Tuzoia
sp
Phylum
Arthropoda, Subphylum
Crustacea, Class Malacostraca, Subclass Phyllocaridae
Geological
Time: Early Middle Cambrian, (~525 million years ago)
Size: Fossil
is 50 mm long
Fossil
Site: Comet Shale Member, Pioche Formation, Lincoln County, Nevada
| Description:
This unusual fossil is an example of a rarely-seen Phyllocarid known
as Tuzoia that comes from the Comet Shale Member of the Pioche Formation
of Nevada. Tuzoia Phyllocarids are classified as bivalved crustaceans,
and are known for their distinctively-reticulated carapace. This
deposit spans the transition of Early to Middle Cambrian which saw
the extinction of the Olenellid
trilobites. It is just younger than the comparable
material from the Chengjiana Biota
of Yunnan Province, China and just older than the Burgess
Shale Fauna of British Columbia, Canada. The genus is known
from the Burgess Shale and from Early/Middle Cambrian deposits of
Utah. Species are largely distinguished by the presence and placement
of spines on the carapace. Few examples of the genus are known from
more than the carapace, as seen here, with its intricate polygonal
decoration. Because of the manner of preservation, specimens are
often fairly faint, as is the case here. There is a partial trilobite
in the upper right corner of the first photograph. It is known as
Eokochaspis nodosa, a member of the order Ptychopariida,
family Ptychopariidae.
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