BERRY: MEsSOzOIC FLORA OF ATLANTIC COASTAL PLAIN 285 
thing is known of the later Upper Cretaceous floras of the Atlantic 
Coastal Plain. The forms identified with their geographical and 
geological ranges are shown in the following table: 
a it oats Syl | 
sis |, Ela lg] aya eB] .| 
as ff ay 3 - B/ 31 3/ a 53]/ @] a 
Po Soe het pe 4a Els e/ eo} 3/@| 3/8 
Pf 1e3/9R [2] 21 al 2] 2] 4/3] 8\ 6 
& lpolacl @\é ae Be ae Gi 21.4) 91.8 
agzindi 3 21318) 218/93] 3] 2) 8 
le 3\2 8] Sieg] 8) 3 2) 3,5, 48| 8 g| 
po es EES ee Ee 
a ate 
oo Ope eae ~ — Milas eps sed ee 
Sabalites sp............. tind s bef OR: Laie ed eek ae hehe es oe Dake 
Morice riplyensi pe ated OF Se epee sean a as 
Salix eutawensis.......... i Ge BA ey Ben sg voles En 
Siphivem wr adia ie oes ene ae ae eB 
Ficus crassipes........... |x| Xj.+-) X X |. es 
Ficus Krausiana........... io x fof MEX | 
Ficus ovatifolia........... x xX |.-- | x | xX |: bee 
al OO SMM 6 oie's West Ml cl eeoes ek So Ged tes heey pel ae 
Cissites crispus........... Bes eae Pe hd ae 
Bauhinia ripleyensis ...... ee ets fee 
Manihotites georgiana... .. Me POR Se Le SE ls 
St nina t | | 
tennesseensis........... lis pe Pee tenes A | 
Pleat perectic tes abacsoay ane +] RK foeefee eters Peace i ee 
ene elegans...... [MR]. fee ef x | xX ed Lie 
m Heerit...... eG ey ar Chel Oe eee 
Cae ach ve pee ts 4 PS aL Oe Pare Gases eee sede e | 
Malapoenna horveliensis. bth [owe tere bow vie Siete 
Myrcia havanensis........ aed Set ve els eh 
Eugenia (?) anceps Py eee free] M fee aleeeleee ee 
Andromeda Wardiana..... xX HK foes} oe ae 
Andromeda novae-caesareae.. X|...|... 4 | x | Xx bse | ne 
Diospyros primaeva........ e. ies Xo) X ae | | x 
Halymenites major Ges pak Oe oe ee oe eae 
This flora as at present known comprises Ses sieoas et 
of which Sabalites sp., Cinnamomum sp., and sii 4 — : 
are poorly characterized. Halymenites major is ated : sae 
plant but it is a very characteristic object common in the 
United States in the Colorado and Montana series. se 
The Tennessee Cretaceous flora is remarkable in not cee 
any traces of ferns or gymnosperms. When the tf rns is 
Coarseness of the sediments is considered the absence 0 a an 
not to be wondered at, but such sediments usually aes hide 
abundance of coniferous twigs and with further pane Lee 
should be discovered. The presence of considerable amber 
