214 
REPORTS ON ORDOVICIAN FOSSILS. 
By Frederick Cliayman, A.L.S. , &*c., Paleontologist, National 
Museum. 
Dr. Wolfenden’s Paddock, Parish of Painswick. Collected by Mr, 
W. H. Ferguson. Nos. 1909, 1913, 1914, 1916. 
A graptolite and some indeterminate (?)organic remains.—1909. 
Stephanella sp. (determined by Dr. T. S. Hall).—1913- 
In addition to Dictyonema sp., determined by Dr. T. S. Hall, there 
is a conical, concretionary body separated by transverse cracks, probably 
the cast of the abdominal somites of a crustacean.—1914. 
(?)Stephanella (determined by Dr. T. S. Hall).—1916. 
Age.—Lower Ordovician: probably at the base of the series. 
Parish of Barp. Collected by Mr. W. H. Ferguson. Nos. 7906,. 
1918, 1919, 1921, 1922, 1925, 1927-1929, 1932, 1936. 
(})Rhinopterocaris maccoyi. —1906, 1918, 1922, 1928. 
(})Crustacean remains.—1927, 1932. 
(?)Dictyonema (determined by Dr. T. S. Hall).—1919? *925, 1929. 
(})Dictyonema (determined by Dr. T. S. Hall) and (?)crustacean re¬ 
mains.—1921. 
No determinable fossil.—1936. 
Age.—Similar to the above. 
[Report sent in r 3.2.08 .] 
Shaly Mudstone, Painswick: near peg 415. Nos. 297-309, 312, and 
326-340. Coll, by Mr. W. H. Ferguson. 
Cast of a branching (?)monticuliporoid.—297-305. 
Small rounded bodies of a problematic nature, possibly of crustacean 
origin, 298, 299, 302, 307-309, 328, 330, 335, 338. 
Phyllocarid carapace and appendages, badly preserved. Probably 
allied to Rhinopterocaris.—$ 03. 
Carbonaceous remains of a crustacean allied either to Hymenocaris or 
Rhinoptero car is, with separated telson.— 329, 333. 
( ?)Appendage of a phyllocarid.—304. 
Organic remains, probably crustacean—indet.—312, 326, 327, 340. 
Fossil remains, indet.—300, 301, 306, 331, 334. 
Painswick: near peg 409. Nos. 310, 311, and 314-321. 
Remains of a (?)crustacean, probably allied to Hymenocaris (retained 
for further examination).—316, 318, 321. 
Obscure organic markings, indet.—310, 311, 314, 315, 317. 
Painswick: 12 chains W. of peg 364. Nos. 322-325 
(?) Crustacean remains and trails, indet. (Retained for further ex¬ 
amination.) 
Taylor’s, Painswick. No. 313. 
(?)Crustacean remains, indet. 
The above specimens are probably from the base of the Lower Ordo¬ 
vician. 
