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140 results for “Brachiopoda”
Figure 5 in Checklist of the phyla Platyhelminthes, Xenacoelomorpha, Nematoda, Acanthocephala, Myxozoa, Tardigrada, Cephalorhyncha, Nemertea, Echiura, Brachiopoda, Phoronida, Chaetognatha, and Chordata (Tunicata, Cephalochordata,
Figure 5. The distribution of the number of Appendicularia (Tunicata) species along the coasts of Turkey. Each grid has a dimension of 15 × 15 km.
Figure 2 in Checklist of the phyla Platyhelminthes, Xenacoelomorpha, Nematoda, Acanthocephala, Myxozoa, Tardigrada, Cephalorhyncha, Nemertea, Echiura, Brachiopoda, Phoronida, Chaetognatha, and Chordata (Tunicata, Cephalochordata,
Figure 2. The number of species of the phyla Platyhelminthes (PLA), Chordata (Tunicata, Cephalochordata, and Hemichordata) (CHO), Nemertea (NEM), Nematoda (NMT), Xenacoelomorpha (XEN), Chaetognatha (CHA), Acanthocephala (ACA), and others (OTH, including Echiura, Myxozoa, Brachiopoda, Cephalorhyncha, Tardigrada, and Phoronida) along the coasts of Turkey. ∑S indicates the total number of species.
Linked collectors and determiners for: Naturalis Biodiversity Center (NL) - Brachiopoda.
Natural history specimen data linked to collectors and determiners held within, "Naturalis Biodiversity Center (NL) - Brachiopoda". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/e66ff065-d823-4a4d-b129-569f649ba0eb">https://bionomia.net/dataset/e66ff065-d823-4a4d-b129-569f649ba0eb</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/e66ff065-d823-4a4d-b129-569f649ba0eb">https://gbif.org/dataset/e66ff065-d823-4a4d-b129-569f649ba0eb</a>. Formatted as a Frictionless Data package.
Linked collectors and determiners for: RBINS Brachiopoda collection.
Natural history specimen data linked to collectors and determiners held within, "RBINS Brachiopoda collection". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/7c4621d3-7b86-4c99-a14e-ff8b3fce5c10">https://bionomia.net/dataset/7c4621d3-7b86-4c99-a14e-ff8b3fce5c10</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/7c4621d3-7b86-4c99-a14e-ff8b3fce5c10">https://gbif.org/dataset/7c4621d3-7b86-4c99-a14e-ff8b3fce5c10</a>. Formatted as a Frictionless Data package.
Linked collectors and determiners for: Bryozoa, Brachiopoda and Entoprocta (TSZBr) The Arctic University Museum of Norway.
Natural history specimen data linked to collectors and determiners held within, "Bryozoa, Brachiopoda and Entoprocta (TSZBr) The Arctic University Museum of Norway". Claims or attributions were made on Bionomia by volunteer Scribes, <a href="https://bionomia.net/dataset/e92bb2ed-1efe-4d2a-a17d-52182c562db8">https://bionomia.net/dataset/e92bb2ed-1efe-4d2a-a17d-52182c562db8</a> using specimen data from the dataset aggregated by the Global Biodiversity Information Facility, <a href="https://gbif.org/dataset/e92bb2ed-1efe-4d2a-a17d-52182c562db8">https://gbif.org/dataset/e92bb2ed-1efe-4d2a-a17d-52182c562db8</a>. Formatted as a Frictionless Data package.
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.
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).
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.
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.
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.
Fig. 7. A in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 7. A. Slab of juvenile specimens of Coenothyris. Note rare disarticulated ventral valve with small hinge teeth (arrow). Subunit 31, AMNH 46519. B. Cross section of Coenothyris Bed showing sparfilled articulated shells (bottom half) indicative of rapid burial that did not allow for the decay of soft tissues with subsequent displacement by sediment. The brachiopods just above the sparfilled zone (upper half) are mud filled, indicative of individuals that had died earlier and decayed to become infilled with sediment; approximately 25% of the shells were spar filled. Subunit 31, AMNH 46520. C. Cross section of Coenothyris Bed showing bivalve hash (composed mainly of the bivalve Myophoria) that served as a pavement for brachiopod spat. Subunit 31, AMNH 46521. Scale bar 5 2 cm.
Fig. 6. A, B in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 6. A, B. Slabs with normal populations of Coenothyris that range from ephebic to gerontic shells. A, Subunit 42, AMNH 46522; B, Subunit 42, NHM 1008. C. Cross section of Coenothyris horizon consisting of jumbled adult specimens similar in appearance to the Triassic German Muschelkalk. Subunit 42, AMNH 46522. Scale bar 5 2 cm.
Fig. 4 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 4. Slab of juvenile specimens of Coenothyris that represents an obrution deposit. Note brachiopods in a horizontal to subhorizontal attitude relative to the sediment–water interface, many in dorsal side up position. Large bivalves under the brachiopods are Pleuromya. Subunit 31, AMNH 46518. See text for further discussion.
Fig. 1 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 1. Location map of Precambrian–Oxfordian exposures in the Levant. 1, Precambrian; 2, Paleozoic–Triassic; 3, Jurassic; 4, Mount Hermon; 5, Alpine thrustfront; 6, 7, Neogene sinistral transform; I, Galilee High; II, Judean Embayment; III, Negev High; IV, Sinai Deep; with extension of Lower Oxfordian Majdal Shams shales (shaded area) and Jurassic isopachs (from Hirsch et al., 1998). ''Ramon'' signifies the Triassic Ramon Group, an anticlinorium that was breached through several phases of erosion, beginning in the Late Tertiary (Miocene–Pliocene), resulting in erosional cirques (Parnes, 1986). Tectonic movements since the Late Mesozoic, including reactivation of faults, resulted in the development of WSW–ENE to S–Ntrending reverse and thrust faults that today consist of several secondary monoclinal and domal buckles with an associated fault system (Zak, 1963).
Fig. 3 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 3. Slab showing bivalve pavement colonized by Coenothyris oweni Feldman, subunit 31, AMNH 46517. Abbreviations: co, Coenothyris; pl, Pleuromya; mo, Modiolus; my, Myophoria; pa, Parallelodon. Note that this slab has relatively few brachiopods (compare with fig. 4). Scale bar 5 4 cm.
Fig. 5 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 5. Slab of juvenile specimens of Coenothyris. Note the large Pleuromya, just offcenter, under which lie disarticulated Myphoria. Some shells are slightly exfoliated, but most are almost perfectly preserved. Subunit 31, AMNH 46524. See text for further discussion.
Fig. 2 in Paleoecology, Taphonomy, and Biogeography of a Coenothyris Community (Brachiopoda, Terebratulida) from the Triassic (Upper Anisian-Lower Ladinian) of Israel
Fig. 2. Generalized columnar section of the Triassic Saharonim Formation at Har Gevanim, Makhtesh Ramon, southern Israel. For detailed stratigraphy, see Druckman (1974b). Arrows represent occurrences of Coenothyris oweni Feldman at marked subunit intervals. Subunit designations are after Zak (1964) in Parnes (1975).
FIG. 1 in Dignomia munsterii (Brachiopoda, Lingulata) from the Ordovician of Bolivia, with redescription of the genus
FIG. 1. — Maps of Bolivia showing the distribution of the Ordovician (from Pareja & Ballon 1978).
FIG. 3 in Dignomia munsterii (Brachiopoda, Lingulata) from the Ordovician of Bolivia, with redescription of the genus
FIG. 3. — Dignomia munsterii: A, B, ventral valves; A, internal face; B, C, external faces; D-F, dorsal valves; D, internal face; E, F, external faces. Scale bars: 2 mm.
Text-fig. 2. (A) Orientation of Schizocrania filosa (HALL, 1847) on articulated shells of benthic brachiopod Rafinesquina sp. (A1–A3 – on dorsal valve of articulated shells, A4 – on ventral valve of articulated shell; forward growth direction is unclear in three specimens) from Upper Ordovician, Corryville Formation, Lawrenceburg, Indiana (after www.drydredgers.org/scizo.htm). (B) Orientation of Schizocrania multistriata (REED, 1905) shells on outer face of conulariid Metaconularia imperialis test (Dobrotivá Formation, Kařízek mine, Barrandian area; after Havlíček and Vaněk 1996); preserved conulariid shell in white, suggested outline of incomplete conulariid test in grey. Arrows indicate direction of forward growth of Schizocrania specimens. in Schizocrania (Brachiopoda, Discinoidea): Taxonomy, Occurrence, Ecology And History Of The Earliest Epizoan Lingulate Brachiopod
Text-fig. 2. (A) Orientation of Schizocrania filosa (HALL, 1847) on articulated shells of benthic brachiopod Rafinesquina sp. (A1–A3 – on dorsal valve of articulated shells, A4 – on ventral valve of articulated shell; forward growth direction is unclear in three specimens) from Upper Ordovician, Corryville Formation, Lawrenceburg, Indiana (after www.drydredgers.org/scizo.htm). (B) Orientation of Schizocrania multistriata (REED, 1905) shells on outer face of conulariid Metaconularia imperialis test (Dobrotivá Formation, Kařízek mine, Barrandian area; after Havlíček and Vaněk 1996); preserved conulariid shell in white, suggested outline of incomplete conulariid test in grey. Arrows indicate direction of forward growth of Schizocrania specimens.
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