This
unique Cambrian inchnofossil comes out of a sensational sandstone
formation 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 Middle 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
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. If
verified to be Middle Cambrian, these ichnofossil 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 an upper bedding plane. 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.
While not as
sharp and distinct as the better specimens, this Climactichnites
is unusual compared with most owing to the curvature of the trackway.
The preponderance of Climactichnites are based on straight locomotion.
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