This article is about the Beaconites trace fossils. For the article on the Quaker controversy, see Quakers §Beaconite controversy.
Beaconites is an ichnogenus known from the Beacon Supergroup, Antarctica, comprising a large, segmented burrow, bearing superficial resemblance to the skeleton of a snake, and probably created by a worm-like organism "shovelling" the substrate out of its way. Some terminate in elliptical pits, around 1.5cm in diameter, presumed to represent burrowing activity. The producer of the trace is thought to have burrowed to a depth of no more than a few tens of centimeters.
Ichnospecies
B. antarcticus (Vialov, 1962) type fossil
B. capronus (Howard and Frey, 1984)
B. coronus (Frey et al., 1984)
B. fliformis (Uchman and Alvaro, 2000)
See also
Trace fossil– Geological record of biological activity
References
12Gevers, 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. JSTOR1302754.
↑Frey, Robert W.; Pemberton, S. George; Fagerstrom, J. A. (1984). "Morphological, ethological, and environmental significance of the ichnogenera Scoyenia and Ancorichnus". Journal of Paleontology. 58 (2): 511–528.