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Fig. 1 in A survey of the parasites of Ural saiga antelopes and Turkmenian kulans of Kazakhstan

Fig. 1. Map of Altyn-Emel National Park, with kulan faecal sample collection locations represented as red diamonds (June–August 2021). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)

opencc-by-4.0Aug 2023View details →

Fig. 2 in A survey of the parasites of Ural saiga antelopes and Turkmenian kulans of Kazakhstan

Fig. 2. Map of the Ural saigas antelopes' distribution range, with study location enlarged. Arrows represent migration direction, while the blue circle represents rutting location, and the red square represents calving location. (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)

opencc-by-4.0Aug 2024View details →

Fig. 3 in Molecular evaluation of Eimeria spp. Infection in the Volga-Ural Saiga antelope population of the Republic of Kazakhstan

Fig. 3. Phylogenetic tree generated by the Maximum Composite Likelihood (MCL) method using partial sequences of the 18S rRNA of the Eimeria species that infect the Saiga tatarica.

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Fig. 2 in Molecular evaluation of Eimeria spp. Infection in the Volga-Ural Saiga antelope population of the Republic of Kazakhstan

Fig. 2. Eimeria spp. Oocyst at 40x magnification. The outer (OL) and the inner (IL) layers of the oocyst wall, micropyle (M), micropyle cap (MC), spores (S).

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Fig. 1 in Molecular evaluation of Eimeria spp. Infection in the Volga-Ural Saiga antelope population of the Republic of Kazakhstan

Fig. 1. Photomicroscope images showing the oocysts of E. elegans (40х magnification). The outer (OL) and the inner (IL) layers of the oocyst wall, cytoplasmic mass (CM), micropyle (M).

Fig. 7. Trace element environmental proxies for the F–F in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

Fig. 7. Trace element environmental proxies for the F–F transition in the Syv'yu River section. Bio−productivity tracers* are normalized according to Schmitzetal.(1997).DownwardarrowedtrendsarebasedonthesinglesampleCB99−222,located2.15mbelow;recognizedMo/Alenrichment,indicative of anoxic−sulfidic deposition, is shown as well. For explanations see Fig. 4.

Fig. 6 in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

Fig. 6. Various upper Frasnian spongiolitic microfacies, Syv'yu River section. A. Sponge boundstone(?); note large growth cavities, and complex and diverse, peloidal to bioclastic geopetal fill up, as well as preserved spicular network; sample Syv96−58. B, C. Sponge relics (Sp) distinguished by a variety of grumeous fabric, pyrite−rich marginal rims, and partly chertified interstitial mudstone matrix (Ch); samples CB99−224 (B) and CB99−314 (C).

Fig. 1 in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

Fig. 1. Location of the studied area in Russia (A) and Timan−Pechora region (B, modified from Becker et al. 2000: fig. 1A), and location of the Kozhym River basin (C) and locality map of studied outcrops along the Syv'yu River section (D), western slopes of the Subpolar Urals; C1t, Tournaisian. D1, Lower Devonian; D2tk,?Middle Devonian, Takata Suite; D2ef−gv, Eifelian–Givetian; D3fr, Frasnian; D3fm, Famennian.

Fig. 4 in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

Fig. 4. Upper Frasnian and lower Famennian lithologic column of the Syv'yu River section (upper Vorota Fm.), sampling pattern and conodont succession across the F–F boundary, with emphasis on principal biotic events and alleged Kellwasser levels (see also Figs. 7, 8); figures in the lithological column refer to microfacies photos (Figs. 5, 6).

Fig. 2. F–F in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

Fig. 2. F–F boundary beds exposed along the right bank of Syv'yu River, outcrop 2 (line marks F–F boundary; for location see Fig. 1D).

Fig. 8 in The Frasnian-Famennian events in a deep-shelf succession, Subpolar Urals: biotic, depositional, and geochemical records

Fig. 8. Stable isotope geochemistry for the Upper Frasnian and lower Famennian in the Syv'yu River section, F–F background values taken from Joachimski and Buggisch (1996: fig. 1); for explanations see Fig. 4.

Fig. 6 in Late Eocene scyliorhinid sharks from the Trans-Urals, Russia

Fig. 6. Foumtizia aff. pattersoni (Cappetta, 1976), Kurgan, Russia; Tavda Formation, Priabonian. A. 8CΠ/Ku−87/02, lateral tooth; in labial (A1), lingual (A2), and occlusal (A3) views. B. 8CΠ/Ku−87/03, anterior tooth; in labial (B1), lingual (B2), and occlusal (B3) views. Digital photo.

Fig. 5 in Late Eocene scyliorhinid sharks from the Trans-Urals, Russia

Fig. 5. Scyliorhinus zhelezkoi sp. nov., Derney, Russia; Tavda Formation, Priabonian. IGG 8CΠ/D−03/01, lower lateral tooth; in labially−occlusal (A), lingual (B), occlusal (C), and lingually−occlusal (G) views; ribs on the labial side of the crown (D), lateral cusplet in the lingual view (E), ribs on the lingual side of the crown (F, H). SEM microphotographs.

Fig. 4 in Late Eocene scyliorhinid sharks from the Trans-Urals, Russia

Fig. 4. Scyliorhinus zhelezkoi sp. nov., Kurgan, Russia; Tavda Formation, Priabonian. A. Holotype. PIN 5088/03, lateral tooth; in labial (A1), lingual (A2), medial (A3), basal (A4), and lingually−occlusal (A5) views. B. Paratype. PIN 5088/04, anterior tooth; in labial (B1), labially−occlusal (B2), and lingually−mesial (B3) views; distal cusplets, enlargement (B4). SEM microphotographs.

Fig. 2 in Late Eocene scyliorhinid sharks from the Trans-Urals, Russia

Fig. 2. Premontreia uralica sp. nov., Kurgan, Russia; Tavda Formation, Priabonian. A. Holotype. PIN 5088/01, anterior tooth; in labial (A1), lingual (A2), labially−occlusal (A3), distally−basal (A4), lingually−occlusal (A5), and basal (A6) views. B. Paratype. PIN 5088/02, anterior tooth; in labial (B1), distally−basal (B2), lingual (B3), labially−occlusal (B4), lingually−occlusal (B5), and basal (B6) views. SEM microphotographs.

Fig. 3 in Late Eocene scyliorhinid sharks from the Trans-Urals, Russia

Fig. 3. Premontreia uralica sp. nov., Kurgan, Russia; Tavda Formation, Priabonian. A. 8CΠ/Ku−87/21, anterior tooth; in labial (A1), lingual (A2), occlusal (A3), distal (A4), and basal (A5) views. B. Lateral tooth; in labial (B1), lingual (B2), distal (B3), and occlusal (B4) views. Digital photographs.

Fig. 1 in Late Eocene scyliorhinid sharks from the Trans-Urals, Russia

Fig. 1. Geographical position of the localities where the studied material came from. A. The distribution of the Peri−Tethyan and West−Siberian waters in Priabonian times. B. Localities studied. C. Schematic local lithostratigaphic section.

Fig. 3. Early Frasnian cyrtospiriferd Uchtospirifer nalivkini Ljaschenko, 1957 from the Kyn Horizon, Urals. A. CNIGR 287 in Early-Middle Frasnian cyrtospiriferid brachiopods from the East European Platform

Fig. 3. Early Frasnian cyrtospiriferd Uchtospirifer nalivkini Ljaschenko, 1957 from the Kyn Horizon, Urals. A. CNIGR 287, ventral (A1), dorsal (A2), anterior (A3), and lateral (A4) views. B. CNIGR 286, ventral (B1), dorsal (B2), anterior (B3), and lateral (B4) views. C. CNIGR 289, ventral (C1), dorsal (C2), anterior (C3), and lateral (C4) views. D. CNIGR 290, ventral (D1), dorsal (D2), anterior (D3), and lateral (D4) views; shell surface showing microornament (D5).

opencc-zeroJan 2024View details →

Linked collectors and determiners for: Moss occurrences in Yugyd Va National Park, Subpolar and Northern Urals, European North-East Russia.

Natural history specimen data linked to collectors and determiners held within, "Moss occurrences in Yugyd Va National Park, Subpolar and Northern Urals, European North-East Russia". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/9192a5a8-5eba-4ec6-a336-797924214175">https://bionomia.net/dataset/9192a5a8-5eba-4ec6-a336-797924214175</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/9192a5a8-5eba-4ec6-a336-797924214175">https://gbif.org/dataset/9192a5a8-5eba-4ec6-a336-797924214175</a>. Formatted as a Frictionless Data package.