Ediacaria is a fossilgenus dating to the Ediacaran Period of the Neoproterozoic Era. Unlike most Ediacaran biota, which disappeared almost entirely from the fossil record at the end of the Period, Ediacaria fossils have been found dating from the Baikalian age (850–650 Ma) of the Upper Riphean[3] to 501 million years ago, well into the Cambrian Period. Ediacaria consists of concentric rough circles, radial lines between the circles and a central dome, with a diameter from 1 to 70 cm.
Ediacaria is possibly a synonym for Aspidella terranovica described in 1872. Although Ediacaria is one of the first described organisms from the Precambrian, Aspidella was described earlier, although its age was not understood to be Precambrian. As Aspidella is apparently a form taxon, Ediacaria may yet be valid and denote one specific genus among several that seem to make up Aspidella. Spriggia wadea is quite likely a synonym of Ediacaria (and consequently, possibly Aspidella); the differences seem to be merely due to different substrate in which the animals were embedded. (Gehling et al. 2000)
Ediacaria was often classified as a jellyfish (a ScyphozoanCnidarian), and has also been interpreted in many of the categories postulated to house the Ediacaran biota. A conspicuous filamentous microstructure preserved in some pyritised specimens suggests that it may have been a microbial colony, which disrupted the surrounding microbial mat to create the distinctive pattern (Grazhdankin, 2007).
^M. A. Fedonkin, J. G. Gehling, K. Grey, G. M. Narbonne, and P. Vickers-Rich. 2007. The rise of animals: Evolution and diversification of the Kingdom Animalia. The Johns Hopkins University Press, Baltimore, MD 1-326 [M. Laflamme/M. Laflamme/M. Laflamme]
Crimes, T.P.; Insole, A. & Williams, B.P.J. (1995): A rigid-bodied Ediacaran biota from Upper Cambrian strata in Co. Wexford, Éire. Geological Journal30(2): 89-109. doi:10.1002/gj.3350300202 (HTML abstract)
Gehling, James G.; Narbonne, Guy M. & Anderson, Michael M. (2000): The first named Ediacaran body fossil, Aspidella terranovica. Palaeontology43(3): 427-456. doi:10.1111/j.0031-0239.2000.00134.xPDF fulltext
Grazhdankin, D. (2001): Microbial origin of some of the Ediacaran fossils. GSA Annual Meeting 2001: Paper 177-0. HTML abstract
Lindsley-Griffin, Nancy; Griffin, John R. & Farmer, Jack D. (2001): Paleogeographic links between Yreka Terrane (Klamath Mountains, Northern California) and Alaska's Nixon Fork and Alexander Terranes. GSA-AAPG-SPE Meeting 2006: Paper 24-6. HTML abstractArchived 2012-02-04 at the Wayback Machine
Pickerill, R.K. (1982): Cambrian Medusoids from the St. John Group, southwestern New Brunswick. Geological Survey of Canada Current Research Part B.82(1): 71-76.
Sprigg, R.C. (1947): Early Cambrian(?) Jellyfishes from the Flinders Ranges, South Australia. Transactions of the Royal Society of South Australia71: 212-224. PDF fulltext
Stasinska, A. (1960): Velumbrella czarnockii n. gen., n. sp. - Meduse du Cambrien Inferieur des Monts de Sainte-Croix. Acta Palaeontologica Polonica5: 337-346.
Vanguestaine, Michel & Brück, Peter (2005): A Middle Cambrian age for the Ediacara-type fauna from the Booley Bay Formation, County Wexford, Ireland: new acritarch data and their implications. In:Steemans, P. & Javaux, E. (eds.): Pre-Cambrian to Palaeozoic Palaeopalynology and Palaeobotany. Carnets de Géologie / Notebooks on Geology, Memoir 2005/02, Abstract 11 PDF fulltextArchived 2016-03-03 at the Wayback Machine
External links
Peripatus Home Page: Ediacaran Survivors. Version of 2006-MAY-10. Retrieved 2007-JUN-06.