All the heavy rains have provided great collecting at the road cuts outside the city. The Ordovician fossils that are the most common is the brachiopod. This brachiopod is a Platystrophia of some type. What I found interesting was this Cornulites that anchored itself in the groove of the brachiopod shell. It is thought to be a tubicolous annelid worm that orientated itself for feeding. Since this one was pointing toward the shell opening, it probably attached and grew there while the brachiopod was still alive.
