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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.

opencc-by-4.0Jun 2024View details →

3D models and raw data for the "Photogrammetric 3D modelling and experimental archaeology reveals new technological insights into engraved soapstone sinker production in Western Norway (6400-3300 cal. BC)" paper, Radchenko et al. in prep.

<p>3D models and raw data for the "Photogrammetric 3D modelling and experimental archaeology reveals new technological insights into engraved soapstone sinker production in Western Norway (6400-3300 cal. BC)" paper, Radchenko et al. in prep.</p> <p>5 models of soapstone sinkers and 5 models of experimentally produced objects.</p>

opencc-by-4.0May 2009View details →

Fig. 4 in Changing climate-changing pathogens: Toxoplasma gondii in North-Western Europe

Fig. 4 Expected increases in T. gondii prevalence in NorthWestern Europe towards 2069 based upon the combination of climatic conditions from Figs. 2 and 3. The dotted bright green areas indicate a small increase in T. gondii prevalence as a result of climatic change, pink areas a limited increase, and red areas a substantial increase

opencc-by-4.0May 2009View details →

Fig. 2 in Changing climate-changing pathogens: Toxoplasma gondii in North-Western Europe

Fig. 2 Total precipitation in North-Western Europe as calculated by the CCSR (Center for Climate System Research, University of Tokyo) and NIES (National Institute for Environmental Studies) model under a SRES A1 scenario. Presented is the total mean precipitation in period from 1970 to 1999 (a), and the projected total mean precipitation from 2010 to 2039 (b) and 2040–2069 (c). Figures obtained from www.ipcc-data.org

opencc-by-4.0Dec 2020View details →

Fig. 1 a in Oviposition of AedeS japoNiCUS japoNiCUS (Diptera: Culicidae) and associated native species in relation to season, temperature and land use in western Germany

Fig. 1 a Study sites in the south of North Rhine-Westphalia, Germany in 2018. Forest types (different shades of green) follow Authorised Topographic-Cartographic Information System data [39]. b Details of study site Bonn SÜd, with three transects and their respective trap locations (different colours represent different land use types). See Additional file 2: dataset S1 for coordinates of trap locations. Background map from http:// www.openstreetmap.org (OpenStreetMap contributors). The map was produced with QGIS version 3.2

opencc-by-4.0Dec 2020View details →

Fig. 2 in Oviposition of AedeS japoNiCUS japoNiCUS (Diptera: Culicidae) and associated native species in relation to season, temperature and land use in western Germany

Fig. 2 Setup of the transects. Trap locations range from oviposition habitat 1 (land use types—arable land, forest or settlement) through the transition zone into oviposition habitat 2 (land use types—forest, settlement or arable land). F100 Forest, 100 m from the transition zone; F10 forest, 10 m from the transition zone; F/S transition zone; S10 settlement, 10 m from the transition zone; S100 settlement, 100 m from the transition zone

Fig. 4 in Variation of shell shape in Solariella obscura (Vetigastropoda: Trochoidea) in the Eurasian Arctic seas and adjacent part of the Western Pacific Ocean

Fig. 4. PCA scatterplots: A–C – varieties of Solariella obscura; typical form – red crosses, «var. intermedia» – black dots, «var. bella» – blue squares; D–F – geographic groups; Arctic – green crosses, Pacific – violet circles.

Fig. 1 in Variation of shell shape in Solariella obscura (Vetigastropoda: Trochoidea) in the Eurasian Arctic seas and adjacent part of the Western Pacific Ocean

Fig. 1. Varieties of Solariella obscura: A – «var. intermedia», Barents Sea, Iokangskie Islands, 68°04.38′ N, 39°34.70′ E, ZIN 28/4289; B – typical form, Bering Sea, 29 m, 64°02.2′ N, 170°04′ W, ZIN 675/56388; C – «var. bella», Barents Sea, 154 m, 69°40.597′ N, 34°06.184′ E. Scale bar 3 mm.

Fig. 2 in Variation of shell shape in Solariella obscura (Vetigastropoda: Trochoidea) in the Eurasian Arctic seas and adjacent part of the Western Pacific Ocean

Fig. 2. Scheme of shell measurements (A–B) and counting of whorls number (C). Shell of «var. bella». SH – shell height; BWH – body whorl height; AH – aperture height; AW – aperture width; SW – shell width; UW – umbilicus width; spiral arrow indicates the first whorl, whorls number of the shell = 3.9.

Fig. 3 in Variation of shell shape in Solariella obscura (Vetigastropoda: Trochoidea) in the Eurasian Arctic seas and adjacent part of the Western Pacific Ocean

Fig. 3. Box plots of conchological parameters: A – shell height; B – body whorl height; C – aperture height; D – shell width; E – umbilicus width; F – whorls number. 1 – «var. intermedia», 2 – typical form, 3 – «var. bella».

opencc-by-4.0Mar 2019View details →

Figure 2 in Notes on the breeding biology of birds in riverine floodplains of western Amazonia

Figure 2. Plain-winged Antshrike Thamnophilus schistaceus fledgling, Rondônia, Brazil, June 2018 (Tomaz Nascimento de Melo)

opencc-by-4.0Mar 2019View details →

Figure 6 in Notes on the breeding biology of birds in riverine floodplains of western Amazonia

Figure 6. Nest and eggs of Euler's Flycatcher Lathrotriccus euleri in a dried cocoa Theobroma cacao fruit (Malvaceae), Rondônia, Brazil, September 2017 (Tomaz Nascimento de Melo)