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Рис. 1. Имаго, общий виΔ: 1 — Selenia ononica, Эрзин; 2 — Eilicrinia subcordaria, Эрзин; 3 — Semidesertobia ubinica, Эрзин; 4 — Orthosia ariuna, Эрзин. ГенитаΛии ♂ и ♀: 5 — Orthosia ariuna, Эрзин Fig. 1. Imago, general view: 1 — Selenia ononica, Erzin; 2 — Eilicrinia subcordaria, Erzin; 3 — Semidesertobia ubinica, Erzin; 4 — Orthosia ariuna, Erzin. Genitalia ♂ and ♀: 5 — Orthosia ariuna, Erzin in New Records Of Heterocera (Lepidoptera) From The Republic Of Tyva (Southern Siberia, Russia)
Рис. 1. Имаго, общий виΔ: 1 — Selenia ononica, Эрзин; 2 — Eilicrinia subcordaria, Эрзин; 3 — Semidesertobia ubinica, Эрзин; 4 — Orthosia ariuna, Эрзин. ГенитаΛии ♂ и ♀: 5 — Orthosia ariuna, Эрзин Fig. 1. Imago, general view: 1 — Selenia ononica, Erzin; 2 — Eilicrinia subcordaria, Erzin; 3 — Semidesertobia ubinica, Erzin; 4 — Orthosia ariuna, Erzin. Genitalia ♂ and ♀: 5 — Orthosia ariuna, Erzin
Fig. 1 in Vasil'Eva, 2001 A As New Specie In The Fish Fauna Of Altai Krai (West Siberia, The Russian Federation)
Fig. 1. Misgurnus nikolskyi Vasil'eva, 2001 (the floodplain water body of the the Burla River, Pankrushikhinsky district of Altai Krai)
Egg and chick size in the nests of common gulls in Lake Chany, West Siberia, Russia from 1993 to 2011
<p>A long-term study of breeding ecology of gulls has been carried in the area of Lake Chany. Lake Chany is located in the Baraba forest-steppe of the West Siberian Plain, Russia, between the Ob and Irtysh rivers. The Lake is protected by the Ramsar Convention on the Wetlands of International Importance, indicating that the lake is an important site for migrating and breeding birds, including the Common gull <em>Larus canus </em>(Linnaeus, 1758). We provided data on the size and fate of all eggs as well as the size of hatched chicks in Common gull nests from 1993 to 2011. The data can be used to assess how environmental changes caused by human activity, including global warming, affect the reproduction and population dynamics of migratory birds. </p>
Fig. 78 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 78. Sponge fragments from the lower Cambrian Erkeket Formation, Khorbusuonka River (A–F, H, I, M, N) and Tyuser Formation, lower reaches of the Lena River (G, J–L, O, P), Siberia, Russia; samples 19/10.25 (B–F, M, N), 19/11.75 (A, H, I), and 22/0 (G, J–L, O, P). A–G. Fragments of archaeocyaths, SMNH Sp11519–11525, respectively. H–P. Fragments of possible heteractinid spicules, SMNH Sp11526–11534, respectively. Scale bar: 250 µm (A, C) and 500 µm (B, D–P).
Fig. 77 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 77. Inflated hexactines from the lower Cambrian Erkeket Formation, Khorbusuonka River (A–N) and Tyuser Formation, lower reaches of the Lena River (O–S), Siberia, Russia; samples 19/10.25 (C, D, H, K), 19/11.75 (A, B, E, F, J, L, M), 19/12.75 (G, I), 11/16.05 (N), and 21/21 (O–S). A, B, G–I. Hexactines with smooth tapering rays, SMNH Sp11500–11504, respectively. C–F, J–S. Strongly inflated hexactines with smooth tapering rays, SMNH Sp11505–11518, respectively. Scale bar 500 µm.
Fig. 75 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 75. Heteractinid spicules from the lower Cambrian Erkeket Formation, Khorbusuonka River, Siberia, Russia; samples 19/11.75 (C–I), and 19/12.75 A, B). A–I. Polyactinal spicules with multiple coplanar rays, SMNH Sp11486–11494, respectively. C1, plainview; C2, lateral view. Scale bar: 250 µm A–H) and 500 µm (I).
Fig. 74 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 74. Heteractinid spicules from the lower Cambrian Erkeket Formation, Khorbusuonka River (A–E, G, I, K–Q, V, Y) and Tyuser Formation, lower reaches of the Lena River (F, H, J, U, W, X, Z), Siberia, Russia; samples 11/16.05 (Y), 19/10.25 (E, I, K, L, O–Q), 19/11.75 (A–D, R–T, V), 19/12.75 (G, M, N), 21/21 (U, W, X), and 22/0 (F, H, J, Z). A–H, J, L–P, S. Polyactinal spicules with an axial ray, SMNH Sp11460–11474, respectively. U, W–Y. Inflated polyactinal spicules from the Tommotian Stage, SMNH Sp11475–11478, respectively. I, K, Q, R, T, V, Z. Microcoryne cf. cephalata Bengtson in Bengtson et al., 1990, SMNH Sp11479–11485, respectively. Scale bar: 250 µm (A–J, N, O, Q, R, V, Y, Z) and 500 µm (K–M, P, S, T, U, W, X).
Fig. 72 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 72. Calcareous (dolomitised) spicules from the lower Cambrian Erkeket Formations, Khorbusuonka River, Siberia, Russia; samples 19/4.25 (H, I), 19/5.5 (A, J), 19/8.5 (D), 19/10.25 (C), 19/11.75 (E, G), 19/25.5 (B, F), and 20/1B (K). A–H. Dodecaactinella sp., SMNH Sp11430–11437, respectively. I–K. Sulugurella sp., SMNH Sp11438–11440, respectively. Scale bar 250 µm.
Fig. 71 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 71. Hexactinellid spicules from the lower Cambrian Erkeket (A–F, H–J, L–O) and Yunkyulyabit-Yuryakh (G) formations, Khorbusuonka River and Emyaksin Formation, Bol'shaya Kuonamka River (K), Siberia, Russia; samples 11/18.7 (A–F, H–J, L), 11/16.05 (M, N), 19/107 (G), 20/1B (O), and 6/0.3 K). A–D, H, J. Polyactine siliceous megascleres with acutely tapering slim curved rays, SMNH Sp11424–11429, respectively. E, F, I, M–O. Pentactines and hexactines with thin smooth rays, SMNH Sp11417–11422, respectively. G. Fragment of a pinnular pentactine, SMNH Sp11423. K, L. Abnormisella sp., SMNH Sp11415 (K) and 11416 (L). Scale bar: 250 µm (A–D, H–J, O) and 500 µm (E–G, K–N).
Fig. 73 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 73. Heteractinid spicules from the lower Cambrian Erkeket Formations, Khorbusuonka River, Siberia, Russia; samples 19/10.25 (A–F, I), 19/11.75 (H, J, P, R), and 19/12.75 (G, K–O, Q, S). A–S. Hexaradiate spicules, SMNH Sp11441–11459, respectively. C–E, S, spicules with dissolved internal parts of the rays reminiscent of axial canals. F1, spicule in lateral view; F2, concave side of the spicule with radiating six paratangential rays. H, I, strongly eroded spicules. G, K–S, hexaradiate spicules with accessory rays. Arrow in O points to fused spicules. Arrow in S points to dissolved inner portion of the ray reminiscent of axial canal. Scale bar: 250 µm (C–G, J, M–O, Q, S) and 500 µm (A, B, H, I, K, L, P, R).
Fig. 70 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 70. Spicules of hexactinellid Thoracospongia sp. from the middle Cambrian Yunkyulyabit-Yuryakh Formation, Khorbusuonka River, Siberia, Russia; sample 19/107. A–E. Follipinules with a modified obese axial ray, SMNH Sp11409–Sp11413, respectively. A1, lateral view on the axial ray; A2, four paratangential rays. Scale bar: 125 µm (A) and 250 µm (B–F).
Fig. 76 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 76. Spicules of Nabaviella sp. from the lower Cambrian Erkeket Formation, Khorbusuonka River, Siberia, Russia; samples 20/1B (A) and 19/5.5 (B–D). A. Calcium phosphatic mould of the spicule with the proximal (proximal part of the spicule) shaft and a terminal knob (arrowed in A2) at the opposite surface of the distal disc (distal part of the spicule) consisting of radiating rays (A1), SMNH Sp11495. B. Calcium phosphatic coatings incompletely replicating the proximal surface of the disc with basal parts of the rays and internal axial canal in the spicule, SMNH Sp11496. B1, plain view; B2, lateral view. C. Internal mould of the proximal shaft with terminal proximal swelling (arrow), SMNH Sp11497. D. Calcium phosphatic internal mould of the axial canal and internal cavity of the distal disc and terminal knob (arrowed in D1), SMNH Sp11498. Scale bar: 125 µm (B) and 250 µm (A, C, D).
Fig. 69 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 69. Problematic fossils from the lower Cambrian Erkeket Formation, Khorbusuonka River, Siberia, Russia; samples 11/16.1 (K), 19/11.75 (A, I), 19/12.75 (B), 19/16 (D, F, G, H), 19/18 (C, E), and 19/5B (J). A. Tubular diagenetically phosphatised cyanobacterial trichomes, SMNH X11337. B–H. Problematic silicified tubes, SMNH X11338–11344, respectively. H2, enlargement showing presumably initial part of the tube. I. Problematic phosphatized tubes longitudinally merged, SMNH X11345. I1, close-up of I2, showing apertures of the tubes. J. Globula, SMNH X11346. K. Disk-like fossil, SMNH X11347. K1, plain view; K2, lateral view. Scale bar: 500 µm (B–G, H1), 250 µm (I2, J, K), 125 µm (I1), 50 µm (A, H2).
Fig. 68. Problematicum Coleoloides Walcott, 1889 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 68. Problematicum Coleoloides Walcott, 1889, internal moulds of tubes, from the lower Cambrian Erkeket (C, D), Tyuser (M), and Pestrotsvet (A, B, E–L) formations, Siberia, Russia; samples 11/2B (C) and 11/16.1 (D) from Khorbusuonka River; sample 21/22 (M) from lower reaches of Lena River; sample M303/2 (B, H, J, L) from Tiktirikteekh Brook (Rozanov et al. 1969: 31, text-fig. 6), sample 171–174 (E) from Bydyangaya Brook (Val'kov 1982: 27, textfig. 8) middle reaches of the Lena River, sample 479a (K) from section "Dvortsy", Aldan River, and sample 510 (A, F, G, I) from section Ulakhan-Sulugur, Aldan River (Fig. 1). A–C, K–M. Coleoloides trigeminatus Missarzhevsky in Rozanov et al., 1969, SMNH X11324–11329, respectively. D. Coleoloides sp., SMNH X11330. E–J. Coleoloides cf. paucistriatus Poulsen, 1967, SMNH X11331–11336, respectively. A1, B2, C2, E1, F2, G1, H2, I1, L2, lateral view; A2, B1, C1, F1, H1, L1, transversal view; E2, G2, I2, transversal view in the apical part. Scale bar: 500 µm (M) and 250 µm (A–L).
Fig. 67 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 67. Anabaritids, internal moulds (A–F) and other problematic tubes G–I) from the lower Cambrian Kessyusa Group (B–D, H, I) and Erkeket Formation (A, E–G), Khorbusuonka River, Siberia, Russia; samples 11/16.05 (A), 11/2B (E, F), 15/23 (B–D, H, I), and 20/1B (G). A. Anabarites tristichus Missarzhevsky in Rozanov et al., 1969, SMNH X11315. A1, transversal view of the tube; A2, lateral view. B. Anabarites hexasulcatus (Missarzhevsky, 1974), SMNH X11316. C. Selindeochrea ternaria Missarzhevsky in Rozanov et al., 1969), SMNH X11317. D. Cambrotubulus sp., SMNH X11318. E, F. Anabarites korobovi (Missarzhevsky in Rozanov and Missarzhevsky, 1966), SMNH X11319 and 11320, respectively. G. Coleolella billinsi (Sysoev, 1962), SMNH X11321. H, I. Platysolenites antiquissimus Eichwald, 1860, SMNH X11322 and 11323, respectively. Scale bar: 250 µm (A) and 500 µm (B–I).
Fig. 66 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 66. Torellella spp. with evidences of bioerosion, from the lower Cambrian Erkeket Formation, Khorbusuonka River (A–C, E, G) and Tyuser (F, H) and Sekten (D) formations, lower reaches of the Lena River, Siberia, Russia; samples 19/4.25 (A), 19/5.5 (E), 19/14.25 (B), 20/1B (C, G), 21/129 (D), and 22/0 F, H). A–G. Fragments of calcium phosphatic tubes penetrated by sub-vertical canals, SMNH X11307–11313, respectively. E2, close-up of E1 showing perforations. H. Fragment of tube with canals sub-parallel to the surface, SMNH X11314. Scale bar: 500 µm (A–D), 250 µm (E1, F–H), and 80 µm (E2).
Fig. 65 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 65. Calcium phosphatic tubes of hyolithelminths from the lower Cambrian Erkeket Formation, Khorbusuonka River (A–C, G–J) and Tyuser Formation, lower reaches of the Lena River (D–F, K, L), Siberia, Russia; samples 11/19.5 (B, C), 19/3.25 (H, J), 19/4.25 (I), 19/5.5 (G), 19/16 (A), 21/21 (D, E, K), and 21/22 (F, L). A, F, H. Hyolithellus sp., SMNH X11299–11301, respectively. B–E. Hyolithellus isiticus Missarzhevsky in Rozanov et al., 1969, SMNH X11295–11298, respectively. G, I–L. Torellella spp., SMNH X11302–11306, respectively. Scale bar: 1 mm (D, L), 500 µm (A–C, E, F, H, I–K), and 250 µm (G).
Fig. 58 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 58. Paleoscolecid Hadimopanella foveata sp. nov., from the lower Cambrian Erkeket Formation, Khorbusuonka River, Siberia, Russia; samples 19/31.75 (A–D, F–I), 19/43.25 (E, J, N, O), 20/5B (L, M), and 20/6B (K). A–O. Disarticulated sclerites, SMNH X11257–11268, 11352–11354, respectively. A, holotype. A1, B–D, G, H, O, oblique apical view; A2, E, F, I–N, apical view. Scale bar 100 µm.
Fig. 61 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 61. Lobopodian (A) and bradoriid (B–D) calcium phosphatic fragments, from the lower Cambrian Erkeket Formation, Khorbusuonka River (B, C) and Tyuser (D), and Sekten (A) formations, lower reaches of the Lena River, Siberia, Russia; samples 19/3.25 (C), 19/31.75 (B), 21/57.75 (D), and 22/67 (A). A. Microdictyon robisoni Bengtson, Matthews, and Missarzhevsky, 1986, sclerite, SMNH X11294. B. Mongolitubulus spinosus (Hinz, 1987), spine, SMNH Ar75002. C. Mongolitubulus reticulatus Kouchinsky, Bengtson, Clausen, Gubanov, Malinky, and Peel, 2011, spine, SMNH Ar75003. D. Cambria sibirica Neckaja and Ivanova, 1956, carapace, SMNH Ar75001; D1, anterior view; D2, D3, dorsal view. Scale bar: 250 µm A–C) and 1.25 mm (D).
Fig. 64 in Early-middle Cambrian stratigraphy and faunas from northern Siberia
Fig. 64. Thecal plates of Echinodermata from the lower Cambrian Erkeket Formation of Khorbusuonka River (B, C, E–O) and the middle Cambrian Sekten Formation, lower reaches of the Lena River (A, D), Siberia, Russia; samples 19/11.75 (O), 19/12.75 (J), 20/2B (I, K–M), 20/5B (B, C, F, G, N), 20/6B (E, H), and 22/67 (A, D). A–O. Thecal plates, SMNH Ec36886–36900, respectively. Scale bar 500 µm.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.