Bear
Gulch Limestone - Heath Shale Formation
The
Bear Gulch Limestone in Montana is fossiliferous strata
dating
to the Mississippian epoch of the Carboniferous period,
at some 318 million years ago. The site meets the stringent
criteria
for a Lagerstatte,
with a diverse Mississippian biota of vertebrate and invertebrate
fossils. The site is most famous for its diverse fishes
that includes members of Orders Chondrichthyes (cartilaginous
fishes), Actinopterygii (ray-fin fishes)
and Sarcopterygii (lobe-fined fishes).
Sediment
studies suggest that fossil formation occurred in
mudflats and lagoons having fresh to brackish waters. The
fossils comprise diverse fishes and less abundant invertebrates,
sometimes preserved in exquisite detail consistent with inhibited
decay in a silty and oxygen-starved bottom. The limestone
is some 30 meters thick and covers about 25 square miles,
and is posited to have been deposited during periodic
episodes of heavy siltation
that
buried
deceased
members of
the diverse ecosystem.