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594 results for “Carboniferous”
Fig. 47 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 47. Stockumites exilis (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63933 from bed 3d. B. Suture line of paratype GPIT-PV-64018 from bed 3c, at dm = 13.0 mm, ww = 8.1 mm, wh = 7.3 mm. C. Constriction course of paratype GPIT-PV-64018 from bed 3c, at dm = 9.5 mm, ww = 6.0 mm, wh = 5.5 mm. D. Constriction course of holotype GPIT-PV-63868 from bed 4, at dm = 15.6 mm, ww = 9.2 mm, wh = 8.3 mm. E–G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 82 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 82. Zadelsdorfia crassa (Schmidt, 1924), paratype GPIT-PV-63954 (Vöhringer Coll.) from the Oberrödinghausen railway cutting, bed 2. Photograph of the unwhitened specimen showing exemplary the often poorly preserved shell surface of the material from Oberrödinghausen. Scale bar units = 1 mm.
Fig. 72 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 72. Gattendorfia valdevoluta sp. nov. from the Oberrödinghausen railway cutting. A. Holotype MB.C.31155 (Weyer 1993–1994 Coll.) from bed 3d2. B. Paratype MB.C.31154 (Weyer 1993–1994 Coll.) from bed 2b. Scale bar units = 1 mm.
Fig. 88 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 88. Kazakhstania evoluta (Vöhringer, 1960from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63965 (Vöhringer Coll.) from bed 2. B. Suture line of holotype GPIT- PV-63963 (Vöhringer Coll.) from unknown bed, at ww = 5.8 mm, wh = 3.5 mm. C. Growth line course of holotype GPIT-PV-63963 (Vöhringer Coll.) from unknown bed, at ww = 8.0 mm, wh = 4.5 mm. D–F. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER). Scale bar units = 1 mm.
Fig. 62 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 62. Nicimitoceras heterolobatum (Vöhringer, 1960), holotype GPIT-PV-63893 (Vöhringer Coll.) from the Oberrödinghausen railway cutting, bed 3b/c. Scale bar units= 1 mm.
Fig. 84 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 84. Zadelsdorfia crassa (Schmidt, 1924) from the Oberrödinghausen railway cutting. A. Cross section of specimen GPIT-PV-63944 from bed 2. B. Cross section of specimen MB.C.5355 from bed 2. C. Suture line of specimen GPIT-PV-63955 from bed 2, at dm = 35.0 mm, ww = 23.5 mm, wh = 14.5 mm. D. Growth line course of specimen GPIT-PV-63953 from bed 2, at wh = 24.0 mm ww, wh = 16.0 mm. E–G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/ dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 46 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 46. Stockumites exilis (Vöhringer, 1960) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Holotype GPIT-PV-63868 from bed 4. B. Paratype GPIT-PV-64021 from bed 3c. Scale bar units = 1 mm.
Fig. 43 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 43. Stockumites voehringeri sp. nov. from the Oberrödinghausen railway cutting. A. Paratype MB.C.31107.1 (Weyer 1993–1994 Coll.) from bed 3b. B. Paratype MB.C.31111.1 (Weyer 1993–1994 Coll.) from bed 3d2b. C. Paratype MB.C.31101.1 (Korn 1977 Coll.) from unknown bed. D. Paratype MB.C.31101.2 (Korn 1977 Coll.) from unknown bed. E. Paratype MB.C.31105 (Korn 1977 Coll.) from unknown bed. F. Paratype MB.C.31109.1 (Weyer 1993–1994 Coll.) from bed 3d1. G. Paratype MB.C.31110.1 (Weyer 1993–1994 Coll.) from bed 3d1b. Scale bar units= 1 mm.
Fig. 40 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 40. Stockumites convexus (Vöhringer, 1960) from the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Cross section of paratype GPIT-PV-63906 from bed 6. B. Cross section of specimen MB.C.31094.1 from bed 6. C. Cross section of specimen MB.C.31094.2 from bed 6. D. Cross section of specimen MB.C.31093.1 from bed 5. E. Cross section of specimen MB.C.31092 from bed 4. F. Cross section of specimen MB.C.31094.3 from bed 6. G. Suture line of paratype GPIT-PV-63904 from bed 5, at ww = 7.5 mm, wh = 7.0 mm. H. Growth line course of holotype GPIT-PV-63903 from bed 6, at dm = 16.0 mm, ww ca. 9.0 mm, wh = 8.5 mm. I–K. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 39 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 39. Stockumites convexus (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Holotype GPIT-PV-63903 (Vöhringer Coll.) from bed 6. B. Paratype GPIT-PV-63905 (Vöhringer Coll.) from bed 5. C. Paratype GPIT-PV-63904 (Vöhringer Coll.) from bed 5. D. Specimen MB.C.31096 (Weyer 1993–1994 Coll.) from bed 6b2. Scale bar units = 1 mm.
Fig. 24 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 24. Kornia sphaeroidalis (Vöhringer, 1960) from the Oberrödinghausen railway cutting.A. Holotype GPIT-PV-63865 (Vöhringer Coll.) from bed 5. B. Constriction course of holotype GPIT-PV-63865 from bed 5, at dm = 22.0 mm, ww = 19.4 mm, wh = 12.0 mm. C. Paratype MB.C.31068 (Weyer 1993–1994 Coll.) from bed 5a1. Scale bar units= 1 mm.
Fig. 37 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 37. Stockumites undulatus (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Holotype GPIT-PV-63877 (Vöhringer Coll.) from bed 5. B. Paratype GPIT-PV-63879 (Vöhringer Coll.) from bed 6. Scale bar units = 1 mm.
Fig. 32 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 32. Stockumites intermedius (Schindewolf, 1923) from bed 6 of the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Cross section of specimen GPIT-PV-63875. B. Cross section of specimen MB.C.31079.1. C. Cross section of specimen MB.C.31079.2. D. Growth line course of specimen GPIT- PV-63875, at dm = 22.5 mm, ww = 16.6 mm, wh = 12.8 mm. E–G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Grey dots = representatives from bed 5. Scale bar units = 1 mm.
Fig. 33 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 33. Stockumites intermedius (Schindewolf, 1923) from bed 5 of the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Cross section of specimen MB.C.31078.1. B. Cross section of specimen MB.C.31078.2. C. Suture line of specimen GPIT-PV-64015, at dm = 28.2 mm, ww = 21.0 mm, wh = 14.8 mm. D. Growth line course of specimen GPIT-PV-63993, at ww = 22.0 mm, wh = 20.0 mm. E–G. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/ dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Grey dots = representatives from bed 6. Scale bar units = 1 mm.
Fig. 28 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 28. Kornia acia sp. nov. from Oberrödinghausen railway cutting; both Weyer 1993–1994 Coll. A. Cross section of paratype MB.C.31072 from an unknown bed. B. Growth line course of holotype MB.C.31073.1 (Weyer 1993–1994 Coll.) from bed 5a2, at dm= 11.1 mm, ww = 11.6 mm, wh = 5.3 mm. C–E. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/ dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 21 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 21. Paragattendorfia patens (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63916 from bed 2. B. Suture line of holotype GPIT-PV-63912 from bed 2, at ww = 12.4 mm, wh = 6.5 mm. D–F. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
Fig. 18 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 18. Globimitoceras globiforme (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Paratype GPIT-PV-63921 (Vöhringer Coll.) from bed 3b. B. Specimen MB.C.31061 (Korn 1977 Coll.) from float material. C. Holotype GPIT-PV-63925 (Vöhringer Coll.) from bed 2. D. Specimen MB.C.31065 (Weyer 1993–1994 Coll.) from bed 3e. Scale bar units = 1 mm.
Fig. 13 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 13. Mimimitoceras perditum sp. nov., paratype GPIT-PV-63873 (Vöhringer Coll.) from the Oberrödinghausen railway cutting, bed 1. Photograph of the unwhitened specimen showing exemplary the often poorly preserved shell surface of the material from Oberrödinghausen. Scale bar units = 1 mm.
Fig. 12 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 12. Mimimitoceras perditum sp. nov., from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Holotype GPIT-PV-63861 from bed 2. B. Paratype GPIT-PV-63864 from bed 2. Scale bar units = 1 mm.
Fig. 41 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 41. Stockumites antecedens (Vöhringer, 1960) from the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Dorsal view reconstruction and photographs of holotype GPIT-PV-63907 from bed 5. B. Cross section of paratype GPIT-PV-63910 from bed 5. C. Cross section of paratype GPIT- PV-63908 from bed 3d. D. Suture line of paratype GPIT-PV-63910 from bed 5, at dm = 14.5 mm, ww = 7.7 mm, wh = 7.5 mm. E. Growth line course of holotype GPIT-PV-63907 from bed 5, at dm = 16.0 mm, ww = 9.0 mm, wh = 8.5 mm. F –H. Ontogenetic development of the conch width index (ww/dm), umbilical width index (uw/dm), whorl width index (ww/wh) and whorl expansion rate (WER) of selected specimens. Scale bar units = 1 mm.
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Allen Brain Atlas
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International Brain Laboratory public data
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OpenNeuro
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