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2010010145<br />

西 西 伯 利 亚 侏 罗 纪 和 石 炭 纪 有 孔 虫<br />

Ammosiphonia He, 1977 属 的 代 表 分<br />

子 = Representatives of the genus<br />

Ammosiphonia He, 1977 (Foraminifera)<br />

from the Jurassic and Carboniferous of<br />

Western Siberia. ( 英 文 ). Marinov V A.<br />

Paleontological Journal, 2006, 40(5):<br />

490-499 2 图 版 .<br />

The wide distribution of the genus<br />

Ammosiphonia in the Upper Jurassic and<br />

Carboniferous of Western Siberia is established<br />

for the first time. Six haplophragmoidid<br />

species of Western Siberia<br />

are assigned to this genus. The diagnosis<br />

of the genus is emended; the taxonomic<br />

positions and scopes of the species<br />

Ammosiphonia nonioninoides (Reuss), A.<br />

beresoviensis (Bulatova), and A. sibirica<br />

(Zaspelova) are revised; two new species,<br />

A. suprajurassica sp. nov. and A.<br />

valanginica sp. nov., are described.<br />

2010010146<br />

显 生 宙 放 射 虫 演 化 中 的 生 物 危 机 和 阶<br />

段 = Biotic crises and stages of radiolarian<br />

evolution in the Phanerozoic. ( 英 文 ).<br />

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

Journal, 2006, 40(4): S453-<br />

S467 3 图 版 .<br />

The questions of ecology and taphonomy<br />

of radiolarians are reviewed and<br />

reexamined. In Recent oceans and seas,<br />

the major part of the “radiolarian rain”<br />

(dead individuals) comes from the layer<br />

of the water column which is not deeper<br />

than 500 m; therefore, the bottom radiolarian<br />

thanatocenoses and taphocenoses<br />

are formed in all oceanic zones, including<br />

the coastal and central oligotrophic<br />

regions of oceans. However, radiolarians<br />

should not be regarded as indicators of<br />

exclusively deepwater oceanic conditions.<br />

The crucial moments in the evolution<br />

of radiolarians at the major Phanerozoic<br />

boundaries are recognized. A<br />

dynamic model of cyclic development of<br />

radiolarians in the Phanerozoic is proposed<br />

and four phases and nine stages in<br />

their evolution are recognized. The absence<br />

of an outburst of radiolarian biodiversity<br />

in the Holocene is shown.<br />

Many great extinctions of radiolarians<br />

occurred at the boundaries between seasons<br />

of galactic years.<br />

2010010147<br />

西 特 提 斯 晚 白 垩 世 rotaliid 类 有 孔 虫<br />

= Late Cretaceous rotaliids (Foraminiferida)<br />

from the Western Tethys.<br />

( 英 文 ). Boix C; Villalonga R; Caus E;<br />

Hottiger L. Neues Jahrbuch fur Geologie<br />

u. Palaontologie / Abhandlungen,<br />

2009, 253(2-3): 197-227<br />

During the global community maturation<br />

cycle starting at the Cenomanian-<br />

Turonian boundary and ending with the<br />

events at the K-T boundary, the rotallid<br />

foraminifera produce for the first time in<br />

Earth History a considerable diversity of<br />

K-strategists that exhibit large shell sizes,<br />

complex umbilical structures and an<br />

imprtant dimorphism of generations. In<br />

the Late Cretaceous Pyrenean Gulf four<br />

groups are distinguished.<br />

2010010148<br />

放 射 虫 Heliodiscidae Haeckel 科 新 种<br />

= New species of the family Heliodiscidae<br />

Haeckel (radiolaria). ( 英 文 ). Vishnevskaya<br />

V S. Paleontological Journal,<br />

2006, 40(2): 134-142 4 图 版 .<br />

The family Heliodiscidae Haeckel,<br />

1881, which includes five genera, is reviewed.<br />

New methods of investigation<br />

are applied to the inner structure of Cretaceous<br />

spherical radiolarian skeletons,<br />

which reveal numerous taxa with an eccentric<br />

microsphere. Three new species,<br />

Astrophacus marinae sp. nov., Excentrosphaerella<br />

kovalenkovi sp. nov., and<br />

Excentrosphaerella kurilovi sp. nov., are<br />

described. The eccentric position of the<br />

microsphere suggests that these forms<br />

are nontypical Mesozoic radiolarians or<br />

new representatives of the family Heliodiscidae<br />

Haeckel, 1881, which was previously<br />

recorded in the Cenozoic.<br />

51

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