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Crail Scotland

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(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 Carboniferous (Visean) from East Fife, Kinkell Braes, Boarhills to Kingsbarns, and Crail respectively. (c) Location details within Linn Park, Glasgow.
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
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, Pittenweem Formation, Strathclyde Group, with three recorded trackways; Crail (Pittenweem Formation), with five plus recorded tracks. Black circle, Boarshills to Kingsbarns, Anstruther Formation, Strathclyde Group, with 13 trackways. At the right-hand side is shown the correlation of European Carboniferous subdivisions with those of the International Commission on Stratigraphy.
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
Journal Article
Published: 15 December 2023
Scottish Journal of Geology (2024) 60 (1): sjg2021-019.
...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...
FIGURES
First thumbnail for: Arthropleura trackway ( Diplichnites cuithensis ) ...
Second thumbnail for: Arthropleura trackway ( Diplichnites cuithensis ) ...
Third thumbnail for: Arthropleura trackway ( Diplichnites cuithensis ) ...
Journal Article
Published: 29 March 2021
Scottish Journal of Geology (2021) 57 (1): sjg2020-019.
...Richard A. Batchelor Abstract A volcanogenic clay bed (tonstein) has been identified in the Balcomie Beds of the Inverclyde Group near Crail, East Fife. Its chemical composition suggests an undersaturated alkaline magma source. This horizon may be contemporaneous with the early Carboniferous...
FIGURES
First thumbnail for: Volcaniclastic deposit (tonstein) in the Balcomie ...
Second thumbnail for: Volcaniclastic deposit (tonstein) in the Balcomie ...
Third thumbnail for: Volcaniclastic deposit (tonstein) in the Balcomie ...
Image
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 was cast (Briggs et al. 1979) in the Serpukhovian Limestone Coal Formation of Laggan, Isle of Arran, Scotland. Stick is 1 m long, inner and outer width of trackway highlighted. (b) D. cuithensis trackway of near-analogous width to the Howick body fossil, Visean Pittenweem Formation, Crail, Fife, Scotland. (c) D. cuithensis trackway >10 m long (arrowed) in the Visean Pittenweem Formation, St Andrews, Fife, Scotland (see Whyte 2018). Geologist is 1.8 m tall. (d, e) Photograph and interpreted sketch of context of D. cuithensis on a true substrate (Davies and Shillito 2018, 2021) recording the passage of two animals between emergent and subaqueous substrates. Convex bedform, colonized with plants, provided small island surrounded by shallow water puddles in a delta-top setting. Trackways are well-defined on emergent substrate and less so on subaqueous parts of substrate. Visean Anstruther Formation, 3.5 km NW of Kingsbarns, Fife, Scotland. Measuring stick 60 cm long.
Published: 21 December 2021
was cast ( Briggs et al. 1979 ) in the Serpukhovian Limestone Coal Formation of Laggan, Isle of Arran, Scotland. Stick is 1 m long, inner and outer width of trackway highlighted. ( b ) D. cuithensis trackway of near-analogous width to the Howick body fossil, Visean Pittenweem Formation, Crail, Fife
Journal Article
Published: 18 April 2018
Scottish Journal of Geology (2018) 54 (1): 63–68.
...Martin A. Whyte Abstract Three closely associated arthropleurid trackways, Diplichnites cuithensis , from the Lower Carboniferous of Fife, Scotland, exhibit signs of interaction between track-makers. An extra file of footprints is found on the downslope side of two trackways (A and C), the upslope...
FIGURES
First thumbnail for: Mating trackways of a fossil giant millipede
Second thumbnail for: Mating trackways of a fossil giant millipede
Third thumbnail for: Mating trackways of a fossil giant millipede
Journal Article
Published: 21 December 2021
Journal of the Geological Society (2022) 179 (3): jgs2021-115.
... was cast ( Briggs et al. 1979 ) in the Serpukhovian Limestone Coal Formation of Laggan, Isle of Arran, Scotland. Stick is 1 m long, inner and outer width of trackway highlighted. ( b ) D. cuithensis trackway of near-analogous width to the Howick body fossil, Visean Pittenweem Formation, Crail, Fife...
FIGURES
First thumbnail for: The largest arthropod in Earth history: insights f...
Second thumbnail for: The largest arthropod in Earth history: insights f...
Third thumbnail for: The largest arthropod in Earth history: insights f...