FORAMINIFERA FROM DEEP WELLS 47 



Buliniiiia sp. 

 Plate 2. tit>:ure 3. 



There is an elongate species with very distinct somewhat re- 

 motely placed chamJjers which occurs at i6o feet in the well of J 

 Wiggins at Eustis, Lake County. 



Buliiiiina sf'. 

 _ Plate 2, figure 4. 



A species of fusiform shape and concave apertural face, with 

 the rounded aperture near the middle, occurs at 2,310 feet in the 

 well at Marathon. Genus BuliniincUa Cushman, 191 1. 



i fV. 



BulimincUa sp. ? 







Plate 2, figure 5. 



Specimens from brown limestone at 1,720 -feet in the well at 

 rathon are distinctive anc 

 iminclla clegantissiina group. 



Marathon are distinctive and are figured. They are of^^the Bid 



Biduninella sp. ? 

 Plate 2, figure 6 a, b. 



In the deepest part of the well at Marathon there occurred a 

 very low-spired form here figured, which seems like a ver}'- short 

 BuUniincUa of the B. elcganfissiiiia group, but very low. A some- 

 what similar form of much larger size is found in the deeper por- 

 tions of the well at 1.421 feet. 



Genus J'irguHna d'Orbigny, 1826. 

 Virgulina sguaiiimosa d'Orbigny. 



Virgulina squammosa d'Orbigny, Ann. Sci. Xat., vol. 7, 1826, p. 267, Mo- 

 deles, No. 64, 1826. Cushman, Bull. 71, U. S. Nat. Mus., pt. 2, 1911, p. 91, 

 fig. 145a, b; Bull. 103, U. S. Xat. Mus., 1918, p. 58, pi. 21, fig. 6. 



The only material which can be referred to this species is that 

 from the well of the Okeechobee Ice and Electric Co., Okeechobee, 

 Florida, at depths of 158-175 feet, and 240-245 feet. 



I have previously recorded it from the Miocene of the Gatun 

 formatio.n of the Panama Canal Zone. 



