This
unique Cambrian inchnofossil comes out of a sandstone
formation recently dubbed Blueberry Hill in Central Wisconsin
that was once a tidal beach, resulting in the distinctive ripples
you
see
on
the
matrix
surface. At present, it is generally accepted that the age of
this
sandstone unit is upper Cambrian and thus represents an outlier
of the Mount Simon Sandstone. This quarry has been producing some
intriguing trace or ichnofossils, including huge madusae,
tentacled jellyfish, Diplichnites,
Protichnites,
and the Climactichnites
ichnogenus you see here, among others.
The
depositional environment in this quarry varies from very shallow
marine
to aerial. This is very significant as the ichnofossils from this
locality may be the earliest evidence of large organisms and carnivores
abandoning their marine habitat to utilize the terrestrial environment.
These ichnofossils may pre-date the Cambrian-Ordovician trackways
from Canada just described in the May 2002 issue of Geology.
Climachtichnites
has been described as looking like the track of a motorcycle
that
drove across rippled sand. The ripples in the sandstone confirm
that the layer is a bedding plane that was once a Cambrian intertidal
zone. If Climachnichnites is a trackway, the traverse ridges can
be viewed as made by muscular undulation as the animal motivated
through the sand above the water. Also note the ridges on the margins
on the tracks, the same as the ridges that build on either side
of blade of a bulldoser. One theory of Climactichnites
is that it was made by a large slug, others believe a mullusk,
and still others
posit an animal in an unknown Phylum that did not survive much
beyond the Cambrian. There are two described inchnogenera, Climactichnites
wilsoni that has paired lateral ridges between which are
undulating bars and
furrows
oriented
at
an angle
to the direction of travel, and Climactichnites youngi that lacks
the paired lateral ridges and has only of undulating transverse
bars
and furrows
This
particular specimen is one of the largest Climactichnites fossils
to become available from the Krukowski quarry, where collecting
is no longer permitted. There are two straight Climactichnites
wilsoni trackways converging from one end to the other. They
overlay and diagonally cross a Climactichnites youngi trackway.
It took several hours with a gas-powered, diamond
blade saw to
cut
this
fossil
down
to its
current size,
and that does not include what it took to originally cut it out
of the quarry floor.
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