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opencc-by-4.0Mar 2022View details →

Dataset of the determination of the topographic spatial resolution of a confocal point sensor with a type ASG material measure

These original measurement data relate to the publication: J. Schaude, A. C. Gröschl, T. Hausotte: Effect of a Misidentified Centre of a Type ASG Material Measure on the Determined Topographic Spatial Resolution of an Optical Point Sensor, Metrology 2(1), p. 19-32, 2022, <a href="https://doi.org/10.3390/metrology2010002">https://doi.org/10.3390/metrology2010002</a>. Please refer to this open access publication for a detailed description of the measurement setup and procedure. All data are in ASCII-format. Each file contains four columns, where column one to three are the x, y, and z-coordinates of the positioning system and column four is the signal of the photodetector. Content of the folders 10_Plane: Axial probings on 18 points just outside the grooves. 20_Edges: Lateral probings from each point just outside the grooves in the direction of the roughly determined centre of the material measure. 30_PlaneArea: Repeated axial probing on a plane area near the material measure. 40_RadialMeasurement: Radial measurement of the material measure by lateral (radial) probings conducted on different heights (referring to the distance to the plane fitted to the measuring points of 10_Plane), and radii (referring to the centre of the circle fitted to the edges determined in 20_Edges). Each radial probing has its own data file, with the name of the data file being “radial_probing {radius in m} {height in m} {data and time of probing}.txt”. 50_LineMeasurement: Lateral probings conducted on different heights (referring to the distance to the plane fitted to the measuring points of 10_Plane), different lateral offsets (referring to the centre of the circle fitted to the edges determined in 20_Edges) and on two angles (on the groove (0°) and the adjacent top level (10°)). Please refer to sec. 5.2 of the aforementioned publication for a detailed description. Each lateral probing has its own data file, with the name of the file being “lateral probing {angle in °} {offset in m} {height in m} {data and time of probing}.txt”. Acknowledgement This project 20IND07 TracOptic has received funding from the EMPIR programme co-financed by the Participating States and from the European Union’s Horizon 2020 research and innovation programme. Funder name: European Metrology Programme for Innovation and Research (EMPIR); Funder ID: 10.13039/10001413

opencc-by-4.0Aug 2022View details →

Text-fig. 5. Mastixiopsis nyssoides KIRCHH. a, b, g–n: Organic preservation. a, b: Lignitic, unpermineralized, early Eocene Dorset Pipe clays at Arne, V. 40762. a: Ventral view (original illustration from pl. 18, fig. 1 of Chandler 1962). b: Transverse fracture, somewhat distorted by compression. c–f: Pyrite permineralization. c: Ventral view, V. 22963(1) from Sheppey, originally listed as Mastixia cantiensis. d: Lateral view, V. 22969 from Sheppey (identified as Mastixia grandis by Reid and Chandler 1933: pl. 25, fig. 8). e: Equatorial transverse physical section from (c). f: Equatorial transverse physical section from (d). g: Detail of pericarp from (e), showing endocarp formed of dense fibrous tissue, surrounded by mesocarp of anticlinally oriented larger cells. h: Detail of pericarp from (f). i–n: Type material from Eocene of Riestadt, Germany, MNB. i: Ventral view. j, k: Ventral and apical views of holotype. l: View of the transversely fractured surface from (j) showing horseshoe shaped locule. m: Equatorial transverse physical cut of the specimen in (i); note yellow resin cavity (arrow). n: Scanning electron microscopy of pericarp from (l) with locule lining at lower edge of image. Note dense endocarp tissue composed of small cells (fibres and sclereids), extending about 3/5 of distance to periphery, surrounded by mesocarp of larger, anticlinally oriented cells. Scale bars 1 cm in (a–f), (i–k), 1 mm in (g), 2 mm in (h), 3 mm in (l), m, 250 Μm in (n). Bar in (d) applies also to (c). Bar in (l) also applies to (m). Bar in (i) also applies to (j) and (k). in Mastixioid Fruits (Cornales) From The Early Eocene London Clay Flora: Morphology, Anatomy And Nomenclatural Revision

Text-fig. 5. Mastixiopsis nyssoides KIRCHH. a, b, g–n: Organic preservation. a, b: Lignitic, unpermineralized, early Eocene Dorset Pipe clays at Arne, V. 40762. a: Ventral view (original illustration from pl. 18, fig. 1 of Chandler 1962). b: Transverse fracture, somewhat distorted by compression. c–f: Pyrite permineralization. c: Ventral view, V. 22963(1) from Sheppey, originally listed as Mastixia cantiensis. d: Lateral view, V. 22969 from Sheppey (identified as Mastixia grandis by Reid and Chandler 1933: pl. 25, fig. 8). e: Equatorial transverse physical section from (c). f: Equatorial transverse physical section from (d). g: Detail of pericarp from (e), showing endocarp formed of dense fibrous tissue, surrounded by mesocarp of anticlinally oriented larger cells. h: Detail of pericarp from (f). i–n: Type material from Eocene of Riestadt, Germany, MNB. i: Ventral view. j, k: Ventral and apical views of holotype. l: View of the transversely fractured surface from (j) showing horseshoe shaped locule. m: Equatorial transverse physical cut of the specimen in (i); note yellow resin cavity (arrow). n: Scanning electron microscopy of pericarp from (l) with locule lining at lower edge of image. Note dense endocarp tissue composed of small cells (fibres and sclereids), extending about 3/5 of distance to periphery, surrounded by mesocarp of larger, anticlinally oriented cells. Scale bars 1 cm in (a–f), (i–k), 1 mm in (g), 2 mm in (h), 3 mm in (l), m, 250 Μm in (n). Bar in (d) applies also to (c). Bar in (l) also applies to (m). Bar in (i) also applies to (j) and (k).

opencc-by-4.0May 2024View details →

Role of bark beetle disturbance and fuel types on fire radiative power and burn severity in the Bohemian-Saxon Switzerland - Data and Material.

This data repository includes different datasets for fuel types, burn severity, fire radiative power and burned area, which were analysed and used in our paper on the Role of bark beetle disturbance and fuel types on fire radiative power and burn severity in the Bohemian-Saxon Switzerland. Study area: National Park Bohemian and Saxon Switzerland and conservation areas, Germany and Czech Republic. Burn severity: dnbr_fire22.nc – Burn severity data covering the burned area, which has been calculated with the Difference Normalized Burn Index (dNBR) using Sentinel-2 and Landsat 8, 9 images. Remote sensing images were reprojected and resampled to 10 m to ensure harmonization before index calculation. cbi.csv – Burn severity surveyed in the field in autumn 2022 as validation data for the dNBR. Contains: ID, coordinates, CBI, CBI values separated for different strata (A to E) and individual strata variables, forest type and species for intermediate trees (strata D) and tall trees (strata E), and the dNBR value that covered the plot extent. Burned area: burned_area.shp – Burned area was mapped by rangers in the Saxon Switzerland National Park and was taken from the dataset provided by the Copernicus Emergency Management Service (EMS) for the Bohemian Switzerland National Park. FRP: frp.nc - Fire Radiative Power gridded to 300 m and clipped to the burned area. FRP during the main fire spread 24/07/22 - 29/07/22.  Fuel: fueltype_bohemiansaxonswitzerland.nc/fueltype_bohemiansaxonswitzerland_postfire.nc – Raster datasets (10m spatial resolution, EPSG:32633) of fuels present in the area before and after the fire. The fuel classification system can be found in the fuel_classification.xlsx. fuel_classification.xlsx – The fuel type classification system for the study area. Fuel type ID's as seen in fueltype_bohemiansaxonswitzerland.nc (pre- and postfire).

Рис. 1. ВоЗмоЖный синтип Mactra sulcataria Deshayes in Reeve, 1854 иЗ коллекции МуЗеЯ естественной истории, Лондон (коллекциЯ Х. Каминга), регистрационный номер № NHMUK 20130005. Рисунок Этого ЭкЗемплЯра опубликован Л. Ривом [Reeve, 1854, pl. 2, fig. 5]; воспроиЗведен в настоЯЩей статье (рис. 2А). in Notes on type material of Mactra sulcataria Deshayes in Reeve, 1854 (Bivalvia: Mactridae) and taxonomic history of the species

Рис. 1. ВоЗмоЖный синтип Mactra sulcataria Deshayes in Reeve, 1854 иЗ коллекции МуЗеЯ естественной истории, Лондон (коллекциЯ Х. Каминга), регистрационный номер № NHMUK 20130005. Рисунок Этого ЭкЗемплЯра опубликован Л. Ривом [Reeve, 1854, pl. 2, fig. 5]; воспроиЗведен в настоЯЩей статье (рис. 2А).

Fig. 2 in Notes on type material of Mactra sulcataria Deshayes in Reeve, 1854 (Bivalvia: Mactridae) and taxonomic history of the species

Fig. 2. Illustrations of Mactra sulcataria Deshayes in Reeve, 1854 in monographs of the 19th century: A – Reeve [1854, pl. 2, fig. 5]; B – Weinkauff [1881, Taf. 18, Fig. 3]; in references as: Küster, Weinkauff [1841–1884].

Рис. 3. ОписаниЯ Mactra sulcataria Deshayes in Reeve, 1854 в статье Ж.П. ДехЭ [Deshayes, 1854, p. 15] (вверху) и монографии Л. Рива [Reeve, 1854, species 5] (вниЗу). in Notes on type material of Mactra sulcataria Deshayes in Reeve, 1854 (Bivalvia: Mactridae) and taxonomic history of the species

Рис. 3. ОписаниЯ Mactra sulcataria Deshayes in Reeve, 1854 в статье Ж.П. ДехЭ [Deshayes, 1854, p. 15] (вверху) и монографии Л. Рива [Reeve, 1854, species 5] (вниЗу).

FIG. 7 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 7. — Batrachopus deweyi (Hitchcock, 1843) Hitchcock, 1845: A-C, trackway ULB-04C10_E, photograph (A), DEM and false-colour depth map (B) and interpretative sketch (C); D-F, pes/manus set 04C10_A_1 (holotype of "B. gilberti" that is here invalidated), photograph (D), DEM and false-colour depth map (E) and interpretative sketch (F); G-I, pes/manus set 04C14_C, photograph (G), DEM and false-colour depth map (H) and interpretative sketch (I); J-L, pes/manus set 04C14_C, photograph (J), DEM and false-colour depth map (K) and interpretative sketch (L). Scale bars represent: A-C, 10 cm; D-L, 1 cm.

FIG. 8 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 8. — Tracks ascribed to Dahutherium sp. by Lapparent & Montenat (1967) and that are here reinterpreted: A-C, two superimposed tridactyl grallatorid footprints, ULB-04C18_B, photograph (A), interpretative sketch of Lapparent & Montenat (1967) (B), and our interpretation (C), showing a small footprint (dark grey) and larger footprint (light grey); D-F, Batrachopus isp., ULB-04C15_A, photograph (D), interpretative sketch of Lapparent & Montenat (1967) (E), and our interpretation (F). Scale bars: A-C, 5 cm; D-F, 2 cm.

FIG. 11 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 11. — Plaster cast of one footprint from the type trackway of "Saltopoides igalensis", that is here invalidated: A-C, track ULB-04C01_B, photograph (A), DEM and false-colour depth map (B) and interpretative sketch (C). Scale bars: 5 cm.

FIG. 3 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 3. — Grallator olonensis Lapparent & Montenat, 1967: A, B, slab ULB-04D19 bearing the trackway T1-Go, as well as T2-Go; photograph (A) and interpretative sketch (B); C-E, track 04D19_A_4 (syntype) of the trackway T1-Go, photograph (C), DEM and false-colour depth map (D) and interpretative sketch (E); F-H, ULB- 04C11_A_6, photograph (F), DEM and false-colour depth map (G) and interpretative sketch (H). Scale bars: A, B, 20 cm; C-H, 2 cm.

FIG. 6 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 6. — "Anatopus palmatus" Lapparent & Montenat, 1967, that is here invalidated: A-C, ULB-04C15_B (holotype of "A. palmatus"), photograph (A), interpretative sketch of Lapparent & Montenat (1967: fig. 16A and pl.XII.3) (B), and our interpretation (C); D-F, ULB-04C15_C, photograph (D), interpretative sketch of Lapparent & Montenat (1967: fig. 16B1) (E), and our interpretation (F). Scale bars: 5 cm.

FIG. 13 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 13. — Other problematic tracks in Lapparent & Montenat 1967: A-C, Batrachopus isp., ULB-04C14_I, photograph (A), interpretative sketch of Lapparent & Montenat (1967) (B) ("Unnamed track n°1" in Lapparent & Montenat 1967: fig. 18), and our interpretation (C); D-F, Grallator cf. variabilis, ULB-04D22_A, photograph (D), interpretative sketch of Lapparent & Montenat (1967) (E) ("Unnamed track n°2" in Lapparent & Montenat 1967: fig. 18 and pl. XIII.5), and our interpretation (F). Scale bars: A-C, 1 cm; D-F, 5 cm.

FIG. 4 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 4. — Footprints from Le Veillon compared to tridactyl tracks from the Early Jurassic of the Causses Basin (based on data from Demathieu et al. 2002; Moreau et al. 2021) and the Early Jurassic of the eastern United States (based on data from Weems 1992, 2019; Gand et al. 2018): A, bivariate diagram L vs (L–D)/D; B, bivariate diagram L vs L/W. L in metres.

FIG. 2 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 2. — Measurements taken on tracks from the Lapparent collection: A, for crocodylomorph manus imprint; B, for crocodylomorph pes track; C, for dinosaur footprint. Abbreviations: L, length of footprint (for dinosaur tracks); LM, LP, length of manus and pes tracks, respectively (for crocodylomorph tracks); W, width of footprint (for dinosaur tracks); WM, WP, width of manus and pes tracks, respectively (for crocodylomorph tracks); LI, LII, LIII, LIV, LV, lengths of digits I, II, III, IV and V, respectively; D, length of the free part of digit III; I-V, I-IV, II-IV, divarication angles between digits I and V, digits I and IV, then digits II and IV, respectively.

FIG. 12 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 12. — Kayentapus isp.: A-C, track ULB-04C02_A (holotype of "Talmontopus tersi" that is here invalidated), photograph (A), DEM and false-colour depth map (B) and interpretative sketch (C). Scale bars: 10 cm.

FIG. 9 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 9. — Eubrontes giganteus Hitchcock, 1845: A-C, track ULB-04D21_A (plaster cast of the holotype of "E. veillonensis" that is here invalidated), photograph (A), DEM and false-colour depth map (B) and interpretative sketch (C). Scale bars: 10 cm.

FIG. 10 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 10. — Grallator minusculus (Hitchcock, 1858), Demathieu, Gand, Sciau & Freytet, 2002: A-C, track ULB-04C13_B (plaster cast of the holotype of "G. maximus" that is here invalidated), photograph (A), DEM and false-colour depth map (B) and interpretative sketch (C); D-F, track ULB-04C10_B, photograph (D), DEM and false-colour depth map (E) and interpretative sketch (F). Scale bars: 10 cm.

FIG. 5 in Crocodylomorph and dinosaur tracks from the lowermost Jurassic of Le Veillon (western France): ichnotaxonomic revision of the type material (Lapparent collection)

FIG. 5. — Grallator variabilis Lapparent & Montenat, 1967: A-C, plaster cast of the holotype, ULB-04C08_D, photograph (A), DEM and false-colour depth map (B) and interpretative sketch (C); D-F, paratype, ULB-04C05_A, photograph (D), DEM and false-colour depth map (E) and interpretative sketch (F); G-I, track ULB- 04C13_A, photograph (G), DEM and false-colour depth map (H) and interpretative sketch (I). Scale bars: 5 cm.

Рис. 2. ИЗобраЖениЯ Mactra sulcataria Deshayes in Reeve, 1854 в работах 19 в.: A – Reeve [1854, pl. 2, fig. 5]; B – Weinkauff [1881, Taf. 18, Fig. 3]; в списке литературы как: Küster, Weinkauff [1841–1884]. in Notes on type material of Mactra sulcataria Deshayes in Reeve, 1854 (Bivalvia: Mactridae) and taxonomic history of the species

Рис. 2. ИЗобраЖениЯ Mactra sulcataria Deshayes in Reeve, 1854 в работах 19 в.: A – Reeve [1854, pl. 2, fig. 5]; B – Weinkauff [1881, Taf. 18, Fig. 3]; в списке литературы как: Küster, Weinkauff [1841–1884].