- Helicoplacus
Taxobox
name = PAGENAME
fossil_range =Early Cambrian
image_caption =
regnum =Animal ia
phylum =Echinodermata
classis =
ordo =
familia =
genus = PAGENAME
species = "H. guthi"
binomial =
binomial_authority ="Helicoplacus" (often misspelled "Helioplacus") is the earliest well-studied
fossil echinoderm. Fossil plates are known from several regions. Complete specimens were found in LowerCambrian strata of the White Mountains ofCalifornia . The animal turned out to be a cigar-shaped creature up to 7 cm long that stood upright on one end. Unlike more typical echinoderms such asstarfish , "Helicoplacus" does not have five-fold symmetry. Instead, there is a spiral food groove on the outside along which food was moved to a mouth that is thought to be located on the side. The respiratory system appears to be primitive. Although the animal does not look like a typical echinoderm, the plates are composed of the characteristic calcareous plates known as "stereom" that are common to all echinoderms. The ambulacral is related toEdrioasteroidea ; that is why Helicoplacoidea may belong toPelmatozoa .Other contemporaneous echinoderms are known to have existed from their dissociated plates, but other than a few possible edrioasteroids, "Helicoplacus" is the earliest echinoderm that is well enough preserved to analyze its characteristics. One much earlier form called "
Arkarua " has been hypothesized to be an ancestral echinoderm because of its five-fold symmetry. But "Arkarua " appears to lack both stereoms and a mouth. Helicoplacoids seem to have existed for about 15 million yearsfact|date=June 2007 in the Lower Cambrian, around mya|525.fact|date=June 2007Helicoplacoids are thought to have been suspension feeders living at moderate depths in highly-oxygenated water with strong enough currents to ensure a steady food supply. They are typically found in greenish
shale s and are rarely found in shallow watersandstone s andlimestone s.External links
* Pictures of 'Helicoplacus' can be found at http://www.usna.edu/Users/oceano/pguth/website/pl00001.htm
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