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Fig. 36 in Plant Type Materials from Kanagawa Prefecture (Japan) in the Herbarium of the Komarov Botanical Institute (LE; Russia): Lycophytes, Ferns, Gymnosperms, and Angiosperms (Monocots and some Dicots)

Fig. 36. Syntype of Polygonatum giganteum A. Dietr var. macranthum Maxim. (LE 01012153; KPMNX0001304).

Fig. 32 in Plant Type Materials from Kanagawa Prefecture (Japan) in the Herbarium of the Komarov Botanical Institute (LE; Russia): Lycophytes, Ferns, Gymnosperms, and Angiosperms (Monocots and some Dicots)

Fig. 32. Syntypes of Lycoris sanguinea Maxim. (LE 01012637, LE 01012635, LE 01012636; KPMNX0001294).

Fig. 4 in Plant Type Materials from Kanagawa Prefecture (Japan) in the Herbarium of the Komarov Botanical Institute (LE; Russia): Lycophytes, Ferns, Gymnosperms, and Angiosperms (Monocots and some Dicots)

Fig. 4. Syntype of Aspidium craspedosorum Maxim. var. japonicum Maxim. (LE 01009865; KPM-NX0001854).

Fig. 6 in Plant Type Materials from Kanagawa Prefecture (Japan) in the Herbarium of the Komarov Botanical Institute (LE; Russia): Lycophytes, Ferns, Gymnosperms, and Angiosperms (Monocots and some Dicots)

Fig. 6. Lectotype (LE 01011614) and syntype (LE 01011615) of Chamaecyparis breviramea Maxim. (KPMNX0001841).

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Figures 11-12 in A new water mite species of the genus Hygrobates Koch, 1837 (Acari, Hydrachnidia, Hygrobatidae) from Far East of Russia

Figures 11-12. Hygrobates (Rivobates) ezoensis: 11-12 – genital field, 11 – female, 12 – male (after Matsumoto et al. 2005).

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Figures 7-10 in A new water mite species of the genus Hygrobates Koch, 1837 (Acari, Hydrachnidia, Hygrobatidae) from Far East of Russia

Figures 7-10. Hygrobates (Rivobates) primoryensis sp. n.: 7 – I-Leg-4-6, 8 – IV-Leg-4-6, 9 – leg claw; 10 – genital field; 7-9 male, 10 – female. Scale bars: 7, 8, 10 = 100 μm, 9 = 50 μm.

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Figures 1-6 in A new water mite species of the genus Hygrobates Koch, 1837 (Acari, Hydrachnidia, Hygrobatidae) from Far East of Russia

Figures 1-6. Hygrobates (Rivobates) primoryensis sp.n.: 1 – seta Fch, 2 – ventral view, 3-4, 6 – genital field, 5 – pedipalp; 1-5 – male, 6 – female. Scale bars: 1, 5 = 50 μm, 2-4, 6 = 100 μm

Figs 1–5. Trichonephila clavata. 1 in NEW FOR THE ASIAN PART OF RUSSIA TAXA OF SPIDERS (ARACHNIDA: ARANEI)

Figs 1–5. Trichonephila clavata. 1– body, dorsal view; 2 – same, ventral view; 3 – epigyne, dorsal view; 4 – same, ventral view; 5 – living specimen. Abbreviation: Re – receptacle. Scale bars = 5 mm (1, 2), 0.2 mm (3, 4).

Figs 1–2 in FIRST RECORD OF HESPERINUS CUSPIDISTYLUS HARDY ET TAKAHASHI, 1960 (DIPTERA: HESPERINIDAE) FROM RUSSIA

Figs 1–2. Male genitalia of Hesperinus spp., dorsal view. 1 – H. rodendorfi; 2 – H. cuspidistylus. Abbreviations: ap aed - aedeagal apodeme; gcx – gonocoxite; gst – gonostylus; t9 – tergite 9.

Fig. 14 in NEW FOR THE ASIAN PART OF RUSSIA TAXA OF SPIDERS (ARACHNIDA: ARANEI)

Fig. 14. Distribution map of Takeoa spp. Squares – T. nishimurai (red symbol – new record, black symbols – previous records); circle – T. huangshan.

Figs 6–12. Takeoa nishimurai. 6 in NEW FOR THE ASIAN PART OF RUSSIA TAXA OF SPIDERS (ARACHNIDA: ARANEI)

Figs 6–12. Takeoa nishimurai. 6 – body, dorsal view; 7 – same, ventral view; 8, 9 – epigyne, dorsal view; 10 – same, ventral view; 11 – habitat; 12 – living specimens. Abbreviations: CD – copulatory ducts, DS – dorsal part of scape, Fo – fovea, HL – handle of lip of epigyne, Li – lip of epigyne, Re – receptacle, RH – receptacle head, Sc – scape, VS – ventral part of scape. Scale bars = 2 mm (6, 7), 0.2 mm (8–10).

Fig. 13 in NEW FOR THE ASIAN PART OF RUSSIA TAXA OF SPIDERS (ARACHNIDA: ARANEI)

Fig. 13. Distribution map of Trichonephila clavata. Red square – new record, black squares – previous records, black squares with question marks – records without precise location.

Fig. 5 in Cenozoic fossil fishes of the extinct alepisauroid family Polymerichthyidae from the Sakhalin Island, Russia

Fig. 5. Alepisauroid fish Polymerichthys sp. from Sakhalin Island, Holmsk Formation, late Oligocene (A) and Kurasi Formation, Middle–Late Miocene (B). A. ZIN 310p, abdominal centrum. B. ZIN 314p, fragment of the dorsal fin.

Fig. 1 in Cenozoic fossil fishes of the extinct alepisauroid family Polymerichthyidae from the Sakhalin Island, Russia

Fig. 1. Location of the Sakhalin Island (A) and sketch map of the studied area (B) showing the fossil fish localities (stars).

Fig. 4 in Cenozoic fossil fishes of the extinct alepisauroid family Polymerichthyidae from the Sakhalin Island, Russia

Fig. 4. Alepisauroid fish Polymerichthys sp. from Sakhalin Island, Kurasi Formation, Middle–Late Miocene, ZIN 314p, outline drawing of specimen (A) and skull (B).

Fig. 2 in Cenozoic fossil fishes of the extinct alepisauroid family Polymerichthyidae from the Sakhalin Island, Russia

Fig. 2. Alepisauroid fish Polymerichthys sp. from Sakhalin Island, Holmsk Formation, late Oligocene (A, B) and Kurasi Formation, Middle–Late Miocene (C–E). A. ZIN 311p. B. ZIN 310p. C. ZIN 313p. D. ZIN 312p. E. ZIN 314p. Scale bars 10 mm.

Fig. 11 in A new type of shell malformation caused by epizoans in Late Jurassic ammonites from Central Russia

Fig. 11. SEM photographs of the pits on the craspeditid ammonite Kachpurites fulgens (Trautschold, 1861) shells from the Late Volgian, Kachpurites fulgens Zone, Eganovo (A) and Mnevniki (B) localities, Moscow region, Central Russia. A. MSU 118/1. Transverse (A1, A2) and longitudinal (A3, A4) cross-sections of the shell layers in the pit area. The bending of shell wall inside the pit is clearly visible. B. MSU 118/9. The phosphatic mineral inside the pit (B1) and the tubercle (reflection of the pit) (B2) located on the dorsal side of the specimen.

Fig. 10 in A new type of shell malformation caused by epizoans in Late Jurassic ammonites from Central Russia

Fig. 10. The pits on the aragonitic shell layers of the craspeditid ammonite Kachpurites fulgens (Trautschold, 1861) from the Late Volgian, Kachpurites fulgens Zone, Mnevniki, Moscow region, Central Russia; MSU 118/10. A. Body chamber with slightly dissolved shell layers. General view in ventro-lateral (A1), ventral (A2), and dorsal (A3) views; on the dorsal side the small tubercle is visible, which reflect the pit on the previous whorl. B. Two pits on the specimen, SEM photograph. C. Two pits on the specimen, optical binocular microscope photographs.

Fig. 6 in A new type of shell malformation caused by epizoans in Late Jurassic ammonites from Central Russia

Fig. 6. Craspeditid ammonite Kachpurites fulgens (Trautschold, 1861) from the Late Volgian, Kachpurites fulgens Zone, Moscow region, Eganovo locality, Central Russia; shell with pits and deformed growth lines, MSU 118/1. A. General lateral view. B. Dorsal view, two tubercles located on the dorsal side of the body chamber, reflecting pits which are located on the previous shell whorl. C. The pits and deformed growth lines, which are related with pits, on the lateral surface of the specimen. D. Outer shell layer with phosphatic mineral inside pits and curved growth lines connected with these pits. Photographs (A, B, C1, D1), explanatory drawings (C2, D2).

Fig. 9 in A new type of shell malformation caused by epizoans in Late Jurassic ammonites from Central Russia

Fig. 9. Craspeditid ammonites Kachpurites fulgens (Trautschold, 1861) from the Late Volgian, Kachpurites fulgens Zone, Moscow region, Central Russia, Eganovo (A, B) and Mnevniki (C, D) localities; shells with pits and epizoans, lateral (A1, B1, C, D) and dorsal (A2, B2) views. A. MSU 118/7, abnormal " scaphitoid" shell shape. There are several pits on the ventral side of the shell (A2). B. MSU 118/16, fragment of the abnormal shell. The fragment of bivalve shell which caused distortion of the shell growth can be seen on the dorsal side (B2). There are no pits on this specimen. C. MSU 118/8, body chamber with pits on both sides of the shell. D. MSU 118/9, fragment of the body chamber with pits, many of them are merged with each other.