Dall for callinc- the '.Lamps. ..... -..a Cli eocene, altlioap;h, as 



Dall (1) 'nas replied, "ooth e that it re-orecents at leact 



(1). Dall, .. .-., --CJ. .-_]. • . ---on, vol. l-^ , nt. 1, 

 p. 58, 1916. 



the lower part of the Aqr^itanian. It is of interest to ohserve 

 that ac Ic - -' "" .Joiiville (2), in a notice concerning 



(g). Bull. SoG. 3eol. France, r'rd cer., vol. 1:6, p. 58'D, loOS. 



Panama paleontology-, calle-'' .■^'-■^-entio-. ^^ ^>i'- '"^ot thst althonp-h 

 the lo7'er :.art of the Bordeaux depoeito ii. ian, the na.jor 



pert is Bixrdigalian anr'^ " vtian, that .'. , ouote:"^ Lliocene. 



In oormecti on with his recent work on the foraminifera of Trini- 

 dad (3) and Panama (4), \7herehy Is has differentiated several 



(5). Gompt . 3pnd. Acad. Sci., vol. lol, pp. .'.-..7, 'v.^-, 1915. 



(4). Oor.TOt. Rend. 3oc. CgOl. Prance, no. 19, op. 129-151, Dec, 

 1915. 



Stampian and Aqiiitanian horizon>3, he continues to -■ the 



rrincipr.l xlntillean horizons Burdigaliaii. 



In the '.Tagner Institnte Papers Dall, ■ ' ' o had r^ade a 



s)relininar3^ suriT'ej- of the Bowden fauna and descriher! nianj' of its 

 new Gpecies, correlated the fauna "perhaps v/ith the Oak Orove 



