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159 results for “limestone mountain”
Fig. 109 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 109. Paprothites kullmanni sp. nov. A. Holotype MB.C.5270 (Kullmann 1968 Coll.) from Oese. B. Paratype MB.C.31211 (Weyer 1993–1994 Coll.) from the Oberrödinghausen railway cutting, bed 3e. Scale bar units = 1 mm.
Fig. 107 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 107. Paprothites ruzhencevi Korn & Weyer, 2003, holotype MB.C.5240.6 (Trostheide Coll.) from Hasselbachtal, bed 57. Scale bar units = 1 mm.
Fig. 106 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 106. Paprothites from the Oberrödinghausen railway cutting.A. Paprothites raricostatus (Vöhringer, 1960), holotype GPIT-PV-63973 (Vöhringer Coll.) from bed 3d. B. Paprothites raricostatus (Vöhringer, 1960), specimen MB.C.31207 (Weyer 1993–1994 Coll.) from bed 3d1b. C. Paprothites beckeri sp. nov., holotype MB.C.31208 (Weyer 1993–1994 Coll.) from bed 3d1. Scale bar units = 1 mm.
Fig. 112. Pseudarietites westfalicus Schmidt, 1924 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 112. Pseudarietites westfalicus Schmidt, 1924 from the Oberrödinghausen railway cutting. A. Specimen MB.C.31214.1 (Weyer 1993–1994 Coll.) from bed 3a. B. Cross section of specimen GPIT- PV-63982 (Vöhringer Coll.) from bed 3c. C. Growth line course of specimen GPIT-PV-63980 (Vöhringer Coll.) from bed 3b, at dm = 24.5 mm, ww = 8.2 mm, wh = 8.2 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. 119 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 119. Eocanites nodosus (Schmidt, 1925) from the Oberrödinghausen railway cutting. A. Specimen GPIT-PV-63968 (Vöhringer Coll.) from bed 3d. B. Specimen GPIT-PV-63972 (Vöhringer Coll.) from bed 3d. C. Specimen MB.C.31234.1 (Weyer 1993–1994 Coll.) from bed 3d1b. D. Reproduction of the figure of "Gattendorfia nodosa" of Schmidt (1925, pl. 23 fig. 2). Scale bar units = 1 mm.
Fig. 116 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 116. Paralytoceras from the Oberrödinghausen railway cutting. A. Paralytoceras crispum (Tietze, 1870), specimen MB.C.31223 (Vöhringer Coll.) from bed 2. B. Paralytoceras sp. 1, specimen MB.C.31225 (Weyer 1993–1994 Coll.) from bed 3d1. C. Paralytoceras (?) sp. 2, specimen MB.C.31227 (Weyer 1993–1994 Coll.) from bed 3d1b. Scale bar units = 1 mm.
Fig. 108 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 108. Paprothites ruzhencevi Korn & Weyer, 2003 from the Oberrödinghausen railway cutting, both Weyer 1993–1994 Coll. A. Specimen MB.C.31209.1 from bed 3d1b. B. Specimen MB.C.31209.2 from bed 3d1b. Scale bar units = 1 mm.
Fig. 126 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 126. Eocanites delicatus sp. nov. from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-64008 (Vöhringer Coll.) from bed 2. B. Cross section of paratype GPIT-PV-63981 (Vöhringer Coll.) from bed 2. C. Suture line of paratype GPIT-PV-63999 (Vöhringer Coll.) from bed 2, at ww = 6.8 mm, wh = 6.5 mm. D. Growth line course of paratype GPIT-PV-64008 (Vöhringer Coll.) from bed 1, at dm = 43.0 mm, ww = 11.0 mm, wh = 13.5 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. 102 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 102. Hasselbachia erronea sp. nov., from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63927 (Vöhringer Coll.) from bed 5. B. Growth line and constriction course of holotype MB.C.31198 (Weyer 1993–1994 Coll.) from bed 3e, at dm = 16.0 mm, ww = 12.2 mm, wh = 7.3 mm. C. Suture line of paratype GPIT-PV-63927 from bed 5, at dm = 16.0 mm, ww = 12.0 mm, wh = 7.6 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. 125 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 125. Eocanites delicatus sp. nov. from the Oberrödinghausen railway cutting. A. Holotype GPIT- PV-63997 (Vöhringer Coll.) from bed 1. B. Paratype MB.C.31247.1 (Korn 1977 Coll.) from an unknown bed. Scale bar units = 1 mm.
Fig. 128 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 128. Nomismocanites raritas sp. nov., holotype MB.C.31253 (Weyer 1993–1994 Coll.) from the Oberrödinghausen railway cutting, bed 3d1. Scale bar units = 1 mm.
Fig. 96 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 96. Weyerella lenis sp. nov. from the Oberrödinghausen railway cutting. A. Holotype MB.C.31192 (Weyer 1993–1994 Coll.) from bed 2a. B. Cross section of paratype GPIT-PV-63929 (Vöhringer Coll.) from bed 2. 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 the holotype and the paratype. Scale bar units = 1 mm.
Fig. 95 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 95. Weyerella reticulum (Vöhringer, 1960) from the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Cross section of paratype GPIT-PV-63991 from bed 5. B. Suture line of paratype GPIT-PV-63975 from bed 5, at dm = 11.5 mm, ww = 6.5 mm, wh = 4.0 mm. C. Growth line course of holotype GPIT-PV-63974 from bed 6, at dm = 14.2 mm, ww = 7.2 mm, ww = 5.4 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. 97 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 97. Hasselbachia multisulcata (Vöhringer, 1960) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Paratype GPIT-PV-63913 from bed 4. B. Holotype GPIT-PV-63911 from bed 3e. Scale bar units = 1 mm.
Fig. 124 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 124. Eocanites supradevonicus (Schindewolf, 1926) from the Oberrödinghausen railway cutting, neotype MB.C.31246 (Weyer 1993–1994 Coll.) from bed 3b. Scale bar units = 1 mm.
Fig. 122 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 122. Eocanites brevis (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63987 (Vöhringer Coll.) from bed 3c. B. Growth line course of holotype GPIT-PV-63985 (Vöhringer Coll.) from bed 3c, at dm = 17.6 mm, ww = 4.2 mm, wh = 5.0 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. 118 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 118. Eocanites ruani (Bartzsch, Korn & Weyer, 2003) from the Oberrödinghausen railway cutting. A. Cross section of specimen GPIT-PV-63970 (Vöhringer Coll.) from bed 4 (after Vöhringer 1960). B. Growth line course of specimen MB.C.31229 (Weyer 1993–1994 Coll.) from bed 5a1, at ww = 9.7 mm, wh = 9.3 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. 115 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 115. Pseudarietitinae from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Rodingites planissimus (Vöhringer, 1960), holotype GPIT-PV-63962 from bed 3a. B. Rodingites carinatus (Vöhringer, 1960), holotype GPIT-PV-64011 from bed 3b. C. Pseudarietites serratus Vöhringer, 1960, holotype GPIT-PV-63964 from bed 1. Scale bar units = 1 mm.
Fig. 111. Pseudarietites westfalicus Schmidt, 1924 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 111. Pseudarietites westfalicus Schmidt, 1924 from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Specimen GPIT-PV-63978 from bed 3b. B. Specimen GPIT-PV-63980 from bed 3b. Scale bar units = 1 mm.
Fig. 121 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 121. Eocanites brevis (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Holotype GPIT-PV-63985 (Vöhringer Coll.) from bed 3c. B. Specimen MB.C.31238 (Weyer 1993–1994 Coll.) from bed 3c1. Scale bar units= 1 mm.
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