Australia: The Land Where Time Began |
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Aspidella,
Form genus from the Ediacaran – Morphology and Taphonomy
Aspidella
is a common disc-like form genus that is a member of the
Ediacara
Biota with global distribution. It is present prolifically, n>1,000,
in locally dense assemblages on the bases of sandstone beds in the
eponymous
Ediacara Member of the Rawnsley Quartz, South Australia.
Aspidella has been
interpreted as a holdfast of a frondose organism that was
Charniodiscus-like,
because of its association with stalks, fronds, and textured organic
surfaces (TOS), which in life had its holdfast secured within or beneath
a sandy
microbial mat with its stalk and frond protruding into the water
column above the substrate.
Aspidella exemplifies
faunal heterogeneity of bed-scale that was characteristic of Ediacara
fossil assemblages, being the dominant component of 4 fossiliferous beds
and a minor component of many others. Moreover,
Aspidella is
characterised by strong morphological variability, which included the
presence or absence of particular distinct features, including
preservation that was variable as external or internal moulds, relief
that was variable and a broad range of sizes. The distribution of
morphological characters is, however, not related to the size of
Aspidella or the
composition of its bed assemblage. In this paper Tarhan et
al. suggest that this
morphological diversity is not an expression of ontogenetic or
anatomical differences at species level, rather it is the product of
differential taphonomy that is related to substrate sedimentology and
biogenic factors, in particular the presence or absence of TOS which is
composed of Funisia, a eukaryotic tubular organism.
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Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading |