NO. II FORAMINIFERA OF VENEZUELA GRAVELL 25 



Lateral chambers regular in size and distribution, in center of test 

 about 10 layers in a tier on each side of the equatorial layer; length 

 of tier about 400 /x, therefore about one chamber to 40 /* ; length of 

 chambers about 50 to 80 /*. Some of the specimens have small pillars 

 in the central part of the test. 



Localities and geologic horison. — L. {LepidocycUna) canellei 

 Lemoine and R. Douville occurs in material from localities 4, 469, 

 476, 957, 960, 1042, 1043. 1206, Cerro Gauche, and possibly 204, 

 San Luis series, middle Oligocene. (See check list for associated 

 foraminifera.) 



L. {LepidocycUna) canellei also occurs at many places in Panama, 

 Jamaica, and Mexico. 



LEPIDOCYCLINA (LEPIDOCYCLINA) FORRESTI Vaughan 



Plate 3, fig. 6 



LepidocycUna (Lcpidocvclina) jorresti Vaughan (55, p. 3, pi. i, figs. 1-4; pi. 2, 



figs. 1-6). 

 LepidocycUna {LepidocycUna) forresfi \^aughan (57, p. 291). 



Specimens which differ in no significant characteristics from the 

 cotypes of LepidocycUna {LepidocycUna) forresti Vaughan (from 

 east of Lynch Point, Willoughby Bay, Antigua, West Indies) were 

 collected by H. G. Kugler from the San Luis series, middle Oligocene, 

 at locality 1206 near Agua Clara, District of Democracia, Falcon, 

 ^'enezuela. 



They are associated with L. {LepidocycUna) canellei Lemoine and 

 R. Douville. 



LEPIDOCYCLINA (LEPIDOCYCLINA) MACDONALDI Cushman 



Plate 5, figs. I, 2. 3 



LepidocycUna macdonaldi Cushmaii (12, pp. 94, pi. 40, figs. 1-6). 

 LepidocycUna macdonaldi Cushman (15, p. yj, pi. 34, figs. 1-3). 

 LepidocycUna {LepidocycUna) macdonaldi Vaughan (47, p. 797). 

 LepidocycUna {LepidocycUna) macdonaldi Vaughan (57, p. 288). 

 LepidocycUna {LepidocycUna) macdonaldi M. Rutten and Vermunt (41, p. 9, 

 pi. I, fig. 13). 



H. G. Kugler and L. Vonderschmitt collected limestone containing 

 this species from the following localities in the upper Eocene of 

 the State of Falcon, Venezuela: 12, 16, 148, and 149, from Gua- 

 characa, Guayaval series ; 163 and 165, from Cerro Campana, Cerro 

 Campana limestone, also out of the Guayaval series. 



