(416 ) 
ANDROMEDA FLEXUOSA Newb. 
(PLATE 79, FIG. 2.) 
Andromeda flexuosa Newb. (Fl. Amboy Clays) Monog. U. S. 
Geol. Surv. 26: 121. pl. 34, f. 1-5. 
Formation and locality: Cretaceous shale; Glen Cove, Long 
Island, N. Y 
ANDROMEDA LATIFOLIA Newb. 
(PLATE 79, FIG. 3.) 
Andromeda latifolia Newb. (Fl. Amboy Clays) Monog. U. S. 
Geol. Surv. 26: 120. £1. 337, f. 6-10; pl. 34, f. 6-11; pl. 36, f. ZO. 
The variety of forms included under this species affords oppor- 
tunity for a wide range of reference. Our specimen may be most 
satisfactorily compared with Newberry’s p/. 37, f. 8, above quoted. 
Formation and locality: Cretaceous shale; Oak Neck, Long 
Island, N. Y. 
PREMNOPHYLLUM TRIGONUM Vel. 
(PLATE 79, FIG. I.) 
Premnophyllum trigonum Vel. Fl. Bohm. Kreideform. 3: 
4 [st]. pl 3 [48], f 2 
Although there can be but little doubt that our specimen is refer- 
able to this species the indicated relationship with the genus 
Premna must be considered as entirely problematical, especially 
in the light of our new material, which apparently represents two 
leaflets of a compound, pinnate leaf. Velenovsky subsequently 
changed the name to Cissophyllum exulum (Kvét. Cesk. Ceno- 
manu, 24. Z/. 6, f. 4, 5), concluding that it was more likely related 
to the genus C7zssus. Until, however, we are in a position to deter- 
mine the true botanical affinities with reasonable certainty it would 
hardly appear advisable to make any change in the original name. 
Formation and locality: Cretaceous shale; Glen Cove, Long 
Island, N. Y. 
Tricalycites major sp. nov. 
(PLATE 72, FIGS. 3-7.) 
Organism normally consisting of three entire, oblong-spatulate 
wings or ‘appendages, tri-palmately arranged and attached to a 
common nucleus by their bases, finely and closely striated longi- 
tudinally, middle one usually the largest, about 4 cm. long by 1.3 
cm. broad. 
These well-defined organisms are evidently generically identical 
