Tribrachidium: Difference between revisions
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''Tribrachidium'' fossils are found in numerous locations throughout the world, including [[Newfoundland]], the [[Northwest Territories]], the cliffs along the shores of the [[White Sea]] in [[Russia]], and [[Ediacara Hills]], [[Australia]], where the first specimens were found. They show a disc-shaped creature about 5cm in diameter on average, with three curved "arms" extending from the centre to nearly the edge. These arms were probably hollow and could be inflated or deflated. This three-fold symmetry is almost unique in animals, which are usually either [[Bilateria|bilateral]]ly or [[radial]]ly symmetric. Fleshy ridges, or possibly loose filaments, extended from the edges of the arms and formed the rest of the body. |
''Tribrachidium'' fossils are found in numerous locations throughout the world, including [[Newfoundland]], the [[Northwest Territories]], the cliffs along the shores of the [[White Sea]] in [[Russia]], and [[Ediacara Hills]], [[Australia]], where the first specimens were found. They show a disc-shaped creature about 5cm in diameter on average, with three curved "arms" extending from the centre to nearly the edge. These arms were probably hollow and could be inflated or deflated. This three-fold symmetry is almost unique in animals, which are usually either [[Bilateria|bilateral]]ly or [[radial]]ly symmetric. Fleshy ridges, or possibly loose filaments, extended from the edges of the arms and formed the rest of the body. |
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Like many Precambrian-era fossils, the relationship of ''Tribrachidium'' to other animals is poorly known. To some extent it has become a [[poster child]] for the problem in general, often being shown as an example of that era's peculiar lifeforms. Among others, ''Tribrachidium'' has been described variously as a [[cnidarian]], [[lophophore]], [[echinoderm]], [[ecdysozoa]]n or even as an odd, outlying member of the [[dipleurozoa]] -- a proposed ancestor of the [[chordate]]s. Some have even speculated that it is not a complete animal |
Like many Precambrian-era fossils, the relationship of ''Tribrachidium'' to other animals is poorly known. To some extent it has become a [[poster child]] for the problem in general, often being shown as an example of that era's peculiar lifeforms. Among others, ''Tribrachidium'' has been described variously as a [[cnidarian]], [[lophophore]], [[echinoderm]], [[ecdysozoa]]n or even as an odd, outlying member of the [[dipleurozoa]] -- a proposed ancestor of the [[chordate]]s. Some have even speculated that it is not a complete animal, but rather the [[holdfast]] of a larger creature. Still others suggest that it was not an animal at all, but, either a protist, or the member of some now-extinct kingdom of multicellular organisms. |
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''Tribrachidium heraldicum'' was named and described by [[Martin Glaessner]] in 1959 in ''The Geology and Late Precambrian Fauna of the Ediacara Fossil Reserve''. Records South Australian Museum 13: 369-401. |
''Tribrachidium heraldicum'' was named and described by [[Martin Glaessner]] in 1959 in ''The Geology and Late Precambrian Fauna of the Ediacara Fossil Reserve''. Records South Australian Museum 13: 369-401. |
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Revision as of 17:17, 19 February 2007
| Tribrachidium heraldicum Temporal range: Ediacaran
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| File:Tribrachidium heraldicum.JPG | |
Fossil
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| Genus: | Tribrachidium
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| Species: | T. heraldicum
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Tribrachidium heraldicum ("Heraldic Three Arms") was an early Ediacaran organism famous for its bizarre tri-radial symmetry.
Tribrachidium fossils are found in numerous locations throughout the world, including Newfoundland, the Northwest Territories, the cliffs along the shores of the White Sea in Russia, and Ediacara Hills, Australia, where the first specimens were found. They show a disc-shaped creature about 5cm in diameter on average, with three curved "arms" extending from the centre to nearly the edge. These arms were probably hollow and could be inflated or deflated. This three-fold symmetry is almost unique in animals, which are usually either bilaterally or radially symmetric. Fleshy ridges, or possibly loose filaments, extended from the edges of the arms and formed the rest of the body.
Like many Precambrian-era fossils, the relationship of Tribrachidium to other animals is poorly known. To some extent it has become a poster child for the problem in general, often being shown as an example of that era's peculiar lifeforms. Among others, Tribrachidium has been described variously as a cnidarian, lophophore, echinoderm, ecdysozoan or even as an odd, outlying member of the dipleurozoa -- a proposed ancestor of the chordates. Some have even speculated that it is not a complete animal, but rather the holdfast of a larger creature. Still others suggest that it was not an animal at all, but, either a protist, or the member of some now-extinct kingdom of multicellular organisms.
Tribrachidium heraldicum was named and described by Martin Glaessner in 1959 in The Geology and Late Precambrian Fauna of the Ediacara Fossil Reserve. Records South Australian Museum 13: 369-401.
Together with two other tri-radially symmetrical organisms, Anfesta stankovskii, and Albumares brunsae, both from the shores of the White Sea, Tribrachidium belongs to the family Tribrachiidae.
Australia Post issued a 50 cent stamp featuring Tribrachidium on 21 April 2005 in a series entitled Creatures of the slime.
Links
- Palaeos dendrogram [1]
References
- Anatomical Information Content in the Ediacaran Fossils and Their Possible Zoological Affinities, Jerry Dzik, Instytut Paleobiologii PAN, Twarda 51/55, 00-818 Warszawa, Poland
- The Ediacaran Biotas in Space and Time, Ben Waggoner, Department of Biology, University of Central Arkansas, Conway, Arkansas 72035-5003
- McMenamin, Mark A. S. The Garden of Ediacara New York: Columbia University Press, 1998. ISBN 0-231-10559-2