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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 />
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