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Dromillopus

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Journal Article
Published: 01 May 1996
Canadian Journal of Earth Sciences (1996) 33 (5): 710–714.
...David J. Mossman; Robert G. Grantham Abstract In 1990, a hypotype of the ichnospecies Dromillopus quadrifidus Matthew, 1905 was discovered preserved as a cast in a rockfall of fine-grained Pennsylvanian (Westphalian B) sandstone at Joggins, Nova Scotia. The hypotype of this tetrapod trackway, while...
Journal Article
Journal: PALAIOS
Published: 01 December 2014
PALAIOS (2014) 29 (12): 624–645.
... of channel abandonment, a wrinkled surface attributed to microbial mats was traversed by large arthropleurids ( Diplichnites cuithensis trackways). Closely associated are smaller Diplichnites gouldi trackways, probably made by myriapods, as well as tetrapod tracks ( Pseudobradypus ?, Dromillopus, Hylopus...
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A ) Specimen NSM 5364110. Block discovered at Coal Mine Point by Don Reid. ...
in > PALAIOS
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
Journal Article
Published: 01 May 2006
Journal of the Geological Society (2006) 163 (3): 561–576.
... ‘Temnospondyli’                  Limnopus vagux (HS, GM)                  Matthewichnus velox (GM)             Order Microsauria                  Dromillopus quadifidus (GM)                  Ornithoides trifudus (GM)     Series Amniota         Class Sauropsida             Order...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.265.01.08
EISBN: 9781862395138
... on optimal track morphology. The most striking example is the small temnospondyl track ichnogenus Batrachichnus , which includes tracks that have been called Anthichnium, Crenipes, Dromillopus, Nanopus, Salichnium, Saurichnites and many others ( Haubold 1996 ; Haubold & Lucas 2001 a ). Fig. 2...
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