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8 results for “Spiriferida”

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zenodo40/100

Fig. 6. A in New and revised taxa of Carboniferous spiriferides (Brachiopoda, Spiriferida) from the Donets Basin (Ukraine) and South Urals (Russia)

Fig. 6. A. Verneuilia cheiropteryx (d'Archiac & de Verneuil, 1842). Lectotype ONCP D568 (Gourvennec 1994 Coll.) from Refrath (Bergisches Land, Germany). Devonian, Frasnian; dorsal, ventral, anterior and posterior views (copy from Gourvennec 1994: pl. 1 figs 1–5). B–E. Johnsoniana oceani (d'Orbigny, 1850). B. Neotype NHM B7923 (Brunton 1984 Coll.) from Visé (Belgium). Visean; ventral, lateral, dorsal, posterior and anterior views (copy from Brunton 1984: text-fig. 160a–e). C. Paratype CNIGR Museum 3085 (Nalivkin 1979 Coll.) from Bashkortostan (Urals, Russia). Upper Tournaisian; ventral, lateral, dorsal and anterior views (copy from Nalivkin 1979: pl. 62 fig. 21). D. Paratype ONCP Museum D306a (Gourvennec 1994 Coll.) from Visé (Belgium). Viséan; ventral, dorsal, lateral, anterior and posterior views (copy from Gourvennec 1994: pl. 1 figs 11–15). E. Paratype ONCP Museum D306e (Gourvennec 1994 Coll.) from same locality; dorsal, ventral, anterior and lateral views (copy from Gourvennec 1994: pl. 1 figs 16–19). Scale bar units = 1 mm.

opencc-by-4.0Nov 2024View details →
zenodo40/100

Fig. 1 in New and revised taxa of Carboniferous spiriferides (Brachiopoda, Spiriferida) from the Donets Basin (Ukraine) and South Urals (Russia)

Fig. 1. Geographical and stratigraphic location of the studied spiriferid-bearing localities (marked by stars) in Ukraine. A. Carboniferous stratigraphy of the Donets Basin and position of the Smolyanynivka Formation. B. Lithologic column of the Smolyanynivka Formation and stratigraphic position of the spiriferid-bearing fossil sites (modified after Nemyrovska et al. 2013). C–D. Geographical location of the studied spiriferid-bearing localities (1 = Donetsk Region, Khartsis'k District, Vovcha River, Illinka village; 2 = Luhansk Region, Bila River, Gorodyshche village).

opencc-by-4.0Nov 2024View details →
zenodo40/100

Fig. 3 in New and revised taxa of Carboniferous spiriferides (Brachiopoda, Spiriferida) from the Donets Basin (Ukraine) and South Urals (Russia)

Fig. 3. Tiramnia davidi sp. nov. from the Donets Basin (Ukraine). Pennsylvanian, Bashkirian. A. Holotype NMNH 1433/85 (Аisenverg 1951 Coll.) Donetsk Region, Illinka village; ventral, dorsal, lateral and anterior views (copy from Аisenverg 1951: pl. 11 fig. 2). B–C. Paratypes NMNH 2446/102, NMNH 2446/103 (Poletaev 2018 Coll.) Luhansk Region, Bila River, Gorodyshche village; ventral views (copy from Poletaev 2018: pl. 13 figs 8–9). D. Paratype NMNH 2446/104 (Poletaev 2018 Coll.) same locality; dorsal view (copy from Poletaev 2018: pl. 13 fig. 7). E. Paratype NMNH 2446/105 (Poletaev 2018 Coll.) same locality; internal view of the ventral valve (copy from Poletaev 2018: pl. 13 fig. 10). Scale bar units = 1 mm.

opencc-by-4.0Nov 2024View details →
zenodo40/100

Fig. 5. Betaneospirifer stepanovi Poletaev, 2018 in New and revised taxa of Carboniferous spiriferides (Brachiopoda, Spiriferida) from the Donets Basin (Ukraine) and South Urals (Russia)

Fig. 5. Betaneospirifer stepanovi Poletaev, 2018 from Bashkortostan (Urals, Russia). A. Holotype CNIGR 8491/48 (Mironova 1967 Coll.) from Tabynskoie; ventral view (copy from Mironova 1967: pl. 4 fig. 6). B. Paratype GMNTSU 79/226 (Alexandrov & Einor 1979 Coll.) from Tash-Asty; ventral and dorsal views (copy from Alexandrov & Einor 1979: pl. 28 fig. 18). C. Paratype VNIGRI 163 (Stepanov 1948 Coll.) from Tabynskoie village; ventral and dorsal views (copy from Stepanov 1948: pl. 7 fig. 12). Scale bar units = 1 mm.

opencc-by-4.0Nov 2024View details →
zenodo40/100

Fig. 4. Meristorygma donakovae Poletaev, 2018 in New and revised taxa of Carboniferous spiriferides (Brachiopoda, Spiriferida) from the Donets Basin (Ukraine) and South Urals (Russia)

Fig. 4. Meristorygma donakovae Poletaev, 2018 from South Urals (Russia). Mississippian. Holotype CNIGR Museum 12065/8 (Donakova 1983 Coll.) from Magnitogorsk District; ventral, dorsal, lateral and anterior views (copy from Poletaev 2018: pl. 112 fig. 3). Scale bar units = 1 mm.

opencc-by-4.0Nov 2024View details →
dryad32/100

Data from: Brachial supporting structure of Spiriferida (Brachiopoda)

<p>The filter-feeding organ of some extinct brachiopods is supported by a skeletal apparatus called the brachidium. Although relatively well-studied in Atrypida and Athyridida, the brachidial morphology is usually neglected in Spiriferida. To investigate the variations of brachidial morphology in Spiriferida, 65 species belonging to eight superfamilies were analyzed. Based on the presence/absence of the jugal processes and normal/modified primary lamellae of the spiralia, four types of brachidium are recognized. Type-I (with jugal processes) and Type-II (without jugal processes), both having normal primary lamellae, could give rise to each other by losing/re-evolving the jugal processes. Type-III, without jugal processes, originated from Type-II through the evolution of the modified lateral-convex primary lamellae, and it gave rise to Type-IV subsequently by evolving the modified medial-convex primary lamellae. Besides, the evolution of brachidia within individual evolutionary lineages must be clarified, as two or more types can be present within a single family. Type-III and Type-IV are closely associated with the prolongation of the crura, representing innovative modifications of the feeding apparatus in response to the probably shift in the position of the mouth towards the anterior, allowing for more efficient feeding on particles entering the mantle cavity from the anterior gape. Meanwhile, the modified primary lamellae adjusted/regulated the feeding currents. The absence of spires in some taxa with Type-IV brachidium might suggest that they developed a similar lophophore to that in some extant brachiopods, which can extend out of the shell.The filter-feeding organ of some extinct brachiopods is supported by a skeletal apparatus called the brachidium. Although relatively well-studied in Atrypida and Athyridida, the brachidial morphology is usually neglected in Spiriferida. To investigate the variations of brachidial morphology in Spiriferida, 65 species belonging to eight superfamilies were analyzed. Based on the presence/absence of the jugal processes and normal/modified primary lamellae of the spiralia, four types of brachidium are recognized. Type-I (with jugal processes) and Type-II (without jugal processes), both having normal primary lamellae, could give rise to each other by losing/re-evolving the jugal processes. Type-III, without jugal processes, originated from Type-II through the evolution of the modified lateral-convex primary lamellae, and it gave rise to Type-IV subsequently by evolving the modified medial-convex primary lamellae. Besides, the evolution of brachidia within individual evolutionary lineages must be clarified, as two or more types can be present within a single family. Type-III and Type-IV are closely associated with the prolongation of the crura, representing innovative modifications of the feeding apparatus in response to the probably shift in the position of the mouth towards the anterior, allowing for more efficient feeding on particles entering the mantle cavity from the anterior gape. Meanwhile, the modified primary lamellae adjusted/regulated the feeding currents. The absence of spires in some taxa with Type-IV brachidium might suggest that they developed a similar lophophore to that in some extant brachiopods, which can extend out of the shell.</p>

opencc-zeroNov 2020View details →
dryad32/100

Data from: Brachial supporting structure of Spiriferida (Brachiopoda)

Open the record for dataset details and reuse information.

publicNov 2020View details →
zenodo28/100

Fig. 2 in New and revised taxa of Carboniferous spiriferides (Brachiopoda, Spiriferida) from the Donets Basin (Ukraine) and South Urals (Russia)

Fig. 2. Geographical and stratigraphic location of the studied spiriferid-bearing localities (marked by asterisks) in Bashkortostan (Urals, Russia). A. Carboniferous stratigraphy of the South Urals (modified from Kulagina et al. 2009: fig. 2). B–D. Geographical location of the studied spiriferid-bearing localities: 3 = the Zilim River, Tash-Asty village; 4 = the Belaya River, Sterlitamak town, Tura Tau and the Yurak Tau Mounts; 5 = the Belaya River, Tabynskoie village, Voskresenka Mount; 6 = the Ural River, Magnitogorsk Region.

opencc-by-4.0Nov 2024View details →

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