This
Protichnites comes from the Krukowski Quarry, believed to be an
outlier of the Mount Simon Sandstone. This quarry is currently under
study as perhaps containing Ichnofossils of the earliest animals
to venture ashore during the Middle Cambrian. Among the different
trackway fossils found in this quarry (including Diplichnites,
Climactichnites,
and madusae
jelly fish), Protichnites is the rarest both in terms of dispersion
and absolute numbers. The sandstone slab here lacks ripples, suggesting
that the tracks were made on a sand flat well above the tide, rather
than underwater. This, in turn, suggests that the animal which made
Protichnites tracks could have been one of the Earth's first air-breathing
animals.
This
Protichnites specimen is unique among all I have seen from the Krukowski
quarry. The matrix is comprised of much finer sandstone that the
vast majority of the quarry horizons. This finer type of matrix
also contains the most well preserved madusae fossils. The Prototypical
tail or body appendage track in epirelief is thicker than most.
The most unique aspect of this specimen is apparent arthropod footprints
running parallel and on both sides of the specimen; these are very
subtle, wider than most Protichnites and difficult to discern in
bright light. They are, however, apparent in the side-lighted photography
used in the pictures below. It is reasonible to assume given the
lack on ripple that the track was made well above the high-tide
waterline, perhaps in a silty pond that would have allowed the more
subtle tracks to be made. Are the footprints and tail drags from
the same animal? Is the animal that made both the same as the one
that made the body impression at this link?
Or, is it a different ichnogenera, given that no similar trackway
has been found in the quarry?
Notable
in Protichnites is the prominent markings of a tail or other body
part being dragged; footprints, when present, are subtle by comparison.
The maker of these fossil trackways might have been an animal resembling
the extant but ancient horseshoe crab, except of an early design
that lacked a hard shell to be preserved. Others have posited that
Protichnites was a soft-bodied progenitor of the large, now extinct
group of early predators, the Eurypterids (Chalicerate "biting
claws" Arthropods). The "Eurypterid theory" is particularly
intriguing since it would imply that just as animals were first
moving to land to feed, hungry new predators were already on the
hunt. If a Eurypterid-like animal made these tracks, it would probably
have been an ancestor of the later eurypterids except with a soft
body with no exoskeleton to preserve.
Also
see: Cambrian
Shadows
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