20 RESEARCH IN CHINA. 
CHINESE LocALItigés—Continued. 
C32. See also C32’, other drift blocks at the same locality. 
Middle Cambrian: A fine-grained bluish-black limestone bowlder believed to have 
come from the lower part of the Ki-sin-ling limestone [Blackwelder, 1907), p. 
272], collected in river drift 1 mile (1.6 km.) south of Chén-p’ing-hién, on the 
Nan-kiang River, southern Shen-si. 
Obolus shansiensis Orthotheca doris Aluta enyo Aluta sterope 
Dicellomus parvus Microdiscus orientalis Aluta eris Aluta woodi 
Acrotreta shantungensis Aluta bergeroni Aluta fragilis 
32’. See C32, another drift block at the same locality. 
Lower Cambrian; A limestone bowlder collected in river drift 1 mile (1.6 km.) south 
of Chén-p’ing-hién, on the Nan-kiang River, southern Shen-si. 
Two species: Obolella asiatica and Hyolithes sp. undt. 
C33. Upper Cambrian: About 100 feet (30 m.) above the base of the Ch’au-mi-tién lime- 
stone, 9 miles (14.4 km.) north of Sin-t’ai-hién, Shan-tung. 
One species, Ptychaspis sp. (free cheeks and fragments). 
C33a. About same horizon as C11, different section. 
Upper Cambrian: Talus near the base of the cliff of Ch’au-mi-tién limestone [Black- 
welder, 19074, p. 41, part of the last list of fossils], 9 miles (14.4 km.) north of 
Sin-t’ai-hién, Shan-tung. 
Two species: Chuangia batia and Anomocarella bergioni. 
C34. About same horizon as C38, C41, and C49, different sections. 
Upper Cambrian: Purplish-gray limestone about roo feet (30 m.) above the base of 
the Ch’au-mi-tién formation [Blackwelder, 19074, p. 36, part of the first list of 
fossils] in road at northeastern corner of small village near Ch’au-mi-tién, Ch’ang- 
hia district, Shan-tung. 
Pagodia macedo A gnostus sp. undt. Piychas pis ceto Illenurus canens 
C35. Below C25, same section. 
Middle Cambrian: Upper part of the Ch’ang-hia limestone [Blackwelder, 19074, p. 33, 
fifth paragraph], at Ch’au-mi-tién, Ch’ang-hia district, Shan-tung. 
One species, Menocephalus acis. 
C36. About same horizon as C45, different section; about same horizon as C50, same 
section; above C68, same section; about same horizon as C47, same section. 
Upper Cambrian: Upper part of the Ch’au-mi-tién limestone [Blackwelder, 19074a, p. 
36 (part of the third list of fossils), and fig. 9 (bed 2), p. 35], at Ch’au-mi-tién, 
Ch’ang-hia district, Shan-tung. 
Two species: Billingsella pumpellyi and Anomocarella baucis. 
C37. About same horizon as C72, same section; about 50 feet above C71, same section; 
about 200 feet below C 73,same section; about 225 feet below C74, same section. 
Middle Cambrian: Upper part of the Ki-chéu limestone,’ in dense black limestone 
nodules in green-gray shales 10 feet (3 m.) below the base of the cliff limestone, 
8 miles (12.8 km.) south of Ting-hiang-hién, Shan-si. 
Obolus shansiensis Acrotreta shantungensis Anomocare megalurus 
C38. About same horizon as C34, C41, and C4o9, different sections; below C43, same 
section. 
Upper Cambrian: Crystalline limestone near the base of the Ch’au-mi-tién limestone 
[Blackwelder, 1907a, p. 36, part of the first list of fossils], at Ch’au-mi-tién, 
Ch’ang-hia district, Shan-tung. 
Coosia carme Ptychas pis ceto Illenurus canens 
Ptychas pis brizo Hysterolenus sp. Illenurus ceres 
‘The fossils from this locality are not listed, but the presence of Cambrian strata at the locality is men- 
tioned by Willis and Blackwelder [1907, p. 146]. 

