TENTATIVE CORRELATION TABLE OF THE TERTIARY MARINE SEDIMENTARY FORMATIONS OF PANAMA. 



American 

 time sub- 

 divisions. 



Southeastern United Slates. 



Toro limestone. 



Manrhioneal 



formation. 



Kingston for- 



Pliocene of Guantanamo, Cuba. 



Pliocene of Yucatan 

 and Limon, Costa 

 Rica. 



Waccamaw marl, Nashua marl, 

 and Caloosahatchee marl (near- 

 ly contemporaneous). 



Yorktown formation, Duplin marl, 

 and Choctawhatchee marl (near- 

 ly contemporaneous). 



St. Marys formation. 



Choptahk formation. 



Calvert for- vr op . —„ . , 

 mation. Marks Hea n mnrl. 



Gatun formation. 



Zones G, H, 

 and I in San- 

 to Domingo. 



i Shoal River 

 member. 

 Oak Grove 

 member. 

 Chipola marl 

 her. 



Culehl'a 



forma- 



Culebraand 

 limestone at 

 Tonosi. 



Coral reef 

 at Guan- 

 tanamo, 

 Cuba. 



Antigua 



formation 

 (Antigua). 



Pepino 



formal ion 



(Porto 



Rico). 



Lower hor- 

 izon in 

 Santo 



Domingo. 



Chattahoo- 

 chee for- 

 mation. 



Tampa formation. 



and lime- 

 stone at Da- 

 vid (contem- 

 poraneous). 



Montpolier 

 white lime- 

 stone. 



Deposits with Pec- 

 ten aff. P. poul- 

 soni and large, dis- 

 coid orbitoids. 



Byram calcareous 



marl. 

 Monannn limi'sUme. 

 Red Bluff clay. 



Jambridge 

 formation. 



Richmond 

 formation. 



St. Bartholomew limestone (St. Bartholomew). 

 Widely distributed in Cuba; also in Haiti. 



mation of 



Nicaragua 

 (typical 

 Brito). 



Ocala limestone. 



Eocene of Tonosi. 



Claiborne 

 group. 



Gosport sand. 



Lisbon formation. 



Tallahatta buhi 



Halcbeligiiec forma- 

 tion. 



BashI formation. 



Tuscahoma forma- 

 tion. 



Nanafalia formation 



■uiAtua* Naheola formation, 

 group. Clayton limestone. 



nr 1 n«JS I i? rU o! ' '\> K ,' ,,mvi116 and referred to " Stampien iuferieur'-^ Vicksburgian-Lattorfian; Cushman thinks these deposits should be referred to the upper Eocene and placed 



"I' 1 "" ' ,hl ' "<■ ivirihnlniru'w )i, m ^ione in the table. 

 "May Mom: si i ;.u i;ji aphirnlly somewhat higher. 



« < oriviii! ion proposed by E. W. Berry. 

 37149—19. (To face page 595.) 



