6 RESEARCH IN CHINA. 
Dr. Henry Woodward reviewed, in 1905, the work of Dr. H. Monke’ and 
discussed some of the species occurring in a collection of fossils obtained from 
“West Shan-tung, and south of Tsing-tshou-fu, 36° 40’ N. lat., 118° 4o’ E. 
long.’’ A slab of the fossils from near Yen-tsy-yai is illustrated. 
Late in 1906 a short memoir by Dr. Th. Lorenz appeared? in which he 
described a number of new genera and species of Cambrian fossils collected by 
him in the province of Shan-tung and assigned stratigraphic horizons to them. 
The fauna from Lai-wu was worked out of a single block found loose in 
the bed of a brook about 9 km. west of Lai-wu. Lorenz concludes that the 
fauna represents the time of the base of the Swedish Andrarum limestone, 
within the limits of the zone with Paradoxides davidis and P. forchhammert.* 
The list of species given by him is as follows: 
Olenoides (Dorypyge) richthofeni (Dames) Amphoton steinmanni n. g. and sp. 
Agnostus fallax laiwuensis n. var. Ptychoparia (Solenopleura) sp. 
Agnostus parvifrons Linnarsson Hyolithes sp. 
Anomocare commune Nn. sp. Rhaphistoma broggeri Grénwall 
Anomocare ovatum n. sp. Acrothele bohemica (Barrande) 
Alokistocare sp. 
From the descriptions and illustrations I have identified the above as 
follows: 
Olenoides (Dorypyge) richthofeni (Dames) -++++-> = Dorypyge richthofeni Dames 
Agnostus fallax laiwuensis Lorenz: +++++++++5 = Agnostus chinensis Dames 
Agnostus parvifrons Linnarsson++++++++++++=Agnostus cf. parvifrons Linnarsson 
Anomocare commune Lorenz ++ +++serseeees = Anomocarella chinensis Walcott 
Anomocare ovatum Lorenz +++++++eseeeeee = Amomocare temenus Walcott 
Alokistocare sp. (not illustrated or described) 
Amphoton steinmanni Lorenz: ++ +++ sees eens = Dolichometopus deois Walcott 
Rhaphistoma broggeri Lorenz +++ +++++++eees = Platyceras willisi Walcott 
Acrothele bohemica Barrande+++++++++++ee-s = Acrothele matthewi eryx Walcott 
The horizon of the Dorypyge richthofeni fauna in Shan-tung was definitely 
established by Messrs. Willis and Blackwelder as in the Middle Cambrian 
below the central part of the Kiu-lung group.* In Shan-si the fauna occurs 
in an oolitic limestone that, by its fauna, is related to the Ch’ang-hia oolite.’ 
The fauna from Wang-tschuang occurs at three horizons. It is listed 
by Doctor Lorenz as follows: 
A lower layer with (a): Eighty meters higher up, a layer with (6): 
Anomocare speciosum Lorenz Teinistion (?) sp. 
Bathyuriscus asiaticus Lorenz Drepanura (?) sp. 
Agnostus fallax Linnarsson At 80 meters above, an upper layer has (c): 
Agnostus parvifrons latelimbatus Lorenz Shantungia buchruckeri Lorenz 
Acrothele granulata Linnarsson Liostracus latus Lorenz 

"On a collection of trilobites from the Upper Cambrian of Shantung, North China. Geological Magazine, 
London, new ser., Dec. V, vol. 1, 1905, pp. 211-215, 251-255, plate XIII. 
*Beitrige zur Geologie und Palzontologie von Ostasien unter besonderer Beriicksichtigung der Provinz 
Schantung in China. II, Paleontologischer Teil. Von Herrn Th. Lorenz in Marburg a. d. Lahn. 
Hierzu Taf. tv—vi u. 55 text fig. 
* Lorenz, 1906, p. 9I. ‘Blackwelder, 1907, p. 40. ‘Idem, p. 145. *Lorenz, 1906, p. 93. 
