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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).

Fig. 9 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 9 Lectotype and paralectotype of Trematoceras elegans (MÜnster, 1841) from the Carnian of the Cassian Formation. A, C SNSB-BSPG AS VII 1014, lectotype. B, D–F SNSB-BSPG AS VII 1015, paralectotype. A External (lateral?) view. B Apertural view. C Longitudinal section. D Apical view. E Lateral view, venter right. F Ventral view

Fig. 2 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 2 Orthoceratoids from the Besano Formation (Middle Triassic) of the Monte San Giorgio, Ticino, Switzerland. A–H: Trematoceras cf. elegans (MÜnster, 1841). A PIMUZ 39056, partially fixed with silicon, bed 41. B PIMUZ 39487, bed 87. C-E PIMUZ 39586, sectioned specimen, bed 45. F–G PIMUZ 39029, bed 61. H PIMUZ 39064, bed 162

Cross section shape: circular elliptical unknown Siphuncle position: central marginal unknown Fig. 4 Morphometrics of orthoconic cephalopods from the Besano Formation. Measurements are compared with discrete characters of the shell. Orange circles represent definite and orange crosses likely orthoceratoids, while blue triangles represent definite and blue crosses likely coleoids. Black crosses are indeterminable. A Apical angle, calculated from length and diameters of the specimens. B Maximum diameter in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Cross section shape: circular elliptical unknown Siphuncle position: central marginal unknown Fig. 4 Morphometrics of orthoconic cephalopods from the Besano Formation. Measurements are compared with discrete characters of the shell. Orange circles represent definite and orange crosses likely orthoceratoids, while blue triangles represent definite and blue crosses likely coleoids. Black crosses are indeterminable. A Apical angle, calculated from length and diameters of the specimens. B Maximum diameter

Fig. 3 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 3 Ticinoteuthis chuchichaeschtli gen. et sp. nov. from the Besano Formation (Middle Triassic) of the Monte San Giorgio, Ticino, Switzerland and a co-occurring orthoceratoid for taphonomic comparison. A–D PIMUZ 39491, holotype, bed 112 A Lateral view. B Adapical view of preserved phragmocone, exposing the ventral position of the siphuncle. C Lateral view of preserved phragmocone, exposing faint traces of inclined septa. D Lateral view of adapical external mould, exposing potential traces of septa. E–G PIMUZ 39493, T. chuchichaeschtli gen. et sp. nov., bed 94. E Lateral view. F Enlarged view of longitudinal ribs. G Lateral view of counterpart. H PIMUZ 39060, bed 94, likely orthoceratoid with similar longitudinal ribs. Note the irregularity in these structures, suggesting that these represent a taphonomic artefact. Abbreviations: si = siphuncle, se = septa

Fig. 10 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 10 Reconstructions of non-ammonoid cephalopods from the Anisian of Monte San Giorgio. A Breviconoteuthis breviconus (Reis, 1907); B Mojsisovicsteuthis sp.; C Ticinoteuthis chuchichaeschtli gen. et sp. nov.; D Trematoceras elegans (MÜnster, 1841); F Enoploceras rieberi Pieroni, 2022

Fig. 1 in Orthoceratoid and coleoid cephalopods from the Middle Triassic of Switzerland with an updated taxonomic framework for Triassic Orthoceratoidea

Fig. 1 Stratigraphic distribution of orthoconic cephalopods in the Besano Formation at Point 902 and corresponding strata at Monte San Giorgio. Each symbol represents one specimen. Stratigraphy modified after Röhl et al. (2001) and Pieroni (2022)

Fig. 7 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 7 Cranium of Ma. patachonica (PIMUZ A/V 5700) in dorsal A and ventral B views. The cranium (PIMUZ A/V 5700) only preserves its posterior portion and basicranium, and was previously subjected to a poor restoration with plaster which covers some of the cranial structures

Fig. 6 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 6 Limb bones of Toxodon cf. T. platensis from the Roth collections in Zurich and Geneva. Right femur (PIMUZ A/V 4216) in A anterior view, and B posterior view. Partial left humerus (MHNG GEPI V3665) in C anterior view, and D posterior view. Left ulna (PIMUZ A/V 4290) in E lateral view, and F medial view

Fig. 2 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 2 Cranium of Mesotherium cristatum (PIMUZ A/V 467). A Ventral view. B Detail (left) and drawing (right) of the upper right dentition in occlusal view. C Lateral view. D Dorsal view. Notice the inflated epitympanic theca, the lateral borders of premaxilla diverging rostrally, the mesiodistally elongated I1 and the lateral orientation of the parastyle of M3 (see Fernández-Monescillo et al., 2023b)

Fig. 3 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 3 Mandible of Mesotherium cristatum. PIMUZ A/V 467 (A–D). A Detail of the left lower dentition in occlusal view. Mandible in B dorsal view, C lateral, and D anterior views. E PIMUZ A/V 4133 in dorsal view. Notice the differences in size and occlusal outlines of i1 and i2, the constricted lateral borders and concave ventral border of the symphysis (see Fernández-Monescillo et al., 2023b)

Fig. 1 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 1 Geographic provenance of the SANUs specimens of the Roth collection from the Pampean Region, Argentina

Fig. 4 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 4 Partial skull of Toxodon cf. T. platensis (PIMUZ A/V 5697). A Caudal portion of the cranium in dorsal view. B Occiput in caudal view

Fig. 5 in Pleistocene South American native ungulates (Notoungulata and Litopterna) of the historical Roth collections in Switzerland, from the Pampean Region of Argentina

Fig. 5 Mandible and dentition of Toxodon cf. T. platensis. Mandible (PIMUZ A/V 4163) in A dorsal and B lateral views. C Mandible (PIMUZ A/V 4210) in dorsal view. D Right p1 (left) and m2 (right) in occlusal view (PIMUZ A/V 4163). E Right m2 in occlusal view (PIMUZ A/V 4233). F Left P4 in occlusal view (PIMUZ A/V 4245). G Right P3 in occlusal view (PIMUZ A/V 4199)

Fig. 5 in Middle Triassic Nautilida from the Besano Formation of Monte San Giorgio, Switzerland

Fig. 5 Syringonautilus sp., PIMUZ 37903, P. 902/Mirigioli (Monte San Giorgio), Middle Besano Formation (bed 104), uppermost Anisian: a lateral view, left side, b oral view, c ventral view

Fig. 3 Germanonautilus aff. ellipticus Parnes, 1986, PIMUZ 29942 in Middle Triassic Nautilida from the Besano Formation of Monte San Giorgio, Switzerland

Fig. 3 Germanonautilus aff. ellipticus Parnes, 1986, PIMUZ 29942, Valle Stelle/Tre Fontane (Monte San Giorgio), Middle Besano Formation (bed 73), Secedensis Zone, Illyrian: a original specimen partially included in the matrix, lateral view, b ventral view, associated with an external mold of Stoppaniceras cf. artinii, c plaster cast replica of the same specimen, lateral view, d plaster cast replica of the same specimen, ventral view, e plaster cast replica of the same specimen, ventrolateral view, f drawing of the ventral view showing the hypothetical whorl section (in grey the flank areas)

Fig. 1 in Middle Triassic Nautilida from the Besano Formation of Monte San Giorgio, Switzerland

Fig. 1 Stratigraphic section of the Besano Formation at Point 902/ Mirigioli (modified after Röhl et al., 2001, Fig. 4). The stratigraphic positions of five described specimens are indicated beside this section and the distribution of some ammonoids (after Rieber, 1973a, 1973b) from the same levels (indicated in grey)

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Fig. 2 in The first Jurassic coelacanth from Switzerland

Fig. 2 Ammonites and bivalves of Les Pueys compared to ammonites and bivalves of the Creux de l'Ours. Invertebrate fossils A–C preserved on the reverse side of the two slabs with Libys callolepis sp. nov. (holotype, NMBE 5034072 and 5034073) from Les Pueys and D–F invertebrate fossils from the Creux de l'Ours. A Dactylioceras? sp. (NMBE 5034073); B Harpoceras renevieri (NMBE 5034072); C Goniomya rhombifera (NMBE 5034072); D Dactylioceras commune Sowerby 1815 (NMBE 5014840); E Harpoceras renevieri (holotype, NMBE 5014830); F Goniomya rhombifera (NMBE 5021902)

Fig. 6 in Middle Triassic Nautilida from the Besano Formation of Monte San Giorgio, Switzerland

Fig. 6 Nautilida gen. et sp. indet., PIMUZ 38668, P. 902/ Mirigioli (Monte San Giorgio), Middle Besano Formation (bed 98), uppermost Anisian: a lateral view, left side, b lateral view, right side, c ventral view, d aboral portion of ventral view showing suture line (ventral saddle). In figs. a and b the umbilical wall is not visible because is embedded in the matrix (here not showed), so it is difficult to judge where exactly the dorsum ends.The black point beside a, b, c, marks where was observed the suture line showed in d

Fig. 2 in Middle Triassic Nautilida from the Besano Formation of Monte San Giorgio, Switzerland

Fig. 2 Enoploceras rieberi sp. nov., PIMUZ 37902, holotype, Point 902/ Mirigioli (Monte San Giorgio), Middle Besano Formation (bed 73), Secedensis Zone, Illyrian. a lateral view, left side, b lateral view, right side, c ventral view, d drawing of the left side, phragmocone with septa (white) and body chamber (grey). e Drawing of the right side showing the sculpture, f drawing of the ventral view showing the depressed ventral area (light grey) and the hyponomic sinus, g suture line