Find research datasets worth reusing
Search datasets from major research repositories and use ShareScore to quickly assess how well each record supports discovery, access, and reuse.
159
datasets available to search
ShareScore release 0.7.1
Dataset results
159 results for “limestone mountain”
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.
Fig. 23. Paragattendorfia sphaeroides Weyer, 1972 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 23. Paragattendorfia sphaeroides Weyer, 1972 from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63937 from bed 2. B. Cross section of paratype GPIT-PV-63935 from bed 2. C. Suture line of paratype GPIT-PV-63935 from bed 2, at ww = 13.2 mm, wh = 6.0 mm. D. Growth line course of holotype GPIT-PV-63909 from bed 3c, at dm = 22.0 mm, ww = 17.5 mm, wh = 11.5 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. 38 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 38. Stockumites undulatus (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Specimen MB.C.31091 (Weyer 1993–1994 Coll.) from bed 6a. B. Cross section of paratype GPIT- PV-63881 (Vöhringer Coll.) from bed 6. C. Suture line of paratype GPIT-PV-63879 (Vöhringer Coll.) from bed 6, at ww = 8.5 mm, wh = 7.6 mm. D. Growth line course of paratype GPIT-PV-63881 (Vöhringer Coll.) from bed 5, at dm = 9.5 mm, ww = 6.0 mm, wh = 5.5 mm. E. Growth line course of holotype GPIT- PV-63877 (Vöhringer Coll.) from bed 5, at dm = 16.3 mm, ww = 9.2 mm, wh = 9.0 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. 7 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 7. Early Tournaisian representative ammonoids of the family Prionoceratidae from the Hasselbachtal section, all Weyer 1993–1994 Coll. A. Mimimitoceras hoennense Korn, 1993, specimen MB.C.5241.2 from bed 59. B. Globimitoceras globiforme (Vöhringer, 1960), specimen MB.C.5240.7 from bed 57. C. Stockumites voehringeri sp. nov., paratype MB.C.5235.1 from bed 46. [Illustrated by Korn & Weyer (2003, pl. 1 figs 1–2) as Acutimitoceras cf. intermedium.] D. Stockumites intermedius (Schindewolf, 1923), specimen MB.C.5248.1 from bed 77. E. Stockumites convexus (Vöhringer, 1960), specimen MB.C.5241.1 from bed 59. F. Stockumites parallelus sp. nov., paratype MB.C.5247.2 from bed 57. (Illustrated by Korn & Weyer 2003: pl. 2 figs 6–7, as Acutimitoceras subbilobatum.) Scale bar units = 1 mm.
Fig. 8 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 8. Early Tournaisian representative ammonoids of the family Gattendorfiidae from the Hasselbachtal section, all Weyer 1993–1994 Coll. A. Gattendorfia rhenana sp. nov., paratype MB.C.5244.1 from bed 71. (Illustrated by Korn & Weyer 2003: pl. 2 figs 10–11, as Gattendorfia subinvoluta.) B. Weyerella molaris (Vöhringer, 1960), specimen MB.C.5240.8 from bed 57. C. Weyerella reticulum (Vöhringer, 1960), specimen MB.C.5242.1 from bed 62. D. Hasselbachia multisulcata (Vöhringer, 1960), specimen MB.C.5240.1 from bed 57. E. Hasselbachia gracilis (Vöhringer, 1960), specimen MB.C.5240.5 from bed 57. F. Pseudarietites westfalicus Schmidt, 1924, specimen MB.C.5236.1 from bed 49. Scale bar units = 1 mm.
Fig. 4 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 4. The lithological succession of the Hangenberg Limestone in the Oberrödinghausen railway cutting section with the occurrence of the ammonoid species of the families Gattendorfiidae Bartzsch & Weyer, 1987 and Prolecanitidae Hyatt, 1884. For explanation of the colours used, see Fig. 3.
Fig. 2 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 2. The Hangenberg Limestone at the western slope of the Oberrödinghausen railway cutting section (reproduced from Vöhringer 1960) and the lithological succession of the Hangenberg Limestone after Vöhringer and the field work by DW.
Fig. 5 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 5. Correlation of the ammonoid stratigraphy schemes of the Hangenberg Limestone and correlation to the conodont stratigraphy.
ScienceDex guides
Understand access before you commit
These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
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.