Anomalocaris
cf saron
Phylum Uncertain,
Family Anomalocarididae
Geological
Time: Early Middle Cambrian
Size (25.4
mm = 1 inch): Anomalocaris fossil is 22 mm long on a 55 mm by 38 mm
matrix
Fossil Site:
Pioche Formation, Comet Shale Member, Eokochaspis nodosa subzone, Lincoln
County, Nevada
Fossil Code:
MMT193
Price: Sold
Description:
This is a juvenile example of one of the “Terrors Of The
Cambrian” known as Anomalocaris. The members of this group
of enigmatic creatures are known from Asia, Australia, Europe,
and North America, and are thought by many to be closely allied
with the Arthropoda, a position not held by all researchers.
The spiniferous grasping appendages are strongly suggestive of
its carnivorous habits; some trilobites from Utah bear evidence
of bite marks that have been attributed to its near
relative Anomalocaris nathorsti. This example comes from a soft-bodied
preservation site known for some ten years. Two species are currently
known; A. pennsylvanica and A. cf saron. The fact that the cranidium
of a trilobite identified as Eokochaspis has been found at the
same level places it in the slightly younger strata that houses
A. cf saron. Both horizons are somewhat older than the celebrated
Burgess Shale of British Columbia. A few examples in a near complete
state have been found, but those are all four to five times the
size of this one at minimum. To my knowledge this is the first
time a juvenile of this taxon has been offered. The flattened
lobes by which this enigmatic creature propelled itself in search
of prey, and its large eyes are readily apparent, The grasping
appendage is only visible as a faint trace. It was either not
preserved or still buried within the matrix. I know from examples
I have had from Chengjiang that as these animals grew their appendages
became more robust, possibly indicative of a change in diet with
age. See my other examples for an Anomalocaris
grasping appendage of what was
obviously a much larger specimen.
Reference:
Journal of Paleontology, 77 (4), 2003, pp 674-690.
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