中国麻螽属四新种记述（直翅目：露螽科）

本文记述麻螽属４新种,海南麻螽Ｔａｐｅｉｎａｈａｉｎａｎｅｎｓｉｓｓｐ．ｎｏｖ细齿麻螽Ｔａｐｅｉｎａｓｐｉｎｉｃａｕｄａｔａｓｐ．ｎｏｖ四齿麻螽Ｔａｐｅｉｎａｑｕａｄｒｉｄｅｎｓｓｐ．ｎｏｖ。和简麻螽Ｔａｐｉｅｎａｓｉｍｐｌｉｃｉｓｓｐ．ｎｏｖ．新种模式标本均保存在中国科学院上海昆虫研究所。     

我国微茎类吸虫的研究Ⅻ.类茎属及多黄属二新种报道：复殖目：微茎科

本文报道在湛江市附近海域海鸟体内获得的两种吸虫,经鉴定为新种,命名为巨口类茎吸虫,新种Ｍｉｃｒｏｐｈａｌｌｏｉｄｅｓ ｍａｃｒｏｓｔｏｎｒｓ ｓｐ．ｎｏｖ．,珊瑚多黄吸虫,新种Ｍｕｌｔｉｖｉｔｅｌｌｕｓ ｃｏｒａｌｉｕｓ ｓｐ．ｎｏｖ．     

广西地区蚱科三新种记述

本文记述采自广西壮族自治区蚱科３新种,即瘤米蚱Ｍｉｓｈｔｓｈｅｎｋｏｔｅｔｔｉｘ ｔｕｂｅｒｃｕｌａｔａ ｓｐ．ｎｏｖ．、拟喀蚱Ｔｅｔｒｉｘ ｃｅｐｅｒｏｉｄｅｓ ｓｐ．ｎｏｖ．及粗股蚱Ｔｅｔｒｉｘ ｇｒｏｓｓｉ ｆｍｅｕｒａ ｓｐ．ｎｏｖ。     

中国齿裂菌属研究IV.*

报道我国齿裂菌属的 ５个分类单元,其中多角齿裂菌 Ｃｏｃｃｏｍｙｃｅｓ　ｍｕｔｔａｎｇｕｌａｒｉｓ Ｙ． Ｒ．Ｌｉｎ　＆ Ｚ． Ｚ． Ｌｉ ｓｐ． ｎｏｖ,中国齿裂菌 Ｃ ｓｉｎｅｎｓｉｓ Ｙ． Ｒ Ｌｉｎ　＆ 　Ｚ． Ｚ． Ｌｉ ｓｐ． ｎｏｖ．和山矾齿裂菌 Ｃｓｙｍｐｌｏｃｉ　Ｙ．Ｒ　Ｌｉｎ　＆　ｚ．ｚ．Ｌｉ　ｓｐ．ｎｏｖ．是新种,辐射状齿裂菌Ｃｒａｄｉａｔｕｓ　Ｓｈｅｒｗ为中国新记录。提供了新种的拉丁文简介、汉文描述和形态特征图。模式标本存放在安徽农业大学森林保护教研室（ＡＡＵＦＰ）。     

广西地区蚱科三新种记述(直翅目:蚱总科)

本文记述采自广西壮族自治区蚱科３新种,即瘤米蚱Ｍｉｓｈｔｓｈｅｎｋｏｔｅｔｉｘｔｕｂｅｒｃｕｌａｔａｓｐ．ｎｏｖ．、拟喀蚱Ｔｅｔｒｉｘｃｅｐｅｒｏｉｄｅｓｓｐ．ｎｏｖ．及粗股蚱Ｔｅｔｒｉｘｇｒｏｓｉｆｅｍｕｒａｓｐ．ｎｏｖ．。     

中国瘿螨科一新属五新种记述（蜱螨亚纲：瘿螨总科）

文内新属为帽瘿螨属Ｍｉｔｒａｔｕｓ Ｋｕａｎｇ,ｇｅｎ．ｎｏｖ．,新种是构帽瘿螨Ｍ．ｂｒｏｕｓｓｏｎｅｔｉａｅ Ｋｕａｎｇ,ｓｐ．ｎｏｖ．,张掖瘿螨Ｅｒｉｏｐｈｙｅｓ ｚｈａｎｇｙｅｅｎｓｉｓ Ｋｕａｎｇ ｅｔ Ｌｕｏ,ｓｐ．ｎｏｖ．,柳刺瘿螨Ａｃｕｌｕｓ ｓａｌｉｃｉｓ Ｋｕａｎｇ ｅｔ Ｌｕｏ,ｓｐ．ｎｏｖ．,拟醋栗花刺瘿螨Ａｎｔｈｏｃｏｐｔｅｓ ｐａｒａｒｉｂｉｓ Ｋｕａｎｇ,ｓｐ．ｎｏｖ．     

中国凹盾象属六新种记述（鞘翅目：象虫科）

本文记述产于我国的凹盾象属Ｓｔｅｎｏｓｃｅｌｉｓ昆虫６新种,分别为赤杨凹盾象Ｓｔｅｎｏｓｃｅｌｉｓ（Ｈｅｘａｓｔｅｎｏｓｃｅｌｉｓ）ａｌｎｉ ｓｐ．ｎｏｖ．,圆窝凹盾象Ｓ．ｆｏｖｅａｔｕｓ ｓｐ．ｎｏｖ．,齿突凹盾象Ｓ．ａｃｅｒｂｕｓ ｓｐ．ｎｏｖ．,小点凹盾象Ｓ．ｐｕｎｃｔｉｃｕｌａｔｕｓ ｓｐ．ｎｏｖ．,洼喙凹盾象Ｓ．ｒｅｃａｖｕｓ ｓｐ．ｎｏｖ．,和蔚县凹盾象Ｓ．ｙｕｘｉａｎｅｎｓｉｓ ｓｐ     

中国犁沟茧蜂属四新种记述：膜翅目;茧蜂科：软节茧蜂亚科

本文报道犁沟茧蜂属Ａｕｌｏｓａｐｈｅｓ Ｍｕｅｓｅｂｅｃｋ４新种,即中华犁沟茧蜂Ａ．ｃｈｉｎｅｎｓｉｓ ｓｐ．ｎｏｖ,福建犁沟茧蜂Ａ;ｆｕｊｉａｎｅｎｓｉｓ ｓｐ．ｎｏｖ．,两色犁沟茧蜂Ａ．ｂｉｃｏｌｏｒ ｓｐ．ｎｏｖ。和缩颊犁沟茧蜂Ａ．ｃｏｎｓｔｒａｃｔｕｓ ｓｐ．ｎｏｖ。该属为我国新记录属。所有模式标本保存在浙江农业大学。     

中国花翅跳小蜂族二新纪录属和二新种(膜翅目:跳小蜂科)

描述了跳小蜂２新种,好寄生蜚蠊Ｂｌａｔｔａｒｉｄ的弯带敌蟑跳小蜂,新种Ｄｉｃａｒｎｏｓｉｓ ｓｉｎｕａｔｉｓ Ｘｕ,ｓｐ．ｎｏｖ．和采自陕西杨陵寄生寄蝇Ｔａｃｈｉｎｌｄ的斜棒蝇克跳小蜂,新种Ｅｘｏｒｉｓｔｏｂｉａ ｈｌｉｎｏｃｌａｖａｌａＸｕ,ｓｐ．ｎｏｖ．。敌蟑跳小蜂属Ｄｉｃａｒｎｏｓｉｓ Ｍｃｒｃｅｔ和蝇克跳小蜂属Ｅｘｏｒｉｓｔｏｂｉａ Ａｓｈｍｅａｄ在我国为新纪录属。     

小腹茧蜂属一新种记述（膜翅目：茧蜂科：小腹茧蜂亚科）

本文记述采自广西的小腹茧蜂属ＭｉｃｒｏｇａｓｔｅｒＬａｔｒｅｉｌｌｅ一新种,黄褐小腹茧蜂Ｍｉｃｒｏｇａｓｔｅｒｒａｖｕｓｓｐ．ｎｏｖ。     

Conodonts from the Permian Jisu Honguer (Zhesi) Formation of Inner Mongolia, China

The Jisu Honguer Formation (“Zhesi Formation”) is a North China marine carbonate unit of Permian age containing a mixed fauna of Tethyan, Boreal and endemic elements. The age of the Jisu Honguer Formation has been thought to range from Artinskian to Kazanian based on previous studies using mostly benthic macrofossils. A typical Mesogondolella aserrata conodont fauna is reported from the lower part of the upper member of the Jisu Honguer Formation in the Ulanqub District, Zhesi area, of northern China. The fauna indicates a Middle Permian (Guadalupian) age, most likely late Wordian to early Capitanian, for the strata yielding conodonts. The whole Jisu Honguer Formation could be assigned to the Wordian to early Capitanian age. The overlying Yihewusu Formation is probably of Capitanian age. There are no Wuchiapingian marine deposits in the Zhesi area. As characteristic of the open sea Guadalupian conodont faunas of the Tethys, smooth Mesogondolella dominate the fauna. The view that all Tethyan Guadalupian conodont faunas consist exclusively of serrated Mesogondolella cannot be confirmed. Three new species are described: Mesogondolella neoprolongata C. - y. Wang, Mesogondolella mandulaensis C. - y. Wang and Wardlawella jisuensis C. - y. Wang.     

滇西保山地区丁家寨组、卧牛寺组牙形刺的时代

本首次描述了滇西保山卧牛寺组及永德丁家寨组的Rabeignathus牙形刺动物群,其中2个新种：Rabeignathus yunnanensis sp．nov．,R．ritterianus sp．nov．,并划分出3个牙形刺带,进一步确定了古生物地层工作争论已久的卧牛寺组的时代为Artinskian晚期-Kungurian早期;丁家寨组上段为Sakmarian晚期-Artinskian早期。该牙形刺动物群为暖温型动物群,结合保山地块当时的古地磁资料,丁家寨组、卧牛寺组沉积之时,应处于边缘冈瓦纳区。卧牛寺组玄武岩喷发时间的确定,预示了保山地块从边缘冈瓦纳区分离出来的时间为Artinskian晚期。     

鄂东南晚二叠世菊石新材料

记述的菊石采自鄂东南大冶柯家湾晚二叠世大隆组,主要产于硅质页岩、硅质岩的灰岩透镜体中,共8属11种.此区大隆组仅相当于长兴阶的上部;Meitianoceras 在本区的出现,表明此属不仅分布于长兴阶的下部,也可延伸到长兴阶的上部.整个大隆组的化石,以自游生物为主,底栖类型很少.菊石中壳体大、壳面肋瘤发育者数量少,而壳饰弱、个体小者大量繁盛,呈现高丰度、低分异度的特点.保存化石的灰岩透镜体中具星散状的黄铁矿.本区晚二叠世晚期处于局部封闭的海湾环境.     

黔南下-中二叠统界线层的牙形刺--瓜达鲁平统底界在华南的确认

本文详细研究了贵州罗甸纳水剖面下－中二叠统界线、即瓜达鲁平统（Ｇｕａｄａｌｕｐｉａｎ）底界附近的牙形刺动物群,并自上而下划分为Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｓｉｃｉｌｉｅｎｓｉｓ－Ｍ．ｐｈｏｓｐｈｏｒｉｅｎｓｉｓ,Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｉｄａｈｏｅｎｓｉｓ－Ｍ．ｐｈｏｓｐｈｏｒｉｅｎｓｉｓ,Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｇｕｊｉｏｅｎｓｉｓ－Ｍ．ｉｎｔｅｒｍｅｄｉａ和Ｍｅｓｏｇｏｎｄｏｌｅ     

Pliensbachian gastropods from Venetian Southern Alps (Italy) and their palaeobiogeographical significance

Abstract: The Pliensbachian gastropods described by De Toni in 1912, coming from an isolated boulder at the foot of Mt Vedana (eastern margin of Trento Platform, Venetian Southern Alps, Italy) are revised. The fauna consists of 13 species representing nine families and eight superfamilies. Despite the low number of species, the assemblage represents the most diverse Early Jurassic gastropod fauna known for the Venetian Southern Alps. The boulder yielding the material was thought to derive from the upper part of the Early Jurassic Calcari Grigi Group, a carbonate platform unit extensively cropping out in the Mt Vedana area. The sedimentological analysis indicates a prevalently bioclastic wackstone‐floatstone, reflecting a lime‐muddy deposit undergone to an early consolidation. This and the high content of ammonoids, which is unusual for the Calcari Grigi Group, are typical aspects of a condensed pelagic sediment, presumably a fissure filling at the top of the carbonate platform succession. Palaeobiogeographical comparisons show that the fauna is composed of species occurring exclusively in pelagic limestones of the western Tethys. By contrast, it shows no relationships with the coeval faunas of the adjacent Trento platform and of the other western Tethyan carbonate platforms. These lines of evidence and the facies analysis would testify to the Pliensbachian drowning of the eastern margin of the Trento platform. In the wider context of the palaeobiogeographical history of Early Jurassic western Tethyan gastropods, the species from Vedana belong to a faunal stock which is typical for pelagic, mainly postdrowning sediments. Thus, appearance and diffusion in space and time of this stock were probably regulated by the direction, rate and pattern of the Neotethyan rifting. A new subgenus, Proarcirsa (Schafbergia) subgen. nov., and three new species, namely Ataphrus (Ataphrus) cordevolensis sp. nov., Guidonia pseudorotula sp. nov. and Proarcirsa (Schafbergia) zirettoensis sp. nov. are erected.     

孤峰组最底部的牙形刺动物群

在孤峰组底部发现了包括Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｎａｎｋｉｎｇｅｎｓｉｓ在内的牙形刺动物群。Ｇｏｎｄｏｌｅｌｌａ ｓｅｒｒａｔａ Ｃｌａｒｋ ｅｔ Ｅｔｈｉｎｇｔｏｎ,１９６２是Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｎａｎｋｉｎｇｅｎｓｉｓ（Ｊｉｎ,１９６０）的同义名,Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｎａｎｋｉｎｇｅｎｓｉｓ已被北美学者推荐为瓜达洛坪统底界的标志化石。因Ｍｅｓｏｇｏｎｄｏｌｅｌｌａ ｎａ     

贵州省惠水县王佑中泥盆世晚期的四射珊瑚(二)

贵州省惠水县王佑镇至翁赖村一带出露中泥盆统上部浅海底栖相翁赖组(新名),该组以陆源碎屑沉积居多、沉积厚度较大、群体珊瑚很少而单体珊瑚却比较发育为主要特征。其中,翁赖组上部层位与贵州独山剖面独山组鸡窝寨段相当,时代为中泥盆世吉维特期的晚期(late Givetian)。翁赖组上部之底非常特征的中华海绵珊瑚化石(Sinospongophyllum)与中泥盆统上部吉维特阶标准的腕足类化石鸮头贝(Stringocephalus)共栖。该属与华南地区中泥盆世晚期标准的内板珊瑚(Endophyllum)的内部骨骼构造非常相似,仅外部形态不同。在华南地区,内板珊瑚和中华海绵珊瑚的层位非常稳定,大致相当于吉维特阶的下varcus带。文中描述翁赖组上部四射珊瑚8属13种,包括Calceola intermediata inflata Yoh,,Cystiphylloides kwangsiense Yoh,C.secundus (Goldfuss),C.sp.,Paramixogonaria wangyouensis sp.nov.,Grypophyllum? sp.,Mictophyllum shawoziense He,M.sp.,Sinospongophyllum planotabulatum Yoh,Temnophyllum waltheri Yoh,T.poshiense Wang,T.complicatum Wang和Thamnophyllum crassum (Kong)等。它们与华南其他地区以及亚洲、欧洲、北非、澳大利亚和北美西部的同期分子都有十分密切的关系,同属于老世界生物地理大区(Old World Realm)。     

中国陕西中三叠世中蝎蛉科三新属新种(昆虫纲,长翅目)

记述中蝎蛉科Mesopanorpodidae 4属4种,其中包括3新属4新种：Longifurcula hejiafangensi gen.et sp.nov,Ladinochorista lata gen.et sp.nov.,Allochorista erdosensis gen.et sp.nov.,Itaphlebia tongchuanensis sp.nov..化石标本采自陕西铜川中三叠统铜川组下段上部的灰绿色泥岩和页岩.这些新属、种系陕西昆虫群铜川昆虫组合的新成员（属陕西动物群、陕西生物群的一个类别）.根据前人的植物、孢子、双壳、叶肢介、介形虫、昆虫化石等的研究结果,铜川组的时代划归中三叠世,相当于欧洲中三叠世拉丁尼期（Ladinian stage）.     

西藏晚白垩世晚Campanian期至早Maastrichtian期菊石群——中国最年轻的菊石群

记述产自西藏南部仲巴县的一个中国目前所知最年轻的菊石群 ,含 2科 4属 6种 ,其中 4新种。据菊石群面貌和它们所产出的层位可以划分出上、下两个组合带 :上部Pachydiscuscf.hidakaensis Libycoceraszhongbaense组合带 ;下部Manambolitescujiangdingensis M .pivaeteaui组合带。产菊石的曲贝亚组的下段和上段的中、下部(82F5 0及其以下层位 )为晚Campanian期 ,上段上部 (即 82F5 2及其以上层位 )为早Maastrichtian期。     

An early Bathonian Tethyan ammonite fauna from Argentina

Evidence for the Lower Bathonian Substage in most of the Pacific area has been lacking or controversial because index ammonoids of the Tethyan Subrealm in southern Europe and North Africa were unknown. During the Bathonian, the East Pacific margin belonged to either the Boreal Realm or the East-Pacific Subrealm of the Tethyan Realm, each with faunas distinctly different from the Eurafrican Tethyan faunas that form the basis for the chronostratigraphical standard. The first representatives of Morphoceras from South America, M. gulisanoi sp. nov., here described from a single locality in southern Mendoza Province, clearly document the Lower Bathonian Substage, probably the Zigzag Zone. Associated ammonoids are the perisphinctoidean Procerites cf. schloenbachi de Grossouvre and the oppeliid Oxycerites ( O. ) cf. aspidoides (Oppel), also typical Tethyan elements but less useful for dating.