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8 results for “tetrapod footprints”
Fig. 6. Putative protorosaurid archosauromorph trace Paradoxichnium isp. A, B in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 6. Putative protorosaurid archosauromorph trace Paradoxichnium isp. A, B. Paradoxichnium isp. from Ulbe (Italy), Lopingian. A. MCV 10, right complete manus, note the proximally-positioned digits I and V and the triangular claw impressions. B. MCV 9, complete left manus impression. Note the proximally-positioned digits I and V, the parallel digits II–IV and the triangular claw impressions. C. Paradoxichnium problematicum Müller, 1959, holotype FG 20/1 from Culmitzch (Thuringia, Germany), Lopingian; right (C1) and left (C2) pes-manus couples; note the manual morphology similar to MCV 9. Convex hyporelief, spacing 0.5 mm. Photo (A1, B1), interpretive drawing (A2, B2), false-color depth map (A3, B3), contour lines (A4, B4). Scale bars 10 mm.
Fig. 5 in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 5. Pareiasaurian parareptile trace Pachypes isp. (MCV 3) from Ulbe (Italy), Lopingian. Left manual imprint showing digits I–IV, convex hyporelief. Photo (A), interpretive drawing (B), false-color depth map (C), contour lines (D). Scale bar 10 mm.
Fig. 2 in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 2. Sedimentary structures of Val Gardena Sandstone. Facies association a, fine-grained sandstone showing cross lamination (A) and parallel ripples B). Facies association b, reddish mudstone with paleosols (C), pedogenic veins and nodules in the mudstone (D). Note the gray dolostone strata on the top. Facies association c, gray dolostone strata interbedded in the reddish mudstone (E), invertebrate burrows in the dolostone (F). G. Bellerophon Formation, gray dolostone.
Fig. 8. A in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 8. A. Undetermined track (MCV 14/30) of therapsid synapsid from Cortiana (Italy), Lopingian. Incomplete right manual impression showing digits III–V and deep expulsion rims. Concave epirelief, spacing 1 mm. Photo (A1), interpretive drawing (A2), contour lines (A3), false-color depth map (A4). B. MGP 9/22, interpretive drawing of a complete left manual impression from the Bletterbach Gorge, Dolomites (Italy), Lopingian, after Conti et al. 1977). Scale bar 10 mm.
Fig. 1 in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 1. Geographic location and stratigraphy of the fossil sites (asterisked). Map showing location of the study area in North Italy (A) and Recoaro area (B). Simplified geological map (C). D. Synthetic stratigraphic log of the Permian of Venetian Prealps (a–c, facies associations). Location of Merendaore and Ulbe (E) and Cortiana (F) fossil sites. G, H. Photographs of the Ulbe outcrops, small scale transition between lithofacies (G) and large scale transition between formations (H), with indicated transition between red bed (Rb) and lagoon (Lg) lithofacies of the topmost strata of the Val Gardena Formation, immediately before the deposition of the Bellerophon Formation. BEL, Bellerophon Formation; GAR, Val Gardena Sandstone; Lg, lagoon lithofacies (dolostone); Ps, incipient paleosol with deep mudcracks; Rb, red bed lithofacies (laminated mudstone). Hammer for scale.
Fig. 3 in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 3. Putative parareptile trace cf. Capitosauroides isp. from Ulbe (Italy), Lopingian. A. MCV 7, left pes impression showing digits I–IV. B. MCV 11/05, right manual impression showing digits I–IV. Convex hyporelief, spacing 0.5 mm. Photo (A1, B1), interpretive drawing (A2, B2), false-color depth map (A3, B3), contour lines (A4, B4). Scale bars 10 mm.
Fig. 7 in Lopingian tetrapod footprints from the Venetian Prealps, Italy: New discoveries in a largely incomplete panorama
Fig. 7. Lacertoid neodiapsid eureptile trace Rhynchosauroides isp. (MCV 65) from Merendaore (Italy), Lopingian. Complete right manual impression. An incomplete track and a continuous tail are preserved on the same slab. Convex hyporelief (plaster cast), spacing 0.5 mm. Photo (A), interpretive drawing (B), contour lines (C), false-color depth map (D). Scale bar 10 mm.
A revision of tetrapod footprints from the late Carboniferous of the West Midlands, UK
<p>This dataset contains data supporting the manuscript 'A revision of tetrapod footprints from the late Carboniferous of the West Midlands, UK', currently in review at PeerJ. The zip folder contains 17 subfolders, each corresponding to a sandstone slab from Hamstead, Birmingham, West Midlands examined in the study. Subfolders are labelled with the slab numbers using the system of RAW and BIRUG numbers described in the manuscript. Within each subfolder there are several distinct file types:</p> <ul> <li>Photogrammetric models, as a "model.ply" file and a "model.jpg" texture file. The models can be opened using free software such as Meshlab, and the .ply and .jpg files need to be in the same folder for the textured model to open correctly. </li> <li>One or more photographs labelled as "details.jpg". These photographs show the specimen labels associated with each of the slabs. Note that taxonomic IDs used on these historical specimen labels may differ from those used in the manuscript. </li> <li>Two files created using CloudCompare 2.7 that show the surfaces of the slabs as digital 3D reliefs with coloured contour intervals ("topology.jpg"), and also reliefs with steep gradients brightly highlighted ("gradient.jpg").</li> </ul>
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