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on inclusions of Lestremiinae (Diptera:<br />

Cecidomyiidae) in Rovno amber. ( 英 文 ).<br />

Jaschhof M. Paleontological Journal,<br />

2007, 41(1): 103-106<br />

Two articles on fossil Lestremiinae<br />

(Diptera: Cecidomyiidae) in Rovno amber<br />

(Perkovsky and Fedotova, 2004; Fedotova<br />

and Perkovsky, 2004) are reviewed<br />

and discussed. As a result, the<br />

following gall midges species are considered<br />

Lestremiinae incertae sedis: +<br />

Aprionus admirandus Fed., + Conarete<br />

laesus Fed., + Heterogenella sparsa<br />

Fed., + Micromyia convoluta Fed., +<br />

Peromyia autonoma Fed., + Peromyia<br />

miranda Fed., + Peromyia sukachevae<br />

Fed., + Peromyia zherikhini Fed. (all in<br />

Perkovsky and Fedotova, 2004), +<br />

Campylomyza falciformis Fed., + Campylomyza<br />

superposita Fed., + Neurolyga<br />

declinata Fed., + Strobliella appropinquata<br />

Fed., and + Strobliella capitata<br />

Fed. (all in Fedotova and Perkovsky,<br />

2004).<br />

2010010378<br />

外 贝 加 尔 东 部 中 生 代 晚 期 Isophlebiid<br />

蜻 蜓 ( 蜻 蜓 目 :Isophlebiidae ) =<br />

Isophlebiid dragonflies from the Late<br />

Mesozoic of eastern Transbaikalia<br />

(Odonata: Isophlebiidae). ( 英 文 ). Pritykina<br />

L N. Paleontological Journal,<br />

2006, 40(6): 636-645 5 图 版 .<br />

Based on the study of more than 300<br />

isophlebiid specimens from several Late<br />

Mesozoic sites in eastern Transbaikalia<br />

(Ukurei, Tergen’, Glushkovo, and Byankino<br />

formations), new genera and<br />

species are described: Xeta olovica, Dahurium<br />

draco, and Sinitsia sophiae. The<br />

insect-bearing deposits are dated Late<br />

Jurassic according to analysis of their<br />

odonatofauna.<br />

2010010379<br />

树 脂 化 石 中 鲜 为 人 知 的 直 翅 类 昆 虫<br />

( 多 新 翅 部 ) 新 发 现 : 第 一 次 交 流 =<br />

New and little known orthopteroid insects<br />

(Polyneoptera) from fossil resins:<br />

Communication 1. ( 英 文 ). Gorokhov A<br />

V. Paleontological Journal, 2006, 40(6):<br />

646-654 3 图 版 .<br />

New taxa of uncertain position within<br />

the infraclass Polyneoptera (Gryllomantidae<br />

fam. nov.: Gryllomantis gen. nov.,<br />

Lower Cretaceous; Mantoblattidae fam.<br />

nov.: Mantoblatta mira gen. et sp. nov.,<br />

Upper Cretaceous) and within the order<br />

Dictyoptera (Pseudojantaropterix gen.<br />

nov., Lower Cretaceous) are described.<br />

The superfamily Umenocoleoidea of uncertain<br />

position within the latter order is<br />

discussed on the basis of new information<br />

on Jantarimantidae and some other<br />

Cretaceous Dictyoptera.<br />

2010010380<br />

球 接 子 类 Pentagnostus proanabarensis<br />

Fedoseev, 1999 的 生 长 阶 段 =<br />

Growth and development of agnostids<br />

Pentagnostus proanabarensis Fedoseev,<br />

1999. ( 英 文 ). Naimark E B. Paleontological<br />

Journal, 2006, 40(5): 541-<br />

552 7 图 版 .<br />

Juvenile development of the Middle<br />

Cambrian agnostid trilobite Pentagnostus<br />

proanabarensis Fedoseev, 1999 is<br />

studied. A sequence of eight juvenile<br />

stages is defined based on changes in<br />

morphology and measurements. Three<br />

of them belong to meraspid degree 0,<br />

another three refer to meraspid degree 1,<br />

and two represent early holaspid stages.<br />

Neither the frequency distribution of the<br />

length of cephalons and pygidia nor the<br />

length-width scatter diagrams give clear<br />

clusters of molts; the number of juvenile<br />

molts can be estimated through the<br />

analysis of the posteroaxis length distribution.<br />

Thus, the measurements and<br />

morphology of some juvenile pygidia<br />

with vestiges of the pleural and postaxial<br />

furrows allow reconstruction of the<br />

number of segments during individual<br />

growth. At the initial stage of development,<br />

the pygidial axis of P. proanabarensis<br />

probably had four segments,<br />

115

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