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Рис. 2. ЗΑание ТЦ «Москва», гΑе быΛо найΑено наибоΛьшее чисΛо погибших от стоΛкновения птиц. Фото Δ. А. БеΛяева Fig. 2. The building of the "Moskva" shopping center, where the highest number of bird window collision deaths was registered. Photo by D. A. Belyaev in Deaths Resulting From Bird Window Collisions In Ussuriysk (Primorsky Krai)

Рис. 2. ЗΑание ТЦ «Москва», гΑе быΛо найΑено наибоΛьшее чисΛо погибших от стоΛкновения птиц. Фото Δ. А. БеΛяева Fig. 2. The building of the "Moskva" shopping center, where the highest number of bird window collision deaths was registered. Photo by D. A. Belyaev

Fig. 10 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 10 Fish teeth from the studied localities: a–e Pshekharus yesinorum Bannikov & Kotlyar, 2015, isolated jaw teeth in lateral (a1, b1, c, d1, e) and dorsal view (a2, b2, d2), arranged in a sequence from distal to proximal positions. f Dasyatis sp., anterior tooth in dorsal (f1), occlusal view (f2), profile (f3) and labial view (f4)

Fig. 7 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 7 Otoliths of Gobionellidae: a–e Deltentosteus aff. telleri (Schubert, 1906), 7a Shydlivshchyna, NMNHU-P PI 2553, b (reversed), d Kozatskyi Yar, NMNHU-P PI 2552, c (reversed), e Mlyntsi, NMB P1209. f, g Economidichthys triangularis (Weiler, 1943), f (reversed) Shydlivshchyna, NMB P1210, g (reversed) Mlyntsi, NMNHU-P PI 2554. h, i Knipowitschia polonica Schwarzhans et al., 2020a, 2020b, h Shydlivshchyna, NMNHU-P PI 2562, i Kozatskyi Yar, NMB P1213. j, k Pomatoschistus elegans (Procházka, 1900), j (reversed) Kozatskyi Yar, NMNHU-P PI 2576, k (reversed) Shydlivshchyna, NMB P1222

Fig. 4 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 4 Otoliths of Gobius spp.: a–e Gobius bratishkoi n. sp., a holotype, NMNHU-P PI 2555, Kozatskyi Yar, b–e paratypes, b (reversed) Mlyntsi, NMNHU-P PI 2556, c–e (reversed) Kozatskyi Yar, NMB P1211. f Gobius reichenbacherae Schwarzhans, 2014, Shydlivshchyna, NMNHU-P PI 2557 (reversed). g–k Gobius ukrainicus n. sp., j holotype, Shydlivshchyna, NMNHU-P PI 2558, g–i, k paratypes, g, i, k NMNHU-P PI 2560, h (reversed) Mlyntsi, NMNHU-P PI 2559

Fig. 1 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 1 Location map and stratigraphy: a schematic map showing the Medobory Reef (after Korolyuk, 1952, and Górka et al., 2012, with modifications) and the studied localities in the vicinities of Horodok, western Ukraine; b schematic geologic cross section of the Badenian sequence through the Medobory region after Wysocka et. al. (2016) and Górka (2018a)

Fig. 13 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 13 Late Badenian paleogeography of the Paratethys and distribution of selected non-gobioid otolith-based taxa through the basin. Most common species are shown in bold printing. Asterisk denotes multiple locations, of which Borský Mikuláš represents the richest and most recently described otolith assemblage (Brzobohatý et al., 2022). Double asterisk for Dentex aff. gregarius tentatively includes records of Dentex aff. maroccanus by Brzobohatý et. al. (2022). Triple asterisk for Argyrosomus sp. denotes record of Argyrosomus aff. regius by Brzobohatý et. al. (2022). Paleogeography based on Rögl (1999), Popov et. al. (2004), and KováČ et. al. (2017)

Fig. 9 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 9 Otoliths of Haemulidae, Serranidae, Sparidae, Leiognathidae and Caproidae: a (reversed)—Brachydeuterus speronatus (Bassoli, 1906), Kozatskyi Yar, NMNHU-P PI 2549. b, c Serranidae indet., b (broken and repaired), c (reversed), Kozatskyi Yar, NMNHU-P PI 2579. d, e Pshekharus yesinorum Bannikov & Kotlyar, 2015, Mlyntsi, NMNHU-P PI 2578. f (reversed)—Leiognathidae indet., Shydlivshchyna, NMB P1214. g Perciformes indet., Shydlivshchyna, NMB P1221. h (reversed) – Capros aper (Linnaeus, 1758), Mlyntsi, NMB P1206

Fig. 12 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 12 Late Badenian paleogeography of the Paratethys and distribution of gobioid otolith-based taxa through the basin. Most common species are shown in bold printing (Gobius reichenbacherae tentatively includes records of Gobius aff. niger by Brzobohatý et al., 2022). Asterisk denotes multiple locations, of which Borský Mikuláš represents the richest and most recently described otolith assemblage (Brzobohatý et al., 2022). Double asterisk denotes species only known in the Vienna Basin from the early Badenian and shown for correlation purposes. Paleogeography based on Rögl (1999), Popov et. al. (2004), and KováČ et. al. (2017)

Fig. 6 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 6 Otoliths of Medoborichthys and Vanderhorstia: a–d Medoborichthys podolicus n. gen. et n. sp., b holotype, NMNHU-P PI 2563, Mlyntsi, a, c, d paratypes, a Mlyntsi, NMNHU-P PI 2564, c Shydlivshchyna, NMNHU-P PI 2565, d (reversed) Kozatskyi Yar, NMB P1215. e–g Medoborichthys renesulcis n. gen. et n. sp., e holotype, NMNHU-P PI 2566, Mlyntsi, f, g paratypes, f Kozatskyi Yar, NMB P1216, g (reversed) Mlyntsi, NMNHU-P PI 2567. h–j Vanderhorstia prochazkai Schwarzhans et al., 2020a, 2020b, h (reversed), j (reversed) Mlyntsi, NMB P1223, h (reversed) Shydlivshchyna, NMNHU-P PI 2582. k Vanderhorstia sp., Shydlivshchyna, NMB P1224

Fig. 3 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 3 Otoliths of Gadiformes: a, b Micromesistius planatus (Bassoli & Schubert, 1906), Mlyntsi, a NMNHU-P PI 2568 and b NMB P1218. c–f Onogadus simplicissimus (Schubert, 1906), c (reversed), d, f Shydlivshchyna, NMB P1220, e Mlyntsi, NMNHU-P PI 2572

Fig. 2 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 2 Photographs of the investigated outcrops: Mlyntsi (a, b), Kozatskyi Yar (c, d), and Shydlivshchyna (e, f) in general view and close-up. The total length of the shovel handle is 72 cm

Fig. 8 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 8 Otoliths of Blenniidae and Labridae: a, b Blennius vernyhorovae n. sp., a holotype, NMNHU-P PI 2547, Mlyntsi, b (reversed) paratype, Kozatskyi Yar, NMB P1205. c, d Coris medoboryensis n. sp., c holotype, NMNHU-P PI 2551, Kozatskyi Yar, d (reversed) paratype, Mlyntsi, NMB P1208

Fig. 11 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 11 Schematic block diagram of the northern part of the Central Paratethys during the late Badenian depicting the main localities from which otolith have been studied and the common species found therein (most common ones shown in bold printing). Diagram not to scale and not proportional; based on KováČ et. al. (2017)

Fig. 5 in A rare window into a back-reef fish community from the middle Miocene (late Badenian) Medobory Hills barrier reef in western Ukraine, reconstructed mostly by means of otoliths

Fig. 5 Otoliths of Odondebuenia, Parenypnias and Bathygobius?: a–d Odondebuenia agiadiae Schwarzhans et al., 2020a, 2020b, a (reversed) Kozatskyi Yar, NMB P1219, b (reversed), d Kozatskyi Yar, NMNHU-P PI 2569, c (reversed) Mlyntsi, NMNHU-P PI 2570. e–h Parenypnias inauditus n. gen. et n. sp., f holotype, Kozatskyi Yar, NMNHU-P PI 2550, e, g (reversed) Shydlivshchyna, NMB P1207, h Žižkov 1 well (1616–1622 m), DGS MU-0395. i Parenypnias kiselevi n. gen. et n. sp., holotype, Mlyntsi, NMNHU-P PI 2574. j Enypnias seminudus (GÜnther, 1861), Recent, USNM 407784, 13° 22′ N 87° 52′ W. k Gobiosoma bosc (Lacépède, 1800), Recent (reversed), LACM coll. Fitch, off Rappahannock. l Bathygobius? sp. (reversed), Kozatskyi Yar, NMNHU-P PI 2548

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FIG. 71. Elytral morphotypes with window punctures. A, B. Morphotype 72, VMNH 49731. C in Remarkable Diversity Of Beetles (Coleoptera) In The Late Triassic (Norian) "Solite Deposit" Of Virginia And North Carolina

FIG. 71. Elytral morphotypes with window punctures. A, B. Morphotype 72, VMNH 49731. C. Zygadenia westraliensis (E. Jurassic, Western Australia; Martin, 2010). Photo courtesy of Sarah Martin. D, E. Morphotype 73, VMNH 94836. Photo courtesy of VMNH. Scale bars: 1 mm.

Fig. 5 in Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity

Fig. 5. Thin sections of trepostome bryozoan Homotrypa cochlea sp. nov. from Upper Leintwardine Formation, Ludfordian, upper Ludlow, Silurian; Delbury Quarry, Shropshire, UK. A. Holotype, NMW 2019.21G.2.3, ramose colony form (A1), thick mesozooecia walls connected by diaphragms, continue cystose shape of earlier growth (A2). B. NMW 2019.21G.2.4, autozooecia rounded in cross-section, some irregularly shaped.

Fig. 4 in Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity

Fig. 4. Thin section of trepostome bryozoan Homotrypa cochlea sp. nov. from Upper Leintwardine Formation, Ludfordian, upper Ludlow; Delbury Quarry, Shropshire, UK. Holotype, NMW 2019.21G.2.3, bryozoan colony encrusting gastropod shell and developing ramose form at shell aperture.

Fig. 2 in Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity

Fig. 2. Trepostome bryozoan Homotrypa cochlea sp. nov. from Upper Leintwardine Formation; Ludfordian, upper Ludlow, Silurian; Delbury Quarry, Shropshire, UK. A. NMW 2019.21G.7.1, bryozoan encrusting the surface of a gastropod shell. B. NMW 2019.21G.33, bryozoan encrusting the surface of a gastropod shell but not growing across aperture.

Fig. 1 in Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity

Fig. 1. Map showing the location and geological setting (asterisk) of Delbury Quarry in Shropshire, UK (amended from https://digimap.edina.ac.uk/roam/ map/geology and https://digimap.edina.ac.uk/roam/map/os; accessed 05/08/21).