88 PKOCEEDINGS OF THE NATIONAL MUSEUM vol.77 



be an abnormal form, because its last chamber is added on the same 

 side as the former one. Such an abnormality often occurs in the 

 Poly morphinidae . 



Distribution. — Fairly common in the various European Tertiary 

 deposits, although it occurs in other continents and as a Recent 

 species. 



Recent. — Tripoli. 



Pliocene. — England, Crag of Sutton. 



Miocene. — France, Helvetian, Pontlevoy; Moulin de Minoy, 

 Salles; Aquitanian superieur, St. Avit, near Mont de Marson; 

 Burdigalien superieur, Merignac; Burdigalien moyen, Le CoquUlat, 

 Leognan. Hungary, Tortonian, Varpolata (very abundant); La- 

 pugy. Austria, Perchtoldsdorf, near Vienna. United States, Choc- 

 tawhatchee formation, 1 mile east of Red Bay, Walton County, Fla. 



Oligocene. — Germany, Ahnatal, near Cassel; Hermsdorf, near 

 Berlin; Hildesheimer Wald, Dickholzen; Doberg, near Biinde. 



Eocene. — England, Bracklesham bed XVIII, White Cliff Bay, Isle 

 of Wight; Thanetian, Pegwell Bay. France, Lutetien, Grignon. 

 Belgium, lower Eocene, Wansin. United States, Cooper marl, dump 

 heap from Charleston Aqueduct tunnel, 1 mile west of Givhans, Dor- 

 chester County, S. C; pit on United States Highway No. 17, three- 

 fourths mUe west of Moncks Corner, Berkeley County, S. C. 



GLOBUUNA ROTUNDATA (Bornemann) var. PYRULA (Fornasini) 



Plate 15, figures 5 a-c 



Polymorphina rotundata Bornemann var. pyrula Fornasini, Mem. Istit. 

 Bologna Accad. Sci., ser., vol. 9, 1900-1902, p. 67, fig. 19 (in text). 



Variety differing from the typical in having spines at the initial 

 end. 



We can not find any specimen like the present variety in our 

 collection; therefore we have copied Fornasini's figures here. 



GLOBULINA TRISERIALIS Cushman and Ozawa, new species 



Plate 22, figures 1, 2 



Test globular to oval, more or less acute toward the initial end, 

 circular in cross section; chambers numerous, rounded, much em- 

 bracing, arranged in an almost triserial series, each succeeding cham- 

 ber farther removed from the base; sutures not depressed, often 

 obscured; wall smooth, but often the last-formed chamber finely 

 spinose; aperture radiate. 



Length 0.40-0.70 mm.; breadth 0.33-0.45 mm.; thickness 0.28- 

 0.35 mm. 



Eolotype. — (Cushman Coll. No. 11653.) From the Miocene, 

 Helvetien, Salles, Moulin de Minoy, France. 



