Skolithos trace fossil. Scale bar is 10 mm.
Skolithos (formerly spelt Scolithus or Skolithus[1]) is a common trace fossil ichnogenus whose original form consisted of approximately vertical cylinders. One well-known occurrence of Cambrian trace fossils is the famous 'Pipe Rock' of northwest Scotland. The 'pipes' that give the rock its name are closely packed straight tubes, which in this case were presumably made by a worm-like organism. The name given to this type of tube or burrow is Skolithos, which may be 35 cm[2] (14") in length and between 2[citation needed] to 5[2] cm (0.8 to 1.6") in diameter. Such traces are known worldwide from sands and sandstones deposited in shallow water environments, from the Cambrian Period () onwards. Some have a helical form.[3] Skolithos is typically marine,[4] but is also known from freshwater lacustrine settings.[2] Trypanites is a similar form but is excavated in hard substrates as a boring trace fossil. Also related are Ophiomorpha and Diplocraterion.
References[]
- ^ Gevers, T.W.; Frakes, L.A.; Edwards, L.N.; Marzolf, J.E. (1971). "Trace Fossils in the Lower Beacon Sediments (Devonian), Darwin Mountains, Southern Victoria Land, Antarctica". Journal of Paleontology 45 (1): 81–94. http://links.jstor.org/sici?sici=0022-3360(197101)45%3A1%3C81%3ATFITLB%3E2.0.CO%3B2-J. Retrieved on 2008-04-21.
- ^ a b c Woolfe, K.J. (1990). "Trace fossils as paleoenvironmental indicators in the Taylor Group (Devonian) of Antarctica". Palaeogeography, Palaeoclimatology, Palaeoecology 80: 301–310.
- ^ E. Volohonskya, M. Wisshakc, D. Blomeierb, A. Seilachera, S. Snigirevskyd and A. Freiwaldc. A new helical trace fossil from the Lower Devonian of Spitsbergen (Svalbard) and its palaeoenvironmental significance. doi:.
- ^ Trewin, N.H.; McNamara, K.J. (1995). "Arthropods invade the land: trace fossils and palaeoenvironments of the Tumblagooda Sandstone (? late Silurian) of Kalbarri, Western Australia". Transactions of the Royal Society of Edinburgh: Earth Sciences 85: 177–210.
