
Parr V. Snor. ii. § L] RECENT OR HUMAN PERIOD. 905 
The fauna found in Paleolithic deposits is remarkable for a 
mixture of forms from warmer and colder latitudes similar to that 
already noted among the oa beds. It has been inferred, 




Ky Hh 




ao a 
ise 
Bis 




AMT: LN 
inh De 
ee 
mK >| {\ 
ABIL ir 
i ! t iyi Witty 1 
‘i \ SOT 
\ nity 
oy 7s 
muy 
i 
ae ul 
< 



ie 
ee 
22 SS 2 eee 
A ee ee =e Sea =f == 
=: =o Ba SRY <= = =e ey 2s 
: See Se 47 = 
So = SS = 
= SS ee 
ETE Mista Ba BE === 
= == Fe er Se 





* c— 
SSE 
A ———F 






sist mnt ni eh . r 
Se tas 
ul ae a OS 

Fic. 428.—Ficvre or Tur Mammoru 
Engraved on ivory by Cave-men, La Madelaine, France (Lartet, Reliquie Aquitan.). 
Ss = 
——FS 
= 
=— 
n= 
— 
—— 
= 






a PN A) esr 
! Oy eS < oy, 
Ve a SS 
C pny 
indeed, that the Paleolithic gravels are themselves referable to 
interglacial conditions. On fe one hand, we meet with a number 
of living species of warmer habitat, as "the lion, hyena, hippo- 
