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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

Fig. 5 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 5 Simplified global paleogeograhic reconstruction during the Late Jurassic, based on Scotese (2014: Map 35, Oxfordian) showing potential dispersal routes of caturoids through the Hispanic Corridor. Stars represent the only known records of caturoids outside Europe: 1, "Caturus" dartoni Eastman, 1899, from the lower Sundance Formation in South Dakota (Bathonian); 2, Caturus deani Gregory, 1923, from the Jagua Formation of Cuba (Oxfordian); 3, Catutoichthys olsacheri and Caturoidea sp. from the Vaca Muerta Formation of Argentina (Tithonian)

Fig. 2 Specimen MPCA 632 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 2 Specimen MPCA 632 from the Jurassic of Neuquén, Argentina: a, fossil of Caturidae sp., including disarticulated skull bones described in Bogan et al. (2013); b, corresponding inventory card of the Museo Carlos Ameghino (MPCA)

Fig. 1 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 1 Geographical setting: a, general location; b, simplified map showing outcrops of the Mendoza and Los Menucos groups in the provinces of Neuquén and Río Negro. Outcrops of the Mendoza Group are redrawn from the regional scheme in the geological map HG 3969-I Zapala (Leanza et al., 2001). Outcrops of the Los Menucos Group are redrawn from the regional scheme (esquema regional) in the geological map HG 4169-II Los Menucos (Cuchi et al., 2001)

Fig. 3 in The early fossil record of Caturoidea (Halecomorphi: Amiiformes): biogeographic implications

Fig. 3 Nannoflora identified in the sediment of MPCA 632: Cyclagelosphaera margerelii (1–4), Crepidolithus sp. (5–6), Watznaueria barnesiae (7–8), Polycostella beckmannii (9–12), Watznaueria britannica (13), Watznaueria fossacincta (14), Watznaueria biporta (15–16)

Fig. 7 in First record of Lepidonotus tenuisetosus (Annelida: Polynoidae) from Tunisia with distributional notes Abstract

Fig. 7: Lepidonotus clava from Greece. HCMR_Nag_ EL_01_2008_0185. A. Anterior end, dorsal view. B. Midbody elytron. C. Midbody elytrophorous parapodium. D. Midbody neurochaetae. HCMR_Nag_EL_01_2008_0194: E. Detail of midbody neurocheatae tips. Photos by G. Chatzigeorgiou.

Fig. 1 in First record of Lepidonotus tenuisetosus (Annelida: Polynoidae) from Tunisia with distributional notes Abstract

Fig. 1: A. Validated Mediterranean locations for Lepidonotus tenuisetosus (white spot: Gulf of Tunis) and Lepidonotus carinulatus (red spot: Alborán Sea; green spot: Peninsula of Sinai). B. Location of Radès area (white spot) in the Gulf of Tunis. D. Collecting site and method at Radès area. A–C: photos from Google Earth (images: © 2020 Landsat/Copernicus, TerraMetrics, Maxar Technologies; data: SIO, NOAA, U. S. Navy, NGA, GEBCO); D: photo by Marwa Chaibi.

Fig. 4 in First record of Lepidonotus tenuisetosus (Annelida: Polynoidae) from Tunisia with distributional notes Abstract

Fig. 4: Lepidonotus tenuisetosus. A. Notochaetae from chaetiger 15. B. Tip of notochaeta. C. Neurochaetae from first chaetiger. D. Neurochaetae from chaetiger 15.

Fig. 15 in New records of rare species in the Mediterranean Sea (March 2021)

Fig. 15: Specimens of Katsuwonus pelamis, captured off Cape Kurtoğlu, Fethiye, southern Aegean Sea (horizontal bar: 100 mm). Photo credit: E. Öçal.

Fig. 13 in New records of rare species in the Mediterranean Sea (March 2021)

Fig. 13: Distolambrus maltzami (Miers, 1881), male, North Aegean Sea, units shown in mm. a) dorsal side of the carapace; b) ventral side of the carapace.

Fig. 8 in New records of rare species in the Mediterranean Sea (March 2021)

Fig. 8: Specimens of Sphyraena viridensis caught in Tarska Cove in Northern Adriatic on 25th January 2020. Photo credit: Antonio Baras.

Fig. 12 in New records of rare species in the Mediterranean Sea (March 2021)

Fig. 12: The Ranzania laevis specimen found stranded on the Kokkini Hani beach in Crete (TL = 63 cm).

Fig. 8 in First record of Lepidonotus tenuisetosus (Annelida: Polynoidae) from Tunisia with distributional notes Abstract

Fig. 8: Size relationships in Lepidonotus tenuisetosus. A. Body width without parapodia (WoP) vs. body length. B. Body width with parapodia (WP) vs. body length.

Fig. 10 in New records of rare species in the Mediterranean Sea (March 2021)

Fig. 10: Bursa scrobilator scrobilator from South Rethymno, Crete (shell height ~5-7 cm). A) Crabbed shell. B) Living specimen. Photo credit: Stelios Mantadakis.

Fig. 6 in First record of Lepidonotus tenuisetosus (Annelida: Polynoidae) from Tunisia with distributional notes Abstract

Fig. 6: Lepidonotus sp., NHMR PMR-17630, Croatia: A. Anterior end, dorsal view. B. Parapodia 7 and 8, right side. C. Neurochaetae from parapodium 8 (right side). D. Neurochaetae from parapodium 8 (left side). E. Neurochaetae from parapodium 9 (right side).