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Figure 15 in An overview on the subterranean fauna from Central Asia

Figure 15. Gastropoda: A, B = Pseudocaspia ljovuschkini Starobogatov, 1972; C, D = Pseudocaspia kainarensis Starobogatov, 1972; E = Pseudocaspia starostini Starobogatov, 1972; F, G = Kainarella minima Starobogatov, 1972; H = Bucharamnicola bucharica (Shadin, 1952); I = Chirgisia alaarchaensis Glöer, Boeters & Pešić, 2014; J = Paladilhiopsis sp.2 Starobogatov, 1962; K = Cincinna pamirensis Starobogatov.

Figure 10 in An overview on the subterranean fauna from Central Asia

Figure 10. Foraminiferida: A = Spiroloculina turkomanica Brodsky, 1928; B = Biloculina elongata turkomanica Brodsky, 1929; C = Biloculina turkomanica Brodsky, 1928; D = Triloculina turkomanica Brodsky, 1929; E, F = Nodosaria turkomanica Brodsky, 1929; G, H = Lagena turkomanica Brodsky, 1929; I, J, K = Trochamminita sp.; L, M = Miliammina sp.; N, O = Borovina zernovi Schmalhausen, 1950. (Figs. A-H, after Brodsky, 1928; figs. I-O, after Birstein & Ljovuschkin, 1965).

Figure 5. A in An overview on the subterranean fauna from Central Asia

Figure 5. A (upper) Tectonical aspect of the Issyk-Kul Lake depression, northern Tien Shan, Kyrghyzstan (After Bowman et al., 2004). B (lower) Sketch of the Issyk-Kul Lake, and its rivers in adjacent lands (After Jankowskaja, 1972; modified).

Figure. 4 in An overview on the subterranean fauna from Central Asia

Figure. 4 Schematic diagram showing the kiariz (khana) concept. 1 = Mother well; 2 = excavation debris (soil crater); 3 = vertical shafts; 4 = kiariz gallery; 5 = land surface; 6 = outlet; 7 = storage tank; 8 = irrigation land (After Jankowskaja, 1972; modified). Kiarizs are present in Tadjikistan, Turkmenistan and Uzbekistan. They are artificial subterranean galleries dug in desert zones to reduce evaporation. They collect water from mountains or foot hills, for alimentation or irrigation. Khana wells are 1.1 to 22 m depth, the water from 0.5 to 9 m depth, the temperature from 12 to 22°C, the pH of 7.2/7.5; water Na Cl or Na-SO4 type.

Figure 2 in An overview on the subterranean fauna from Central Asia

Figure 2. Central Asia. Collecting sites of subterranean fauna. Map A: numbers 1 = Kendyrli Bay; 2 = Kushka. a and b = Two detailed mountain ranges: A Kuldzhuktau Mountains, b - Nuratau Mountain range: H = Pit for hyporheic fauna; K = Kanat, artificial subterranean gallery groundwater collector and conveyer; W = Well (after A. I Jankowskaya, 1972, modified). Aral Sea in 2010. B 3 = Cholpon-Aty river and the Biological Station at Cholpon-Aty; 4 = Aksu and Dzhirgalan rivers, affluents Issyk-Kul lake; 5 = Vannovka; 6 = Shimkent; 7 = Fergana valley; 8 = Urgut; 9 = Bakhmal; 10 = Khaydarkan; 11 = Varzob; 12 = Khodzhambass; 13 = Gaurduk; 14 = Kaptar-Khana cave; 15 = Cupp-Coutunn cave system; 16 = Kugitangtau Mountains; 17 = Fergansky Mts; 18 = Alaiskiy Mts; 19 = Surkhob River; 20 = Gissarkiy (Hissarkiy) Mts; 21 = Kyzyl-Ravata.

Fig. 7 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 7. Monchenkocyclops changi gen. et sp. nov., allotype male. A. habitus, dorsal view. B. urosome, ventral view. C. right caudal ramus, dorsal view. D. right caudal ramus, lateral view. E. second endopodal segment of fourth swimming leg, anterior view. F. sixth leg, ventrolateral view. Arabic numerals indicating sensilla and pores consecutively from anterior to posterior end of body, and from dorsal to ventral side (excluding appendages). Scale bars 100 µm.

Fig. 1 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 1. Monchenkocyclops changi gen. et sp. nov., holotype female: A. habitus, dorsal view. B. antennula, dorsal view. Arabic numerals indicating sensilla and pores consecutively from anterior to posterior end of body, and from dorsal to ventral side (excluding appendages; those on cephalothorax not presented). Scale bars 100 µm.

Fig. 6 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 6. Monchenkocyclops changi gen. et sp. nov., A-E. holotype female. F. allotype male. A. second endopodal segment of third swimming leg, anterior view. B. left fourth swimming leg, anterior view. C. second endopodal segment of right fourth swimming leg, anterior view. D. fifth leg, anterior view. E. sixth leg, lateral view. Scale bar 100 µm.

Fig. 4 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 4. Monchenkocyclops changi gen. et sp. nov., A-E. holotype female. F. paratype female. A. urosome, dorsal view. B. antenna, dorsal view. C. labrum, anterior view. D. maxillula, posterior view. E. mandibula, anterior view. F. cutting edge of labrum, anterior view. Arabic numerals indicating sensilla and pores consecutively from anterior to posterior end of body, and from dorsal to ventral side (excluding appendages). Scale bars 100 µm.

Fig. 5 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 5. Monchenkocyclops changi gen. et sp. nov., holotype female: A. maxilla, anterior view. B. maxilliped, posterior view. C. first swimming leg, anterior view. D. second swimming leg, anterior view. Scale bar 100 µm.

Fig. 3 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 3. Monchenkocyclops changi gen. et sp. nov., holotype female: A. urosome, ventral view. B. urosome, lateral view. Arabic numerals indicating sensilla and pores consecutively from anterior to posterior end of body, and from dorsal to ventral side (excluding appendages). Scale bars 100 µm.

Fig. 2 in A new cyclopoid copepod from Korean subterranean waters reveals an interesting connection with the Central Asian fauna (Crustacea: Copepoda: Cyclopoida)

Fig. 2. Monchenkocyclops changi gen. et sp. nov., holotype female: A. cephalothoracic shield, lateral view. B. cephalothorax, dorsal view. C. pleurons of free prosomites, lateral view. D. rostrum, dissected and flattened, original anterior view. E. pleuron of second free prosomite (third pedigerous somite), dissected and flattened. Arabic numerals indicating sensilla and pores consecutively from anterior to posterior end of body, and from dorsal to ventral side (excluding appendages). Scale bars 100 µm.

Figure 7 in Subterranean fauna from Siberia and Russian Far East

Figure 7. On the left: - Isopoda Janiridae Mackinia continentalis Birstein & Ljovuschkin, 1965, from a small cave near Boetc-Kuznetcovo, Far East. On the right: - Isopoda Asellidae Sibirasellus parpurae Henry & Magniez, 1993, from a pit-hole, Primory, Far East.

Figure 3 in Subterranean fauna from Siberia and Russian Far East

Figure 3. Main caves on the Irkutsk Plateform (after Trofimova, 1996, and Pulina, 2005; drawing Bernard Juberthie and George Nazareanu).

Figure 2 in Subterranean fauna from Siberia and Russian Far East

Figure 2. Karts of the Irkutsk plateform. 1. Karstic regions with limestone, dolomite, gypsum and anhydrite. 2. Potential karstic regions. I. Southern part of the Irkutsk plateform. II. Western region of the Khamar-Daban Mts. III. Tounkinsk Alps. IV. Around Niznieudinsk (after Marian Pulina, Karstologia, 2005).

Figure 1 in Subterranean fauna from Siberia and Russian Far East

Figure 1. Karst of Siberia and Russian Far East. – 1. Carbonated rocks and locally sulfated (studied and recorded). – 2. Carbonated rocks and locally sulfated (estimated). – 3. Sulfated rocks (salt). – Numbers: 4 – Altai, Kuznetski, Saiansk. – 5. Irkutsk Plateform. – 6. Patomskoye Mountains. – 7. Middle Lena valley. – 8. Anabar region. – 9. Anhydrite karst of Kempendal. – 10. Anhydrite karst of Norwinsk. – 11. Gypsum and Anhydrite karst of the Poutoran Plateau. – 12. Karst of the Uchur and Maia rivers and valleys. – 13. Amur, Khor valleys and Sikhote-Alin Mountain ridge (after Pulina, 2005; modified; map Bernard Juberthie).

Figure 5 in Subterranean fauna from Siberia and Russian Far East

Figure 5. Ulsinsk karstic region, Mar-Kyouzl Plateau. Karstic lake (1), The Aardach River (2), Ponor (3), Subterranean stream of the Aardach River and Selendinskye karstic spring (6), Dolines (4 -5) (after Bersenev 1989; Pulina 2005).

Figure 9 in Subterranean fauna from Siberia and Russian Far East

Figure 9. Amphipoda Pseudocrangonyctidae Procangronyx primoryensis Stock & Young Won Jo, 1990, from a pithole, Primory, Far East.

Figure 8. Amphipoda Pseudocrangonyctidae Pseudocrangonyx febras Sidorov, 2009, from a in Subterranean fauna from Siberia and Russian Far East

Figure 8. Amphipoda Pseudocrangonyctidae Pseudocrangonyx febras Sidorov, 2009, from a pit-hole, Primory, Far East.

Figure 4 in Subterranean fauna from Siberia and Russian Far East

Figure 4. Regions with main caves in the Far East. – 1. Uchur-Maya karst. – 2. Ulsinsk karst. - A. Leno-Aldanskyi. B. Aldano-Stanovoyi. C. Amuro-Ochotskyi. D. Buryenskyi. E. Shikote-Alin Mountain ridge. F. Sakhalin Island (after Bersenev, 1989 and Pulina, 2005; drawing Bernard Juberthie and George Nasareanu).