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58 results for “Tarim Basin”
Figure 13. A–K in Middle to Late Ordovician (Darriwilian-Sandbian) Conodonts from the Dawangou Section, Kalpin Area of the Tarim Basin, Northwestern China
Figure 13. A–K, Dzikodus?tablepointensis (Stouge, 1984). A–B, Pb element; A, NIGP 152952, Nj297, upper view (IY150-001); B, NIGP 152953, Nj297, upper view (IY150-002). C–G, Sa element; C, NIGP 152954, Nj297, posterior view (IY150-003); D–E, NIGP 152955, Nj297, D, lateral view (IY150-008), E, anterior view (IY150-010); F–G, NIGP 152956, Nj297, F, lateral view (IY159-006), G, posterior view (IY159-007). H–I, Sb element, NIGP 152957, Nj297, H, outer lateral view (IY150-006), I, inner lateral view (IY150-007). J–K, Sd element, NIGP 152958, Nj297, J, postero-outer lateral view (IY159-005), K, posterior view (IY159-004). L–N, Polonodus sp. B. L, P element, NIGP 152959, Nj291, upper view (IY158-002); M, P element, NIGP 152960, Nj291, upper view (IY158-001); N, Sc element, NIGP 152961, Nj291, inner lateral view (IY158-003). Scale bars 100 µm.
Figure 9. A–C in Middle to Late Ordovician (Darriwilian-Sandbian) Conodonts from the Dawangou Section, Kalpin Area of the Tarim Basin, Northwestern China
Figure 9. A–C, Dapsilodus viruensis (Fåhraeus, 1966). A, Sc element, NIGP 152896, Nj375, outer lateral view (IY159-024). B–C, Sa element; B, NIGP 152897, Nj375, lateral view (IY159-025), tentatively assigned to this species; C, NIGP 152898, Nj375, lateral view (IY159-026). D–O, Scabbardella altipes (Henningsmoen, 1948). D–E, long-based acodiform element; D, NIGP 152899, Nj378, outer lateral view (IY153-016); E, NIGP 152900, Nj403, outer lateral view (IY161-021). F–G, medium-based acodiform element; F, NIGP 152901, Nj297, outer lateral view (IY159-012); G, NIGP 152902, AFT-X-K13/13, outer lateral view (IY167-002). H–O, asymmetrical distacodiform element; H, NIGP 152903, Nj376, outer lateral view (IY159-029); I–K, NIGP 152904, Nj378, I, outer lateral view (IY160- 017), J, inner lateral view (IY160-017), K, basal view (IY160-020); L–N, NIGP 152905, Nj379, L, upper view, close up of cross section of the cusp (IY160-035), M, inner lateral view (IY160-036), N, upper view (IY160-034); O, NIGP 152906, Nj379, outer lateral view (IY160-033). Scale bars 100 µm, unless otherwise indicated.
Figure 3 in Middle to Late Ordovician (Darriwilian-Sandbian) Conodonts from the Dawangou Section, Kalpin Area of the Tarim Basin, Northwestern China
Figure 3. Conodont occurrences recorded in this study from the Dawangou section (Dawangou, Saergan and Kanling formations), Kalpin, Xinjiang Autonomous Region, China.
Figure 6 in Middle to Late Ordovician (Darriwilian-Sandbian) Conodonts from the Dawangou Section, Kalpin Area of the Tarim Basin, Northwestern China
Figure 6. Costiconus ethingtoni (Fåhraeus, 1966). A–D, M element; A–B, NIGP 152866, A, posterior view (IY166-016), B, basal-posterior view (IY166-017); C, NIGP 152867, posterior view (IY166-008); D, NIGP 152868, anterior view (IY166-015). E–I, Pb element; E–F, NIGP 152869, E, basal view (IY166-002), F, inner lateral view (IY166-001); G–H, NIGP 152870, G, outer lateral view (IY166-013), H, basal view (IY166-014); I, NIGP 152871, outer lateral view (IY166-009). J–L, Pa element; J, NIGP 152872, inner lateral view (IY166- 010); K–L, NIGP 152873, K, inner lateral view (IY166-004), L, inner-basal view (IY166-003). All from sample AFT-X-K13/13, scale bars 100 µm.
Figure 16. Periodon aculeatus Hadding 1913. A–B, M in Middle to Late Ordovician (Darriwilian-Sandbian) Conodonts from the Dawangou Section, Kalpin Area of the Tarim Basin, Northwestern China
Figure 16. Periodon aculeatus Hadding 1913. A–B, M element; A, NIGP 152979, posterior view (IY145-001); B, NIGP 152980, anterior view (IY145-002). C–E, Sa element; C–D, NIGP 152981, C, anterior view (IY145-003), D, lateral view (IY145-004); E, NIGP 152982, lateral view (IY145-006). F–I, Sb element; F–G, NIGP 152983, F, inner lateral view (IY145-010), G, outer lateral view (IY145-013); H–I, NIGP 152984, H, upper view (IY145-018), I, inner lateral view (IY145-020). J–K, Sc element; J, NIGP 152985, outer lateral view (IY145-016); K, NIGP 152986, inner lateral view (IY145-017). L–N, Pa element; L, NIGP 152987, inner lateral view (IY145-023); M, NIGP 152988, outer lateral view (IY145-024); N, NIGP 152989, basal view (IY145-025N). O–P, Pb element; O, NIGP 152990, outer lateral view (IY145-027); P, NIGP 152991, inner lateral view (IY145-026). All from sample Nj294; scale bars 100 µm.
Figs 1–3 in A new species of the genus Cymindis Latreille, 1805 (Coleoptera: Carabidae: Lebiini) from the Tarim River basin, China
Figs 1–3. Cymindis (Tarsostinus) rolandi sp. n., female. 1 – holotype, habitus, dorsal
Water and energy fluxes measurements over a riparian Tamarix spp. stand in the lower Tarim River basin, northwestern China
<p>This dataset includes water and energy fluxes measurements over a riparian <em>Tamarix spp.</em> stand in the lower Tarim River basin, northwestern China. Details of field site and measurements can be found in the paper: Yuan, G., P. Zhang, M.-a. Shao, Y. Luo, and X. Zhu (2014), Energy and water exchanges over a riparian Tamarix spp. stand in the lower Tarim River basin under a hyper-arid climate, Agricultural and Forest Meteorology, 194(0), 144-154.</p> <p>This dataset also accompanies the published paper in the Water Resources Research: Implementing Dynamic Root Optimization in Noah‐MP for Simulating Phreatophytic Root Water Uptake. Water Resources Research 54(3), 1560-1575. With this dataset, we tested the Noah-MP land surface model with implementation of a soil moisture-responsive root dynamics scheme (VOM-ROOT). </p>
Limited Northward Expansion of the Tibetan Plateau in the Late Cenozoic: Insights from the Cherchen Fault in the Southeastern Tarim Basin
<p>Supporting information submitted: Figure S1 to Figure S3</p> <p>Figures, captions, and introduction text are included in the uploaded file. </p>
First identification of the Ediacaran Yukengou Formation in western Kuruktag, northeastern Tarim and its implications for the Neoproterozoic rift basin evolution
<p>This supporting information provides three supplemental tables containing the sandstone composition counting and zircon U-Pb dating results.</p>
Early Silurian chondrichthyans from the Tarim Basin (Xinjiang, China)
<p>The Sinacanthida ordo nov. and Mongolepidida are spine- and scale-based taxa whose remains encompass some of the earliest reported fossils of chondrichthyan fish. Investigation of fragmentary material from<b> </b>the Early Silurian Tataertag and Ymogantau Formations of the Tarim Basin (Xinjiang Uygur Autonomous Region, China) has revealed a diverse mongolepidid and sinacanthid fauna dominated by mongolepids and sinacanthids in association with abundant dermoskeletal elements of the endemic 'armoured' agnathans known as galeaspids.</p> <p>Micro-computed tomography, scanning electron microscopy and histological sections were used to identify seven mongolepid genera (including <i>Tielikewatielepis</i> <i>sinensis</i> gen. et sp. nov., <i>Xiaohaizilepis</i> <i>liui</i> gen. et sp. nov. and <i>Taklamakanolepis</i> <i>asiaticus</i> gen. et sp. nov.) together with a new chondrichthyan (<i>Yuanolepis</i> <i>bachunensis </i>gen. et sp. nov.) with scale crowns consisting of a mongolepid-type atubular dentine (lamellin). Unlike the more elaborate crown architecture of mongolepids, <i>Yuanolepis </i>gen. nov.<i> </i>exhibits a single row of crown elements consistent with the condition reported in stem chondrichthyans from the Lower Devonian (e.g. in <i>Seretolepis</i>, <i>Parexus</i>). The results corroborate previous work by recognising lamellin as the main component of sinacanthid spines and point to corresponding developmental patterns shared across the dermal skeleton of taxa with lamellin and more derived chondrichthyans (e.g. <i>Doliodus,</i> <i>Kathemacanthus, Seretolepis</i> and <i>Parexus</i>).</p> <p>The Tarim mongolepid fauna is inclusive of coeval taxa from the South China Block and accounts for over two-thirds of the species currently attributed to Mongolepidida. This demonstrates considerable overlap between the Tarim and South China components of the Lower Silurian Zhangjiajie Vertebrate Fauna.</p>
FIGURE 2 in A brief review of Triplophysa (Cypriniformes: Balitoridae) species from the Tarim Basin in Xinjiang, China, with description of a new species
FIGURE 2. Triplophysa laterimaculata (Holotype KIZ 200408220489, 43.33mm SL): (A) lateral view; (B) mouth; (C)
Databases and scripts for Calvo, et al. Assessing the effect of glacier runoff changes on basin runoff and agricultural production in the Indus, Amu Darya, and Tarim Interior Basins.
<p>This repository has the necessary script and databases to reproduce the figures and tables presented in Calvo et al. (in press) Assessing the effect of glacier runoff changes on basin runoff and agricultural production in the Indus, Amu Darya, and Tarim Interior Basins. Earth´s Future. Wiley.</p>
Subspecies and Distribution. E. n. naso Sclater, 1891 — W China (Tarim Basin in S Xinjiang). E. n. alashanicus A. B. Howell, 1928 — N China (Helan [= Alashan] Mts, Ordos Desert, and Qaidam Basin in Gansu, W Inner Mongolia [= Nei Mongol], and N Qinghai) and S Mongolia. E. n. ywuensis Ma Yong & Li Sirua, 1979 — NW China (E Dzungarian Basin in NE Xinjiang). in Dipodidae
Subspecies and Distribution. E. n. naso Sclater, 1891 — W China (Tarim Basin in S Xinjiang). E. n. alashanicus A. B. Howell, 1928 — N China (Helan [= Alashan] Mts, Ordos Desert, and Qaidam Basin in Gansu, W Inner Mongolia [= Nei Mongol], and N Qinghai) and S Mongolia. E. n. ywuensis Ma Yong & Li Sirua, 1979 — NW China (E Dzungarian Basin in NE Xinjiang).
Distribution. Steppes of the Tarim Basin around the edge of the Taklamakan Desert, S Xinjiang (NW China). in Leporidae
Distribution. Steppes of the Tarim Basin around the edge of the Taklamakan Desert, S Xinjiang (NW China).
Early Silurian chondrichthyans from the Tarim Basin (Xinjiang, China)
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FIGURE 1 in A brief review of Triplophysa (Cypriniformes: Balitoridae) species from the Tarim Basin in Xinjiang, China, with description of a new species
FIGURE 1. Collection locality of Triplophysa laterimaculata, new species.
Fig. 11. Heliolitine tabulate coral Acdalopora sokolovi Bondarenko, 1958 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 11. Heliolitine tabulate coral Acdalopora sokolovi Bondarenko, 1958, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 201009. A1, A2, transverse sections. A3, longitudinal section. B. NIGP 201008. B1, B2, transverse sections. B3, longitudinal section.
Figure 20. A–E in Middle to Late Ordovician (Darriwilian-Sandbian) Conodonts from the Dawangou Section, Kalpin Area of the Tarim Basin, Northwestern China
Figure 20. A–E, Protopanderodus cooperi (Sweet & Bergström, 1962), from the Pratt Ferry Formation of Alabama. A–C, M element, OSU 52802, from the topotype locality, A–B, posterior views (IY170-024, IY170-025), C, anterior view (IY171-011). D–E, Sb element, OSU 52803, from the topotype locality, D, outer lateral view (IY171-012), E, inner lateral view (IY170-023). F–L, Protopanderodus varicostatus (Sweet & Bergström, 1962); from the Pratt Ferry Formation of Alabama. F–H, M2 element, OSU 52804, topotype, sample 64B2-12 from the top bed of the formation, F–G, posterior views (IY170-002, Iy170-001), F, anterior view (IY171-015); I–J, M2 element, OSU 52805 from the topotype locality, I, posterior view (IY170-007), J, anterior view (IY171-018). K–L, M1 element, OSU 52806, topotype, sample 64B2-12 from the top bed of the formation, K, posterior view (170-026), L, anterior view (IY171-013). Scale bars 100 µm.
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