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Figure 2 in An alien species or another perspective to the freshwater gobies puzzle: a new finding in Lake Prespa

Figure 2. Economidichthys pygmaeus from Lake Prespa (a), and the perianal organ of one of the specimens (b).

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Figure 1 in An alien species or another perspective to the freshwater gobies puzzle: a new finding in Lake Prespa

Figure 1. Distribution of Economidichthys sp. in western Greece (a) the location of Lake Prespa, and the sampling sites (b).

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Figure 1 in New finding of Convolvulus hawkmoth - Agrius convolvuli (Linnaeus, 1758) (Lepidoptera, Sphingidae) in the south of Western Siberia

Figure 1. Agrius convolvuli (Linnaeus, 1758), male, Russia, Altai Krai, near Barnaul, Turina Gora, 4.x.2020, leg. I. Volgin (private collection of I. Volgin, Barnaul, Russia).

Figure 4 in A surprising finding of Ecclisopteryx asterix Malicky, 1979 (Insecta, Trichoptera) in Croatia with notes to DNA barcoding and new distributional data of the subfamily Drusinae

Figure 4. Spatial distribution of the Drusinae species in Croatia, literature data supplemented with new records.

Figure 3 in A surprising finding of Ecclisopteryx asterix Malicky, 1979 (Insecta, Trichoptera) in Croatia with notes to DNA barcoding and new distributional data of the subfamily Drusinae

Figure 3. Maximum likelihood phylogram based on the COI sequences of Ecclisopteryx asterix from Croatia and haplotypes of Ecclisopteryx species available in BOLD database. Numbers at the nodes indicate maximum likelihood (ML) bootstrap support values (BS). Terminal codes represent BOLD Process IDs.

Figure 2. A in A surprising finding of Ecclisopteryx asterix Malicky, 1979 (Insecta, Trichoptera) in Croatia with notes to DNA barcoding and new distributional data of the subfamily Drusinae

Figure 2. A Larva of Ecclisiopteryx asterix in its case; B morphological character important for identification: shape of the pronotum (p); C pronotum (p), mesonotum (me), and sclerites at metanotum (mt) in dorsal view; D abdominal segments I-VI with gills (g) and lateral fringe (lf), right lateral view.

Figure 1. A in A surprising finding of Ecclisopteryx asterix Malicky, 1979 (Insecta, Trichoptera) in Croatia with notes to DNA barcoding and new distributional data of the subfamily Drusinae

Figure 1. A New record of Ecclisopteryx asterix Malicky, 1979 in Croatia (red dot) and hitherto known range in Austria, Slovenia and Italy (yellow area) (Robert, 2015); B the crenal reach of the Šumi Spring, and C a close up of the habitat where E. asterix larvae were collected.

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Fig. 1 in From incidental findings to systematic discovery: locating and monitoring a new population of the endangered Harlequin Toad

Fig. 1 Location and boundaries of the Alexander Skutch Biological Corridor (ASBC) in the province of San José, Costa Rica.

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Fig. 3 in From incidental findings to systematic discovery: locating and monitoring a new population of the endangered Harlequin Toad

Fig. 3 Males, females, and juveniles of Atelopus varius found in the Alexander Skutch Biological Corridor. (A) Male found during February surveys. (B) Sleeping male in the leaf litter in the same location of a male in Fig. 2(A). (C) and (E) are juveniles high above the river bank, at least 3–4 m high in the vegetation of the understory, and juvenile (C) is sleeping. (D) A female Harlequin Toad sleeping on the vegetation five m above the river.

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Fig. 2 in From incidental findings to systematic discovery: locating and monitoring a new population of the endangered Harlequin Toad

Fig. 2 Detail of Atelopus varius individuals found during February and June 2017 in the ASBC. The left column includes males; the right column includes females. Males (B) and (C) were photographed as found, as were females (E), (G), and (H). Note the spread-out basking position of female (G).

Fig. 5 in New Finds of Stegosaur Tracks from the Upper Jurassic Lourinhã Formation, Portugal

Fig. 5. Scatter diagram showing the relationship between pes footprint length (L) and footprint width (W) for specimens of Deltapodus from England, Portugal, Spain (1 Asturias, 2 Teruel), USA and Morocco. The example from Teruel is a mean value (Cobos et al. 2010).

Fig. 4 in New Finds of Stegosaur Tracks from the Upper Jurassic Lourinhã Formation, Portugal

Fig. 4. The two associated natural casts of Deltapodus manus tracks found at Porto Barcas, Lourinhã Formation (Upper Jurassic, Portugal). Both tracks show a pronounced semilunate shape. A. Manus track PBS 5 (ML 1351) seen from below. B. Manus track PBS6 (ML 1352) seen from below (B1), caudal view (B2), and enlarged section of the front (B3), showing the vertical striations covering the front and sides of the cast.

Fig. 3. Deltapodus track PBS 2 in New Finds of Stegosaur Tracks from the Upper Jurassic Lourinhã Formation, Portugal

Fig. 3. Deltapodus track PBS 2 (ML 1347) from the Lourinhã Formation (Upper Jurassic, Portugal). A. Plantar view. B. Detail of scaly skin impressions. C. Vertical striations of the skin on the cast surface.

Fig. 1 in New Finds of Stegosaur Tracks from the Upper Jurassic Lourinhã Formation, Portugal

Fig. 1. Location map. The eleven new specimens of Deltapodus were found along the coast west of the town Lourinhã, in the central−west of Portugal. Each specimen has been given an abbreviation corresponding to the locality where it was found.

Fig. 3 in New finds of skeletal fossils in the terminal Neoproterozoic of the Siberian Platform and Spain

Fig. 3. SEM images of late Ediacaran Cloudina. A, C–E. Cloudina ex gr. C. riemkeae Germs, 1972; Kyyry−Ytyga (1.6 km downstream from Ulakhan−Ytyga Creek mouth), Yudoma River, right bank, Siberian Platform, Russia, Ust'−Yudoma Formation. A. SNIIGGiMS 1630/1, tube fragment with abraded shell wall. C. SNIIGGiMS 1630/2, fragment of tube with holes formed after microdolomite crystal dissolution. D. SNIIGGiMS 1630/3, detail of tube fragment with holes formed after microdolomite crystal dissolution. E. SNIIGGiMS 1630/4, tube nested funnels. B, F–H. Cloudina ex gr. C. hartmanae Germs, 1972; Tirteafuera River, Abenójar Anticline, East Lusitanian–Alcudian Zone, central Spain, lower La Grajera−Cañuelo unit, Ibor Group. B. MPZ 2007/3918, abraded tube fragment with imprints of mica crystals of the matrix. F. MPZ 2007/3919; F1, tube fragment with wall preserved; F2, detail of F1; F3, detail of F1, wall microstructure. G. MPZ 2007/3920, abraded tube fragment. H. MPZ 2007/3921; H1, tube fragment with wall preserved; H2, detail of H1 showing wall microstructure. Scale bars A, D, E, H1 100 µm; B, C, F2 300 µm; F1, G 1 mm; F3 50 µm; H2 30 µm.

Fig. 6 in New finds of skeletal fossils in the terminal Neoproterozoic of the Siberian Platform and Spain

Fig. 6. Microstructure of late Ediacaran and early Cambrian microfossils. A. Namacalathus hermanastes Grotzinger, Watters, and Knoll, 2000, Kuibis Subgroup, Nama Group, Upper Ediacaran, Zaris Subbasin, Namibia; MNHN Ca 370−1; A1, cross−section of stem; A2, detail of A1 showing blade−like elongate parallel crystals (laths) of calcite. B. Cribricyath Szecyathus cylindrucus Vologdin, 1957, Usa Formation, Botoman Stage, Lower Cambrian, Batenevskiy Range, Altay Sayan Foldbelt, Russia; MNHN Ca 194; B1, detail of skeleton outer wall; B2, detail of B1 (rectangle) showing microgranular microstructure. C. Cloudina hartmanae Germs, 1972, Birba Formation, Ara Group, Upper Ediacaran, Oman; MNHN Ca 361; C1, oblique longitudinal section; C2, detail of C1; C3, oblique longitudinal ultrathin section, crossed nicols. D. Cloudina hartmanae Germs, 1972, Birba Formation, Ara Group, Upper Ediacaran, Oman; MNHN Ca 360; D1, longitudinal section showing two primary skeletal layers; D2, detail of D1 showing secondary elongated crystals initiated at primary layer surface; D3, longitudinal ultrathin section showing several primary layers, crossed nicols; D4, detail of D3, transmitted light; D5, detail of D4, crossed nicols. Scale bars A1, B1, C1, D3 1 mm; A2, B2, C2, D1, D4 100 µm; C3, D2, D5 10 µm.

Fig. 2 in New finds of skeletal fossils in the terminal Neoproterozoic of the Siberian Platform and Spain

Fig. 2. Stratigraphic distribution of Ediacaran skeletal fossil assemblages from around the world. A. Zaris (Kuibis Subgroup) and Witputs (Schwarzrand Subgroup) subbasins, Nama Basin, Namibia (Grotzinger et al. 1995, 2000, 2005; Saylor et al. 1998; Wood et al. 2002). B. Yangtze Platform, southern Shaanxi, China (Hua et al. 2000b; Steiner et al. 2007; Zhu et al. 2007: lower C isotope curve; Ishikawa et al. 2008: upper C isotope curve; Pb/U radiometric data after Condon et al. 2005; Compston et al. 2008; Zhu et al. 2009). C. Abenójar (Abenójar Village and Tirteafuera River) Anticline, East Lusitanian–Alcudian Zone, central Spain (Ortega Girones and Sánchez Vizcaíno 1987). D. Yudoma River, Uchur−Maya region, Siberian Platform, Russia (C isotope data after Brasier et al. 1994; Podkovyrov and Davydov 1998; Pb−Pb radiometric data after Semikhatov et al. 2003). E. South Oman Salt Basin (Brasier et al. 2000; Amthor et al. 2003; Schröder and Grotzinger 2007). Abbreviations: Dolom., dolomite; Fm., formation; Gr., group; Mb., member.

Fig. 5 in New finds of skeletal fossils in the terminal Neoproterozoic of the Siberian Platform and Spain

Fig. 5. Late Ediacaran Sinotubulites sp. MPZ 2007/3922; Tirteafuera River, Abenójar Anticline, East Lusitanian–Alcudian Zone, central Spain; Ibor Group. A. Tube inner mold fragment with a longitudinal crack. B. Detail of A. Scale bars A 200 µm; B 100 µm. Both SEM images.

Fig. 4 in New finds of skeletal fossils in the terminal Neoproterozoic of the Siberian Platform and Spain

Fig. 4. Late Ediacaran calcareous fabrics from Ibor Group, Abenójar Anticline, East Lusitanian–Alcudian Zone, central Spain. A, B. Cloudina ex gr. C. hartmanae Germs, 1972, lower La Grajera−Cañuelo unit, Tirteafuera River. A. MPZ 2007/3923, longitudinal section showing wall fragments or bacterial microburrowing within skeleton ̕arrow). B. MPZ 2007/1465, oblique longitudinal section. C. MPZ 2009/496, longitudinal section of corolla−bearing "Cloudina" carinata Cortijo, Martí Mus, Jensen, and Palacios, 2010, lower La Grajera−Cañuelo unit, Tirteafuera River. D. MPZ 2007/3925, thrombolite structure, breccia unit "calizas de Abenójar", Abenójar. Scale bars 250 µm.

Fig. 1. Maps indicating studied localities. A in New finds of skeletal fossils in the terminal Neoproterozoic of the Siberian Platform and Spain

Fig. 1. Maps indicating studied localities. A. Map of Uchur−Maya region showing reference sections of the Yudoma River: 1, Nuuchchalakh; 2, Kyyry−Ytyga; 3, Ust'−Yudoma (Suvorovella and Majaella locality). Inset map indicates location within Siberian Platform. B. Pre−Hercynian outcrops and tectonostratigraphic zones of Iberian Peninsula. Valdelacasa, Ibor, Navalpino, and Abenójar anticlines are outlined. Zones: CZ, Cantabrian; ELAZ, East Lusitanian–Alcudian; GCZ, Galician–Castilian; OMZ, Ossa−Morena; SPZ South Portuguese; WALZ, West Asturian−Leonese.