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870 results for “Ordovician”
Fig. 10 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 10. Heliolitine tabulate coral Wormsipora sp. from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. NIGP 201004. A1, A2, transverse sections. A3, A4, longitudinal sections.
Fig. 13 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 13. Heliolitine tabulate coral Navoites irregularis (Lin and Chow, 1977), from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. NIGP 201013. A1–A3, transverse sections. A4, longitudinal section.
Fig. 5 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 5. Heliolitine tabulate coral Plasmoporella xinjiangensis Lin and Wang in Wang, 1981, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 200955. A1, A2, transverse sections. A3–A5, longitudinal sections. B. NIGP 200946. B1, transverse section. B2, longitudinal section.
Fig. 9 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 9. Heliolitine tabulate coral Mongoliolites sp. from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. NIGP 201003. A1–A3, transverse sections. A4, A5, longitudinal sections.
Fig. 1 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 1. Map of the Xinjiang Uygur Autonomous Region (A) and southern Kuruktag, northeastern Tarim Basin (B) in Northwest China showing location of the studied area (star). C. Stratigraphic column of the studied section of Queerqueke Montain, southern Kuruktag with position of the studied material (star)
Fig. 15. Heliolitine tabulate coral Apekinella zeravshanica Ospanova, 2012a in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 15. Heliolitine tabulate coral Apekinella zeravshanica Ospanova, 2012a, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 201016. A1, A2, transverse sections. A3, A4, longitudinal sections. B. NIGP 201017. B1, B2, transverse sections. B3, longitudinal section.
Fig. 4 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 4. Heliolitine tabulate coral Plasmoporella xinjiangensis Lin and Wang in Wang, 1981, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 200945. A1, A2, transverse sections. A3, A4, longitudinal sections. B. NIGP 200973. B1, B2, transverse sections. B3 longitudinal section.
Fig. 12. Heliolitine tabulate coral Acdalopora sokolovi Bondarenko, 1958 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 12. Heliolitine tabulate coral Acdalopora sokolovi Bondarenko, 1958, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 201012. A1, A2, transverse sections. A3, A4 longitudinal sections. B. NIGP 201007. B1, B2, transverse sections.
Fig. 7. Heliolitine tabulate coral Plasmoporella grandis Bondarenko, 1958 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 7. Heliolitine tabulate coral Plasmoporella grandis Bondarenko, 1958, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 200991. A1, A2, transverse sections. A3, A4, longitudinal sections. B. NIGP 200993. B1, B2, transverse sections. B3, longitudinal section.
Fig. 6. Heliolitine tabulate coral Plasmoporella grandis Bondarenko, 1958 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 6. Heliolitine tabulate coral Plasmoporella grandis Bondarenko, 1958, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. NIGP 200990. A1, transverse section. A2, A3, longitudinal sections.
Fig. 8 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 8. Heliolitine tabulate coral Mongoliolites obliterans (Bondarenko, 1958), from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. A. NIGP 201001. A1, A2, transverse sections. A3, A4, longitudinal sections. B. NIGP 201002. B1, B2, transverse sections. B3, B4, longitudinal sections.
Fig. 3 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 3. Heliolitine tabulate coral Plasmoporella xinjiangensis Lin and Wang in Wang, 1981, from the Yuanbaoshan Formation (lower Katian) of southern Kuruktag, Tarim Basin, Northwest China. NIGP 200961. A1–A3, transverse sections. A4, A5, longitudinal sections.
Fig. 2 in Early Katian, Late Ordovician, heliolitine corals from southern Kuruktag in northeastern Tarim Basin of China
Fig. 2. Distribution of major tectonic units in the early Katian (Late Ordovician), with the Tarim Block (marked in purple). Modified from Torsvik and Cocks (2013).
Fig. 6 in The tarphyceratid cephalopod Trocholites in the Middle-Upper Ordovician of the Prague Basin -the Baltican element in peri-Gondwana
Fig. 6. Tarphyceratid cephalopod Trocholites chaloupkai sp. nov. from Praha-Štěrboholy, central Bohemia, Czech Republic, upper part of the Zahořany Formation (lower Katian, Upper Ordovician). A. Holotype NM L 63626, detail of apicalmost part of the phragmocone (A1) and drawing (A2) indicating line of contact of whorls, position of siphuncle, position of (partly fragmented) septa and shape of initial chamber and umbilical window.
Fig. 4 in The tarphyceratid cephalopod Trocholites in the Middle-Upper Ordovician of the Prague Basin -the Baltican element in peri-Gondwana
Fig. 4. Tarphyceratid cephalopod Trocholites fugax Babin and GutiérrezMarco, 1992, from Březová Hůrka near Starý Plzenec, central Bohemia, Czech Republic, Dobrotivá Formation (upper Middle–lower Upper Ordovician). A. NM L 63625a, b, counterpart (A1) and part (A2).
Fig. 3 in The tarphyceratid cephalopod Trocholites in the Middle-Upper Ordovician of the Prague Basin -the Baltican element in peri-Gondwana
Fig. 3. Parameters used to measure and describe the specimens studied herein (after Korn 2010). Abbreviations: ah, apertural height; cl, cameral length; dm, shell diameter across centre of umbilicus; fh, foramen height; iz, imprint zone; uw, umbilical width; wh, whorl height; ww, whorl width. Line drawings are based on NM L 63626 (holotype of Trocholites chaloupkai sp. nov.).
Fig. 6 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 6. Echiura gen. et sp. indet. from the Darriwilian (Middle Ordovician) of Castle Bank, Wales, UK, NMW.2021.3G.102. A1, overall view; A2, proboscis; A3, caudal region; A4, close up showing projections from anal region. A1 in plane-polarised light, A2–A4 in cross-polarised light.
Fig. 2 in The tarphyceratid cephalopod Trocholites in the Middle-Upper Ordovician of the Prague Basin -the Baltican element in peri-Gondwana
Fig. 2. Correlation of the Dobrotivá and Zahořany formations (greyed-out levels) with global and Ibero-Bohemian chronostratigraphic units, and the herein discussed occurrence of Trocholites. Modified from Kraft et al. (2015), Fatka and Budil (2022), and Kraft et al. (2023).
Fig. 5 in A new thalassematid echiuran worm from the Middle Ordovician Castle Bank Biota of Wales, UK
Fig. 5. Reconstruction of Llwygarua suzannae gen. et sp. nov.; observed size range: 5.5 to 7 mm long.
Fig. 1 in The tarphyceratid cephalopod Trocholites in the Middle-Upper Ordovician of the Prague Basin -the Baltican element in peri-Gondwana
Fig. 1. Map of Ordovician rocks of the Prague Basin and position of the localities, from which the two studied specimens originate: Locality 1, Březová Hůrka near Starý Plzenec; Locality 2, Praha-Štěrboholy. Modified from Manda (2008).
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