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''Ausia fenestrata'' is a curious Ediacaran period (630 – 542 million years ago) fossil represented by only one specimen 5 cm long from the Nama Group, a Vendian to Cambrian group of stratigraphic sequences deposited in the Nama foreland basin in central and southern Namibia.〔 It has similarity to ''Burykhia'' from Ediacaran (Vendian) siliciclastic sediments exposed on the Syuzma River of northern Russia.〔(IGCP 493 Annual Report 2003 )〕〔〔 This fossil is of the form of an elongate bag-like sandstone cast (Nama-type preservation) tapering to a cone on one end. Surface of the fossil is covered with oval depressions ("windows") regularly spaced over the surface in the manner of concentric/parallel rows. The taxonomic identity of ''Ausia'' is unresolved. ==Interpretations== * G. Hahn and H.D. Pflug suggested that ''Ausia'' is a pennatulacean coral from the Veretillidae family, but there are no signs of secondary polyps on the fossil, which are nonetheless represented in Hahn and Pflug's reconstruction.〔 No veretillids are represented in the fossil record as far as is known. * Some researchers have assumed that these depressions are pores and interpreted ''Ausia'' as an ancestor of archeocyathans and other sponge-like organisms〔M. A. Fedonkin (1996). "Ausia as an ancestor of archeocyathans, and other sponge-like organisms". In: Enigmatic Organisms in Phylogeny and Evolution. Abstracts''. Moscow, Paleontological Institute, Russian Academy of Sciences, p. 90-91.〕 or real sponge.〔Mark A. S. McMenamin (1998). "The Sand Menagerie". In: ''The Garden of Ediacara: Discovering the First Complex Life''. Columbia University Press. New York. pp.11-46.〕 But Adolf Seilacher has argued that the "windows" are merely dimples.〔 * ''Ausia'' may represent ascidians (sea squirts), an invertebrate group related to the chordates.〔〔Vickers-Rich P. (2007). "Chapter 4. The Nama Fauna of Southern Africa". In: Fedonkin M.A., Gehling J.G., Grey K., Narbonne G.M., Vickers-Rich P. ''The Rise of Animals: Evolution and Diversification of the Kingdom Animalia'', Johns Hopkins University Press. pp. 69-87〕 Results of a new study of a ''Burykhia'' from Russia have shown a possible affinity of these organisms to the ascidians, which are urochordates. The Russian species is more than 90 mm across, and the rows of oval depressions are separated by structures which were probably grooves in the internal wall surface of the living organism. The study's authors interpret these fossils as the internal sand casts of a vast bag-like cavity, possibly a pharynx or branchial basket.〔M.A. Fedonkin, P. Vickers Rich, B. Swalla, P. Trusler, M. Hall. (2008). "A Neoproterozoic chordate with possible affinity to the ascidians: New fossil evidence from the Vendian of the White Sea, Russia and its evolutionary and ecological implications". HPF-07 Rise and fall of the Ediacaran (Vendian) biota. International Geological Congress - Oslo 2008.〕 The animals represented by these two genera were thought to live in the shallow waters of an epicontinental sea, slightly more than 555-548 million years ago, and the authors feel this is probably the oldest evidence of the chordate lineage of metazoans.〔 * Jerzy Dzik has suggested that ''Ausia'' bears some similarity to the halkieriids, and resembles the body plan that might be expected of halkieriid ancestors under the coeloscleritophoran hypothesis. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Ausia (animal)」の詳細全文を読む スポンサード リンク
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