240 



DESCRIPTION. 



Mijrcia havanensis Berry. r" 



Plate XI, figure 4 ; Plate XXVIII, figure 7. 



Myrcia havanensis Berry, " Torrey Bot. Club Bull.," vol. 43, p. 300, 1916. 



Eucalyptus attemtata Ward (not Newberry), " U.S. Geol. Survey, Fifteenth Annual Report,' 1 

 p. 371, 1895. 



Leaves linear-lanceolate in outline, falcate, about 9 centimeters in length by 1 centimeter in maximum 

 width, which is in the lower half of the leaf. Margins entire. Apex gradually narrowed, acuminate. 

 Base narrowly pointed, decurrent. Petiole very stout, tapering upward, 1-75 centimeters in length. 

 Midrib stout, curved. Secondaries numerous, thin, somewhat irregularly spaced, 2 to 6 millimeters apart, 

 branching from the midrib at angles of about 40°, running with but slight curvature to the well- 

 marked and nearly straight longitudinal vein which forms a marginal hem less than 0-5 millimeter from the 

 margin. Texture coriaceous. 



The present species is very close to some of the numerous forms which from time to time have been 

 referred to Eucalyptus Geinitzi (Heer) Heer. It is, however, distinct from that species, especially when 

 compared with Heer*s type or with the more typical Americal material. In general it is a smaller leaf, 

 has a larger and longer petiole and an outline less inclined toward ovate, and is "relatively much more 

 produced apically. It is typically Mt/rcia-Wkc in all of its characters and is readily distinguishable from 

 the forms from the Tuscaloosa formation which have been referred to Eucalyptus Geinitzi in this work. It 

 is confined to the basal beds of the Eutaw formation in Hale County, Ala., and the Ripley formation in 

 western Tennessee, and takes its name from the town of Havana, near which the leaf-bearing laminated 

 clays of this formation outcrop. A single specimen collected by R. T. Hill in 1891 at the big cut on the 

 Southern Railway east of Pocahontas, Tenn., and identified by Ward as Eucalyptus attenuata Newberry, 

 proves to belong to this species (pp. 125-G). 



D. Eucalyptus Geinitzi (He3r) Heer. 



Plate XXVIII, figure 8. 



(See the bibliography at p. 23G.) 



Eucalyptus Geinitzi Hollick, New York Acad. Sci. Ann., vol. 11, p. GO, pi. 4, figs. 1-3, 1898. The 

 Cretaceous Flora of Southern New York and New England, p. 96, pi. 35, figs, 1-8, 10-12, 1906. 



This species has a wide range. It was described originally from the Cenomanian of Moravia, and 

 has sine* orded from a number of other European Cenomanian localities, from the Atane beds 



of Greenland, the Dakota sandstone of the West, and from Martha's Vineyard to Alabama along the 

 Atlantic coast. It r;inys upward into the Black Creek formation of North Carolina, and is not ran; in the 

 Middendorf arkose member of the Black Creek formation of South Carolina. In Alabama the species 

 i not eommon, but this may simply be due to accidents of preservation, (pp. 126-7.) 



s. Eucalyptus latifolia Hollick. 



The Cretaceous Flora of Southern New York and New England, p. 97, pi. 36, figs. 1-5, 1906. 



p. 237.) 

 . . . An-.. . i, ag therefore, tliis species and Eucalyptus Geinitzi and 



/. ■< ■■, i i.: are referred to | [though it seems more probable that the.- represent the 



•'.' • -in.- family, or its ancestral stock, (p. 126.) 



