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Fig. 3 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 3 Associated ammonoid fauna recorded at the locality Harmanecká Cave—Kozelník. A–C Lardaroceras sp. aff. krystyni Balini, 1992a

Fig. 10 A in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 10 A Reconstruction of cephalopod habitat within Western Carpathian Ráztoka Limestone, Illyrian Trinodosus—Reitzi Zones. Reconstruction: Petr Modlitba, with courtesy of author. B 1. Nautiloids. 2. Diverse ammonoids. 3. Aulacoceratids. 4. Mojsisovicsteuthis. 5. Breviconoteuthis. The benthic fauna is composed by abundant crinoids, echinoids, bivalves and brachiopods. Algae meadows are supposed based on geochemical data. C Fragment of partly tectonically deformed phragmocone of undetermined aulacoceratid; scale bar equals 1 cm

Fig. 1 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 1 Geographical position of the areas of interest (A, B) and close-up views of the satellite photo with precise localization of the studied outcrops in the village Podhradie (C), and near Dolný Harmanec (D). E Outcrop in the roadcut in the village Podhradie. The fossiliferous Bed 3 is outlined. Orange circles with acronyms TO represent the sampling points for the organic geochemistry

Fig. 9 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 9 Plot of Pr/n-C17 versus Ph/n-C18 cross plot showing the source and depositional environments of the natural samples (from Beds 3, 6 and 7, locality Podhradie)

Fig. 11 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 11 Detailed reconstruction of the sea-bottom rich in algae, sponges and crinoid meadows, showing also the common presence of conodonts and a representative of coleoid cephalopod. Petr Modlitba, with courtesy of author

Fig. 8 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 8 Palaeobiogeographic distribution of genera Mojsisovicsteuthis and Breviconoteuthis (Anisian–Carnian). While Mojsisovicsteuthis (larger straight phragmocone) shows large geographic distribution, the genus Breviconoteuthis (smaller phragmocone) is known only from few sites in the Alpine-Carpathian system

Fig. 4 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 4 Associated conodont fauna recorded at the locality Podhradie. All specimens come from the Bed 3. A Paragondolella trammeri (Kozur, 1972). B Paragondolella cf. alpina (Kozur & Mostler, 1982). C Paragondolella slugovensis (Ramovš, 1996). D Paragondolella ex gr. praeszaboi (Kovács et al., 1996). E, F Neogondolella constricta (Mosher & Clark, 1965). G Paragondolella praeszaboi (Kovácset al., 1996). H Paragondolella cf. praeszaboi (Kovács et al., 1996). I–K Paragondolella bifurcata Budurov & Stefanov, 1972. Scale bar 200 μm (A) and 200 μm (B–K)

Fig. 5 in Rare Middle Triassic coleoids from the Alpine-Carpathian system: new records from Slovakia and their significance

Fig. 5 Mojsisovicsteuthis boeckhi (StÜrzenbaum, 1875). A–D Specimen No. KGP-KO-001, upper Anisian, lower Illyrian, Harmanecká Cave—Kozelník, Slovakia. A Dorso-ventral view; B lateral view; C cross-section; D position of the siphuncle (s). E–H Specimen No. T.3593. E Dorso-ventral view; F lateral view; G, H Cross-section with position of the siphuncle (H. enlarged); I Cross-section of the apical part. J–P. Holotype No. T.829. Bakony (Hungary), Anisian, Reitzi Zone. J Original figure of StÜrzenbaum (1875), lateral view; K lateral view; L dorso-ventral view; M cross-section; N original figure of StÜrzenbaum (1875) with missinterpreted position of the siphuncle; O, P longitudinal section of the phragmocone with septa arrangement (partly seen). Q The largest specimen No. T.3137 in the lateral view. Scale bar equals 1 cm

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Figure 2. A in First record of Phlebotomus (Transphlebotomus) mascittii in Slovakia

Figure 2. A barn on the farm in Pernek, Slovakia where the female Phlebotomus mascittii specimen was collected.

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Fig. 4 in The Chorthippus Albomarginatus-Group (Orthoptera: Acrididae: Gomphocerinae) In The Carpathian Basin: Traces Of Hybridization Between C. Albomarginatus And C. Oschei In Southern Slovakia

Fig. 4. Oscillograms of the courtship song (parts of the songs showed in Fig. 2) of four males of Chorthippus oschei from Slovakia (in each group of three lines, the two upper lines represent leg-movements and the third line represents sound). a, b – males no. 1–2 from NE Ardovo, c, d – males 3–4 from SW Ardovo (in d – the recording of only one leg is shown). B1, A1 and C elements are indicated. Drawings show the stroke with the hind tibiae at the beginning of the C element and the

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Fig. 1 in The Chorthippus Albomarginatus-Group (Orthoptera: Acrididae: Gomphocerinae) In The Carpathian Basin: Traces Of Hybridization Between C. Albomarginatus And C. Oschei In Southern Slovakia

Fig. 1. Male (on the left) and female (on the right) of Chorthippus oschei from locality Ardovo in southern Slovakia

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Fig. 3 in The Chorthippus Albomarginatus-Group (Orthoptera: Acrididae: Gomphocerinae) In The Carpathian Basin: Traces Of Hybridization Between C. Albomarginatus And C. Oschei In Southern Slovakia

Fig. 3. Oscillograms of the courtship song (parts of the songs showed in Fig. 2) of four males of Chorthippus oschei from Slovakia (in each group of three lines, the two upper lines represent leg-movements and the third line represents sound). a, b – males no. 1–2 from NE Ardovo, c, d –

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.