SCIENTIFIC ABSTRACT MIKLOVICH, N. - MIKLUKHO-MAKLAY, A. D.

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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

F-17 7
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rj C, P J 3.
3 171 A C, 11
com-
cont d
with (,Ys r.

szsa' A., 4nd 'mmovic~ N. 0, the S'gta Institute of ATIL-'Ial ~Vglen~a
(1-Arectort !~ArAR, To), M '.1 apa5t EorljL'nal version not given!..
"Histopathological Changes in the Rat Kidney Follo-w-Ing A&-,-Anistration
of Sulmamethylthiazole"
Dludapest~ Acta Va orinari-A. ~ol 12, No 4, 1962; pp 3,q-371.
AWjr,q.ct '2nelizh article, author3l ~~ngli,~h swfisry]t 1111btopathological
L
changes folio-wring protracted a-,1rdMistration of D-artinobenzenosulfoa-
imldo-k-xethylthiazole (UltrasepTyl [US], Chinoin - Eudzq'ect) ha"re
6tudied in rats. Forty-eiiht young animals of both sexat and an average
boc~- ---relght of 110 ;.; wure used. US W43 adnixed to the food A.n ,,onaen-
trati.ons of 0.29 0.5 and 1.0 parcent. The animals were killed on the 1st,
2nd' 3rd, 4th, 6th, 14tji, 35t.1, and 70ti- &L.y; their liver, 5plotm, kidneys
and adranal glands -Alw:..ye topther u-Ith tt~o correspor,6-inr orr-.ans of
tvitreated cont.ro'l anl.,.als- warr) hil!stlologiaally tixaninod. Meml.el~s of tt~B
groups that had 0.2 ittnd O.-~ percent US, ihowed no es~-bntiaj- his-
tological changeo Rats trGated ;rith l.G parcont US presented, chror")-
'logioAlly, the following renal losiop.3: (1) Nephrosis from t'lia first
J/z

Yarta, Dr, Furenc, Dr; Vi.-terinii-y
Medical University, 'R-Lvirtpic-nt of -1 ReL
R
A Y (chaii-,an: 50,
Dr, professor, academi~iari) an-j National LnLnal Hygiene in-stitute (dlr-a~:tor:
YADAR, Tibor, Dr, candidate of veterinarj sciences) (Allator-.rostudormnyi
E--zyetem Jarvanytani Tanszeke es Orszagos Allategeszsegugyi Intezet).
"Comparative Study on the Antibiotical and Chemotherapeutical Treatment of
Borreliosis (Spirochaetosis) in Fowl."
Budapest, 1-1ap-,yar Allatorvosok Lapja, V0118, 110 7, -Tuly 63, pages 265-267.
Abstract: [Authors' English summar-I modified] Co-riparative studies have been
carried out on the treatment of septicemia caused by Borrelia anserina on
chicks. Oil and water suspensions of oxytetracycline and chloramphenicol,
crystalline streptomycin, penicillin, Atoxyl Supraseptyl and Furazolidone
were tested. Acute infection develops in 3-4 day-old chicks infected ex-
peerimentally, to which they all succumb within 7-9 days. The following doses
were effective for the treatment of the infection: oxytetracycline in both
oily and crystalline form, 1.5-10 mg/chick, penicillin 10,000 U/chick, strep-
tomycin 10 mg/chick; amon-- the chemotherapeutical, preparationsAtoxyl 2 mg/
chick subcutaneously. Preparations of chloramphenicol in doses of 5-10 Mg/
chick showed no satisfactory effectivene5s. Supraseptyl and Furasolidone
were completely ineffective. Field experlences shvzed that a single dose of
10 mr,
,Ikv. body weight of Tetran was as effective as ei-jstalline penicillin
in doses of 20,000-40,000 U/kg body weight. 9 Western, 2 Hungarian references.
1/1

a

:4ff.WlllCZ, A.
ItQuality and stanfianiization." D. 200, Vol. . n-j. L, ik;,)r. i;,'.3.
Budape s t. )
I - Vol. 2, L2~rury of t,-mf,ress
Su. MoniA,.I.%- List of Last 4uropean Acces:jions,
.~uc,lfsc, D53, Uncl.

RIKLOVICZ, A.
International standardization. p. 11~.
MUSZAKI ELET, No. 10, May 1955
(huszaki es Termeszettudomanyos Egyesuletek Szovetsege) Budapest
SOURCE: East European Accessions List Vol. 5, No. 1, September, 1956

A.
~-'JKLCNIC-Z, 6th IiE-ti,nn- '-'-~nferercc- of the Teytile lzi--',ustry.
1", Oct. 195f
T-ECHNUCCY
Budapest, IfUngijry
So: East Euror-c-an Accession, Vol. 5, No. y 1956

I:or-k ccr-inittf,'!~5 01' le i: --
UJITOK L'PJA, Budapest, Vol. 7, no. 15, Au -. 1955
Il'ontinly Llst of i~ast Sliropean Accessiomi, LC, Vol. 1~, no. ucL. 1.,,55
,Jr,,cl.

I I A -.
I 'T'. 117111j, V TC. i ). .
-1 u P. 1~5
On the eve of the 5th Genernl lkssembly of the Association.
m~.r,,JJP T74TTLTEPIWrKA ThOapest Vol. 119 TTo. 51 lr~y 1955
.10711CE: Enst European Accessions List (EEAL) Librnry of Congress
Vol. 5, 71o. 6, Jime 19515

MIKLOVICZp A.
MIKLOVICZ, A. Proposals of
Textile Industry in regard
Plan. p. 24. Plans for ou,
of capitalistic countries.
Vol. n, no. 16, Aug. 1956
14USZAKI ELET
TECHNOLOGY
Budapest,, Hungary
the Technical and Scientific Association of the
o the guiding principles of the second Five-Year
machine industry. p. 26. The steel production
p. 29.
So: East European Accession, Vol. 6, No. 5, May 1957

MIYJ,OVICZ, A.
The 1958 session of the Technical Committee on Synthetic Materials of
Technical Commission 61 of the International Organization for Standar-
dization. p. 109
SZA13VA,mr,YI KOZLr2-1FYfT!7. (Mapyar Szabvanyugyi, Hivatal) Budapest, Hungary.
Vol. 11, no. 5, 1959.
July
Monthly list of East European Accessions (F-IAI). LC. Vol. 8, no. 2,/1959.
Uncl.

H/003/6o/coo/oog,
A054/AO26
AUTHOR: Miklovicz, AndrAs
TITLE. The Chemical Industry at the Exhibition of Standardization
PERIODICAL. Szabvhny4Jgyi K8zlem6nyek, 1960, Vol, 12, No, 9, pp~ 202 - 205
TEXT: In Hungary an exhibition of standardization was organized, giving a
comprehensive picture of the work done.by the experts and institutions in the
field of standardization; of the practical value and economic importance in ap-
plying standards for both the individual and national economy. The article deals
only with the section of the chemical industry and describes in detall~ the as-
pects of standardization as applied to the production of synthetic materials and
products;- specimens were exhibited in order to show the various possibilities
of their application in industry and households; the exp6sition of standardized
lubricating oils (of which in all 7 types are produced in Hungary at present);
the standards referring to the corrosion protection (demonstration of all biolog-
1c&l, electrochemical and mechanical causes of corrosion, the effects of wrong
surface treatment as compared with the corrosion-proof methods prescribed by
standards); standardized detergents and their advantages. The most up-to-date
Card 1/2

H/()03/6Q/CO,j/O0,9/001/001
A054/AO26
The Chemioal Industry at the Exhibition of 3 t andardl za Lion
test methods and equipment applied to quality control, i1mulating the ~Ptual op-
!e -te kt-I P
erational conditions. The methods of non-destructive'materlLIL- %!~`were also
demonstrated, e.g., with the aid of a complete examination of a tire In moveriEnt.
Standardized laboratory test apparatus were also exhibited, and mainly devices
operating with replaceable microsections are described In detail. They make it
possible that the basic apparatus can be used for various tests by exchanging
some parts of the apparatus. The exhibits were suitable for different intellec-
tual levels and gave simple and easy to understand models and demonstrations of
processes. The exhibiticm will also be shown in B3rsod Megye (District of Bors-
od), in the center of the Hungarian chemical lnduE7try, There are '3 f1spires
Card 2/2

MIXLOWICZ Andrasne; WECIAWOWICZ, M. (translator]
y
Activities of the Hungarian Soientific-Technical Asooclation
of the Textile Industry in Budapest. Przegl w1okien 16
no.V8.-429-431 J'-,-Ag 162.
1. Generalny Sekretarz Wegierskiego Techniczno-Naukowego
Stowarzyszenia PrzemAlu W:Lokienniczego, Budapest (for
Riklowicz).

MIKLOVICZ,.Andras, okleveles vegyeszmernok
Significance of the Council for Mutual Economic Assistance
standard recommendations in the international eychange of
goods. Szabvany kozl 16 no.12:213-214 D 164.
The 1965 plan of the Standing Committee on Standardization
of the Council for Mutual Economic Assistance and the
Institute of Standardization of the Council for Mutual
Economic Assistance. lbid.016-217
1. Hungarian Er-treau of Standards, Budapest.

PoLkrlD
BOHOSIEVICZ, Michal; and '-IIKOLAJCZA,'(-EQZ;~kqLl,.,~rbara; Chair of Ihamiacolozy,
Veterinary College of- sity_~(FG~tcd
In'Trc-Uitural Univer ra :azaakoiGgll
Wydzialu Wet. I-ISR,) Ifead (Kierownik) Docent Dr T. GAaWLINSKI, Wroclaw;
and Department of Toxicology (Zaklad Toksycologii,) Head Docent Dr M.
BOIIOSIEIIIICZS
"Cyanide Intoxication of Cattle."
Lublin, Medycna Weterynaryina, Vol 21, No 10, Oct 65; pp 616-618.
Abstract [English summary modified]. Description of poisoning of 12 head of
cattle who drank from puddles of water with high cyanide content due Co
contamination from nearby chemical factory; all 12 had to be slaughtered on
an emergency basis. Table; 4 Polish and 5 Western referaces.

SWK, B.; MIKLOWSKA. A.
Effect of mineral fertilizers in conjunction of enclosing of
animals on soil microbiology, of pastures in the mountains. Act&
microb. polon 5 no.1-2:165-171 1956.
1. Z Katedry Mikrobiologit Rolnej WSR w Krakowie.
(SOIL, microbiology,
off. of mineral fertilizers on pastures In mountains(Pol))
(TWILIZERS, effects,
on soil microbiol. on pastures in mountains (POI))

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MIKLYKHIN, Gleb Panteleymonovidh
Academic Degree of Doctor of Chemical Sciences, based on his
defense, 9 October 1954, in the Council of the Inst of Physical
Chemistry imeni Pisarzhevskiy, Acad Sci UkSSR, of his
dissertation entitled: "The Sources and Means for the Transfer
of Hydrogen during Reactions of Organic Combinations."
Acader:dc degree and/or title: Doctor of Sciences
SO: Decisions of VAK, List no. 10, 30 Apr 1955, Byulleten' ~170 353RJI
No. 15, Aug 56, Moscow, pp 5-24, Uncl. JPRS/UY-537

'1KYT(III 11, Gn .; FT -,~ F iV77,A . F. :
---TI __. - -
1'7astnFowanie izotop6w do badania i kontroll chemicznych proces6w techno-
loeiczn7tch" (IFotopes used for the examination and control of the che:~ical t"!ch-
nological proc-sses), by G. P. Mituchin and A. F. Fiekaszewa. in N-w
Fooks (Nowe Ksigzki), No. 12, June 15, 1,-,56.

MKLUKH, V.N., avenevaya
We spars no efforts. Rab.i sial. 38 no.9:4 S 162.
09RA 15,9)
(Tolochin District-Flax)

MIKLUKHI, N.; KOVALENKO, S.; SEICNOVI~H, ra.
Herosim. Posh.delo 7 no.5:24 My 161. OMIRA 14:5)
(Lifesaving at firejo)

MIKLUIHIN, DnItrIjv Yefloovich; VOLPYANSKIY, L.M.. rodaktor; DUGDU, N.A.,
--- "': ''tiftfilbhookWiedaktor.
(Aluminum alley castlW Otllvkl In allualniewykh splavow. Pod
red. L.N.Volptanskego. gookwa, Goo.noutho-tokhn. Isd-vo mashino-
strolt. lit-ry, 1955. 49 p. (Nauchno-popultarnata bibliottka ra-
bochW-litelshchiks. no.17). (MM 9:5)
(Alunimus f crunding)

_D-a.lousov, L.A. SOV-128-58--8-11/21
AUTHORS: Miklukhin, D.Ye._,
TITLE: A New Method for the Preparation of
Alloy (No-iyy metod prigotovleniya kremnevomagniyevoy liga-
tury)
PERIODICAL: Liteynoye proizvodstvo, 1958, Nr 8, p 19 (USSR)
ABSTRACT: In the production of cast iron with graphite, metallic mag-
nesium or magnesium alloys are used. The production of mal
nesium alloys by the usual methods is expensive. In the
article, a new method is described in which ferrosilicon
is melted in a three-electrode electric arc iurn-
ace. The method considerably reduces production costs,
1. t1agnesium-silicon alloys--Preparation 2. Electric fu-naces
--Applications 3. Cast iron--Production
Card 1/1

SOV/137-59-3-681
Translation from: Referativnyy zhurnal. Metallurgiya, '-959, Nr 3, D Z7.' (USSR
AUTHOR: Miklukhin, D. Ye.
TITLE: Peeling of the Chilled Surface of Two-layer, Mg-treated Cast-iron
Rolls and Methods of Preventing This Condition (Otslaivaniye
otbelennogo sloya na dvukhsloynykh valkakh iz chuguna, obrabotanno
go magniyem, i metody bor'by s nim)
PERIODICAL: Tr. Ural'skogo politekhn. in-ta, 1958, Nr 73, pp 251-Z58
ABSTRACT: The service life of Mg-treated cast-iron rolls (R) is reduced as a
result of peeling (P) of a portion of the chilled surface layer, which,
in turn, is brought about by increased reductions and an over-all
intensification of the rolling process as compared with rolling in
carbon R's. Concurrently with an increase in stresses during rollir
the temperature of the R's increases from 400 to 6000C. Studies re
vealed that R's which had begun to peel did not have a transitional
zone and that P occurred in majority of the R's in their lower (with
regard to casting) portion, i.e., in a zone where the sharpness of
transition from the chilled layer to the core is at a maximum. All
Card 1/2 R's which had been in operation until they were no longer serviceab)

SOV/1 37- 59-3 -6811
Peeling of the Chilled Surface of Two-layer, Mg-treated Cast-iron Rolls (cont. )
exhibited a transition zone of 5-15 mm. As was confirmed by the performance of
experimental R's, P of the chilled layer occurs in R's devoid of a transition zone.
A computation of stresses arising under normal conditions of rolling indicates that
these stresses alone are not bufficient to produce 0; however, increased tangen-
tial [shear] stresses exceeding the strength characteristics of the R material are
possible in certain small regions of the contact surface under increased pressures
(at the time of entry and delivery of the packs from the Ws, during cooling of ends,
or in the case of nonuniform elongation of the packs, at low temperatures of the
packs, etc.). Owing to the presence of stress concentrations on the transition
boundary between the chilled layer and the core, the destruction of this region ma~
occur also under the action of tangential stresses which do not exceed the strength
of the material. The following methods were tested and were found to be successh
in eliminating the P of the chilled layer: 1) Reduction of tangential stresses by
avoiding abnormal conditions of rolling; 2) improving the uniformity of compositic
of the chilled layer; 3) creating a transition zone. An increase in the depth of the
chilled layer significantly reduces the incidence of P.
P - G
Card Z/2

I.JKLUKIIIII, D.Yu., C: nd Toch Sci - (diss) 5tudy c,f p4o'lilik-
oi -tvio-lriyGr rollers and develop-.atint of buti iiotullod uf cor~b-tr*414
it btilmroimbrovok, 19'j9- 14 PI) of, "Irlic;r Ecilic'Ition
UI-SSR. Daepropetruvek Zletndlurgical List). 150 copio,-,
(YJ,93U0-59,117)
IV

MIKLUIGIIII, D.Yo., inzh.
Production of two-layer 2-olle with transition zone. Trudy
Ural.politekh.inst. no.89:95-98 '59. (MIRA 12:8)
(Rolls (Iron mills)) (Cast iron)

MIKWKffO-MAXLAY A-.D
" ~-.
Date, on the stratigraphy and microfausa of the Upper Paloozoic of
Fergana; a thesis for tho "candidate" degree. Test.Lea.ua.2 so.2:
142-144 7 147. NT-Rh 9:6)
(Fergana,-Geology, Stratigraphic)

I 'i 114 L'' t:;e ~ ~'- ~! !, ~*
"br., inst. 77cirQ's Crust, Lenin~y.;d ~'njv-,-1947-- " Ulf- -' - i .. L
Fxc;,v.~ted 14icroor,-.-misms in the Study of Ancient Soils," ':nst, r,c- L., i;o. i,
191t*i; of P.-.Ieozoic Lyvf-5 in Fcl. ;-11~; Moilnta~l; I'Carqc," 1)14~.An, la, :;k). -", -1114,t3
it I L;'I
"New r~;~ta on Fauna of For,7minifer;~ In P rt%i~;n Dorosits , j- Cauc3s~.-,, I .,I.
5F, 111o. 2, 190

- ~ I . - - 7 1, -t . - - 7 1 - -,- I i--- r . - . -,, ~ * - , I
I . I - I :I 0~.- ": !-, I, . ~ ~ . ! .
'Tt-. A!'- of Z--tratlir-. ~,' ";, Ftr,,.,Y. t," Dol~- - .', -,) ' I

". 1). :, 1 ; -,T!,.
-. I 'I

7,ru-,t, Lin; n r~d Sta!,~ Univtrs~
I n t,,a o n li F~! u 11 f I r [w. 0
V~47

YB
IjUYHC--AJLAZ, A. P.
"The si-nit'icance of the forar.-dnifera for the strai,iiTraph~ c
fl)e TJ_PFr rllYFlI~IZ`o3-c-fT~uoSits of tet.is", Ijaucb. Byu3leten' Leningr. -,oz. un-ta im.
Zhdanova, No. 21, 1).
SO: U-31OL2, 11 i'arch .`3, 17:,urrial InYlich Statey, i"o. 7 1~)19).

MIKWKHO-MAIMAY. A.D.
(The Upper Phleozoic Fusulinid" of Central Asia: Fergana, D&rwas&,
and Pbmir] Torkhnep&leor-olskis fusulliddy Srednei Asii: Forpm.
Darwas i Psair. lxd-wo lonLagradkogo gas. univ. 1949. 126 po
OUA 90)
(Asia, Central--Geology, Stratigraphic) (Formainifors., Fossil)

MIKUMO-KAKJAY, A.D.
TrIticites forg^nonsis spon, from tWer Carboniferous deposits of
the Karvt-Chatyr Range in southern Fergam. Uch.rmp.len.un. no.102:59-
?0 150, (MmA 10:1)
I* Institut Zemnoy kory 4fedr^ istoricheskoy ge'sIsgil.
(UrR-Chatyr Rnrco-Joraviinifers, Fossil)

MIKLUKHO-MAKLAY, A. D.
Caucasus, Northern - Forarunifera, Fossil
Triassic foranLinifers of Nurthern Caucasus. Vest. Len. un. 7, No. 10, 1952.
Ser. Biol, ~Ieog, Geol,
Discovers that scrapings of limestone fodnd in Tiviassic deposits it) the basins
of i-~aia Laba and Bela rivers contain a fairly abundant aiao6nt of iucrofauna.
Three basic varieties of microfauna can be dintinguished: (1) the almot;t black,
slightly bituminous brachyi,odal 11riestones (13ela), (2) the dark a,-,411,nitro limestones
with a loat.7 texture (Bela), aiid (3) the red hetrogeneous
"". PAR
limestones with ruany spicules of s-ponges, seaweed, and br-jozoa. (A-1alla Laba niver
and Bela River Basin.)
9. Monthly List of Russian Accessions, Library of Congress, june 1953. Unclassifi

WFLffIJO-MKLITq A. D.
Data on the Carboniferous deposits
AN SSSR 83 No, 2 1952.
Stan Ancemplons,
of the Yaritime Territor7. Dokl.
Library of Congress, August, 1952.

MIXWXHO-KAnAY, A.D.
MW
Systewtics of the family A-rchaodisaidae. 3zhegodJoes.paleont.
ob-va 14:127-134 153. (MLEA 8:3)
(Foraminifer&, Fossil)

I ~~
,_.IKLUY,H(-MAXLAY, A. 1).
LU,SR/Geology - Limestone of Tuarkyr, 11 May 53
"Devonian Limestones from the Red-Colored Stratum
of Tuarkyr," A..B. Vistelius, A. D. Miklukho-
Maklay, and V. N. Ryabinin, Lab of Aeromethods,
Acad Sci USSR
DAN SSSR, Vol 90, No 2, pp 231-234
Describe these limestones which were found in a
nodule of conglomerates of red-colored stratum
in the region of Tuarkyr. Also presents a short
explanation of their structure. Presented by
Acad D. V. Nalivkin 9 Mar 53.
2~kT33
260T33

MIKLUKRA-KAKUT, A.D.
- .
Systematics of the family Fusulixidas Moeller. Uch.zap.Ian.un.
no.159:12-24 153. (KRA 9:6)
(Foraminifer&, Fossil)

15-1957-3-2609
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 3,
p 6 (USSR)
AUTHORS: Miklukho-Maklay, A. D., Porshnyakov, G. S.
TITLE: The Stratigraphy and Structure of the Carboniferous
Rocks of Southern Fergana (K stratigrafil i tektonike
karbona yuzhnoy Fergany)
PERIODICAL: Vestn. Leningr. un-ta, 1954, Nr 4, pp 193-205
ABSTRACT: Bibliographical entry
Card 1/1

PORSHNTAMOT, G.S.; KIKLUVID-KAXIAT, A.D.
Stratigraphy and facles of Devonian deposits in southern Fergana.
Test.lon.un.9 no.1:127-134 Ja 154. (KULA 9:7)
(Fergana--Cleologr, Stratigraphic)

MIKWKHO-KMUAT.A.D.; PORSHMAKOY.G.S.
-- e~
Stratigmphy of Jurassic deposits of the Bodrak River Basin;
from data of students' field study in geology. Vast. Len. un.
9 no.4:208-210 Ap '54. OCRA 8:6)
(Bodrak Valley--Geology. Stratigraphic)

IKIUKHU
M
49=4.1- ~.Ir
Some problems of paleo-scological research of Paleozoic marine
fauna. Vest,len.un.10 no.1:119-224 Ja 155. (KaA 8:4)
(Paleontology)

HIKLMO-HULAY'A.D.
-
Conference of July 7-11. 1954 on the problem of the extent
of the Nasurian series and Its position In,the Carboniferous
system. Vest.Len.un. 10 no.4:145-148 Ap 55. (KLRA 8:8)
(Geology, Stratigraphic-Congresses)

EMMWM. 6.S.. NIUMMO-MMUT. A.D.
_-.- , .
Occurrence of Devonian deposits on the seutborn slopes of the
Greater Caucasus range. Dokl. AN SM 104 no.6:890-891
0 155. (NLRA 9:3)
1. Leningradekly gosudarstvswW univereltst liment A.A. Zhdanova.
Predstawleno skademikom D.I. Sherbakewyn.
(Caucasus, Southern--Geology, Strattgraphic)

-KIKLUMK~-KMAY. A.D.
Mew data on Formlan fusullnids In the southern parts of the U.S.S.R.
Dokl.AN SM 105 no.3:573-576 If 155. (KLU 9: 3)
1. Leningradekiy gosudaretyeanyy univeraltet Iment A.A. Zhdanova.
Predstayleno akadealkom D.I. Shcherbakovym.
(Russia. Southern--yorminifera. lrossil)

15-57-12-16781
Translation from: Referativnyy zhurnal. Geologiya, 1957, fir 12,
p 11 (USSR)
AUTHOR: Miklukho-Maklay, A. D.
TITLE: The Zoogeographical Regional Divisions of the Marine
Permian in the USSR and the Correlation of the Upper
Paleozoic Deposits in Central Asia I the Caucasus, the
Trans-Caucasus, and the Ussuri Region (Nekotoryye
vopros K zoogeograficheskogo rayonirovaniya morskoy
permi SSR i korrelyatsiya verkhnepaleozoyskikh
_
otlozheniy Sredney Azii, :Kavkaza, Zakavkazlya i
Ussuriyskogo kraya)
PERIODICAL: Uch. zap. LGU, 1955, Nr 189, pp 3-20
ABSTRACT: The Permian rocks (except the lower Sakmara) were
deposited in different environments in the north-
northeastern and the southern regions of the USSR.
Two faunal realms are distinguished, the Siberian and
Card 1/9

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.
the Caucasian. The first was characterized by low temperatures of
the water and by comparatively few species. It has been divided into
the Russo-European and the Kolyma provinces. The Russo-European
province was characterized by the abundant development of Productidae
and Spiriferidae, monotypic groups of bryozoans, and but slight de-
velopment of small foraminifers. The fauna of the Kolyma province,
with Inoce AM12 -like pelecypods (A2hanaia and Kolymi4 were developed
Tif a 666' OT normal salinity but of -661der water (indicated by the
absence of reef-building organisms). In the southern or Caucasian
region, it is possible to distinguish a Northern Caucasian province
(sponges, stromatoporoids, planktonic foraminifers, brachiopods),
a Crimea-Famir province (ammonoids, rugose corals--Waagenophyllum,
ranophyllum--numerous benthonic fusulinids), and --U-
I an ssuri-- province
tbryozoans corals, crinoids--Codonofusiella. Yabeina--and others).
The'Russo-Lltic land mass and the Siberian continent are dis-
tinguished. The latter was characterized by the abundant formation
of coal-bearing deposits. The fact that the Ussuri region contained
Card 2/9

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.
marine Permian fauna belonging to the zoogeographic region of the
Caucasus leads to the assumption that there existed a warm southerr
connection between the two regions. Furthermore, the marine fauna
of the Siberian region are similar to the fauna of the eastern trar
Baykal region and of Mongolia. Individual horizons have been dis-
tinguished in the upper Paleozoic for the different regions of the
southern USSR on the basis of foraminifers. These horizons are
compared in the Table.
Card 3/9

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.)
orizon
Main
Caucasus
P23 Horizon with
Ammonea and
NaTI-olaria
P22 Horizon with small
foraminifers and
Reichelina
P21 Horizon with
Neoschwagerina
colaniae and N.
-
Tf-f.margarit
ae
and wTth -small
foraminifers
Card 4/9
Trans-
Caucasus
Horizon with small
foraminifers
Horizon with
Ploydiexodina
Cant on Card r*19

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.
Central Asia
Horizon with small
foraminifer and
Reichelina
Horizon with
Sumatrina and
Polvdiexodina
Ussuri Region
Continental beds
Regressive series,
small foraminifers in
layers of limestone
Marine deposits with
Lepodolina,
Doliolina s.s.,
Yabeina.
Card 5/9

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.
Pi3
Pi2
Pi1
Card 6/9
Continental and
littoral deposits
with Walchia
In pebble-cobble
Triassic con-
glomerates
Schwagerina s. 1.
Undifferentiated
horizons with
Parafusulina and
Misellina.
Horizon with
Paraschwagerina,
'Pseudofusulina, and
'roverbeekina
conf. on C&V-01 519

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Fermi-an (Cont.
Horizon with
Misellina
Marine and Continental
deposits, coralline
limestones
Horizon with
Parafusulina
Horizon with
Paraschwage-ina,
Fseudoschwalzeri a,
Schwaigerina, and
E-overbeekina
Card 7/9

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.
C3 21 Continental deposits
with Stephanian plants
C31
023
C22 Continental deposits
with Westphalian plants
C2I
Deposits not
verified, probably
absent
Card 8/9

15-57-12-16781
The Zoogeographical Regional Divisions of the Marine Permian (Cont.
Horizon with
Pseudofusulina
Horizon with
Triticites
Horizon with
Fusulina and
Tu-s-u Tin e J L 1 a
Horizon with
Profusulinella
Continenta~-marine
deposits (?)
Horizon with
Triticites
Horizon with
Fusulinella
Horizon with Pseudo-
stafella Are-h-&-eMscus, and
the first rrofusulinella
Continental
deposits
Card 9/9 B. K. Likharev

T-1
PORSHITYAKOV,G.S.;MIKLUEiO-NAXLAY,A.D.
Stratigraphy of the southern Fergana Silurian. Uch.zap.Imn.un.
no.189:21-26 155. (MMA 8: 12)
(Fergana--Geology, Stratigraphic)

WKWUM-MAKIAT. A.D.
----- -1- ~tw%
Systematics of ftlaozoic foraminifem Test.1an.mm.11
156. (Foraminifera, Fossil) (NLRA 9:7)
". t

14IKLUKIU-MAKLAY, A.D.
Stage scale of the middle Carboniferme. Vest.Lon.un 11 no.18:
14-28 156. (KERA 9t12)
(Geology, Stratigraphic)

VIMMUS, A.B.; NIXIUXHO-
IMLUL 0
The middle series of the productive stratum of the Apsheron Peninsula
and the problem of Its genesis. 1sv.AN SM.Ser.gool. 21 ao.4:
77-94 AP 156. (KIJA 9: 8)
1. Laboratorlys asrometodov AN SM. Leningrad.
(Apsheron PeaInsula-Geology, Stratigraphic)

KnMO-KAK~AT. A.D.
I Blostratigraphl subdivision of tho or ftleemic In the lorao-
0
Chatyr Mountain Ridge (South ForganTa. Dokl. A SSSR 108 no*6:1152-
1155 Ja 156. (Kw 9 110)
1.,,Lenlagradskiy go4udAratvenWy unIversitet iment AjA. Zhdmnm~&. Pred-
stavlono'almdemikow D.V. NallvkInym.
(Karg-Ch.tyr Mount pl, ns-~-Paleontoloff. Stra t Igraphic)

)aKLUKHO-KMAY. A.D.; RUMMITSBY, Y.Te.
I
ftunal characteristics of the upper Carboniferous from the
Kara-Chatyr Range In southern Fergana. Dokl. AN SSSR 110
no.3:07-09 S 156;. - (MLRA 9:12)
1. Leningradskly gosudarstvanyWy universitst iment A.A. Zhdanova.
Paloontologicheakiy institut Akadenti nauk SSSR.
(Pargagh-Geoloff , Stratigraphic)

KDaM06-MAKUT, A.D.
Now data on the systematics and #71logeny of Archaedisaidas-
fwith mmoLry in lbglishj. rest. IW 12 noo'24:-34-" 157.
(Foraminifera, lbasil) (MIRA 11:5)

KMMO-KAIUAr, A.D.
DivIsion into Soogeographical regione of Ckrboniferous and Permian
sea basins I a the U,SR. [with su==7 In lbgllnhl. rest. MU 12
no,'24:,176-179 157. (Kim 1115)
(Zoogeography) (Paleogeography)

KBILUKO-MMAY, A.D.
Homomorphy in fusulinids. 12hagod. Vees. palsont. ob-va 16:48-57 157.
(MIR& 11: 4)
(Poraminifera, Fossil)
(Morphology (Admls))

L
VOTAINv V,I,l MIKUMIOJLkKIAY.
AL-a of the Kisyl-Kiya Carboniferous band (southern Yeregana). T-r-Ay
Ion, ob-TR set. 69 no.2:47-51 '57. (KIR-k 110)
(Yergana-Rocks, Sedimentary)

/A-4 Z? AW 0 - A14 11_Ll~ ~~ A - P,
AUTHORS: Zubtsov, Ye. I., Zubt3ova, Ye, 1. 20-4-42/51
I.liklukho-Maklay, A. D.
TITLE: New Discoveries of Marine Permian Deposits in the Tien-Shan
(Novyie nakhodki morslr-.ikh permskikh otlozhenii v Tian'-Shane)
PERIODICAL: Dokludy Ali SSSH, 1957, Vol. 116, lir 4, pp. 6ai-663 (65610
ABSTRACTs It in customary to consider the northern wargin of the Fergana
and Tarim depression as the northern boandarj of the marintj P'.,r,
mian deposits in Central Asia. There is an assumption according
to which the coast line of the Permian sea took its course some-
what northwards in the east of tile- line Bogbu-Tau Liouritains -
south eastern slope of the Chatkal chain. Sinct; this assumption
was up to now not confirmed, the discoverj of marine loaer Per-
mian deposits in the north wetit of the Fergana, i. v. ill the dis
trict of the Narju depression bj the two first authuro ill 1956
is interesting,. Tile finds Lire of two differnet places (their dio
in the eastern part of the Bajbiche-Tau ch,-i
tance is 6o kia). a
(Ulan river vallf-ly and b) on the suathern olop(, of tile 11ardli-
~
Tau chain. At the Ulan river the exposarea have a uruadth (if Go(
and 3 km. They are covered bj UllC0nf0rW red-colored tertiary de.
posits in the north and border in the south along the fracture i
Card 1/3 a thick chalk iaa-ss of lower carboniferous. Th~: real charact~:r oj

New Discoveries of blarinu Pernian Deposits ir, th.~_, 2 2/5 3.
the Permian-carbonif erous -relation is not quite clear ',(.re. The
cross section is described in detail and the naiies of the foss-4'
of single horizons are given. The total thickness of the lo*ier
Periaian amounts here to 470 m. In the 11a-r.;n chain a thick com-
plax of terrigonous deposits of the upper )-LlaeoCoicU,,a is devel.
oped. Final conclusions. According to th--- juantitj ar.L t1lie ;isti
matic composition of the foraminifera the PvrL.~ian ex-.cjurts cf
the B-tybiche-Tau chain are much richur than ti,.oje of sa:..e a,
of Naryn-Tau. The differences are apparently connectt:d wit1i the
facial peculiarities of' the sites. The knowledge r7iv.--r, in ti.e
per concerning the systeLlatic aLioant of the fusulinide~i in the
Baybiche-Tau exposure shows that the two fauna zores (the lower
1th a r 1.
w
iarasch--ap-erine~quantiti; the upper with -a lot of parafu
sulines) on the- yr, hole- corres;.)ond to the cF.,,.tral
zon of Fer~~anaa( according to the stratigra;.i-.ic
kho-Mall-.14Ly). AzV oriL;inal species which do not oczur ir.
Permian of the Fergana depression lack here. The occurronce of
rather great quantity of forms is striking; they art., si:_ilar to
those of the upper part of Tay-yuan' serii~s of I'lorth C`.ina -and t
those of the Chuan'-Shanl series of South China. Ver,: fnt,_~res'14~
Card 213 is the discovcri- of 3 species which are described fr.-~L t-'-e

Rew Discoveries of Marine Permiar Depo3its in the Tien-Shan. 2o-,,-42,/51
nic Alps Shollvin), here in great nuaber of individualo.
There are onlj fuw apecloa which could bo found in thu lichwago-
rine layers of the Russian Plateau and in the neur-Ural rv~;ion.
From the occurrence of the same species in the Carnic kl,,s. icr-
.ana, and China it car. be concluded to espeoially .1avora ,01,2 ;ai-
gration conditions of thc faanu in the latitudinal extention.
There are 3 Slavic referencea.
ASSOCIJkTION: AU-Tbd- Scientific Geological Reoearch In3titute, State Jrii-
versitj imeni A. A. Zlidanov in Leningrad
isaledovatellskiygeologicheskiy institut,
venn,yy univeraitet L,U- A . A. Adanova)
PRESENTEDs May 11, 1957, by D. V. 14alivkin, Academi.-ian.
SUBMITTED: May 8, 1957
AVAILABLE: Library of Congress
(7seso..uz:-Vj nau.-;-.o-
Lenin6radsk.i~r Gosudarst
Card 3/3

VT.TTVM rr. n-4 . -
KALETSEArA. Harlys Samoylovna; MIKLUKHD- Q4-
FEWROVICH, B.A., dokio~r'geogr, nauk, otv. redi; TOLTNSKAYA, V.S.,
red. Isd-va: KAWVICH, S.G.. takhn.red.
[Characteristics of the Quaternary history of the eastern part of
the Pechora Basin and of ihe western slope of the Polar Urals]
Nakotorye.cherty-chetyerichnol istorli vostochnoi chasti Pecherskogo
basseIns 1,sapedubgo sklom.Pollarnogo Urala. *skva. Izd-vo Akad.
nauk 6SSR 11 1958. 65 p. (Akadmtia hauk SSSiL Institut goografit.
Trudy, Tol. 76) (MIRA 11:10)
(Pechora Valley--Geology. Stratigraphic)
(Ural Mountains--Geology. Stratigraphic)

MJUMO-MAXL&L A.D.: VIWTOV, M.Y.
Carbonlferous and Permian rocks in the Crimean 114untains.
Izv. vys. ucheb. zav.; geol. i razv. 1 no-8:30-35 Ag '58.
(MIRA 12:9)
l.Loningradskiy gosudarstvennyy universitet im. A.A. Zhdanova,
Moskovskiy goologorazvedochnyy inatitut im. S. Ordzhonikidze,
Kafedra iotorichaskor geologii.
(Grimoan Mountains--I'etrolog7)

MIKLIMO-KkMT. A.D.; IIAUZU-CIDMOMVA, D.M.; R(YZOVSKATA. S.Te.
Systematics and phylogeny of fusulinide. Top.mil=opaleont,
no.2:5-21 '58. (KIRA 11:12)
lo Leningradekly gosudaretvennyy univereitet i Geologicheskiy
Falsontologichookiy instituty Akademii nauk SM.
(Formainifera. Yossil)

HIMUM04OULTAT, A.D..
Tuberitinidas K.-Kaclay fam. nov., a new family of foraminifers.
Vop.mlkropaleont. no.2:130-135 '58- (KIRA 11: 12)
1. Lenin&-adekiy gosud%rstve=yy ordena Lenina universitet imeni
AA.Zhdanova.
(Foraminifera. Fossil)

HINLUKHOW-Ku"T, A.D.
Systematics of higher FusulinidAs; superfaoil;r Terbeekinaceae
[with stsemary in Analish]. V*st.LW 13 novI2:5-14 '58.
(MINA 11:12)
(Foraminifers, Fossil)

AUTHORS: Miklukho-Maklay, A. D., Ruaakov, I. hl. 20-118-6-35/43
TITLE: The Foraminiferal Complexes of the Paleozoic Era of the
Koryakskiy-Mountain Chain (KomplekBy foraminifer paleozoya
Koryakskogo khrebta)
PERIODICAL: Doklady Akademii Nauk SSSR, 1958, Vol- 118, Nr 6, pp. 1173-11'
(USSR)
ABSTRACT: Until recently the cretaceous sediments were considered as
the oldest existing,in this mountain-chain (references 1, 3,5
ftunjstj6LJJj* characterized paleozoic rocks have been found
here since 1955. Later, also brachiopodae and crinoideae
were found besides foraminifers. The foraminifers were in-
vestigated by A. D.Ydklukho -Maklay and the following aEe-
complexes were separated: Visean-, Visean-flamuri~n-,
Podmoskovskiy, Sakmarskiy and Artinako-Kungurskiy-complexes.
A number of foraminifer species are Giy2n-for each complex.
It hence results that sufficient specific forms are contained
In cacti complex. The corresponding rock-pi-ofile in fully
described suboequontly. The analyt3ln ot dltjtrtblitt~-n of' thi,
Card 1/4 afore-said foraminiferal complexes leads to so-ie conclusions

The Foraminiferal Complexes of th(i Palcozoic Era of the 20-118 - 6- 3 5/4 3
Koryakskiy-Mountain Chain
of general interest: 1) Upper-visean-Namurian contains species
which are ordinary for such sediments as occiir in the
sumpean part of the USSR, Ural arid Central Asia. This
leads to the conclusion that rej;iono so far 4ist&nt from
each other had a sufficiently free connection which favored
the exchange of species. 2) Faunistic data on the
Bashkirskiy and lower-Moscovian lack in the Koryakskiy-chain.
Nor can there be any question of a stratigraphic dis-
continuity for these stages. 3) The specific character of
the late Moskovskiy foraminiferal complex is not clear
because of insufficient investigation. 4) The occurrence of
upper carboniferous may be presumed here (discovery of
Brachytiris quadriradiatus Ver.). 5) The Sakmarskiy-complex
is of great interest. Species of the Sakmarskiy-stage of the
Russkaya plateau and of the near-Ural region (reference 6)
and simultaneously such species which are correlated in
Japan with the Sakmarskiy stai;e-species (reference 7) are
found here. Therefore a free connection of the seas of the
region of the Koryakskiy-chain with those of the European
part of the USSR and of Japau is assumed. 6) The Occurrence
Card 2/4 of species characteristic for the upper half of the Lower

The Foraminiferal Complexes of the Paleozoic Era of the 20-118-6-35/43
Koryakskiy- Mountain Chain
Permian of various Thetio-(Tethys)dietriota, in the Permic
complex, is not less remarkable. Their numerous occurrence
indicates toat since that time a permanent connection between
the seas of the Koryakskiy-chain region and of Japan was
established'rOn the other hand, the lack of the species
which are characteristic for the Artinskiy and Kun6ur sediment
in North-Eastern Siberia, proves that approximately since the
limit of the Sakmarskiy and Artinskiy ages, the faunal ex-
change between the seas in the region of the Koryakskiy-chain
and the regions situated in the West of them, was either
interrupted or rendered more difficult. 7) For the time being,
no accurate correlations of the local foraminifers with
concrete cross-aections of the carboniferous system can be
made. Only analogous ones can be dealt with. Comparisons with
the sand-slate-suite of the small Khingan (reference 3). with
sediments with Poeudoschwagerina and Parafusulina of
japm (references 7, 6)# aa well as with the Karacbatyrakly
Ud DarvazakiX (reference 4) sedimnts
can be made in the Fermian. There are 0 references, 6 of
Card 3/4 which are SovIet.

The Foraminiferal Complexes of the Paleozoic Era of the 2o-118 6-35/43
Koryakakiy-Mountain Chain
ASSOCIATION: State University of the Lenin Order irieni A. A. Zhdanov,
Leningrad (Leningradskiy gosudarstvennyy ordena Lenina
universitet im. A. A. Zhdanova)
All-Union ScientiTic Research Institute for the Geology of
the Arctic Region (Vsesoyuznyy nauchno-isaledovatellskiy
institut geologii Arktiki)
PRESENTED: October 18, 1957, by D. I. Shcherbakov, Member of the Academy
SUBMITTED: October 14, 1957
Card 4/4

AUTHORj Kidukho-Maklay, A. D. 30V/2o-12o-1-48/63
TITLE i On the Stage_Su_li~~on of the Marine Permian Sediments in
the Southern Regions of the USSR (0 yarusnom delenii morskikh
permakikh otlozheniy yuzhnykh rayonov SSSR)
PERIODICALs Dokl a
Mademii nauk 33SR, 19581 Vol- 12o, Nr 1, pp. 175-178
(USSR
~
ABSTRACTs The study of faunal groups of the Permian shows that the se-
diments of this age were formed in 3 different zoogeographical
regionst a) Siberian, b) Caucasian and 0) Australian
The Soviet geologists worked out a bio-stratigraphical stage
-scale in the range of the Russ'ian-European zOOgeographi -
cal province % Siberian zoogeographical region). Por the both
remaining mentioned regions a similar subdivision is missing.
In the USSR on the contrary a correlation of the Permian sedi-
ments on the range from the Crimes, to the Ussuriyskiy Kray
can be made. Thus the question on the subdivision named in the
title has become ready for judgement. k literature survey on
efforts of this kind (references 1-5,10-15) is given. Because
of the results by various research workers (Ref 16 and other
ones) the following conclusions can be mades In the sediments
Card 1/4 of the Lower Permian in the whole region of t11G Caucasian

On the Stage Subdivision of the Marine Permian Sediments in 3QV/'.eo-12o-1-48/63
the Southern Regions of the USSR
zoogeographical district of Balkans and Asia Minor in the
West as far as Ja~an in the East the following sequence of the
fusulina-complexes is indioated3 Stratigraphically the low-
est are layers with-Schwagerins. 6.1. They are gradually re-
placed by layers in which the first primitiye representatives
of the higher fusulinidae occurt EoYerbeekina, Brevaxina,
Misellins. In accordance with the above mentioned facts the attt
or raises the former layers, called horizons, to-self su--
tabrd stages. These aret a) Darvazakiy stage of the Lower
rermian, b) Murgabskiy stage of the Upper Permian, and c) the
Pamirs. stage. Because of the changes of the..foraminifer com-
plexes in the Upper Permian cross sections of North-East-Sibir-
is and in the southern regions Cauc%-=,Pamir5) it can be claim-
ed that in spite of clearly expressed temperature diffeiences
between the boreal seas of the Siberian and the warm
seas of the Caucasian zoogeographical district the total
process of change of the fusulinidae association took'place
in only one direction, namely of the relief by the lagena-
ria association. '1h fusulinid~e mostly disappeared almost
Card 2/4 for one geological :9e before the end of the Permian period,

On the Stage Subdivision of the Marine -1'ermian Sediments in
the Southern Regionu of the USSR 3OV/20-120-1-ju/65
and their finding in the Triassic therefore is little prdr
.able. The mentioned disappearance in the Tethys in the north
and in the south seems to be due to the temperature de-
crease in the world. ocean. A scheme of the biostratigraphi -
cal subdivision of the Upper Paleozoio era of Central Asia
is given in table 1. In the Middle Carboniferous still joint
stratigraphic subdivisions (Ref 6) could be used. Already in
the Upper Carboniferous the time of the correlation applica,
tons becomes shorter and shorter (Refs 4-8). Therefore one can-
not say yet how far the Upper Carboniferous horizons of Cen-
tral Asia correspond with the stages of the European '
part of the USSR. During the Permian time oxi the contrary the
faunal differences in the Sibeiiian and Caucasian regions
become so striking that the separation of special stages be-
comes necessary. There are 1 table and 17 references, 14 of
which are Soviet.
ASSOCIATIONt Leningradskiy gosudarstyennyy uniYersitet im. A. A. Zhdanoya
(Leningrad State University imeni A.A.Zhdanov)
PRESENTEDt January 13, 1958, by D.V.Nalivkin, Member, Academy of Sciences,
Card 3/4 USSR

On the Stage Subdivision of the Marine Permian Sediments in
the Southern Regions of the USSR SOV/20-120-1-48/63
. SUBMITTED: Januaz7 8, 1958
1. Geology--USSR 2. Geological time--Determination 3. Sedimentati
--Sampling
Card 4/4

MIKLUKHO-14AKLAY, A.D.
,
:-- I
ImportaneWof horeoriorphy for the systematics of Fuvulinids.
Uch.zap.LGU no.268:155-172 '58. (MIM 12:6)
I (Foraminifera, Fossil)

MIKLUKHO-MAKLILY. A*D.; YERSHOV, Yu.P.
Strattgrapbjv of upper Permian marine sediments in the Koryak
Rane.a. Nanch.dokl.vys.shkoly; geol.-geog.nanki no.2:90-94
'59. (MIRA 12:8)
1.,Leningradakiy universitet, geologicheskiy fakul'tet i
Institut geolo i Arktiki.
~Koryak Range--Geology, StratigraDhic)

MIKLUKHO-MAKIAYS A.D.
New Fwulinidae of the Upper Faleazoic in the U.S.S.R. Mat.k
*Osn.paleont.1 no.3:3-6 059. (MIRL 15.7)
(Fumilinidae)

JUKLUKHO-I"MY. A.D.
I* A,
-
stematics and ph7-logezq of fusulinids; genus triticites and
associated gannra. Vest.UW 14 no-6:5-23 '59. (JGRL 12:6)
(Foraminifers. Fossil)

17(4)
AUTHORs Miklukho-Maklay, A. D. SOV/20-125-3-47/6"
TITLE: The Stratigraphic Significance, Taxonomy and Phylogeny of
Staffella-Like Foraminifers (0 stratigraficheskom znacherdi,
sistematike i filogenii shtaffelloobraznykh foraminifer)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 3, pp 626-6~1
(USSR)
ABSTRACT: The author gives the 100-year-old history of investigation of
the Staffella-like foraminifers (Refs 2-9, 11-17). Individual
paleontologists have approached the taxonomy differently.
Taking the observations of reference 15 into account as well a
those made by the author (Ref 5) the division of all
foraminifers into two families is to be regarded as useful:
Ozawainellidae and Staffelidae (Refs 5,6). According to presen
concepts, the first family can be subdivided into 3 subfamilie
a. Ozawainellinae Thompson et Poster, 1937, b. Pseudo-
staffelininae Putrja, 1956 and a. Reichelininae M.-Maclay
subfam. n. Figure I shows their phylogenetic relationshipo,and
for each of the subfamilies, a. - c., a diagnostic description
Card 1/3 is given. In the subfamily a. a new subgenus

The Stratigraphic Significance, Taxonomy and SOV/20-125-3-47/63
Phylogeny of Staffella-Like Foraminifers
Eontaff4lloides M.-Maclay gen. n. is selected and described
with the holotype, E. orientalis M.-Maclay sp. n. (Fig 2) from
the Upper Permian of the Soviet Far East, Southern China, and
Sumatra. In the subfamily b. the now genus Neostaffella
M.-Maclay gen. n. with the typical species N. sphaeroidea
Ehrenberg (Ref 9) is presented and described apart from genus
Pseudostaffella Thompson,1942. Among the subfamily Reichelinina
the author classifies the genera: Reichelina Erk., 1941,
Parareichelina K.M.-Maclay, 19589 Dunbarulla Cirj,1946 and
Rausorella Dunbar, 1944. The indicated grouping of these
fusilinids (Table 1) speaks clearly of their great stratigraph
role. Not only the species complex but also individual genera
allow the determination of individual Carboniferou~-, st-,ges. Th
above mentioned subfamilies allow identification of the sub-
divisions of the Carboniferous and Permian Systems. Th6re are
2 figures, 1 table, and 17 references, 8 of which are Soviet.
Card 2/3

The Stratigraphic Significance, Taxonomy and SOV/20-125-3-47/63
Phylogony of Staffella-Like Foraminifers
ASSOCIATION: Leningradskiy gosudarstvennyy universitet im.A. A. Zhdanova
(Leningrad State University imeni A. A. Zhdanov)
PRESENTED: November 12, 1958, by S. I. Mironov, Academician
SUBMITTED: November 12, 1958
Card 3/3

3(5)
SUTHORS: Barkhatov, B. F.,Miklukho-Maklay,.I.D., SOV/20-125-6-T7,!-'!
Roman1ko, Ye,
TTTLE: New Data Concerning Perclian Deposits of "'he -,1,-orth Pamirn (Novyye
dannyye o permskikh otlozheniyakh Severnogo Pamirs)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 6, pp 1303-1306
(USSR)
ABSTRACTs Permian deposits characterized by their fauna predominate in
the northern and south-eastern structural-facial zone of Pamir
(Ref 1). The stratigraphy of the Permian deposits in the sout]
east of Pamir could be precisely defined in the last years by
investigations of the Upravleniye geologii i okhrany nedr pri
Sovete Ministrov SSSR (Administration of Geology and Protectioi
of Mineral Resources o:' the Council of Ministers of the USSR)
as well as of Leningradskiy universitet (Leningrad University)
New Permian exposures were found in addition. The separation
of the individual zones is indicated (Refs 1,4,5) (see Scheme
in Fig 1). On the strength of a tectonic and paleontological
analysis the authors draw the conclusion that the stratigraphi,
position of the so-called "violet" suite (earlier ascribed to
Card 1/3 the central part of the Lower Permian by M. 1. Shabalkin) has

New Data Concerning Permian Deposits of Northern Pamir SOV/20-125-6-37/061
to be revioed. The "Violet" suite., W-hich contains Upper Permi
fauna in the conglomerate, is obviously bound to have a strati
graphically higher position; it is, however, as well possible
that these deposits belong to the Mesozoic (Jurassic, and even
Cretaceous). The detection of Lower Permian fauna in the rock
of the northern metamorDhic zone of Pamir indicates the unifor
ity in the geological development of the entire northern zone
during the Paleozoic and Mesozoic or at least up to the Upper
Permian. The southern boundary of maximum downwarpings in the
Upper Paleozoic is distinctly marked; it is in accordance wit
the nouthern boundary of the Darvaz-Sarykol lower zone. Thus,
the development of the northern branch of the Pamir geosynclin
in the Upper Paleozoic was better determined. There are 1
fi,-Iure and 5 Soviet references.
ASSOCIATIONs Leningradskiy gosudarstvennyy universitet im. A. A. Zhdanova
(Leningrad State University imeni A. A. Zhdanov) Upravleniye
geologii i okhrany nedr pri Sovete Minis trov, Ta dzhf~,:s-*-,-t,4P-
(Administration of Geology and Protection of Mineral Resources
Card 2/3 o'L the Council of Ministers of the TH;Iz!-tt!e.SSR)

New Data Concerning Permian Depoeits of Nortbern Pamir SOV/20-125-6--7/--l
.,,I I - -
PRESENTED: December 9, 1958, by D. V. Nalivkin, Academician
SUBMITTED: December 2, 1958
Card 3/3

SINITSM, Mikolay Kikhaylovich (deceased); SINITSM, TX, prof., oty.
red.; -MILLOCE[O-KAKLAY. A.P., red.; OMM, T.N.. red.;
PORSHNMOT. G.S.. red.; KTIUG33U, T.I., red.; VaDaUGIM,
S.D., tokhn.red,
[Tectonics of mountains forming the borders of larganal Tektonlks
gornogo obramlenile Fergenr. Leningrad. Isd-vo Leningrounlyet
196o. 218 p. (Marona-Geology, Structural) (KM 14:1)