BERRY: MESOZOIC FLORA OF THE COASTAL PLAIN 185 
it is equally distinct from the various species of Protophyllo- 
cladus which have been recorded from the Raritan and later 
Cretaceous formations of North America. It seems equally dis- 
tinct from Z/znnfeldia but may possibly prove to be related to 
Moriconia. The comparisons of Androvettia statenensis with the 
Lower Cretaceous species Ctenopteris insignis, Zamiopsis insignis, 
Thinnfeldia marylandicum and FPlantaginopsis marylandica are 
singularly unhappy. The writer will show in another place that 
the last two are monocotyledons and the others either ferns or 
cycads and not even remotely related to the forms under discussion, 
OccuRRENCE: Three miles below Dunbars Bridge, Tar River, 
Edgecombe County. 
DAMMARA BOREALIS Heer (?), Fl. Foss. Arct. 6°: 54. 
Me Df Go A BSE 
This species was collected at the same timeas the Brachyphyl- 
dum referred to above and was likewise destroyed during shipment 
and is consequently queried, although there can be little doubt 
but that the specimens were of this species, which is so abundant 
at homotaxial horizons to the northward. It has also been dis- 
covered recently by the writer to the southward of North Carolina 
in the Tuscaloosa formation of Alabama. 
OccurRENCE: Court House Bluff, Cape Fear River. 
Sequoia REICHENBACHI (Gein.) Heer, FI. Foss, Arct £533 
pl. 23. f. 1d, 21, $4. “1868 
Characteristic twigs of this widespread Mesozoic conifer occur 
at a number of localities in North Carolina. They are indistin- 
guishable from the similar remains so common at a large number 
of localities in the Atlantic coastal plain. 
OccurRENCE : Rockfish Creek near Hope Mills ; Parker Land- 
ing, Tar River ; 92 mile-post, Neuse River. 
SEQUOIA MINOR Velen. Sitz. K. Bohm. Gesell. 1886: 638. 
f. rI-13. 1887 
This species, which was described by Velenovsky from the 
Cenomanian of Bohemia and based on cone-bearing twigs, is new 
to the American flora unless possibly the specimen from the New 
