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tion of the genus Pseudosiderolites are<br />

discussed.<br />

2010010134<br />

乌 拉 尔 山 南 部 泥 盆 纪 放 射 虫 新 发 现 :<br />

2. 中 - 晚 泥 盆 世 = New radiolarians from<br />

the Devonian of the southern Ural<br />

Mountains: 2. Middle-Late Devonian.<br />

( 英 文 ). Afanasieva M S; Amon E O. Paleontological<br />

Journal, 2009, 43(1): 34-<br />

49 6 图 版 .<br />

Middle-Late Devonian Radiolarians<br />

are recorded for the first time in the<br />

southern Ural Mountains in Bashkortostan,<br />

in a section of Kariukmas Mountain<br />

(Upper Eifelian) and on the southern<br />

slope of Argagan Mountain (Middle<br />

Frasnian). The new Late Eifelian assemblage<br />

is composed of 17 species of 11<br />

genera, and Middle Frasnian radiolarians<br />

comprise 13 species of 7 genera of<br />

spherical, discoidal, pylomate, and spiny<br />

radiolarians. A new species, Primaritripus<br />

kariukmasensis, sp. nov., is described.<br />

The prevalence of discoidal<br />

forms in the oryctocenosis suggests shallow<br />

marine conditions in the Late<br />

Eifelian and Middle Frasnian basins.<br />

Two new biostratons, the Upper Eifelian<br />

beds with Primaritripus kariukmasensis<br />

and Middle Frasnian beds with Primaritripus<br />

chuvashovi, are established based<br />

on radiolarians.<br />

2010010135<br />

放 射 虫 Adamas Afanasieva, 2000 和<br />

Wonella Afanasieva, 2000 属 新 名 =<br />

New replacement names for the genera<br />

Adamas Afanasieva, 2000 and Wonella<br />

Afanasieva, 2000 (Radiolaria). ( 英 文 ).<br />

Afanasieva M S. Paleontological Journal,<br />

2009, 43(1): 115<br />

2010010136<br />

乌 拉 尔 山 南 部 泥 盆 纪 放 射 虫 新 发 现 :<br />

1. 早 - 中 泥 盆 世 ( 埃 姆 斯 期 晚 期 — 艾 菲<br />

尔 期 早 期 ) = New radiolarians from<br />

the Devonian of the southern Ural<br />

Mountains: 1. Early-Middle Devonian<br />

(Late Emsian-Early Eifelian). ( 英 文 ).<br />

Afanasieva M S; Amon E O. Paleontological<br />

Journal, 2008, 42(5): 451-<br />

467 5 图 版 .<br />

Late Emsian-Early Eifelian radiolarians<br />

from the southern Ural Mountains<br />

are recorded and described for the first<br />

time. They come from the Kamennaya<br />

Gora section on the Tanalyk River near<br />

the town of Buribay, Bashkiria. The new<br />

Late Emsian-Early Eifelian radiolarian<br />

assemblage consists of 20 species of 11<br />

genera of spherical, discoidal, spindleshaped,<br />

pylomate, and spiny radiolarians.<br />

Four new species, i.e., Entactinia rostriformis<br />

sp. nov., Palaeodiscaleksus tumefactus<br />

sp. nov., Primaritripus buribayensis<br />

sp. nov., and P. chuvashovi sp.<br />

nov., are described. The diagnosis of the<br />

genus Primaritripus Afanasieva, 2000 is<br />

amended. The fact that the oryctocenosis<br />

is dominated by discoidal radiolarians<br />

suggests that, in the Late Emsian-Early<br />

Eifelian, the area under study was occupied<br />

by a relatively shallow marine basin.<br />

Based on radiolarians, a new Upper<br />

Emsian-Lower Eifelian biostraton, beds<br />

with Primaritripus buribayensis-<br />

Entactinia rostriformis, is established.<br />

The history of the study of Early Devonian<br />

radiolarians is considered.<br />

2010010137<br />

古 生 代 放 射 虫 Entactinia Foreman,<br />

1963 和 Stigmosphaerostylus Rüst,<br />

1892 属 的 分 类 位 置 = Taxonomic status<br />

of the genera Entactinia Foreman, 1963<br />

and Stigmosphaerostylus Rüst, 1892<br />

(Radiolaria of the Paleozoic). ( 英 文 ).<br />

Afanasieva M S; Amon E O. Paleontological<br />

Journal, 2008, 42(4): 343-<br />

349 1 图 版 .<br />

The genera Entactinia Foreman, 1963<br />

and Stigmosphaerostylus Rüst, 1892 are<br />

revised. The major differences between<br />

the two genera are manifested in the<br />

structure of the outer shell, internal spicule,<br />

and the number of the main spines;<br />

this suggests that they should be as-<br />

48

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