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Fig. 5. A in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 5. A. Stratigraphic column of section 8 (see Fig. 3B); distribution of Globulirhynchia minima sp. nov. and other co−occurring brachiopods within the Evlanovo Horizon. B. Stratigraphical column of section 5 (see Fig. 3B); the uppermost part of the Frasnian, Livny Horizon. C. Stratigraphical column of section 6 (see Fig. 3B); appearance and distribution of Ripidiorhynchushuotinus (Verneuil, 1845) in Zadonsk Horizon. D. Stratigraphical column of section 1 (see Fig. 3B); distribution of Ripidiorhynchus griasicus (Nalivkin, 1934) in Elets horizon.

Fig. 12. A in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 12. A. Transverse serial section of Ripidiorhynchus huotinus (Verneuil, 1845). Numbers refer to distances in mm from the top of the ventral umbo, CNIGR 7/13076. B. Longitudinal section. CNIGR 8/13076. C. Reconstruction of the crural plates, CNIGR 9/13076. Early Frasnian, Zadonsk Horizon, Kamenka village, Elets region. D. CNIGR 10/13076 Zadonsk Horizon, Zadonsk region.

Fig. 8 in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 8. Early Frasnian (Pa.transitansZone)Ripidiorhynchus from Main Devonian Field, northwestwern Russia. A–D. Ripidiorhynchusaldogus (Nalivkin, 1941), CNIGR 40/6993, ventral, dorsal, anterior, and lateral views. Pskov beds, Sjas River, Konopljankina village. E–P. Ripidiorhynchuslivonicus (Buch, 1834). E–H. CNIGR 45/6993, ventral, dorsal, anterior, and lateral views. Chudovo beds, Velikaya River, Vybuty rapids. I–L. CNIGR 47/6993, ventral, dorsal, anterior, and lateral views. Chudovo beds, Kerest River, Luki village. M–P. CNIGR 37/6993, in ventral, dorsal, anterior, and lateral views. Pskov beds, Velikaya River. All × 1.5

Fig. 1 in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 1. Diversity dynamics of the Late Devonian rhynchonellids in the East European Platform (EEP). Three radiation levels of the Late Devonian rhynchonellids are marked as dotted areas. Devonian sea−level curve (after Johnson et al. 1985) and curve of relative Devonian sea−level changes in Moscow Syneclise (after Alekseev et al. 1996). The Standard Conodont Zonation by Klapper and Ziegler 1979, Ziegler and Sandberg 1990 and Conodont Zonation for Devonian of the East European Platform (EEP) proposed by Aristov 1988.

Fig. 14. A–E in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 14. A–E. Globulirhynchia minima sp. nov. from late Frasnian, Evlanovo Horizon, Chlevnoe village, Don River Basin. A–D. Holotype, CNIGR 13/13076, ventral, dorsal, lateral, and anterior views, × 5. E. CNIGR 14/13076, × 2. F–M. Paromoeopygma koscharica (Nalivkin, 1934) from early Famennian, Zadonsk Horizon, Koschary village, Zadonsk region. F–I. Neotype, CNIGR 1085/4572 ventral, dorsal, anterior, and lateral views, × 1.5. J–M. CNIGR 1083/4572, × 1.5.

Fig. 11 in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 11. Growth changes of shell of the Ripidiorhynchushuotinus (Verneuil, 1845) from the early Famennian, Zadonsk Horizon, Kamenka village, showing different fold deflection of the dorsal valve. A. CNIGR 5/13076. B. CNIGR 6/13076. C. CNIGR 4/13076.

Fig. 13 in Frasnian-Famennian extinction and recovery of rhynchonellid brachiopods from the East European Platform

Fig. 13. Transverse serial sections of Ripidiorhynchus griasicus (Nalivkin, 1934) from the early Famennian, Elets Horizon. Numbers refer to distances in mm from the top of the ventral umbo. A. CNIGR 11/13076. Argamach quarry, Elets region, B. CNIGR 12/13076. Lavy quarry, Elets region.

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).

opencc-by-4.0Nov 2023View details →

Precipitation hydrogen isoscape for East China from 1969 to 2017 generated based on data fusion of iGCMs simulations

<p>The dataset includes the stable hydrogen isotope of precipitation for East China over the 1969-2017 period, at a spatial resolution of 50-60 km and a monthly temporal resolution. This dataset was built based on the Convolutional Neural Network (CNN) method, fusing observations and isotope-equipped general circulation models (iGCMs) simulations of hydrogen isotope composition. Some physical-based ancillary data are also introduced in the fusion methods, including elevation and meteorological data, to enrich the climate and terrain information in the process of data fusion.</p>

FIGURE 7 in Telychian (Llandovery, Silurian) conodonts from the LaPorte City Formation of eastern Iowa, USA (East-Central Iowa Basin) and their implications for global Telychian conodont biostratigraphic correlation

FIGURE 7. Simple cone elements from Garrison Core. All specimens in lateral view except for 6. 1-2, Panderodus equicostatus, graciliform, GC 124.66–124.93 m, SUI 142251 (1) and graciliform, GC 121.92-121.88 m, SUI 142253 (2). 3-5, Panderodus panderi, graciliform, GC 124.66–124.93 m, SUI 142252 (3); arcuatiform, GC 131.95–132.23 m, SUI 142254 (4); and graciliform, GC 111.38–111.63 m, SUI 142255 (5). 6, Psuedooneotodus beckmanni, oral view, GC 135.65–136.10 m, SUI 142256. 7, Panderodus cf. P. unicostatus, falciform, GC 135.65–136.10 m, SUI 142257. 8- 11, Panderodus unicostatus, falciform, GC 131.95–132.23 m, SUI 142258 (8); fused cluster of 8 elements, GC 130.20–130.48 m, specimen destroyed processing for SEM (9); fused cluster of 6 elements, GC 131.95–132.23 m, SUI 142260 (10); and tortiform element, GC 131.95–132.23 m, SUI 142261 (11); 12-13, Walliserodus curvatus, dyscritiform, GC 134.06–134.31 m, SUI 142262 (12) and curvatiform, GC 128.85–129.11 m, SUI 142263 (13). 14-15, Panderodus greenlandensis, arcuatiform GC 118.20–118.41 m, SUI 142264 (14) and graciliform, GC 134.06–134.31 m, SUI 142265 (15). White scale bar represents 0.5 mm.

FIGURE 3 in Telychian (Llandovery, Silurian) conodonts from the LaPorte City Formation of eastern Iowa, USA (East-Central Iowa Basin) and their implications for global Telychian conodont biostratigraphic correlation

FIGURE 3. Cross section of Silurian strata in eastern Iowa. The lower two members of the Hopkinton Formation become indistinguishable in the western part of the cross section. The Sweeney and Marcus members are referred to as Hopkinton A, the Farmers Creek Quarry Member as Hopkinton B, and the Picture Rock Member as Hopkinton C in this manuscript. Note the change in datum at the CC core in Linn County. Modified from Witzke (1992, figure 6).

FIGURE 11. P1 in Telychian (Llandovery, Silurian) conodonts from the LaPorte City Formation of eastern Iowa, USA (East-Central Iowa Basin) and their implications for global Telychian conodont biostratigraphic correlation

FIGURE 11. P1 elements of Wurmiella? polinclinata estonica and Wurmiella? polinclinata polinclinata. 1-11 are classified as W.? polinclinata polinclinata. 12 and 14 show some characteristics of each subspecies, but compare most closely to W.? polinclinata polinclinata. 13, 15-17 are classified as W.? polinclinata estonica. All specimens in lateral view. 1, GC 121.92–121.88 m, SUI 142321; 2, GC 128.85–129.11 m, SUI 142322; 3-5, GC 130.20–130.48 m, SUI 142323 (3), 142324 (4), and 142325 (5); 6, GC 130.79–131.09 m, SUI 142326; 7-11, GC 131.95–132.23 m, SUI 142327 (7), 142328 (8), 142329 (9), 142330 (10), and 142331 (11); 12-14, GC 134.06–134.31 m, SUI 142332 (12), 142333 (13), and 142334 (14); and 15-17, GC 135.65–136.10 m, SUI 142335 (15), 142336 (16), and 142337 (17).

FIGURE 5 in Telychian (Llandovery, Silurian) conodonts from the LaPorte City Formation of eastern Iowa, USA (East-Central Iowa Basin) and their implications for global Telychian conodont biostratigraphic correlation

FIGURE 5. Stratigraphic column and conodont range chart for the LPC in the Garrison Core. Dashed lines indicate uncertainty in range. M = mudstone, W = Wackestone, P = Packstone, F = Floatstone for carbonate lithologies. L.H. = Lower Hopkinton. Log colors represent the color of the rock. Correlation of conodont biozonation to chronostratigraphic units from Cramer et al. (2011).