Pemphiz, Glyphea, and Areosternus. 143 
G. solitaria, Opp. Inferior Oolite, Wiirttemberg. 
G. pustulosa, Meyer. Inferior Oolite, Wirttemberg. 
. G. crassa, Opp. Inferior Oolite, Moselle. 
G. Martini, Etall. Callovian. 
. G. ornata, Quenst. (Orphnea). Callovian, Wiirttem- 
berg. 
11. G. Udressier’, Meyer (incl. G. Dressiert, Mey., Palin. 
squammifer, Desm., and G. Udressvert, Etall.). 
Oxfordian. 
12. G. Miinstert, Voltz (incl. Palin. Miinstert, Voltz, G. 
speciosa and Miinstert, Mey., G'. speciosa, Rom., 
and G. Miinstert, Etall.). Oxfordian. 
13. G. Regleyana, Opp. (incl. Palin. Regleyanus, Desm., 
G. Regleyana and vulgaris, Mey., Palin. longebrachi- 
atus, Desm., and G. Kegleyana, Ktall.). Oxfordian. 
14. G. Bronnz, Rim. Corallian. 
15. G. rostrata, Phill. 
16. G. Hialloni, Opp.,=G. rostrata, Etall. 
17. G. Perroni, Etall. Corallian. 
18. G. gratiosa, Meyer (Selenisca). Kimmeridge. 
19. G. pseudoscyllarus, Schl. (incl. Ast. fluviatilis, Bajer, 
Macrourites pseudoscyllarus, Schl., Scyllarus dubius, 
Holl, Orphnea pseudoscyllarus, striata, levigata, 
and pygmea, and Brisa dubia and lucida, Minst., 
Orphnea pseudoscyllarus and striata, Frischm. 
Lithographic stone of Solenhofen and Hichstadt. 
20. G. squamosa, Miinster (Orphnea). Solenhofen. 
21. G. tenuis, Opp. Hichstadt. 
22. G. Semanni, Opp. Lithographic stone of Cirin. 
23. G.jurensis, Opp. Kimmeridge. 
24. G. Meyert, Romer. 
In 1870 C. Schliiter (Neues Jahrb. 1870, p. 962) noticed 
Glyphea Lundgreni from the Lower Cretaceous of Sweden. 
Other Cretaceous species are G. neocomiensis, R.-Desy., G. 
cretacea, M‘Coy, and G. Cartert, Bell. Four years later the 
same author (Verh. naturh. Ver. Rheinl. und Westf. 1874, 
p- 48) fully described G. Lundgreni from Saltholm, in Swe- 
den, which may be identical with a Crustacean figured by 
Dixon. 
SONND 
IV. The Glyphez of the Teyler Museum. 
The Teyler Museum possesses ten slabs of the lithographic 
limestone of Bavaria, seven from Solenhofen, and three from 
Schernfeld, near Hichstadt, which present more or less com- 
plete remains of Macrurous Crustacea. No doubt these fossil 
