442 .MESOZOIC FLORAS OF rMlFD STATES. 



Weight in 

 kiloKnitns. 



W. C, B., Xo. 14SS, the Riddlo fragment. 7.n:! 



W. C. B., No. 14S9, t.ho Mufinider fra<,nn!'iit :;. 11 



W. C, B., No. 1658, the Comofiys fragment 1 . (»•_> 



W. C. B.. No. .■?046. the Tnrner trunk ("ehieken trough") !). (i4 



W. C. B., No. .3122, the Cole fragment .211 



W. C, B.. No. .3326, the R. T. Donaldson fragment, No. 4 .6] 



W. C, B., Xo. 3327, the R. T. Donaldson fragment, No. .5 , .31 



W. C, B., No. 3346, the Enunoas fragment 3. 20 



W. C, B., No. 3347, the Odensoss fragment 1 . 80 



W. C, B., No. 3350, the R. W. Clark fragment _* .17 



W. C. , B. , No. 6346, the Andersoi\ fragment 1 . .")<) 



W. C, B., No. 6347, the Tnglehart fragment, No. 2 3. 06 



W. C, B.. No. 6348, the R. P. Disney fragment. No. 2 1 . OS 



W. C. B., Xo. 63.52, the R. P. Disney trunk, No. 2 3. .57 



M. G. S.-W. C, B., No. 9051, the Whitehead trunk, Xo. 2 •_ 9. 30 



M. G. S.-W. C, B., No. 9053, the R. T. Donaldson fragment. No. 10 . 51 



M. G. S.-W. C, B., No. 9056, the R. T. Donaldson fragment No. 12 .15 



M. G. S.-W. C, B., No. 9061, the Marlowe fragment. No. 3 .14 



M. G. S.-W. C, B., No. 9062, the R. T. Donald.son fragment. No 15 . 58 



M. G. S.-W. C, B., No. 9064, the R. T. Donaldson fragment. No. 16 .45 



PI. LXXXVI shows the outer surface of the South CaroHiia CoUege 

 cycad sent me by Mr. Glenn, an account of which was given in the 

 historical part of this paper (see p. 414.) It is a triangular frag- 

 ment from one side of a rather large, short, subconical, laterally and 

 perhaps vertically compressed trunk. It evidently comes from near 

 the base, but no part of the true base is preserved. It extends inward 

 to the inner wall of the woody zone. The small end of the wedge is 

 downward and the specimen broadens upward. The radial fractures 

 are nearly even; the upper fracture passes ol)liquely upward and out- 

 ward, becoming horizontal near the surface; the basal fracture is a 

 small, irregular area. The specimen is in a fair state of preservation, 

 of a reddish-brown color, rather soft, and nearly uniform consistency 

 and low specific; gravity. The length or height parallel to the axis is 

 22 cm. The maximum tangential width (near the upper end) is 25 

 cm. and the minimum at the lower end 6 cm.' These measurements 

 are on the outer surface. The greatest distance across the concave 

 inner surface is 12 cm. The thickness measured on the radial frac- 



