1-20 OF 22 RESULTS FOR

Diplichnites cuithensis

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 15 December 2023
Scottish Journal of Geology (2024) 60 (1): sjg2021-019.
...James O. Buckman; Simon J. Cuthbert; Paul G. Polson Abstract The arthropleurid trackway Diplichnites cuithensis has previously been described from Scotland from the Upper Carboniferous Serpukhovian Limestone Coal Formation on the Isle of Arran and the Lower Carboniferous Visean Pittenweem...
FIGURES | View All (7)
Image
Stratigraphic location of Scottish  <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span>  withinin the C...
Published: 15 December 2023
Fig. 3. Stratigraphic location of Scottish Diplichnites cuithensis withinin the Carboniferous sequence of the Midland Valley of Scotland. White square, D. cuithensis , Isle of Arran, Serpukhovian, Limestone Coal Formation, and Linn Park, Glasgow (herein). White circle, Visean, Kinkell Braes
Image
Images of  <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span>  recorded from the Linn Park location. (...
Published: 15 December 2023
Fig. 5. Images of Diplichnites cuithensis recorded from the Linn Park location. ( a ) As first recorded (1995); ( b ) current state (2020); ( c ) 3D digital reconstruction of same area.
Image
Image of  <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span> , from Linn Park, showing detail of track...
Published: 15 December 2023
Fig. 6. Image of Diplichnites cuithensis , from Linn Park, showing detail of trackway. ( a ) Actual photograph of part of the trackway; ( b ) 3D digital reconstruction of similar parts of trackway.
Image
<span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span>  sesqui-trackways from the Lower Carboniferous (Mis...
Published: 18 April 2018
Fig. 2. Diplichnites cuithensis sesqui-trackways from the Lower Carboniferous (Mississippian; Asbian) Pittenweem Formation of the Kinkell Braes, near St Andrews, Fife [NO530158]. ( a ) Panoramic view of the dipping rock exposure showing the three trackways. ( b ) Map of the panoramic view
Image
Features of  <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span>  sesquitrackways. ( a ) Oblique view a...
Published: 18 April 2018
Fig. 3. Features of Diplichnites cuithensis sesquitrackways. ( a ) Oblique view along Trackway A, showing double grooves and the track deviation (X on Fig. 2b ). Hammer is 34 cm long. ( b ) Detail of Trackway A showing double grooves with multiple transverse footprints (arrowed; enlargement
Image
<span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span>  trackways on upper surface of Block A, derived fro...
Published: 01 December 2014
Fig. 6.— Diplichnites cuithensis trackways on upper surface of Block A, derived from Unit 2. A , B ) Photo and tracing of trackways 1 and 2 traversing wrinkled microbial mat, with rippled area partly covered with modern green algae. C , D ) Photo and tracing of Trackway 1. E , F ) Photo
Image
Figure  3 — <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span> , specimen PC-5. Trackway preserved as ...
Published: 01 January 2009
Figure 3 — Diplichnites cuithensis , specimen PC-5. Trackway preserved as convex hyporelief. Note footfall clusters in right series toward top, and gutter cast along left side of trackway. Scale bar is 10 cm. Low angle illumination is from top
Image
Figure  4 — <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span> , specimen PC-6, convex hyporelief. Not...
Published: 01 January 2009
Figure 4 — Diplichnites cuithensis , specimen PC-6, convex hyporelief. Note cast of tetrapod manus ( Limnopus glenshawensis ) below 10 cm bar scale in upper left of photo. Crescentic shaped footfalls in middle of photo indicate changing direction of Arthropleura toward “left.” Fracture in lower
Image
Figure  6 — <span class="search-highlight">Diplichnites</span> <span class="search-highlight">cuithensis</span> , specimen PC-7. Bar scale = 5 cm, low ...
Published: 01 January 2009
Figure 6 — Diplichnites cuithensis , specimen PC-7. Bar scale = 5 cm, low angle illumination from top
Journal Article
Published: 18 April 2018
Scottish Journal of Geology (2018) 54 (1): 63–68.
...Fig. 2. Diplichnites cuithensis sesqui-trackways from the Lower Carboniferous (Mississippian; Asbian) Pittenweem Formation of the Kinkell Braes, near St Andrews, Fife [NO530158]. ( a ) Panoramic view of the dipping rock exposure showing the three trackways. ( b ) Map of the panoramic view...
FIGURES | View All (4)
Journal Article
Journal: PALAIOS
Published: 01 December 2014
PALAIOS (2014) 29 (12): 624–645.
...Fig. 6.— Diplichnites cuithensis trackways on upper surface of Block A, derived from Unit 2. A , B ) Photo and tracing of trackways 1 and 2 traversing wrinkled microbial mat, with rippled area partly covered with modern green algae. C , D ) Photo and tracing of Trackway 1. E , F ) Photo...
FIGURES | View All (11)
Journal Article
Published: 21 December 2021
Journal of the Geological Society (2022) 179 (3): jgs2021-115.
... in Arthropleura , and the first instance of a giant arthropleurid body fossil within the same regional sedimentary succession as the large arthropod trackway Diplichnites cuithensis . The remains represent 12–14 anterior Arthropleura tergites in the form of a partially sand-filled dorsal exoskeleton. The original...
FIGURES | View All (13)
Image
Microbial mat in Unit 2.  A ) Upper surface of Block A showing wrinkle mark...
Published: 01 December 2014
Fig. 5.— Microbial mat in Unit 2. A ) Upper surface of Block A showing wrinkle marks and two intersecting trackways of Diplichnites cuithensis . B ) Close-up of wrinkle marks on Block A. C ) Upper surface of Block C illustrating concentric wrinkles around a hollow on the sediment surface. D
Image
A ) Specimen NSM 5364110. Block discovered at Coal Mine Point by Don Reid. ...
Published: 01 December 2014
Fig. 8.— A ) Specimen NSM 5364110. Block discovered at Coal Mine Point by Don Reid. Two Diplichnites cuithensis trackways (arrowed) on bed surface associated with wrinkles. B ) Close-up of wrinkled surface. C ) Close-up of Dromillopus tracks in view A, discussed by Mossman and Grantham
Image
( a ) Map of Scotland showing the location of detailed map ( b ), illustrat...
Published: 15 December 2023
Fig. 1. ( a ) Map of Scotland showing the location of detailed map ( b ), illustrating locations of known Carboniferous Diplichnites cuithensis in Scotland, within the Carboniferous Midland Valley of Scotland (MVS). A, New occurrence from Linn Park Glasgow; B, Isle of Arran; C–E, Lower
Image
Trace fossil evidence for  Arthropleura  from the trackway  <span class="search-highlight">Diplichnites</span> cu...
Published: 21 December 2021
Fig. 12. Trace fossil evidence for Arthropleura from the trackway Diplichnites cuithensis , preserved in strata, near contemporaneous in age to the Howick specimen, from adjacent basins in northern Britain (see Fig. 3 for localities). ( a ) Trackway from which the D. cuithensis holotype
Image
Reconstruction of the Howick  Arthropleura . (a) Scale of the Howick  Arthr...
Published: 21 December 2021
Fig. 11. Reconstruction of the Howick Arthropleura . (a) Scale of the Howick Arthropleura relative to other articulated giant specimens (preserved remains highlighted pink) and the largest Diplichnites cuithensis trackways known from each Carboniferous-Permian stage. Note that the previously
Journal Article
Published: 01 January 2009
Journal of Paleontology (2009) 83 (1): 140–146.
...Figure 3 — Diplichnites cuithensis , specimen PC-5. Trackway preserved as convex hyporelief. Note footfall clusters in right series toward top, and gutter cast along left side of trackway. Scale bar is 10 cm. Low angle illumination is from top ...
FIGURES | View All (8)
Journal Article
Published: 01 January 2003
Geological Magazine (2003) 140 (1): 63–72.
... Diplichnites based on similarity with D. cuithensis Briggs, Rolfe & Brannan, 1979 , distinguishing the two forms on the basis that D. gouldi has ‘fewer [tracks per series] than D. cuithensis and each [track] lacks the slight transverse element of the Scottish form’. Bradshaw considered that ‘fresh...
FIGURES | View All (7)