168 
It was chiefly on account of the fauna described in the pre- 
vicus pages that a Lower Oligocene transgression was asumed in 
these regions but as we have seen, it is highly improbable that it 
is a Lower Oligocene fauna. A marine fauna equivalent to te fauna 
of the Harkow Series or of the attorfian of N. Germany is not 
known in Western Asia except perhaps the „Taxodonta Beds“ .of 
Bogachev,“!) above which come the beds which contain continental 
plants. This and the reappearance in Europe of the Artiodactyls du- 
ring the Ludian shows that by this time the sea here was either 
very much reduced or had altogether disapeared, and it was not 
before the beginning of the Miocene that the sea again invaded the 
West Asiatic regioos. 
že a že 
N 0BOj pacipaBu H3HeTu cy pesyJiTaTu 1poyuaBawa 3Ö0HPRe 
MOAYCaRa (OKO 3000 NPHMepara), Kojy je cakyımo W. Bateson, 
GHB. IpezaBaq 300JI0THje Ha JIOHAOHCKOM YVHMBEPCHTETY, H3  CJIO- 
jeBa A0Bbe-TepnmjapHe crapocTu usmeby Apanckora Mopa u jesepa 
UaTkap. Uryamja oBe dayHe or ocoćurTor je HHTepeca #3 OBHX 
paz.1ora : 
1. [local ey TIpoyqTaBaHe caMo BP.IO Malle 36HpKe, JIOR Gy GIO- 
jeu Kojm cazpme oBe dbocme, jeAHHN J10Caa TI03HATH CJIOjeBH 
crapıjera Tepunjapa. y oÖ1actn Typkecrana m 3aı. Um6npa, 6oraTi 
(POCILIHMA. 
2. CrapocT dbayre joni je yBeR Hepeniena, jep ce panuju rnucnu 
He C.IaSKVY V MHNIJBEIY, IIPuHIacyjyhu joj pase cTapocTH, 1OYeB OA 
A1olBera eoneHa, Ia 10 /10Eer OJIHTONeHa. 
3. Opa bayra, saje Ino ca bayHoM MOIycaKa HCTe crapocTH Y j. 
Pyeuju, uare/a 1a 1pe/icTaBIba opurunaay dpayvay. H3 Koje ce 1o- 
CTYIIHO PA3ZBHJIA /IOEE-OJIHTONEHCKA (aya MOTycaka j. Pyenje u 
(Gap A@JIHMHYHO) c. Hemayke. Ilomro ce cMaTpa Aa ce murpanuja 
oBe (PayHe BPIIMIa ća HCTORA Ka sama/iv, AIysR »IloctxymHe TeocHH- 
KIIHA.Ie«.?) HOTIYHMje nmosnaBawe dbayne na HCTORY, IIPHPOJIHO. 
MOpa ÖHTH 0/1 HHTepeca. : 
4. Ca IMTaIbeM crapocTu OBe ()ayHe croje y TeCHO] Beau Ba 
Bp.IO BaskHa IIPOÖ.IeMA, HAHME, A) Kal je MOPE IIPEILIABHJIO HCTOIHH 
HU CeBepoOHCTOYHH Neo »llocrxyMHe TeocHHKTMHaAne«, jep ce Ha 
OCHOBY OBe dbayne (no B. KoeHeH-y, Koju je CMAaTpa OJIHTOILEHCKOM) 
Apu. Aa je TO ÖMMIO 34 BpeMe /I0er OJIUTONeHA; MH 6) samro je sa 
BpeMe OBep3HjeHa MH ÖApTOHHjeHa IIPekKHHYTa umurpannja CHHO- 
CHÖNPCRUX Artiodactyla y Eppony. 
Illro ce THue CTapocTH OBe dayne, JaHac je TOTOBO oImITe 
IIPIHM-beHO B. JKOCHEH-OBO MHILNBEIBe, a je OHa OJuronencka. Me- 
byTHM V HAjHOBHjHM PANOBHMA PYCKHX TeO.IOra BEIM ce Ma je OHA, 
MIH 11Pe/1A3HA COUCHCKO-OJIHTONEHCKA PayHa. MIM 1a Y TOj OGTACTH 
“Opa GUTH H CONCHCKHX H OJIMTONEHCKHUX CIOjeBa. TIA. Gy POCHAH TIPH 
IPHRVILJBAIV MellaHH. UTYyAHjoM came (bayHe, a HAPOYHTO iwenum 
VnopebelbeM Ca eOIMECHCKUM H OJIHTOMEHCKUM (bayHama CYCeAHHX 
) Bogachev: Depöts tertiaires du littoral de la mer d’ Aral, I. c. See table. 
> Yıopein. E. Haug: Traite de Geologie, II, 1908-11) erp. 1560, 1566 
u 1567. 
