CHAP. X.] THE PALZARCTIC REGION. 225 
ORIENTAL GENERA—continued. 
TIMALIIDE—(continued). MuscicaPip&. Picip&. 
Pomatorhinus. Xanthopygia. Vivia. 
Suthora. Niltava. Yungipicus. 
PANvRID&. Tchitrea. Gecinus. 
Paradoxornis. 
Corvip#. Coracrip#. 
CiNcLIDz. Urocissa. Eurystomus. 
Enicurus. 
Myiophonus. N "Ethous EID. ALCEDINID. 
thopyga. 
TROGLODYTID. Ee Hen a 
Pneepyga. MoraciLuip&. eryie. 
LIoTRIcHID&. DCT: Upupip2. 
Liothrix. DicxI1Dz. Upupa. 
. ,, 
x ae Zosterops. PsITTACIDA. 
teruthius. FRINGILLID2. - Paleornis. 
PYCNONOTIDA. Melophus. 
Microscelis. Pyrgilauda. gr 
Pycnonotus, : 
Hypsipetes PLOcEID#. Tanthznas. 
; Munia. Macropygia. 
CAMPEPHAGID. 
Pericrocotus. STURNIDS, PHASIANIDE. 
D Acridotheres. Phasianus. 
Eee Sturnia. Ceriornis. 
Dicrurus. 
Chibia. PITTIDz. STRIGIDA. 
Buchanga. Pitta. Scops. 
In the above lists there are rather more Oriental than Pale- 
arctic genera; but it must be remembered that most of the 
former are summer migrants only, or stragglers just entering the 
sub-region; whereas the great majority of the latter are per- 
manent residents, and a large proportion of them range over the 
greater part of the Manchurian district. Many of those in the 
Oriental column should perhaps be omitted, as we have no exact 
determination of their range, and the limits of the regions are 
very uncertain. It must be remembered, too, that the Palzearctic 
genera of Sylviide, Paride, and Fringillide, are often represented 
by numerous species, whereas the corresponding Oriental genera 
have for the most part only single species; and we shall then 
find that, except towards the borders of the Oriental region the 
Palearctic element is strongly predominant. Four of the more 
especially Oriental groups are confined to Japan, the southern 
