﻿GEOLOGY AND PALEONTOLOGY OF THE CANAL ZONE. 495 



The lower end of each specirnen and the tops of Nos. 3 and 4 are 

 l)rokon. Some eoralla are, evidently formed of rather tliin, branching 

 plates. 



Calices polygonal, usual diameter 3 mm., young calices about 2 

 mm. in diameter, an occasional large one as much as 4 mm.; depth 

 from 1 to 1.25 mm.; separated by walls from 0.75 to 1.25 mm. thick. 

 The walls are crossed by costae and usually form a fairl\' regular 

 network around the calicular cavities, but in places there is con- 

 siderable intercalicular reticulum. In places there are low, rather 

 indefinite ridges which may extend the length of as many as four 

 calices. The tops of the walls are rounded or subacute. 



The septa are normal gonioporid in number- and arrangement; 

 they are thick at the wall, becomes thinner toward the center; 

 their upper part narrow, gradually sloj)ing to the columella tangle, 

 which is joined by the primaries a7id secondaries; margins with about 

 fine dentations. 



Columella tangle not very conspicuous. 



Localit;/ and geologic horizon. — Canal Zone, station G016, quarry in 

 the Emperador limestone, Empire, collected by T. W. Vaughan and 

 D. F. MacDonald. 



Anguiila, station ()96G, middle bed. Crocus Bay, collected by 

 T. W. Vaughan. 



Cotj/jfes.—'N OS. 325052, U.S.N.M. (3 specimens). 



I am not certain the (r. canalU is really different from G. impera- 

 foris. 



GONflOPORA PORTORICENSIS, niw species. 



Plate 140, figs. 4, 5. 



Corallum ramous, branches rounded in cross section or very com- 

 pressed, a bi-anch of the latter form is 34 mm. wi(h^ with a maximum 

 thickness of about 9 mm. 



Calices poh^gonal, shallow, usual diameter 2 mm. The outer ends 

 of the septa are flattened and fused together, separating the calicular 

 depressions by a wall about 0.5 mm. thick. 



vSepta deUcate, very perforate, iii three complete cycles. Margins 

 finely and delicately denticulate; about five small thin teeth on a 

 long septum. Pali appear to be poorly developed, not specially 

 differentiated from the ordinary septal dentations. 



Columella weakly developed. 



Locality and geologic occurrence. — Porto Rico, station 3191, 4 

 miles west of Lares, Pepino formation, collected by R. T. Hill. 



Antigua, stations G854, Rifle Butts; 6881, Willoughby Bay, in the 

 Antigua formation, collected l)v T. W. Vaughan. 



Type.—^o. 325061, U.S.N.M. 



Paraiype.—^o. 325060, U.S.N.M. 



