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Fig. 11 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 11. Serpulid polychaetes from the Jurassic of Poland. A. Placostegus planorbiformis (Münster in Goldfuss, 1831) encrusting a sponge fragment from the Oxfordian of Zalas (GIUS 8-3746/8). B. Pseudovermilia sp. encrusting a rock fragment from the Callovian of Zalas (GIUS 8-3589/15). Scale bars 1 mm.

Fig. 4 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 4. Serpulid polychaetes from the Jurassic of Poland. A. Metavermilia? sp. encrusting a belemnite rostrum from the middle Bathonian of Gnaszyn Dolny (GIUS 8-3730/9). B–E. Filogranula runcinata (Sowerby, 1829), specimens encrusting: an oncoid from the upper Bajocian–lower Bathonian of Ogrodzieniec-Świertowiec (B, GIUS 8-3750/3); a hiatus concretion from the upper Bajocian of Mokrsko (C, GIUS 8-3751/4); shell fragments from the middle Bathonian of Gnaszyn Dolny (D, GIUS 8-3730/10), the Callovian of Zalas (E, GIUS 8-3589/6). F, G. Filogranula spongiophila sp. nov. encrusting sponge fragments from the Oxfordian of Zalas (F, holotype, GIUS 8-3746/2; G, paratype, GIUS 8-3746/3). Scale bars 1 mm.

Fig. 1 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 1. Palaeogeography and geology of the investigated area. A. Paleogeographical sketch-map of Europe during the Middle Jurassic (from Leonowicz 2016, modified after Ziegler 1990). AM, Armorican Massif; BM, Bohemian Massif; CEBS, Central European Basin System; CNSD, Central North Sea Dome; IBM, Iberian Meseta,; IM, Irish Massif; LBM, London-Brabant Massif; MCA, Meta-Carpathian Arc; RHB, Rockall-Hatton Bank; UH, Ukrainian High. B. Geological sketch-map of Poland without the Cenozoic cover with three sampled localities indicated. HCM, Holy Cross Mountains; PJ, Polish Jura; 1, Bolęcin; 2, Zalas; 3, Małogoszcz. C. Geological map of the Polish Jura area without Quaternary cover, with sampled localities indicated (after Zatoń and Taylor 2009b).

Fig. 14 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 14. Dendrogram showing clustering of substrates sharing similar taxa of tube-dwelling polychaetes from the Polish Basin.

Fig. 10 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 10. Serpulid and sabellid polychaetes from the Jurassic of Poland. A. Mucroserpula tricarinata (Sowerby, 1829) (white arrow) and sabellid Glomerula gordialis (black arrow) encrusting a fragment of a shell from the Callovian of Zalas (GIUS 8-3589/14). B. Mucroserpula? sp. encrusting a fragment of a shell from the middle Bathonian of Gnaszyn Dolny (GIUS 8-3730/26); top (B1) and cross-section view (B2). Notice the characteristic pentagonal cross-section (B2) due to the presence of three keels. Scale bars 1 mm.

Fig. 13 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 13. Serpulid polychaetes from the Jurassic of Poland. A. Unattached Serpulidae sp. 2 from the middle Bathonian of Gnaszyn Dolny (GIUS 8-3730/27). B. Dense aggregation of closely spaced Serpulidae sp. 3 encrusting a fragment of a belemnite rostrum from the middle Bathonian of Gnaszyn Dolny GIUS 8-3730/28). C. Serpulidae sp. 4 from the lower Kimmeridgian of Małogoszcz (GIUS 8-3747/3).

Fig. 6 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 6. Serpulid polychaetes from the Jurassic of Poland. A. Cementula cf. circinnalis (Münster in Goldfuss, 1831) encrusting an oncoid from the upper Bajocian–lower Bathonian of Ogrodzieniec-Świertowiec (GIUS 8-3750/4). B. "Serpula cingulata Münster in Goldfuss, 1831" encrusting a sponge fragment from the the Oxfordian of Zalas (GIUS 8-3746/7). C. Propomatoceros lumbricalis (Schlotheim, 1820) (arrowhead) and Cementula cf. circinnalis arrow) encrusting an oncoid from the upper Bajocian–lower Bathonian of Ogrodzieniec-Świertowiec (GIUS 8-3750/5). D–F. Propomatoceros lumbricalis, specimen encrusting: a piece of a belemnite rostrum from the middle Bathonian of Gnaszyn Dolny (D, GIUS 8-3730/11); an oyster shell from the middle Bathonian of Gnaszyn Dolny (E, GIUS 8-3730/12); a shell fragment from the Callovian of Zalas (F, GIUS 8-3589/11).

Fig. 2 in A Lujiatun-like dinosaurian assemblage from the Jehol Biota of Ningcheng, Inner Mongolia, Northeast China

Fig. 2. Fossils found in the Xidayingzi site from the Early Cretaceous Ningcheng Basin, Inner Mongolia. A. Sinovenator-like troodontid dinosaur (SDUST-V1062), the left pes is exposed in medial view. B. Ceratopsian dinosaur Psittacosaurus sp. (PMOL-AD00163), the maxilary teeth are loosely arranged and exposed in lateral view. C. Neornithischian dinosaur Jeholosaurus sp. (SDUST-V1063), the scapulocoracoid, humerus, ulna, and radius in lateral view. D. Euhelopus-like sauropod (SDUST-V1064), digital image of the tooth crown in medial view. E. Indeterminated lizard (PMOLAR00268), digital image of the fragmentary mandible in lingual view. F. Symmetrodont-like mammal (PMOL-AM00036), digital image of the mandible in lingual view.

Fig. 12 in Middle and Late Jurassic tube-dwelling polychaetes from the Polish Basin: diversity, palaeoecology and comparisons with other assemblages

Fig. 12. Serpulidae sp. 1 from the Jurassic of Poland. A. Serpulidae sp. 1 and a tiny Glomerula gordialis (Schlotheim, 1820) (arrowed) encrusting a shell fragment from the upper Bathonian–lower Callovian of Bolęcin (GIUS 8-3745/4); top (A1) and lateral (A2) view; A2 shows a flattened shape of the tube. B. Serpulidae sp. 1 and a tiny, presumably juvenile Filogranula runcinata (Sowerby, 1829) (above, arrowed) encrusting a shell fragment from the Callovian of Zalas (GIUS 8-3589/16). Scale bars 1 mm.

Fig. 1 in A Lujiatun-like dinosaurian assemblage from the Jehol Biota of Ningcheng, Inner Mongolia, Northeast China

Fig. 1. Map of the Inner Mongolia, Liaoning and Hebei (A) showing location of the Xidayingzi site and the outcrops of the Lujiatun Unit of the Yixian Formation of the Jehol Biota in Beipiao, western Liaoning Province, China. Stratigraphic column (B) and corresponding photographic image (C) of the Early Cretaceous Xidayingzi site.

Fig. 33 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 33. Rarefaction curves of Cassian assemblages from Misurina Landslide, Lago Antorno (assemblages studied herein), Settsass Scharte (Nützel and Kaim 2014) and Stuores Wiesen (Hausmann and Nützel 2015). Only bulk samples are used.

Fig. 28 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 28. Cardiid bivalve Septocardia pichleri (Bittner, 1895) from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic. PZO 12866, in ventral (A1), dorsal (A2), and lateral (A3, A4) views.

Fig. 24 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 24. Stuoraxid gastropod Ampezzogyra angulata Nützel and Hausmann sp. nov. from Lago Antorno (A, C) and Misurina Landslide (B, D), Cassian Formation, northern Italy, Late Triassic. A. Paratype PZO 12848, in oblique lateral (A1), apical (A2), and apertural (A3) views; A4, detail teleoconch at adapical whorl angulation with micro-ornament of fine tubercles; A5, protoconch in oblique lateral view; A6, protoconch in apical view; A7, crossed lamellar shell structure. B. Paratype PZO 12733, in oblique lateral (B1), apical (B2), and apertural (B3) views. C. Holotype PZO 12847, in apical (C1), basal (C2), and apertural (C3) views; C4, detail of C3; C5, detail teleoconch with micro-ornament of fine tubercles; C6, protoconch in apical view; C7, protoconch in oblique view. D. Paratype PZO 12734, in apical (D1) and apertural (D2) views.

Fig. 23. Hyalogyrinid gastropod Alexogyra marshalli Bandel, 1996 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 23. Hyalogyrinid gastropod Alexogyra marshalli Bandel, 1996 from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12842, in apical view. B. PZO 12843, in apertural view. C. PZO 12844, protoconch in oblique lateral view. D. PZO 12845, in oblique apertural view to show base.

Fig. 20 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 20. Mathildid gastropod Jurilda elongata (Leonardi and Fiscon, 1959) from Misurina Landslide, northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12716, in lateral view (A1), A2, early whorls including heterostrophic protoconch, in lateral view. B. PZO 12717, in apical (B1) and lateral (B2) views; B3, early whorls including heterostrophic protoconch, in lateral view. C. PZO 12718, in apertural (C1) and oblique basal (C2) views. D. PZO 12719, in lateral (D1) and oblique basal (D2) views. E. PZO 12720, detail teleoconch whorl, in lateral view.

Fig. 16 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 16. Protorculid gastropods from Lago Antorno (A–D) and Misurina Landslide (E), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. Atorcula sp., PZO 12816, in lateral view with drill holes (A1), A2, close up showing incomplete drill hole (right) and complete one (left). B. Atorcula sp., PZO 12817, in lateral view (B1), B2, close up showing drill hole. C. Atorcula canalifera (Münster, 1841), PZO 12819, in apertural view. D. Atorcula canalifera (Münster, 1841), PZO 12888, in apertural view. E. Atorcula canalifera (Münster, 1841), PZO 12697, axially ribbed larval shell and first smooth teleoconch whorls, in lateral view.

Fig. 13 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 13. Coelostylinid gastropods Helenostylina convexa (Nützel and Kaim, 2014) from Lago Antorno (A, B, C), Misurina Skilift (D), and Misurina Landslide (E), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. PZO 12812, relatively large specimen with well-preserved base with spiral ribs, in apertural view (A1); A2, early whorls in lateral view; A3, basal view showing spiral ribs; A4, oblique basal view showing spiral ribs on base. B. PZO 12813, relatively large specimen with spiral ribs on base and protoconch with tubercles, in apertural view (B1); B2, close up of base showing spiral ribs on base; B3, early whorls with tubercles on larval shell, in lateral view. C. PZO 12814, juvenile shell with tubercles on larval shell, in lateral view. D. PZO 12694, juvenile shell with tubercles on larval shell and healed shell fracture, in apertural (D1) and lateral (D2, D4) views; details showing end of larval shell (arrows), in lateral (D3) and apical (D5) views. E. PZO 12695, relatively large specimen with well-preserved base with spiral ribs and protoconch with tubercles, in apertural view (E1); E2, oblique apertural view to show base with spiral ribs; E3, protoconch in lateral view.

Fig. 12 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 12. Caenogastropods from Lago Antorno (A) and Misurina Landslide (B–F), northern Italy, Cassian Formation, Carnian, Upper Triassic. A. Unidentified caenogastropod, PZO 12829, in lateral view. B. Coelostylina sp. 1, PZO 12691, in apertural view. C. Coelostylina sp. 2, PZO 12692, in lateral view. D. Flemingella bistriata (Münster, 1841), PZO 12713, in apertural view. E. Coelochrysalis pupaeformis (Münster, 1841), PZO 12714, in lateral view, with constriction of last whorl. F. Coelochrysalis pupaeformis (Münster, 1841), PZO 12715, deformed specimen in lateral view, showing constriction of last whorl.

Fig. 10 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 10. Coelostylinid gastropod Coelostylina conica (Münster, 1841) from Lago Antorno (A–D) and Misurina Landslide (E, F), northern Italy, Cassian Formation, Carnian, Late Triassic. A. PZO 12803, in apertural (A1) and abapertural (A2) views; A3, spire whorls in lateral view; A4, close up of spire whorl showing faint spirally arranged micro-pits; A5, close up of apical whorls in lateral view. B. PZO 12804 in apertural view. C. PZO 12805, with drill hole, in apertural view (C1); C2, early whorls including protoconch, in lateral view. D. PZO 12806, in lateral view (D1); D2, early whorls including protoconch, in lateral view; D3, whorl detail with boring. E. PZO 12686, in apertural view. F. PZO 12687, with drill hole in apertural view (F1); F2, detail, in apertural view.

Fig. 7 in Palaeoecology of tropical marine invertebrate assemblages from the Late Triassic of Misurina, Dolomites, Italy

Fig. 7. Naticopsid gastropod Hologyra? expansa (Laube, 1869), PZO 12802, from Lago Antorno, northern Italy, Cassian Formation, Carnian, Upper Triassic; apertural view showing callus on inner and parietal lip.