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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.
Fig. 3 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 3. The lithological succession of the Hangenberg Limestone in the Oberrödinghausen railway cutting section with the occurrence of the ammonoid species of the family Prionoceratidae Hyatt, 1884 and the ammonoid zonation.
Fig. 27 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 27. Kornia acia sp. nov. from the Oberrödinghausen railway cutting; holotype MB.C.31073.1 (Weyer 1993–1994 Coll.) from bed 5a2. Scale bar units = 1 mm.
Fig. 30 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 30. Stockumites kleinerae (Korn, 1984) from the Oberrödinghausen railway cutting. A. Cross section of specimen GPIT-PV-63879 from bed 5. B. Cross section of specimen MB.C.31075.1 from bed 5. C. Suture line of specimen GPIT-PV-64016 from bed 5, at ww = 10.5 mm. D. Growth line course of specimen GPIT-PV-64004 from bed 6, at dm = 23.0 mm, ww = 19.4 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. Scale bar units = 1 mm.
Fig. 42 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 42. Stockumites voehringeri sp. nov. from the Oberrödinghausen railway cutting; all Vöhringer Coll. A. Holotype GPIT-PV-63995 from unknown bed. B. Paratype GPIT-PV-63885 from bed 3b. C. Paratype GPIT-PV-64005 from bed 2. D. Paratype GPIT-PV-63850 from bed 3e. Scale bar units = 1 mm.
Fig. 35 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 35. Stockumites parallelus sp. nov. from the Oberrödinghausen railway cutting and the Oese section. A. Paratype MB.C.31087 (Weyer 1993–1994 Coll.) from bed 6b of Oberrödinghausen; dorsal reconstruction and lateral view. B. Cross section of paratype GPIT-PV-63890 from bed 5 of Oberrödinghausen. C. Cross section of paratype SMF 43081 (Korn 1982 Coll.) from the Stockum Limestone at Stockum (from Korn 1984). D. Cross section of paratype MB.C.5292 from the lower part of the Hangenberg Limestone at Oese (from Korn & Weyer 2003). 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 = specimens from the type locality Stockum). Scale bar units = 1 mm.
Fig. 22. Paragattendorfia sphaeroides Weyer, 1972 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 22. Paragattendorfia sphaeroides Weyer, 1972, from the Oberrödinghausen railway cutting, (Vöhringer Coll.), holotype GPIT-PV-63909 from bed 3c. Scale bar units = 1 mm.
Fig. 14 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 14. Mimimitoceras perditum sp. nov. from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Cross section of paratype MB.C.31054.1 from an unknown bed. B. Cross section of paratype MB.C.31052.1 from bed 2. C. Cross section of paratype MB.C.31052.2 from bed 2. D. Cross section of paratype MB.C.31054.2 from an unknown bed. E. Cross section of paratype MB.C.31052.3 from bed 2. F. Suture line of paratype GPIT-PV-64013 from bed 1, at dm = 25.0 mm, ww = 16.5 mm, wh = 13.0 mm. G. Growth line course of paratype GPIT-PV-63862 from bed 5, at ww = 26.0 mm, wh = 25.5 mm. H–J. 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. 17. Mimimitoceras hoennense Korn, 1994 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 17. Mimimitoceras hoennense Korn, 1994 from the Oberrödinghausen railway cutting, all Vöhringer Coll. A. Cross section of paratype GPIT-PV-63867 from bed 3d. B. Suture line of paratype GPIT-PV-63866 from bed 4, at ww = 13.5 mm, wh = 12.0 mm. C. Growth line course of specimen GPIT- PV-63884 from bed 5, at dm = 28.5 mm, ww ~ 15.0 mm, wh = 14.6 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. 29 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 29. Stockumites kleinerae (Korn, 1984) from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Specimen GPIT-PV-63880 from bed 5. B. Specimen GPIT-PV-64004 from bed 6. Scale bar units = 1 mm.
Fig. 16. Mimimitoceras hoennense Korn, 1993 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 16. Mimimitoceras hoennense Korn, 1993 from the Oberrödinghausen railway cutting, both Vöhringer Coll. A. Holotype GPIT-PV-63884 from bed 2. B. Paratype GPIT-PV-63866 from bed 2. Scale bar units = 1 mm.
Fig. 34 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 34. Stockumites intermedius (Schindewolf, 1923) from bed 5 of the Oberrödinghausen railway cutting. A. Cross section of specimen MB.C.31078.3 (Vöhringer Coll.). B. Cross section of specimen MB.C.31080.1 (Weyer 1993–1994 Coll.) from bed 5a2. C. Cross section of specimen GPIT-PV-64000 (Vöhringer Coll.). D. Cross section of specimen MB.C.31078.4 (Vöhringer Coll.) from bed 5. E. Cross section of specimen GPIT-PV-63860 (Vöhringer Coll.). Scale bar units = 1 mm.
Fig. 20 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 20. Paragattendorfia patens (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Holotype GPIT-PV-63912 (Vöhringer Coll.) from bed 2. B. Paratype GPIT-PV-63914 (Vöhringer Coll.) from bed 2. C. Specimen MB.C.31067 (Weyer 1993–1994 Coll.) from bed 3d2. Scale bar units = 1 mm.
Fig. 1 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 1. The geographic position of the Oberrödinghausen railway cutting section and other Devonian–Carboniferous boundary sections at the northern margin of the Rhenish Mountains east of the Rhine. Abbreviations: APR = Apricke; DRE = Drewer; EFF = Effenberg; HAS = Hasselbachtal; KAT = Kattensiepen; MÜS = Müssenberg; OES = Oese; O-R = Oberrödinghausen; STO = Stockum; WOC = Wocklum.
Fig. 19 in The ammonoids from the Gattendorfia Limestone of Oberrödinghausen (Early Carboniferous; Rhenish Mountains, Germany)
Fig. 19. Globimitoceras globiforme (Vöhringer, 1960) from the Oberrödinghausen railway cutting. A. Cross section of paratype GPIT-PV-63923 from bed 2. B. Cross section of paratype GPIT-PV-63934 from bed 3e. C. Suture line of holotype GPIT-PV-63925 from bed 2, at ww = 20.5 mm, wh = 9.4 mm. D. Constriction course of specimen MB.C.31061, at dm = 32.5 mm, ww = 30.0 mm, wh =18.5 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.
Data set for the ensemble postprocessing of 2m surface temperature forecasts in Germany for five different lead times
<p>Full data set for the ensemble postprocessing of 2m surface temperature forecasts at 462 observation stations in Germany for the lead times 24, 48, 72, 96 and 120 hours in the years 2015-2020. The data set is provided in .RData format supported by the statistical software <a href="https://www.r-project.org">R</a>. The ensemble forecasts are retrieved from <a href="https://www.ecmwf.int">ECMWF</a> and the observation data from the <a href="https://opendata.dwd.de/climate_environment/CDC/observations_germany/climate/hourly/air_temperature/historical/BESCHREIBUNG_obsgermany_climate_hourly_tu_historical_de.pdf">German Weather Service</a> (<a href="https://www.dwd.de/">DWD</a>). <br> <br> For more information about the data set see: <a href="https://github.com/jobstdavid/paper_tsEMOS">https://github.com/jobstdavid/paper_tsEMOS</a></p>
Whole-genome sequences of Cercospora beticola isolates from Germany and Italy.
<p>Sequences used in the manuscript <strong>"Large-scale analyses reveal the contribution of adaptive evolution in pathogenic and non-pathogenic fungal species"</strong></p>
Spatiotemporally independent heavy precipitation events for the state of Hesse (Germany)
<p>This data set contains a collection of spatiotemporally independent convective precipitation objects for the German state of Hessen. The data set was generated on the basis of the <em>RADKLIM‑YW Version 2017.002 (</em>https://doi.org/10.5676/DWD/RADKLIM_YW_V2017.002) radar precipitation data of the German Weather Service (DWD). It is grouped into precipitation duration stages of 15, 30, 45, 60, 75 and 90 minutes as well as a spatial aggregation of 9 and 25 grid cells. This results in 12 separate event lists. </p>
Fig. 14 in The first dsungaripterid pterosaur from the Kimmeridgian of Germany and the biomechanics of pterosaur long bones
Fig. 14. Mechanical properties in bending by variation of R/t. Solid bone with R/t−value of 1 is defined as 1. Level of dsungaripterid R/t−value dashed. After Currey (1984).
Fig. 3 in The first dsungaripterid pterosaur from the Kimmeridgian of Germany and the biomechanics of pterosaur long bones
Fig. 3. Dsungaripteridae gen. et sp. indet., DFMMh/FV 500. A. Left lateral view of pelvis. B. Interpretative drawing. Scale bar 10 mm.
ScienceDex guides
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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.