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2010010082
哈 萨 克 斯 坦 南 部 法 门 阶 牙 形 石 新 属
Barskovella 和 Bizignathus = New
genera Barskovella and Bizignathus
(Conodonts) from the Famennian of
southern Kazakhstan. ( 英 文 ). Gatovsky
Yu A. Paleontological Journal, 2009,
43(5): 550-557 5 图 版 .
New genera Barskovella gen. nov.
and Bizignathus gen. nov. are described
from the Famennian deep-sea carbonate
deposits of the Bolshoi Karatau Mountain
Range (southern Kazakhstan).
2010010083
哈 萨 克 斯 坦 中 部 晚 奥 陶 世 硅 质 岩 中 的
牙 形 石 = Conodonts from the upper Ordovician
siliceous rocks of Central Kazakhstan.
( 英 文 ). Tolmacheva T Yu;
Degtyarev K E; Ryazantsev A V; Nikitina
O I. Paleontological Journal, 2009,
43(11): 1498-1512 6 图 版 .
Several conodont localities of the upper
Sandbian Stage are known in siliceous
deposits of Central Kazakhstan.
All of them produced similar assemblages
overwhelmingly dominated by
Periodon grandis with insignificant admixture
of Scabbardella altipes, Hamarodus
europaeus, Pygodus anserinus,
Protopanderodus sp., and Drepanodus
sp. The main feature of this fauna is in
the co-occurrence of H. europaeus and P.
grandis, forms characteristic for deepwater
facies at shelf or microcontinents
margins of temperate and warm-water
paleobiogeographic provinces. The Ordovician
paleo-oceanic basin of Kazakhstan
and southern Urals were parts of the
uniform biogeographic area as indicated
by similarity of Ordovician conodont
assemblages in siliceous deposits of
these regions.
2010010084
沃 罗 涅 什 台 背 斜 ( 苏 联 地 台 中 心 区
域 )Evlanovian 和 Livnian 亚 阶 ( 晚 泥
盆 世 )Polygnathus 属 牙 形 石 新 发 现 =
New conodonts of the genus Polygnathus
from the Evlanovian and Livnian
(Upper Devonian) of the Voronezh Anteclise
(central Devonian Field). ( 英 文 ).
Kirilishina E M; Kononova L I. Paleontological
Journal, 2010, 44(1): 68-78 4
图 版 .
New conodont species of the genus
Polygnathus (P. krutoensis sp. nov., P.
makhlinae sp. nov., P. menneri sp. nov.,
P. obruchevae sp. nov.) are described
from the Evlanovian-Livnian (Upper
Devonian) deposits of the Voronezh Anteclise
(central regions of the Rassian
platform). The ontogenetic series of the
new species are presented.
2010010085
塔 吉 克 斯 坦 中 部 Palmatolepis 属 弗 拉
斯 阶 牙 形 石 新 发 现 = New Frasnian
conodonts of the genus Palmatolepis
from the Central Tajikistan. ( 英 文 ).
Bardashev I A. Paleontological Journal,
2009, 43(3): 300-305 3 图 版 .
New Lower-Middle Frasnian conodonts
of the genus Palmatolepis Ulrich
et Bassler, 1926 are described from the
Kalagach and Kulyali formations of the
Sishkat key section of Central Tajikistan.
Palmatolepis manzuri sp. nov. descends
from Pa. punctata (Hinde) and is an ancestor
of P. kireevae Ovnatanova, Pa.
salibaevi sp. nov., and also of the P.
rhenana Bischoff branch.
2010010086
俄 罗 斯 地 台 东 部 弗 拉 斯 阶 牙 形 石 =
Frasnian conodonts from the eastern
Russian Platform. ( 英 文 ). Ovnatanova N
S; Kononova L I. Paleontological Journal,
2008, 42(10): 997-1166 49 图 版 .
The Frasnian conodonts of the eastern
Russian Platform from the Timan in the
north to the Orenburg Region in the
south are characterized in detail both paleontologically
and stratigraphically.
This paper is a continuation of a previously
published monograph (Ovnatanova
and Kononova, 2001) on the
Frasnian conodonts of the shallow-water
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