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synclines and assigned to the family<br />

Parahexacrinidae. Furthermore, “Hexacrinites<br />

sp.” sensu Głuchowski (1993),<br />

from the Upper Frasnian of the Holy<br />

Cross Mountains (Poland), is transferred<br />

to the family Parahexacrinidae and classified<br />

as Parahexacrinitidae sp. I. comb.<br />

nov. Numerous parahexacrinitid species<br />

were erected based on the description of<br />

isolated columnals. New material from<br />

the Eifel proved that several of these<br />

species are not distinguishable from<br />

other crinoid groups, which is demonstrated<br />

for “Parahexacrinus ellipticus”<br />

and Melocrinites pyramidalis.<br />

2010010399<br />

泥 盆 纪 Helianthasteridae 科 ( 海 星 纲 :<br />

棘 皮 动 物 门 ) 的 重 新 评 价 = Reevaluation<br />

of the Devonian family Helianthasteridae<br />

Gregory, 1899 (Asteroidea:<br />

Echinodermata). ( 英 文 ). Blake D B. Palaeontologische<br />

Zeitschrift, 2009, 83(2):<br />

293-308<br />

Because of their taxonomic and morphologic<br />

diversity, the asteroids of the<br />

Lower Devonian Hunsruck Slate of<br />

Germany are important to both an understanding<br />

of the history of the class<br />

Asteroidea and to the interpretation of<br />

community evolution during the Paleozoic.<br />

The Helianthasteridae Gregory is<br />

restricted to Helianthaster and Arkonaster<br />

Kesling, 1982 (Middle Devonian,<br />

Canada); Lepidsterella Schuchert is<br />

similar to other two genera but known<br />

specimens are of poor quality and as resut<br />

the status of the genus is uncertain.<br />

Neither Helianthaster nor other Hunsruck<br />

asteroids appear closely linked to<br />

the crown group; instead, functional patterns<br />

apparently re-emerged through<br />

time, although identification of specific<br />

behavior of ancient asteroids is difficult<br />

to impossible.<br />

2010010400<br />

前 乌 拉 尔 早 二 叠 世 Catillocrinidae 科<br />

的 多 臂 海 百 合 新 发 现 = New multiarmed<br />

crinoids of the family Catillocrinidae<br />

from the Lower Permian of<br />

the Fore-Urals. ( 英 文 ). Arendt Yu A.<br />

Paleontological Journal, 2007, 41(1):<br />

61-68 2 图 版 .<br />

New Catillocrinidae Allocatillocrinus<br />

rarus sp. nov., with a previously unknown<br />

tegmenal structure, Paracatillocrinus<br />

shamovi sp. nov., and P. shakhtauensis<br />

sp. nov., with an unusual relative<br />

position of the crown and stem are<br />

described from the Artinskian Stage<br />

(Lower Permian) of the western slope of<br />

the Middle and Southern Ural Mountains<br />

(Boets, Krasnoufimsk, and Shakh-<br />

Tau localities). The genus Allocatillocrinus<br />

has not previously been recorded<br />

from the Permian, while Paracatillocrinus<br />

has only previously been reported<br />

from the Upper Permian of Timor<br />

Island.<br />

2010010401<br />

西 伯 利 亚 Lena 河 下 游 中 寒 武 统<br />

Mayaktakh 组 的 Carpozoan 类 棘 皮 动<br />

物 = Carpozoan echinoderms from the<br />

Middle Cambrian (Mayaktakh Formation)<br />

of Siberia (lower reaches of the<br />

Lena River). ( 英 文 ). Rozhnov S V. Paleontological<br />

Journal, 2006, 40(3): 266-<br />

275 7 图 版 .<br />

Two new monotypic genera and a<br />

new monotypic family Rozanovicystidae<br />

of the class Cincta are described from<br />

the Middle Cambrian (Mayaktakh Formation)<br />

of the northeastern part of the<br />

Siberian Platform. Based on data obtained<br />

by morphofunctional analysis,<br />

there is a possibility that these animals<br />

could move by jet propulsion by ejecting<br />

water from the opercular aperture. Probable<br />

homologies of the main skeletal<br />

parts are discussed.<br />

分 类 位 置 不 明<br />

2010010402<br />

巴 西 北 部 亚 马 孙 盆 地 Trombetas 群 几<br />

丁 虫 = The Trombetas Group chitinozoans<br />

of the Amazon Basin, Northern Bra-<br />

121

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