COI+ND2 phylogeny calibrated for the last separation of Crete (values above nodes, BEAST chronogram estimations; values below nodes, RelTime timetree estimations); c BEAST chronogram inferred from the 16S rRNA+12S rRNA phylogeny calibrated for the TMRCA (interval) of P. jonicus group (node 12) as suggested from the COI+ND2 chronogram. Different topologies of the trees are marked with "*" for the COI partitions and "**"for the ND2 partition on (a) and different topology of the BEAST and RelTime trees on (b). Numbers in white circles corre- spond to data in Supplementary material C. Light blue vertical band marks the onset of the northern hemisphere glaciation and dark blue lines mark major climatic switches in the Pleistocene. Uniform gray areas below the trees show united Aegean landmass (left) and re- unification of large areas in Messinian (right), while striped areas show disintegrated state of the Aegean

Fig. 4 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 4 Phylogenetic relationships of the members of the Poecilimon jonicus group sensu lato with four outgroups from the genus Poecilimon and two outgroups from additional genera (P, Poecilimon; L., Leptophyes; I., Isophya). a Combined maximum likelihood and Bayesian inference phylogenetic trees based on a 1659 bp alignment of the COI+ ND2 mitochondrial dataset and b Bayesian inference phylogenetic tree based on a 1835 bp alignment of the 16S rRNA+12S rRNA mitochondrial dataset (Ullrich et al. 2010). Node values at branches show node support: above, ML bootstrap proportions; below, BI posterior probabilities; asterisk (*) indicates branches resolved by one of the analyses

Fig. 5 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 5 Phylo-spatial dimension of the P. jonicus group based on the mtDNA phylogeny (data combined from COI+ND2 and 16S rRNA+12S rRNA datasets). Blue, "Anatolian" lineage; green, "Cretan" lineage; orange, "Balkan" lineage including Poecilimon inflatus

Fig. 3 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 3 Phylogenetic relationships of the members of the Poecilimon jonicus group sensu lato with four outgroups from the genus Poecilimon and two outgroups from additional genera of Barbitistini (P, Poecilimon; L., Leptophyes; I., Isophya) based on Bayesian inference analysis of ITS1+ITS2 sequences. a 665 bp alignment-tree of sequences obtained in this study and from GenBank (Ullrich et al. 2010) and b 717 bp alignment-tree of sequences available from Ullrich et al. (2010). Node support is shown at (below) resolved branches

Fig. 2 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 2 Distribution of the members of the Poecilimon jonicus group sensu lato—ranges of all species currently considered within the groups P. jonicus and P. inflatus including subspecies of P. jonicus shown with different colors as marked in the plates

Fig. 1 in Evolution of Poecilimon jonicus group (Orthoptera: Tettigoniidae): a history linked to the Aegean Neogene paleogeography

Fig. 1 General appearance of representatives of the Poecilimon jonicus group. a, b P. jonicus lobulatus (a male, b female); c P. werneri (female); d, e P. erimanthos (d male, e female); f P. inflatus lyciae (male); g, h