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Australia: The Land Where Time Began |
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Cambrian Explosion - Cnidaria The most basal cnidarian group are the Anthozoans,
burrows attributed to sea anemones being found near, and possibly below
the base of the Cambrian. It is possible that calcitic tubes and cones
found in the small shelly fauna may represent Cnidarians, though there
are other possible relationships. Body fossils that have been described
from the Fortunian-age, Stage 1, strata in China have been assigned to
sea anemones (Han et al.,
2010). A considerable degree of diversification of cnidarians by the
time of the basal Cambrian strata is suggested by the interpretation of
these exquisitely preserved polyps as stem-group hexacorals. In the
Chengjiang Fauna there are additional body fossils (Hou et
al., 2005). These fossils
have 12 tentacles and have a similar symmetry to extant scleractinian
corals, which have 6-fold symmetry. Undoubted pelagic cnidarians (Medusozoa)
have been reported from faunas that were exceptionally well preserved in
the Stage 4 Marjum Formation, Utah (Cartwright et
al., 2008)
and also from Wisconsin. A considerable degree of morphological
variety is shown by these forms, the features of some specimens
suggesting that had affinities with Cubozoa, some to Hydrozoa, and
others to Scyphozoa – the 3 major classes of crown medusozoans, though
none of these possible assignments are considered to be conclusive. It
has been concluded that only Scyphozoa can be recognised from the
Cambrian with any certainty (G. A. Young & Hagadorn, 2010), though some
of the specimens from Utah may represent hydrozoans. Among these fossils
the nature of the disparity suggests that there was a significant early
radiation or medusozoans which produced a variety of linages that were
morphologically distinctive, a common evolutionary pattern among
metazoans from the Cambrian.
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| Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading | ||||||||||||||