We then went to Central East See, T.J.S., R./E., or two miles east and 4 miles south of Ardmore. Here we collected a Permian like small fauna in a blue clay that is 2200 above the base of the Pennsylvanian or 4600 below the Spirifer alignment zone. This whole fauna is restricted to a zone 3 feet thick. See the small list of crinoid facts/ords. Nearly dark for a few pieces of Fusulina limetnes but the zone in place was not located; Other crinoidal linmetes seem daily associated. There's a fourth locality on the road side in A.W 1/2 See, 28 T.J.S., R./E., or two miles east and one mile south of Brock. This is in the vicinity of the Creicer Hills. It is the second limestone from the base of the Pennsylvanian on west side of Creicra hills anticlisis. Or about 350 feet above base of Penn. The fauna is a very small one and has Fusulina. In a muddy sand limestone with the crinoidal matter, not common. Nor does here a Spirifer canematus. Finally to another shale Permian like fauna in S. Central See, 4, T.J.S., R./E., or two miles south and 2 miles east of Ardmore. The zone is 600 feet