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Text-fig. 5. Fossil remains of a leafy Lepidodendron ophiurus BRONGN. shoot bearing a Flemingites strobilus produced by a tree similar to that shown in Text-fig. 2a; Middle Coal Measures Formation (Duckmantian – upper Bashkirian), Brymbo, near Wrexham, UK (see Thomas et al. 2020: fig. 16b); National Museum Wales specimen 2013.43G.120. in Naming Of Parts: The Use Of Fossil-Taxa In Palaeobotany

Text-fig. 5. Fossil remains of a leafy Lepidodendron ophiurus BRONGN. shoot bearing a Flemingites strobilus produced by a tree similar to that shown in Text-fig. 2a; Middle Coal Measures Formation (Duckmantian – upper Bashkirian), Brymbo, near Wrexham, UK (see Thomas et al. 2020: fig. 16b); National Museum Wales specimen 2013.43G.120.

opencc-by-4.0Dec 2021View details →
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Text-fig. 2. The distinction between fossil plants (a) and plant fossils (b). a: Reconstruction of a late Carboniferous arborescent lycopsid, often referred to as the Lepidodendron-tree; artwork by A. Townsend (formerly of National Museum Wales, Cardiff, UK; see Townsend et al. 1998); b: Lepidodendron aculeatum STERNB.; Middle Coal Measures Formation (Duckmantian – upper Bashkirian), Brymbo, near Wrexham, UK (see Thomas et al. 2020: fig. 16b); National Museum Wales specimen 2013.43G.88. in Naming Of Parts: The Use Of Fossil-Taxa In Palaeobotany

Text-fig. 2. The distinction between fossil plants (a) and plant fossils (b). a: Reconstruction of a late Carboniferous arborescent lycopsid, often referred to as the Lepidodendron-tree; artwork by A. Townsend (formerly of National Museum Wales, Cardiff, UK; see Townsend et al. 1998); b: Lepidodendron aculeatum STERNB.; Middle Coal Measures Formation (Duckmantian – upper Bashkirian), Brymbo, near Wrexham, UK (see Thomas et al. 2020: fig. 16b); National Museum Wales specimen 2013.43G.88.

opencc-by-4.0Dec 2021View details →
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Fig. 8 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 8. Transverse (A1–A5, A8) and longitudinal (A6, A7) thin sections of aulophyllid rugose coral Heritschioides simplex sp. nov. (GSC 140526, holotype) from Liard Basin, Northwestern Territories, Canada, Mattson Formation, perhaps lower Bashkirian. Corallites in different growth stages (A1–A3), dissepimentarium and peripheral parts of septa (A4, A5), laterally offsetting corallite (A6), detail of parent/offset common tissue (A7), fragment of colony with twins (arrow) (A8). Black dots correspond to cardinal (lower) and counter (upper) septa.

opencc-by-4.0Dec 2019View details →
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Fig. 7 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 7. Lithostrotionid rugose coral Nemistium liardense sp. nov. from Liard Basin, Northwestern Territories, Canada, Mattson Formation, perhaps lower Bashkirian. A. GSC 140520, holotype, longitudinal section of offsetting corallite (A1), transverse section of colony fragment (A2). B. GSC 140526, transverse section showing broken corallites (white arrows) at periphery of colony of Heritschioides simplex sp. nov.; upper part (black arrows) indicates fragment of colony of Nemistium liardense sp. nov.

opencc-by-4.0Dec 2019View details →
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Fig. 4 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 4. Thin sections of lithostrotionid rugose coral Nemistium liardense sp. nov. from Stikine Terrane, Northwestern Territories, Canada, Mattson Formation, lower Bashkirian (A, B), and Liard Basin, Northwestern Territories, Canada, Mattson Formation, perhaps lower Bashkirian (C–E). A. GSC 140524, transverse (A1) and longitudinal (A2) section. B. GSC 140525, transverse (B1) and longitudinal (B2) section. C. GSC 140522, longitudinal section of two corallites (C1) and transverse section (C2). D. GSC 140523, longitudinal section of offsetting corallite with strong pseudocolumella (D1) and transverse section of part of colony (D2). E. GSC 140520, holotype, oblique section of two young corallites.

opencc-by-4.0Dec 2019View details →
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Fig. 9 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 9. Transverse (A2–A4) and longitudinal (A1, A5) thin sections of aulophyllid rugose coral Heritschioides simplex sp. nov. (GSC 140526, holotype) from Liard Basin, Northwestern Territories, Canada, Mattson Formation, perhaps lower Bashkirian. Trabecular microstructure of septum and sclerenchymal cover unequally distributed (A1–A3), detail demonstrating doubled major septa (A4), microstructure of septum (A5); arrow in A3 points to primary septum lacking sclerenchymal cover. Black dots correspond to cardinal (lower) and counter (upper) septa.

opencc-by-4.0Dec 2019View details →
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Fig. 5 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 5. Transverse thin sections of lithostrotionid rugose coral Nemistium liardense sp. nov. from Liard Basin, Northwestern Territories, Canada, Mattson Formation, perhaps lower Bashkirian. A. GSC 140520, holotype, beginning of offsetting (arrow). B. GSC 140523, early (B1, B2) and advanced (B3) development of offsets. C. GSC 140522, offset with elongated septum at early growth stage (arrow).

opencc-by-4.0Dec 2019View details →
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Fig. 1 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 1. Map showing location of study area and Carboniferous lithofacies assemblages subcropping beneath Permian and Mesozoic deposits in the Western Canada Sedimentary Basin (modified from Richards et al. 1994). In the Liard Basin, western occurrences of the Rundle and Mattson lithofacies assemblages overlie and pass westward into the Besa River lithofacies assemblage. See Fig. 3 for the formational composition of the Banff, Rundle, and Mattson lithofacies assemblages.

opencc-by-4.0Dec 2019View details →
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Fig. 2 in Bashkirian rugose corals from the Carboniferous Mattson Formation in the Liard Basin, northwest Canada -stratigraphic and paleobiogeographic implications

Fig. 2. Simplified geological map of study region showing distribution of outcrops of Carboniferous Mattson Formation in southwest corner of the Northwest Territories and southeastern Yukon Territory (modified from Harker 1963 and an unpublished Geological Survey of Canada 1:1 000 000 scale map prepared by Andrew Okulitch in 2005).

opencc-by-4.0Dec 2019View details →
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Text-fig. 12. Ammonoids from the Mospyne Formation. a–e: Bisatoceras sp., dorsal view (a), lateral view (b, d), ventral view (c), surface ornamentation on the flank of specimen IGSU-7/500a (e); a–c – specimen IGSU-7/500, d, e – specimen IGSU-7/500a. f:?Owenoceras sp., lateral view; specimen IGSU-4/1367. Scale bars 2 mm (e) and 5 mm (a–d, f). in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 12. Ammonoids from the Mospyne Formation. a–e: Bisatoceras sp., dorsal view (a), lateral view (b, d), ventral view (c), surface ornamentation on the flank of specimen IGSU-7/500a (e); a–c – specimen IGSU-7/500, d, e – specimen IGSU-7/500a. f:?Owenoceras sp., lateral view; specimen IGSU-4/1367. Scale bars 2 mm (e) and 5 mm (a–d, f).

opencc-by-4.0Dec 2022View details →
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Text-fig. 10. Gastrioceras sp., lateral view (a), ventral view (b– d); a, b – specimen IGSU-4/6390, c – specimen IGSU-4/6390a, d – specimen IGSU-4/6390b. Scale bar 10 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 10. Gastrioceras sp., lateral view (a), ventral view (b– d); a, b – specimen IGSU-4/6390, c – specimen IGSU-4/6390a, d – specimen IGSU-4/6390b. Scale bar 10 mm.

opencc-by-4.0Dec 2022View details →
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Text-fig. 9. Ammonoids from the Mospyne Formation. a–d: Gastrioceras angustum PATTEISKY, 1964, lateral view (a, c), ventral view (b, d); a, b – specimen IGSU-7/8100, c, d – specimen IGSU-7/669b. e–i: Gastrioceras lupinum POPOV, 1979, lateral view; e – specimen IGSU-4/687, f – specimen IGSU-4/687a, g – specimen IGSU-4/687b, h – specimen IGSU-4/644, i – specimen IGSU-4/1516. j, k: Gastrioceras kutejnikovense POPOV, 1979, lateral view; j – specimen IGSU-7/3254, k – specimen IGSU-7/3254a. Scale bar 5 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 9. Ammonoids from the Mospyne Formation. a–d: Gastrioceras angustum PATTEISKY, 1964, lateral view (a, c), ventral view (b, d); a, b – specimen IGSU-7/8100, c, d – specimen IGSU-7/669b. e–i: Gastrioceras lupinum POPOV, 1979, lateral view; e – specimen IGSU-4/687, f – specimen IGSU-4/687a, g – specimen IGSU-4/687b, h – specimen IGSU-4/644, i – specimen IGSU-4/1516. j, k: Gastrioceras kutejnikovense POPOV, 1979, lateral view; j – specimen IGSU-7/3254, k – specimen IGSU-7/3254a. Scale bar 5 mm.

opencc-by-4.0Dec 2022View details →
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Text-fig. 8. Ammonoids Melvilloceras rotaii (LIBROVITCH in POPOV, 1979) from the Mospyne Formation. a, b: A slightly laterally compressed specimen IGSU-7/8040, lateral view (a), ventral view (b). c, d: A slightly laterally compressed specimen IGSU-7/472, lateral view (c), ventral view (d). e, f: Specimen IGSU-7/540, lateral view (e), ventral view (f). g–i: Specimen IGSU-7/468, dorsal view (g), lateral view (h), ventral view (i). j: Specimen IGSU-7/6538, dorsal view. k, l: Specimen IGSU-7/620, lateral view (k), ventral view (l). m–q: Lateral views of the conchs showing the different relief of the umbilical nodes; m – specimen IGSU-4/4148, n – specimen IGSU-7/522, o – specimen IGSU-7/468a, p – specimen IGSU-7/472a, q – specimen IGSU-7/316. Scale bars 10 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 8. Ammonoids Melvilloceras rotaii (LIBROVITCH in POPOV, 1979) from the Mospyne Formation. a, b: A slightly laterally compressed specimen IGSU-7/8040, lateral view (a), ventral view (b). c, d: A slightly laterally compressed specimen IGSU-7/472, lateral view (c), ventral view (d). e, f: Specimen IGSU-7/540, lateral view (e), ventral view (f). g–i: Specimen IGSU-7/468, dorsal view (g), lateral view (h), ventral view (i). j: Specimen IGSU-7/6538, dorsal view. k, l: Specimen IGSU-7/620, lateral view (k), ventral view (l). m–q: Lateral views of the conchs showing the different relief of the umbilical nodes; m – specimen IGSU-4/4148, n – specimen IGSU-7/522, o – specimen IGSU-7/468a, p – specimen IGSU-7/472a, q – specimen IGSU-7/316. Scale bars 10 mm.

opencc-by-4.0Dec 2022View details →
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Text-fig. 7. Ammonoids from the Mospyne Formation. a: Anthracoceratites sp., lateral view; specimen IGSU-4/3634. b, c: Cymoceras sp., lateral view (b), fragment of the suture line in a 42 mm diameter conch (c); specimen IGSU-4/573. d, e: Neodimorphoceratidae indet., lateral view (d), surface ornamentation on the flank (e); specimen IGSU-4/5350. Scale bars 10 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 7. Ammonoids from the Mospyne Formation. a: Anthracoceratites sp., lateral view; specimen IGSU-4/3634. b, c: Cymoceras sp., lateral view (b), fragment of the suture line in a 42 mm diameter conch (c); specimen IGSU-4/573. d, e: Neodimorphoceratidae indet., lateral view (d), surface ornamentation on the flank (e); specimen IGSU-4/5350. Scale bars 10 mm.

opencc-by-4.0Dec 2022View details →
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Text-fig. 5. Remains of the jaw apparatus of ammonoids from the Mospyne Formation. a: Part of the upper jaw of an unknown ammonoid (stratigraphic level No. 5). b: Part of the jaw of an unknown ammonoid (stratigraphic level No. 5). c: Upper jaw of an unknown ammonoid (stratigraphic level No. 4). d: Part of the upper jaw of an unknown ammonoid (stratigraphic level No. 4). e: Lower (?) jaw of an unknown ammonoid (stratigraphic level No. 4); the arrow indicates the trace fossil. f: Part of the lower jaw of an unknown ammonoid (stratigraphic level No. 8). Scale bars 2 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 5. Remains of the jaw apparatus of ammonoids from the Mospyne Formation. a: Part of the upper jaw of an unknown ammonoid (stratigraphic level No. 5). b: Part of the jaw of an unknown ammonoid (stratigraphic level No. 5). c: Upper jaw of an unknown ammonoid (stratigraphic level No. 4). d: Part of the upper jaw of an unknown ammonoid (stratigraphic level No. 4). e: Lower (?) jaw of an unknown ammonoid (stratigraphic level No. 4); the arrow indicates the trace fossil. f: Part of the lower jaw of an unknown ammonoid (stratigraphic level No. 8). Scale bars 2 mm.

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Text-fig. 4. Taphonomic features of the studied localities of ammonoids. a: Sandstone slab with fragmentary remains of productid and spiriferid brachiopods, orthocerids, coiled nautiloids and ammonoids (stratigraphic level No. 3). b: Shell debris cluster and fragment of crushed ammonoid conch (stratigraphic level No. 1). c: Epibionts on the surface of an ammonoid conch (stratigraphic level No. 5). d: Cluster of bivalves, gastropods and cephalopods remains in a siderite nodule (stratigraphic level No. 5). e: Fragment of an ammonoid conch (stratigraphic level No. 3). f: Fragment of an ammonoid conch (?) with terminal aperture and brachiopod valve (stratigraphic level No. 3). g: Specimen of?Anthracoceratites sp. with conch injuries (shown by arrows) (stratigraphic level No. 8). h, i: Bioerosion trace fossils Cyclopuncta girtyi ELIAS, 1958 on the fragments of cephalopod conchs (stratigraphic level No. 5). j: Limonitized conchs of the ammonoid (stratigraphic level No. 7). k: Fragment of an ammonoid conch (stratigraphic level No. 5). Scale bars 10 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 4. Taphonomic features of the studied localities of ammonoids. a: Sandstone slab with fragmentary remains of productid and spiriferid brachiopods, orthocerids, coiled nautiloids and ammonoids (stratigraphic level No. 3). b: Shell debris cluster and fragment of crushed ammonoid conch (stratigraphic level No. 1). c: Epibionts on the surface of an ammonoid conch (stratigraphic level No. 5). d: Cluster of bivalves, gastropods and cephalopods remains in a siderite nodule (stratigraphic level No. 5). e: Fragment of an ammonoid conch (stratigraphic level No. 3). f: Fragment of an ammonoid conch (?) with terminal aperture and brachiopod valve (stratigraphic level No. 3). g: Specimen of?Anthracoceratites sp. with conch injuries (shown by arrows) (stratigraphic level No. 8). h, i: Bioerosion trace fossils Cyclopuncta girtyi ELIAS, 1958 on the fragments of cephalopod conchs (stratigraphic level No. 5). j: Limonitized conchs of the ammonoid (stratigraphic level No. 7). k: Fragment of an ammonoid conch (stratigraphic level No. 5). Scale bars 10 mm.

opencc-by-4.0Dec 2022View details →
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Text-fig. 11.?Agastrioceras sp., dorsal view (a), lateral view (b), ventral view (c); specimen IGSU-7/389. Scale bar 10 mm. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 11.?Agastrioceras sp., dorsal view (a), lateral view (b), ventral view (c); specimen IGSU-7/389. Scale bar 10 mm.

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Text-fig. 2. Geological setting of the studied sites. a: Stratigraphic position of the Mospyne Formation in the Carboniferous succession of the Donets Basin. b: Stratigraphic position of the studied locality of ammonoids (numbers in circles to the right of the lithological column). c–f: Some studied localities, c – stratigraphic level with ammonoids No. 8, d – stratigraphic level No. 4, e – stratigraphic level No. 3, f – part of the section of the Mospyne Formation in Sukha Ravine and the position of stratigraphic levels with ammonoids. Abbreviations: Tour. – Tournaisian, Serpukhov. – Serpukhovian, Kasimov. – Kasimovian. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 2. Geological setting of the studied sites. a: Stratigraphic position of the Mospyne Formation in the Carboniferous succession of the Donets Basin. b: Stratigraphic position of the studied locality of ammonoids (numbers in circles to the right of the lithological column). c–f: Some studied localities, c – stratigraphic level with ammonoids No. 8, d – stratigraphic level No. 4, e – stratigraphic level No. 3, f – part of the section of the Mospyne Formation in Sukha Ravine and the position of stratigraphic levels with ammonoids. Abbreviations: Tour. – Tournaisian, Serpukhov. – Serpukhovian, Kasimov. – Kasimovian.

opencc-by-4.0Dec 2022View details →
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Text-fig. 6. Stratigraphic distribution of ammonoids in the Mospyne Formation. The lithological symbols are the same as in Text-fig. 2. in Late Bashkirian Ammonoids From The Mospyne Formation Of The Donets Basin, Ukraine

Text-fig. 6. Stratigraphic distribution of ammonoids in the Mospyne Formation. The lithological symbols are the same as in Text-fig. 2.

opencc-by-4.0Dec 2022View details →
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Data from: Evolution of the conodont Diplognathodus ellesmerensis from D. benderi sp. nov. at the Bashkirian-Moscovian (Lower-Middle Pennsylvanian) boundary in South China

Conodont assemblages from the Bashkirian-Moscovian boundary interval in the Naqing section, South China have been studied in detail. A landmark-based geometric morphometric analysis to study the evolution of Diplognathodus ellesmerensis is presented. This analysis helped recognize a distinct new species, D. benderi sp. nov., which represents the direct evolutionary ancestor of D. ellesmerensis. The potential of using the First Appearance Datum (FAD) of D. ellesmerensis as the Bashkirian-Moscovian boundary marker is re-evaluated via biostratigraphic correlations of conodonts and other fossil groups between different palaeogeographic basins. The FAD of D. ellesmerensis from within the D. benderi sp. nov.–D. ellesmerensis lineage is an excellent marker to recognize a global Bashkirian-Moscovian boundary because of its global distribution, an abundance of supplementary marker species at similar stratigraphic levels, and the close stratigraphic proximity of the FAD to the traditional Bashkirian-Moscovian boundary, thus largely preserving the original concept for the base of the Moscovian Stage.

opencc-zeroMar 2020View details →

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