1-20 OF 56 RESULTS FOR

Duntulm Formation

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: 01 April 2004
Scottish Journal of Geology (2004) 40 (1): 13–21.
...N. D. L. Clark; P. Booth; C. Booth; D. A. Ross Synopsis The first in situ dinosaur tracks from Scotland were discovered at the top of the Duntulm Formation (Bathonian, Jurassic) near to Staffin in northeastern Skye. Fifteen individual tridactyl footprints were recorded of which two pairs appear...
FIGURES
First thumbnail for: Dinosaur footprints from the <span class="search-h...
Second thumbnail for: Dinosaur footprints from the <span class="search-h...
Third thumbnail for: Dinosaur footprints from the <span class="search-h...
Image
Dinosaur track-bearing sedimentary section of the Duntulm Formation exposed at An Corran.
Published: 01 April 2004
Fig. 2. Dinosaur track-bearing sedimentary section of the Duntulm Formation exposed at An Corran.
Image
Figure 5. Detailed schematic log of Duntulm Formation showing bed numbers and lithologies (based on Andrews and Walton, 1990). Paleosalinities are calculated from Sr material balance considerations as described in text.
Published: 01 October 2003
Figure 5. Detailed schematic log of Duntulm Formation showing bed numbers and lithologies (based on Andrews and Walton, 1990 ). Paleosalinities are calculated from Sr material balance considerations as described in text.
Journal Article
Published: 02 April 2018
Scottish Journal of Geology (2018) 54 (1): 1–12.
.... A theropod trackmaker is inferred for some of the tridactyl impressions with several indicative of the ichnotaxon Eubrontes . This new site strengthens the inference, originally based on a previously discovered locality near Duntulm Castle (Duntulm Formation) in northern Skye, that sauropods habitually spent...
FIGURES
First thumbnail for: A sauropod-dominated tracksite from Rubha nam Brat...
Second thumbnail for: A sauropod-dominated tracksite from Rubha nam Brat...
Third thumbnail for: A sauropod-dominated tracksite from Rubha nam Brat...
Journal Article
Journal: GSA Bulletin
Published: 01 October 2003
GSA Bulletin (2003) 115 (10): 1249–1264.
...Figure 5. Detailed schematic log of Duntulm Formation showing bed numbers and lithologies (based on Andrews and Walton, 1990 ). Paleosalinities are calculated from Sr material balance considerations as described in text. ...
FIGURES
First thumbnail for: 87 Sr/ 86 Sr and Sr/Ca Investigation of Jurassic m...
Second thumbnail for: 87 Sr/ 86 Sr and Sr/Ca Investigation of Jurassic m...
Third thumbnail for: 87 Sr/ 86 Sr and Sr/Ca Investigation of Jurassic m...
Journal Article
Published: 01 December 2015
Scottish Journal of Geology (2016) 52 (1): 1–9.
... and terrestrial deposits of Middle Jurassic age, which have yielded sparse bones, teeth, footprints and small segments of trackways belonging to dinosaurs. We report the discovery of the most extensive dinosaur fossil site yet known in Scotland: a coastal outcrop of the Duntulm Formation (Bathonian) at Cairidh...
FIGURES
First thumbnail for: Sauropod dinosaur trackways in a Middle Jurassic l...
Second thumbnail for: Sauropod dinosaur trackways in a Middle Jurassic l...
Third thumbnail for: Sauropod dinosaur trackways in a Middle Jurassic l...
Image
Rose diagram of dinosaur track directions with ripple crest data superimposed from the Duntulm Formation, An Corran level A.
Published: 01 April 2004
Fig. 9. Rose diagram of dinosaur track directions with ripple crest data superimposed from the Duntulm Formation, An Corran level A.
Image
Mean shapes of landmark data of footprints: (a) Kilmaluag Formation; (b) Valtos Sandstone Formation; (c) Duntulm Formation; (d) large footprints from Valtos Sandstone Formation and Lealt Shale Formation; (e) Sundance Formation; (f) Gypsum Springs Formation.
Published: 01 October 2008
Fig. 9. Mean shapes of landmark data of footprints: (a) Kilmaluag Formation; (b) Valtos Sandstone Formation; (c) Duntulm Formation; (d) large footprints from Valtos Sandstone Formation and Lealt Shale Formation; (e) Sundance Formation; (f) Gypsum Springs Formation.
Image
Graph showing the relationship between the divarication angle and the ratio between the length of digit III and the length of the track (pIII.FL) of the tracks from the Duntulm Formation, the Valtos Sandstone Formation (see Fig. 7) and the Lealt Shale Formation.
Published: 01 April 2004
Fig. 8. Graph showing the relationship between the divarication angle and the ratio between the length of digit III and the length of the track (pIII.FL) of the tracks from the Duntulm Formation, the Valtos Sandstone Formation (see Fig. 7 ) and the Lealt Shale Formation.
Image
Dinosaur tracks from the new Skye tracksite (Cairidh Ghlumaig, Duntulm Formation, Bathonian). Photographs of (a) convex hyporelief and (b–c) concave epirelief trackways in bed 35. (d) Line drawing of trackways in (c), illustrating the narrow-gauge nature of the trackway. Diameter of lens cap 5 cm.
Published: 01 December 2015
Fig. 2. Dinosaur tracks from the new Skye tracksite (Cairidh Ghlumaig, Duntulm Formation, Bathonian). Photographs of ( a ) convex hyporelief and ( b–c ) concave epirelief trackways in bed 35. ( d ) Line drawing of trackways in (c), illustrating the narrow-gauge nature of the trackway. Diameter
Image
Typical dinosaur footprints from the Middle Jurassic of the Isle of Skye: (a) from the Lealt Shale Formation of Rubha nam Brathairean (scale bar 10 cm); (b) from the Valtos Sandstone Formation at Dun Dearg (scale bar 2 cm); (c) from the Duntulm Formation at An Corran (scale bar 10 Cm); (d) from the Kilmaluag Formation at Score Bay (scale bar 5 cm).
Published: 01 October 2008
Fig. 7. Typical dinosaur footprints from the Middle Jurassic of the Isle of Skye: (a) from the Lealt Shale Formation of Rubha nam Brathairean (scale bar 10 cm); (b) from the Valtos Sandstone Formation at Dun Dearg (scale bar 2 cm); (c) from the Duntulm Formation at An Corran (scale bar 10 Cm); (d
Image
Locality maps. (A) The locations of the previous dinosaur footprint discoveries on Skye are marked with crosses (1 to 3) along the eastern coastline of the Trotternish peninsula. Location 1, Lonfearn Member, Lealt Shale Formation; Location 2, Valtos Sandstone Formation; Location 3, Duntulm Formation. (B) The footprints described in this paper are preserved in the outcrops of the Valtos Sandstone Formation (marked with a cross) to the north of Elgol on the western coastline of the Strathaird peninsula.
Published: 01 November 2005
, Duntulm Formation. ( B ) The footprints described in this paper are preserved in the outcrops of the Valtos Sandstone Formation (marked with a cross) to the north of Elgol on the western coastline of the Strathaird peninsula.
Image
(a, b) Sr isotope data for concretion VR1 and dyke vein 189-7a from Valtos (Trotternish) compared with other relevant Sr isotope data. Whiskers show minima/maxima, boxes show third to first quartiles, the vertical bar shows the median and the cross shows the mean. In (b), the GEG clay data from the Duntulm Formation (DF) and Kilmaluag Formation (KF) are omitted for ease of comparison. UOM, Upper Ostrea member.
Published: 22 May 2023
data from the Duntulm Formation (DF) and Kilmaluag Formation (KF) are omitted for ease of comparison. UOM, Upper Ostrea member.
Image
Fragment of the anterior portion of a right ichthyosaur pterygoid from the Middle Jurassic (Bathonian) Duntulm Formation of Skye, Scotland (GLAHM 152379) in (a) ventral, (b) dorsal, (c) medial, (d) lateral and (e) anterior views. Abbreviations: dl, dorsal lamella; pf, parasphenoid facet; vf, vomer facet. Scale bars: (a–d) 2 cm; (e) 1 cm.
Published: 11 January 2015
Fig. 6. Fragment of the anterior portion of a right ichthyosaur pterygoid from the Middle Jurassic (Bathonian) Duntulm Formation of Skye, Scotland (GLAHM 152379) in ( a ) ventral, ( b ) dorsal, ( c ) medial, ( d ) lateral and ( e ) anterior views. Abbreviations: dl, dorsal lamella; pf
Image
(a) Photograph and (b) line drawing of a section of a sauropod track from bed 34 (Cairidh Ghlumaig, Isle of Skye, Scotland, Duntulm Formation, Bathonian) showing substrate deformation below the bed surface. The arrow marks a region of isolated deformation within the deformed zone likely representing internal substrate deformation from the first digit claw. Diameter of lens cap 5 cm.
Published: 01 December 2015
Fig. 4. ( a ) Photograph and ( b ) line drawing of a section of a sauropod track from bed 34 (Cairidh Ghlumaig, Isle of Skye, Scotland, Duntulm Formation, Bathonian) showing substrate deformation below the bed surface. The arrow marks a region of isolated deformation within the deformed zone
Image
Graph showing the relationship between the divarication angle and the length to width ratio of the third digit (pIII:wIII) of the dinosaur tracks from the Valtos Sandstone Formation, the Duntulm Formation and the Lealt Shale Formation. The Valtos Sandstone Formation is split into those tracks that were identified as Grallator (small) and those identified as Eubrontes (large). Track 16 from level B at An Corran is shown separately from the tracks of level A. The width of the third digit was measured as the maximum width within the proximal two-thirds of the length of the digit as the digit pads were not clear.
Published: 01 April 2004
Fig. 7. Graph showing the relationship between the divarication angle and the length to width ratio of the third digit (pIII:wIII) of the dinosaur tracks from the Valtos Sandstone Formation, the Duntulm Formation and the Lealt Shale Formation. The Valtos Sandstone Formation is split into those
Image
Figure 6. Strontium isotope evolution curve for Middle Jurassic seawater. A belemnite analyzed in this study from Belemnite Sands Member yielded 0.70688. This curve is used to determine 87Sr/86Sr ratio of seawater at time of deposition of Staffin Bay and Duntulm Formations and Kildonnan Member. Marine 87Sr/86Sr ratios are used as reference points for comparing molluskan 87Sr/86Sr ratios from Great Estuarine Group and for paleosalinity calculations based on Sr material balance considerations. Fm.—formation; Mbr.—member.
Published: 01 October 2003
Figure 6. Strontium isotope evolution curve for Middle Jurassic seawater. A belemnite analyzed in this study from Belemnite Sands Member yielded 0.70688. This curve is used to determine 87 Sr/ 86 Sr ratio of seawater at time of deposition of Staffin Bay and Duntulm Formations and Kildonnan Member
Image
Provenance information for the new Skye dinosaur tracksite (Cairidh Ghlumaig, Duntulm Formation, Bathonian). Map of Skye, Scotland, showing the (a) geographical and (b) geological context for the tracksite, and (c) graphic log of the section at Cairidh Ghlumaig shore showing the horizons that preserve dinosaur footprints. Maps adapted from BGS 1:50 000 [Shapefile geospatial data], Scale 1:50 000, Tile: SC090, Version 2014, British Geological Survey, UK. Using: EDINA Geology Digimap Service, http://edina.ac.uk/digimap; downloaded April 2015.
Published: 01 December 2015
Fig. 1. Provenance information for the new Skye dinosaur tracksite (Cairidh Ghlumaig, Duntulm Formation, Bathonian). Map of Skye, Scotland, showing the ( a ) geographical and ( b ) geological context for the tracksite, and ( c ) graphic log of the section at Cairidh Ghlumaig shore showing
Journal Article
Published: 01 October 2008
Scottish Journal of Geology (2008) 44 (2): 139–150.
...Fig. 9. Mean shapes of landmark data of footprints: (a) Kilmaluag Formation; (b) Valtos Sandstone Formation; (c) Duntulm Formation; (d) large footprints from Valtos Sandstone Formation and Lealt Shale Formation; (e) Sundance Formation; (f) Gypsum Springs Formation. ...
FIGURES
First thumbnail for: A comparison between dinosaur footprints from the ...
Second thumbnail for: A comparison between dinosaur footprints from the ...
Third thumbnail for: A comparison between dinosaur footprints from the ...
Image
Dinosaur tracks from the new Skye tracksite (Cairidh Ghlumaig, Duntulm Formation, Bathonian). (a–b) Photograph of well-preserved sauropod convex hyporelief pes print from bed 35. (c) Sauropod convex hyporelief manus and pes set in bed 35. (d) Photograph of tridactyl footprint, with grey outline denoting the preserved edges of the print, from bed 9b. (e–f) Sauropod convex hyporelief pes prints from bed 35. (g) Sauropod convex hyporelief manus print from bed 35. (h) Sauropod concave epirelief tracks from bed 35. I–IV, pedal digits; Ic, manual digit I claw impression; m, manus; p, pes; pp, imprint of fleshy pedal pad. Diameter of lens cap 5 cm.
Published: 01 December 2015
Fig. 3. Dinosaur tracks from the new Skye tracksite (Cairidh Ghlumaig, Duntulm Formation, Bathonian). ( a–b ) Photograph of well-preserved sauropod convex hyporelief pes print from bed 35. ( c ) Sauropod convex hyporelief manus and pes set in bed 35. ( d ) Photograph of tridactyl footprint