ANNUAL REPORT SMITHSONIAN INSTITUTION, 1914. 
284: 
From the evidence of the Lower Cambric life, to 
section is here broken between the tillite and the Cambric deposits, 
indicating that the age of the former is rather late Proterozoic than 
early Paleozoic. 
“OJOZOIOJOLT Poyepun ore sour] [eMoserp Aq po}vorpur sooue1M900 oY Ose PUL UIeI_ }eerH Ur eoueLIND0 
OL “OVP JOVX9 OY} 0} SB 4qnop st O10} Inq “o10z0I9}01g 948[ oq 0} posoddns st ‘deur sty} uo ojomo Aidume ue Aq wMoYs ‘aoue1mn990 ULIZIMION ITT, 
“UOVIDBIS O1IOZOIOJOIg jodew—e ‘vig * 
200! Ka) -091 
(fh) 
Gp 
NOD nal <) 
RSC Pet 
OLyNn os “ee 
See Aart tet TT 
“Poi Naa |. | | ga aH 
is time, the world 
we shall see that the waters of th 
) 
sented later 
over, were of tropical or subtropical temperature, conditions not at 
all in harmony with the supposed glacial climates of earliest Cambric 
time. 
e€ 
be pr 
