BrerRkY: MEsozoIC FLORA OF THE COASTAL PLAIN 193 
has been found in the Black Creek formation of North Carolina. 
The present occurrence is based on leaflets, while the type material 
from the Atane beds of Greenland included not only leaflets, but 
also characteristic nuts and supposed aments. The present is the 
most southerly known occurrence of this species. 
OccuRRENCE: Court House Bluff, Cape Fear River. 
SALICALES 
SALIX FLExUOSA Newb. Ann. N. Y. Lyceum g: 21. 1868 
This willow, which is very common in the Magothy formation 
in the northern and central coastal plain, occurs sparingly in the 
Black Creek formation. It is present also in South Carolina and 
Alabama. 
OccURRENCE: Prospect Hall, Elizabethtown, Cape Fear 
River ; Big Bend, Black River. 
SaLtix NEWBERRYANA Hollick, in Newb. Fl. Amboy Clays 
68. pl. 14. f. 2-7. 1896 
This serrate-margined willow leaf is present from the bottom 
to the top of the Raritan formation of New Jersey, but has not 
heretofore been found outside of that state. It is sparingly repre- 
sented in North Carolina. 
OccurRRENCE : Court House Bluff, Cape Fear River. 
Salix eutawensis sp. nov. 
Leaves lanceolate, somewhat falcate in some specimens, vari- 
able in size, from 5 cm. to 12 cm. in length and from 0.5 cm. to 
2.3 cm. in greatest width, which is in the basal half of the leaf. 
Base lanceolate. Apex gradually narrowed to the attenuate tip. 
Margin entire for a short distance below, above which it is very 
finely dentate, even in the largest leaves collected. Petiole short 
and moderately stout. Midrib moderately stout, becoming thin 
in the apical part of the leaf, inclined to be curved or somewhat 
flexuous. Secondaries very fine and numerous, branching from 
the midrib at an acute angle and curving upward, becoming in 
their terminal portions approximately parallel with the margin, 
sending short curved tertiaries to the marginal teeth and from sec- 
ondary to secondary. (PLATE 22, FIGURES I-II. 
This species is abundant at the upper Tar River localities but 
has not been detected at any other localities in the Black Creek 
