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159 results for “limestone mountain”
Fig. 80 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 80. Zadelsdorfia crassa (Schmidt, 1924), holotype BGRB X5714 (Schmidt 1920 Coll.) from the Oberrödinghausen railway cutting. Scale bar units = 1 mm.
Fig. 76 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 76. Gattendorfia costata Vöhringer, 1960 from the Oberrödinghausen railway cutting; photographs and dorsal view reconstruction of holotype GPIT-PV-63941 (Vöhringer Coll.) from bed 2. Scale bar units = 1 mm.
Fig. 58 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 58. Nicimitoceras trochiforme (Vöhringer, 1960) from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Cross section of specimen MB.C.31129 from bed 2. B. Cross section of paratype GPIT-PV-63851 from bed 3d. C. Cross section of paratype GPIT-PV-63992 from bed 2. D. Suture line of holotype GPIT-PV-63848 from bed 3c, at ww = 17.0 mm, wh = 21.5 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. 64 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 64. Nicimitoceras heterolobatum (Vöhringer, 1960) from the Oberrödinghausen railway cutting (narrowly umbilicate morphotype). A. Cross section of specimen MB.C.31140.1 from unknown bed. B. Cross section of specimen MB.C.31140.2 from unknown bed. C. Cross section of specimen MB.C.31142 from bed 3b. D. Cross section of specimen MB.C.31138.1 from bed 3c. E. Cross section of specimen MB.C.31134 from bed 1. F. Cross section of specimen MB.C.31138.2 from bed 3c. G. Cross section of specimen MB.C.31135.2 from bed 2. H. Cross section of paratype GPIT-PV-63898 from bed 3e. I. Suture line of paratype GPIT-PV-63898 from bed 3e, at dm = 9.5 mm, ww = 5.8 mm, wh = 5.6 mm. J–L. 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. 59 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 59. Nicimitoceras subacre (Vöhringer, 1960) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Paratype GPIT-PV-63853 (Vöhringer Coll.) from bed 3e. B. Holotype GPIT- PV-63854 (Vöhringer Coll.) from bed 3b/c. C. Specimen MB.C.31130.1 (Weyer 1993–1994 Coll.) from bed 3d1b. Scale bar units = 1 mm.
Fig. 53 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 53. Acutimitoceras ucatum sp. nov. from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63902 from bed 6. B. Suture line of paratype GPIT-PV-63899 from bed 5, at ww = 7.2 mm, wh = 8.5 mm. C. Growth line course of holotype GPIT-PV-63900 from bed 6, at ww = 7.3 mm, wh = 8.8 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. 75 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 75. Gattendorfia schmidti sp. nov. from the Oberrödinghausen railway cutting. A. Cross section of paratype MB.C.31156.1 (Vöhringer Coll.) from bed 2. B. Cross section of paratype MB.C.31157.2 (Vöhringer Coll.) from bed 3c. C. Suture line of holotype GPIT-PV-63952 (Vöhringer Coll.) from bed 1, at ww = 16.5 mm, wh = 9.5 mm. D. Constriction course of holotype GPIT-PV-63952 (Weyer 1993–1994 Coll.) from bed 1, at ww = 16.5 mm, wh = 9.5 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. 57 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 57. Nicimitoceras trochiforme (Vöhringer, 1960), holotype GPIT-PV-63848 (Vöhringer Coll.) from the Oberrödinghausen railway cutting, bed 3c. Scale bar units = 1 mm.
Fig. 51 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 51. Stockumites depressus (Vöhringer, 1960) from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Cross section of paratype GPIT-PV-63889 from bed 2. B. Cross section of paratype GPIT-PV-63887 from bed 2. C. Cross section of specimen MB.C.31119 from bed 2. D. Suture line of holotype GPIT-PV-63872 from bed 2, at dm = 23.0 mm, ww = 11.2 mm, wh = 7.5 mm. E. Growth line course of holotype GPIT-PV-63872 from bed 2, at dm = 23.0 mm, ww = 11.2 mm, wh = 7.5 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.
Fig. 50 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 50. Stockumites depressus (Vöhringer, 1960) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Paratype GPIT-PV-63886 from bed 3b. B. Holotype GPIT-PV-63872 from bed 2. Scale bar units= 1 mm.
Fig. 48 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 48. Stockumites similis (Vöhringer, 1960) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Paratype GPIT-PV-63874 from bed 1. B. Holotype GPIT-PV-63894 from bed 1. Scale bar units = 1 mm.
Fig. 49 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 49. Stockumites similis (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Cross section of specimen MB.C.31115 (Weyer 1993–1994 Coll.) from bed 2a. B. Cross section of paratype GPIT-PV-63878 (Vöhringer Coll.) from bed 1. C. Suture line of paratype GPIT-PV-63876 (Vöhringer Coll.) from bed 3c, at ww = 12.2 mm, wh = 9.5 mm. D. Constriction course of holotype GPIT-PV-63894 (Vöhringer Coll.) from bed 1, at ww =15.0 mm, wh = 13.0 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. 54 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 54. Acutimitoceras paracutum sp. nov. from the Oberrödinghausen railway cutting. A. Paratype MB.C.31126 (Korn 1989 Coll.) from bed 6a. B. Holotype MB.C.31127 (Weyer 1993–1994 Coll.) from bed 6a. Scale bar units = 1 mm.
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.
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International Brain Laboratory public data
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OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.