鸟疟原虫一新种—竹鸡疟原虫的记述（孢子纲：疟原虫科）

本文描述采自粤北灰胸竹鸡Ｂａｍｂｕｓｉｃｏｌａ ｔｈｏｒａｃｉｃａ的一种小型疟原虫,该虫与近似种海南联核疟原虫Ｐ．ｊｕｘｔａｎｕｃｌｅａｒｅ甚接近,但存在显著的差别,经鉴定为诺维虫亚属Ｎｏｖｙｅｌｌａ中一新种,即竹鸡疟原虫Ｐｌａｓｍｏｄｉｕｍ（Ｎｏｖｙｅｌｌａ）ｂａｍｂｕｓｉｃｏｌａｉ ｓｐ．ｎｏｖ．。模式标本保存在中山大学生物学系寄生虫学研究室。     

中国叉木蛾属Metathrinca研究及三新种记述（鳞翅目：木蛾科）

记述中国叉木蛾属３新种：银叉木蛾Ｍｅｔａｔｈｒｉｎｃａ ａｒｇｅｎｔｅａ,ｓｐ．ｎｏｖ．,佛坪叉木蛾Ｍｅｔａｔｈｒｉｎｃａ ｆｏｐｉｎｇｅｎｓｉｓ,ｓｐ．ｎｏｖ．和梅花山叉木蛾Ｍｅｔａｔｈｒｉｎｃａ ｍｅｉｈｕａｓｈａｎａ,ｓｐ．ｎｏｖ．,绘出了雌雄外生殖器特征图,并提供了中国已知种检索素。模式标本保存在南开大学生物系。     

河北大锥蚤—新亚种记述(蚤目:角叶蚤科)

报道采自湖北省神农架林区大锥蚤属ＭａｃｒｏｓｔｙｌｏｐｈｏｒａＥｗｉｎｇ,１９２９一新亚种,即河北大锥蚤神农架亚种Ｍａｃｒｏｓｔｙｌｏｐｈｏｒａｈｅｂｅｉｅｎｓｉｓｓｈｅｎｎｏｎｇｊｉａｅｎｓｉｓｓｐ．ｎｏｖ．。模式标本保存于湖北省医学科学院寄生虫病研究所媒介昆虫研究室。     

中国大疣蛛属一新种（蜘蛛目：六疣蛛科）

本文记述了我国六疣蛛科大疣蛛属一新种,命名为单卷大疣蛛,Ｍａｃｒｏｔｈｅｌｅ ｍｏｎｏｃｉｒｃｕｌａｔａ ｓｐ．ｎｏｖ．,本文量度单位ｍｍ。模式标本保存在湖南师范大学省生物研究所。     

中国蝙蝠体翼手恙螨属一新种（蜱螨亚纲：恙螨科）

本文记述采自江西的翼手恙螨属一新种,由毛翼手恙螨,新种Ｃｈｉｒｏｐｔｅｌｌａ ｃｕｒｖｉｓｅｔｏｓａ ｓｐ．ｎｏｖ．,模型标本保存于江西医学院寄生虫学教研室。     

FIVE NEW SPECIES OF MACROPHYA(HYMENOPTERA:TENTHREDINOMOR-PHA:TENTHREDINIDAE)FROM CHINA

本文记述中国宽腹叶蜂属５新种：长腹宽腹叶蜂Ｍ．ｄｏｌｉｃｈｏｇａｓｔｅｒＷｅｉｅｔＭａ,ｓｐ．ｎｏｖ．,缨鞘宽腹叶蜂Ｍ．ｐｉｌｏｔｈｅｃａ,ｓｐ．ｎｏｖ．,童氏宽腹叶蜂Ｍ．ｔｏｎｇｉＷｅｉｅｔＭａ,ｓｐ．ｎｏｖ．,赵氏宽腹叶蜂Ｍ．ｚｈａｏａｅＷｅｉ,ｓｐ．ｎｏｖ．,郑氏宽腹叶蜂Ｍ．ｚｈｅｎｇｉＷｅｉ,ｓｐ．ｎｏｖ．。模式标本均保存于中南林学院昆虫标本室。文中还将尖唇宽腹叶蜂黄柄亚种ＭａｃｒｏｐｈｙａｖｅｒｔｉｃａｌｉｓｔｏｋｉｎｅｎｓｉｓＭａｌａｉｓｅ提升为种：黄柄宽腹叶蜂ＭａｃｒｏｐｈｙａｔｏｋｉｎｅｎｓｉｓＭａｌａｉｓｅｓｔａｔ．ｎｏｖ．。     

陕西环蛱蝶属一新亚种（鳞翅目：蛱蝶科）

本文记述陕西省环蝶属Ｎｅｐｔｉｓ Ｆａｂｒｉｃｉｕｓ １新亚种－茂环峡蝶宁陕亚种Ｎ．ｎｅｍｏｒｏｓａ ｎｉｎｇｓｈａｎｅｎｓｉｓ,ｓｓｐ．ｎｏｖ．模式标本保存在河南师范大学生物系。     

藤高腹茧蜂属及一新种记述：膜翅目：茧蜂科：高腹茧蜂亚科

本文报道采自浙江西天山目的藤高腹茧蜂属Ｒａｔｔａｎａ ｖａｎ Ａｃｈｔｅｒｂｅｒｇ一新种：中华藤高腹茧蜂Ｒ．ｓｉｎｉｃａ,ｓｐ．ｎｏｖ。该属为我国新记录,该亚科为我国大陆新记录。模式标本保存在浙江农业大学。     

山东危害槐树的三刺角蝉属一新种：同翅目：角蝉科：露盾角蝉亚科

本文记述在山东省危害槐树ＳｏｐｈｏｒａｊａｐｏｍｉｃａＬｉｎｎａｅｕｓ的三刺角蝉属Ｔｒｉｃｅｎｔｒｕｓ１新种；槐树三刺角蝉Ｔｒｉｃｅｎｔｒｕｓｓｏｐｈｏｒａｅｓｓｐｎｏｖ，其寄主除槐树外，还有龙爪槐Ｓ．ｊａｐｏｎｉｃａｆ．ｐｅｎｄｕｌａＬｏｎｄ．刺槐ＲｏｂｒｉｎｉａｐｓｅｕｄｏａｃａｃｉａＬｉｎｎ，紫穗槐ＡｍｏｒｐｈａｆｒｕｔｉｃｏｓａＬｉｎｎ，模式标本保存于西北农业大学昆虫博物馆。     

云南省宏痣泥蜂属二新种（膜翅目：泥蜂科）

本文记述采自云南省的宏痣泥蜂属２新种：皱胸宏痣泥蜂Ｓｐｉｌｏｍｅｎａ ｒｈｙｔｉｔｈｏｒａｃｉｃａ,ｓｐ．ｎｏｖ．和突唇宏痣泥蜂Ｓｐｉｌｏｍｅｎａ ｃｈｙｐｅｉ,ｓｐ．ｎｏｖ．。模式标本保存在浙江农业大学昆虫标本室。     

疑源类Tianzhushania在贵州瓮安震旦纪陡山沱组磷块岩中的发现

首次报道贵州瓮安地区震旦系陡山沱组磷块岩中的大型具刺凝源类Tianzhushania spinosa及其新种Tianzhushania tuberifera sp.nov.前者形态特征及内部结构与湖北峡尔地区震旦系陡山沱组隧石结核中发现的典型Tianzhushania spinosa 标本（硅化）完全相同,但多数未遭受重力挤压呈球形保存。新种特征明显,也呈球形保存,但内层表面具有明显瘤突,瘤突顶端向外延伸出单一或多条管状制,另外还探讨大型具刺疑源类Tianzhushania属的特征,已定种的地理分布,地层意义和亲缘关系。     

湖北峡东地区九龙湾剖面震旦系陡山沱组微体化石的新发现

中国南方扬子地台震旦系陡山沱组产出丰富的微体化石,它们主要保存在磷块岩以及燧石结核和条带中。文章详细报道湖北峡东地区九龙湾剖面震旦系陡山沱组微体化石,描述以前未曾在峡东地区碳酸盐相燧石中发现的8属8种微体化石。研究九龙湾剖面陡山沱组大型带刺疑源类、微体多细胞藻类和动物胚胎化石的分布特征,发现Tianzhushania spinosa是最早出现的大型带刺疑源类分子,大冰期后微体生物的辐射是一个阶段性渐进的过程。同时．本项研究进一步证实华南扬子区陡山沱组碳酸盐相燧石和磷块岩地层中保存的微体化石面貌基本一致。     

Sphenobaiera ikorfatensis (Seward) Florin from the Lower Cretaceous of Huolinhe, eastern Inner Mongolia, China

Sphenobaiera ikorfatensis (Seward) Florin from the Lower Cretaceous Huolinhe Formation in the Huolinhe coal–mining area, eastern Inner Mongolia, China, is identified, described and figured. Comparison with the type material of Sphenobaiera ikorfatensis (Seward) Florin from West Greenland confirms its identity. About 20 Chinese leaf specimens are known with well preserved cuticle which is closely similar to the Greenland leaves but more papillate. The palaeoclimatic and phytogeographic significance of the occurrence of this species is discussed in relation to the suggestion that West Greenland, north–east China and eastern Siberia were in the same phytogeographic region during the Lower Cretaceous.     

安徽淮南寒武纪一新三叶虫属——Huaiaspis

安徽淮南八公山地区寒武纪毛庄-徐庄期地层出露良好,化石丰富。在老鹰山剖面徐庄组底部的紫色页岩内所采集大量三叶虫标本中发现的一种新的三叶虫,命名为Huaiaspishuainanensisgen.etsp.nov.,它代表了一个尚未描记的且科级分类位置待定的新属新种。该三叶虫特点突出,是头部特征极度消隐且不具眼、眼叶、眼脊的“盲三叶虫”。该三叶虫为小尾型后颊类,主要特征为:壳面光滑,背壳呈次椭圆形,头盖半圆形;头鞍呈钟形向前收缩;背沟浅,仅在侧光下可见;活动颊平滑宽大,具有宽阔的活动颊刺;胸部由14节组成;尾部中轴粗壮,无边缘沟。     

Age constraints of the Hungshihyen Formation (Early to Middle Ordovician) on the western margin of the Yangtze Platform,South China: New insights from chitinozoans

The Hungshihyen Formation represents the Lower to Middle Ordovician near-shore siliciclastic deposits on the western margin of the Yangtze Platform, South China. However, its age is still debated, largely because of insufficient studies. Here we documented the Bursachitina maotaiensis–B. qianbeiensis chitinozoan assemblage from the lower part of the Hungshihyen Formation at Songliang, Qiaojia County, eastern Yunnan Province. This assemblage is remarkably similar to an assemblage that roughly correlates to the middle part of the Corymobograptus deflexus graptolite Biozone in northern Guizhou Province, indicating that the Hungshihyen Formation at Songliang is probably of late Floian age and may extend into the early Dapingian. Additionally, a revision on the chitinozoans previously documented from the strata assigned to the same formation in the Wuding area was made according to the latest classification. The revision allows the recognition of the Euconochitina symmetrica–Eremochitina brevis assemblage, and therefore suggests a late Tremadocian age for this interval based on regional and global chitinozoan biostratigraphic correlations. Considering also its lithologic succession, we argue that the chitinozoan-bearing strata in the Wuding area previously assigned to the Hungshihyen Formation correspond most likely to the uppermost part of the underlying Tangchi Formation or the lowermost part of the Hungshihyen Formation. The base of the Hungshihyen Formation appears therefore to be diachronous in eastern Yunnan Province.     

RE-ASSESSMENT OF THE TYPE COLLECTIONS OF CORALLINALEAN GENERA (CORALLINALES, RHODOPHYTA) DESCRIBED BY V. P. MASLOV

Abstract:  From 1935 to 1962 Maslov published two monographs and several other papers on the taxonomy of fossil calcareous algae of diverse ages from the large geographical area of the former USSR. Among many other taxa, he described five new genera ( Solenophyllum , Palaeophyllum , Mesolithon , Bicorium and Tomilithon , as a subgenus of Parachaetetes Deninger) which he attributed to the Corallinaceae, and the new genus Karpathia , which he included in the Squamariaceae. Type material of these taxa, except for Mesolithon , is housed in the Geological Institute of the Russian Academy of Sciences, Moscow. Re-examination of the genus types from a modern perspective of coralline algal taxonomy shows that Karpathia is a validly published genus of corallinaceans (subfamily Mastophoroideae) to which several Cenozoic fossil species can be assigned. In contrast, the holotype of P. elegans , the type species of Palaeophyllum , cannot be assigned to any subfamily within the Corallinaceae and its preserved features are inadequate for confidently delimiting a separate genus. Solenophyllum is a valid genus in which Palaeozoic representatives of Corallinales formerly attributed to Parachaetetes Deninger can be included. Tomilithon is considered a younger heterotypic synonym of Solenophyllum . The algal nature of the bioclasts in the type of Bicorium is uncertain.     

湖北三峡地区埃迪卡拉系灯影组Hiemalora stellaris生物属性及埋藏分析

Hiemalora stellaris是湖北宜昌三峡地区埃迪卡拉系灯影组石板滩生物群中数量最为丰富的化石类型之一,由位于中心位置的圆盘和围绕盘缘向外伸出的似触手状结构组成,似触手状结构长度与圆盘直径具有较好相关性。同时也发现少量Hiemalora与茎干相连,其中一枚产自石板滩段底部的标本保存完整,与茎干连接有叶状体。叶状体呈卵形,可见一级分枝与二级分枝,顶部有呈"牛角状"的尖刺,叶状体形态与Charniodiscus spinosus相似。结合纽芬兰地区发现的Primocandelabrum hiemaloranum,表明Hiemalora作为生物体的固着器官,起到抵御水流冲刷、支撑和固定整个生物体的作用,但与其相连的叶状体表现出不同的形态类型,表明Hiemalora化石可能具有较为多样的生物来源。根据化石的形态特征和埋藏状态分析,Hiemalora在生物生活时位于藻席层之下的沉积物内,常呈正凸起保存于岩层顶面,而茎干和叶状体位于水体中,生物死亡后,叶状体倒伏在藻席层之上,当岩层沿藻席层劈开后,在顶面保存为凹陷的印痕。     

A new dasycladalean alga from the Lower Cretaceous of the Eastern Carpathians (Romania): Andreiella rajkae nov. gen., nov. sp.

Lower Cretaceous limestones from Bicaz Gorges (Eastern Carpathians, Romania), developed in Urgonian facies, frequently contain dasycladalean algae. In limestone samples collected from the eastern sector of the Bicaz Gorges, we have identified a large dasycladalean alga that we assign here to a new species and genus: Andreiella rajkae nov. gen. nov. sp. The general morphological features and the calcification pattern distinguish this new alga from previously known dasycladaleans with two orders of laterals.     

New data on the Devonian and Carboniferous Graptolithina (Dendroidea) from Belgium with notes on possible occurrences of Rhabdopleuridae in the Belgian Carboniferous

An old find of a graptolite from the Eifelian Jemelle Formation, combined with the recent discovery of an exceptionally well-preserved specimen from the Upper Frasnian (Matagne Formation), allow documentation of the geologically oldest and youngest dendroid fossils from the Devonian of Belgium. Both are ascribed to the long-ranging genus Callograptus (Acanthograptidae). These records enlarge the sparse knowledge of graptolite diversity and occurrences along the southern margin of Laurussia during the mid-Paleozoic. In Belgium, Devonian dendroids are exclusively known from the Dinant Synclinorium. The Devonian dendroid faunas previously reported from the Eifelian, Givetian and Frasnian of the Ardenne–Rhenish massifs (Belgium and Germany) are of low diversity (one to five species per locality). The specimens, generally inedaquatelly preserved, were ascribed to the genera Callograptus, Dictyonema, Palaeodictyota?, and Ruedemannograptus? In these massifs, Carboniferous dendroids are only known from the Viséan (Moliniacian) Denée Konservat-Lagerstätte. Other but undocumented reports of dendroids (and rhabdopleurids) are from the historical type area of the Tournaisian Stage (Tournai area, Brabant Parautochthon). Rhabdopleuridae from the Viséan–Serpukhovian of the Campine Basin (Turnhout borehole) remain incompletely known in the absence of the previously described material.