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 is sometimes considered
to meet the criteria for a Lagerstatt. 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 was likely
deposited during periodic episodes of heavy siltation that
buried deceased members of the diverse ecosystem.