Strophomena and Other Fossils 
31 
Numerous bryozoans and a few Rhynchotrema 5 ft. 
Strophomena vicina fairly common in a coarse-grained limestone. . 1 ft. 6 in. 
Dinorthis ulrichi, Rhynchotrema inaequivalve, and Hehertella frank- 
fortensis range throughout this section. Strophomena vicina 
occurs only within one foot of the top 6 ft. 
Interval. 1 ft. 
Crossing of farm road over railroad. 
Interval . . 2 ft. 6 in. 
Short railroad bridge, No. 31. 
Loose cherty specimens of Dinorthis ulrichi and Rhynchotrema near 
the top and Dalmanella at the base 5 ft. 6 in. 
One Strophomena vicina and Rhynchotrema in place 2 ft. 
Rhynchotrema and Herbertella frankfortensis 9 ft. 
Flanagan railroad station. 
This section undoubtedly belongs to the upper part of the Lex- 
ington limestone, probably the Paris bed. The nearest known 
outcrop of the Perryville bed is 28 miles southwestward, at Todd- 
ville, in Garrard county, and it is not known at present whether 
the Perryville bed and the overlying Cornishville bed may be 
traced beyond Toddville, northward; hence a more exact corre- 
lation is impossible. An interesting feature of the section along 
the railroad north of Flanagan is that it suggests the presence of 
Strophomena at a horizon 15 feet lower than that at which it is 
associated with Dinorthis ulrichi. Going northward along the 
railroad, Hehertella frankfortensis and Rhynchotrema inaequivalve 
occur at still higher levels, but the possibility of faulting can 
not be excluded. 
It should be noted that at Flanagan, the Flanagan chert be- 
longs immediately above the Strophomena vicina and Dinorthis 
ulrichi horizon. This is true also 4 miles northwest of Flana- 
gan, at the northern edge of the C. H. Bowyer farm, nearly a 
mile north of Becknerville. 
Strophomena vicina, associated with Dinorthis ulrichi and 
Rhynchotrema inaequivalve, occurs in the upper part of the Lex- 
ington limestone also, in the western edge of Valley View, half- 
way between Flanagan and Toddville. Twenty miles north- 
west of Flanagan, the same association of fossils, including also 
Hehertella frankfortensis, occurs at the G. C. Gorham quarry, 
4 miles northeast of Lexington, on the Newtown pike. Less 
than 9 miles northwest of the last locality, half a mile west of 
Georgetown, on the Franklin pike, Strophomena vicina and Di- 
northis ulrichi are found associated, but both are very rare. 
