38 MEMOIRS OF THE NEW YORK BOTANICAL GARDEN 
It is unfortunate that in no instance have we found the cones and 
branches attached, but other investigators have also suffered the same 
disappointment. Thus Newberry remarks :33 “ Unfortunately, none 
of the specimens establish beyond all doubt the connection between 
the cones and the branches, but some of the cones are borne on 
pedicels which are marked with scales essentially like those of the 
branches under consideration | В. macrocarpum]." The cones figured 
by Newberry (1. c., pl. 7, figs. 3, 4, 6) are too imperfect for com- 
parison with ours, but his fig. 3 has a striking resemblance to the 
cone described and figured by Velenovsky under the name Pinus pro- 
topicea,?* from the Cretaceous deposits of Bohemia, where Brachy- 
phyllum likewise occurs, and the latter author also figures a basal por- 
tion of one of these cones (1. c., fig. 12) showing scales somewhat 
suggestive of ours; but all of the above mentioned figures represent 
specimens which are much larger. A cone found in the Drummond 
pit, depicted in fig. 10, Pl. 3, and described on p. 68 of this Memoir, 
should be incidentally mentioned here, as may be understood by 
reference to the discussion in connection with it. 
Locality: Androvette pit. Collected by E. C. Jeffrey and Arthur 
Hollick. Specimens in Jeffrey collection, Cambridge, Mass. 
Genus GEINITZIA Endlicher 
Geinitzia Reichenbachi (Geinitz) comb. nov. 
Plate 5, figs. 7-10; Pl. 8, figs. 3, 4; Pl. 16, figs. 2-4; Pl. 17, figs. 1-4; Pl. 18, figs. 1-4 
Ятаисатиез Reichenbachi Gein. Charakter. Schichten u. Petref. 
Sächs.-Böhm. Kreidegeb. 3: 98. pl. 24. f. 4. 1842. 
Geinitzia cretacea Endl. Synops. Conif. 281. 1847. 
Sequoia Reichenbachi (Gein.) Heer, Fl. Foss. Arct. 1: 83. pl. 43. f. 
Id, 2b, 5а, 5d, 544, 8, 8b. 1868.—Hollick, Monog. U. S. Geol. 
Surv. 50 (Cret. Fl. 5. N. Y. and N. Eng.) : 42. pl. 3. f. 4, 5 
1906. 
“Sequoia Couttsiz, Heer.” Hollick, Trans. М. Y. Acad. Sci. 12: 
30. pl. I. f. 5. 1892. 
The specimens which we have figured and included under the above 
name are unquestionably identical with most of the fossil coniferous 
* Monog. U. $. Geol. Surv. 26 (Fl. Amboy Clays): 52. 
^ Gymnosp. Böhm. Kreidef., зт. pl. 7. f. 4. 
