肯尼亚早三叠世叶肢介一新属-Kenyaestheria

报道的叶肢介新属(Kenyaestheriagen.nov.)采自肯尼亚MajiyaChumvi地区的一钻孔,属下三叠统上马几牙楚姆维组(UpperMajiyaChumviFormation),其特征为壳瓣后背缘最后几条生长线靠近背缘处形成一个凹缘构造,但生长线在背缘并不反转弯曲,同时具有放射线纹饰,据此将其归于凹缘叶肢介科(Ulugkemiidae)。该科是一个灭绝的类群,分布于中泥盆统至上三叠统,古生代的类型都发现于欧亚大陆,晚三叠世的Triasulugkemia见于阿根廷,新属首见于早三叠世,也是在南大陆出现的第二例凹缘叶肢介类。孢粉Lunatisporitespellucidus和叶肢介AquilonoglyptaCorniaPalaeolimnadiaFalsisca组合指示含化石的地层时代为早三叠世早期。     

贵州早三叠世早期的介形类

该文报道的介形类化石系采自贵州省贞丰、遵义等地的飞仙关组,计7属11种,其中包括3新种和1未定种。这些介形类化石的发现,对认识我国早三叠世早期的介形类面貌,进一步提供了有意义的资料。Carinaknightina属在我国的首次发现,为我国二叠系与三叠系界线的研究,特别是与巴基斯坦盐岭地区相关地层的对比提供了可靠的生物依据。     

江苏句容青山早三叠世鱼类

记述了在江苏句容东昌青山早三叠世下青龙组上部发现的鱼类,计有6属8种,其中4新属6新种,为属两目两科。属裂齿鱼目裂齿鱼科的有Perleidus piveteaui,Perleidus aff.P.madagascariensis.“Perleidus”eu-rylepidotrichia sp.nov.和Zhangina cylindrica gen.et sp.nov;属骨鱼目副半椎鱼科的有Stensionotus dongchangensis sp.nov.,Jurongia fusiformis gen.et sp.nov.,Qingshania cercida gen.et sp.nov.和Suius brevis gen.et sp.nov.。上列绝大部分属种的特征充分显示这个鱼群与马达加斯加北部早三叠世鱼群的亲密关系,少数属种的特征也反映其与东格陵兰早三叠世鱼群有某些关系。     

浙江长兴早三叠世裂齿鱼类一新属

报道发现于浙江长兴全球二叠-三叠系界线层型剖面下三叠统殷坑组下部的一类裂齿鱼化石--长兴副裂齿鱼(新属、新种)Paraperleidus changxingensis gen.etsp.nov.,其左、右鼻骨在中间相接,独特的前鳃盖骨形状、位置以及宽长的膜质翼耳骨等特征,可区别于其他属。     

福建大田崆峒山晚二叠世和早三叠世介形类

报道福建大田崆峒山晚二叠世大隆组、长兴组及早三叠世溪口组介形类35属67种,其中描述8属9种(包括5新种)。产自长兴组的介形类化石被划分为3个组合,自下而上分别是：Polylites magnituberos-Or-thobairdia meishanensis-Pustulobairdia mailinensis组合,Baitrdia urodelofot-OS-orthobairdia exilimarginata-Bairdia subcontracta组合和Petasobairdia bicornuta-Neoamphissites costatus-Kegelites datianensis组合。大田崆峒山介形类动物群在二叠-三叠系界线上下具有明显的突变性质,这与世界其它地区一样,是遭受二叠纪末期的生物大灭绝事件重创所致。根据介形类化石组合特征,并参考共生或共存化石的内容,福建大田地区长兴组大致相当于浙江煤山长兴组的中、上部,长兴灰岩下伏的海相碎屑岩应划归长兴阶。大隆组、长兴组及溪口组的岩性和化石组合特征．显示古环境从滨海沼泽开始,经历浅海盆地→浅水碳酸盐台地→浅海近岸环境的演化过程。     

辽宁西部早三叠世苏铁植物一新属--Mediocycas gen. nov.及其演化意义

报道苏铁植物大孢子叶化石一新属———中间苏铁属(Mediocycasgen.nov.)。标本采集于辽宁省西部,喀左县杨树沟煤矿后山的早三叠世红砬组。这些标本以前曾被处理为疑问化石(Problematicum)。因当时资料不足,所以没有确定属种名称。但鉴于这些化石在苏铁类早期起源与演化研究中具有重要意义,故对它们作了重新研究。文中除了以喀左中间苏铁(Mediocycaskazuoensisgen.etsp.nov.)为典型种进行描述以外,还对新属、种在苏铁类起源与演化方面的意义作了较为详细的讨论。     

福建早二叠世叶肢介一新属

中国古生代的叶肢介知之甚少,南方早二叠世的叶肢介迄今尚无正式文献记载。1974年4月,福建地质一团在该省进行煤田勘探时,曾于钻孔中发现叶肢介化石,标注层位为龙潭组。只因化石数量太少,壳瓣保存不完整,产地又不详尽,因此,一直未作报道。之后,福建196煤田地质勘探队王信,在下二叠统童子岩组也找到了这一类型的叶肢介。1982年11月,     

湖北京山早三叠世有孔虫动物群的发现及其意义

本文首次报道了湖北京山地区早三叠世有孔虫动物群,计６属１５种,其中包括４新种,在对该动物群分析基础上,作者建立了Ａｕｌｏｔｏｒｔｕｓｃｈｉａｌｉｎｇｃｈｉａｎｇｅｎｓｉｓ－Ｄｉｃｈｏｓｐｉｒａｓｉｎｅｎｓｉｓ组合带,通过对其古生态特征及生物相研究,揭示了该动物群的生活习性与生态环境的关系,简述了该有孔虫动物群的发现在地层划分对比及油气勘探中的意义。     

宽网叶肢介属重要分类特征的发现

通过扫描电镜重新研究了产自俄罗斯维特奴河流域下三叠统维特奴宽网叶肢介(Loxomegaglypta wetlugiana Novo-jilov, 1958)的正模标本。扫描电镜成像揭示了光学照相无法分辨的重要分类学新特征, 其中包括: 生长带饰有圆形、角状或椭圆形小筛坑状装饰(直径15–25 μm), 筛坑被不同形状的隆起包围。均匀分布的针孔(直径4–6 μm)不但出现在筛坑里, 而且布满了筛坑周围的隆起。这种装饰与该属建立时描述的多角状大网格装饰区别较大。在此基础上,本研究修订了宽网叶肢介属生长带的装饰特征。     

陕北米脂上三叠统的进步古鳕类一新属——Mizhilepis

记述在陕西北部米脂县李家站乡张崖村上三叠统延长群瓦窑堡组中发现的进步古鳕类一新属新种Mizhilepiszhangyaensisgen.etsp.nov.,它与美国西部上三叠统钦尔组(ChinleFormation)和东北部上三叠统纽瓦克超群(NewarkSupergroup)中的TanaocrossusSchaeffer有密切的亲缘关系。文章还讨论了斯堪的纳维亚鳕科(Scanilepidae)的系统分类位置。     

昆明地区早寒武世三叶形虫新属——Panlongia Liu et Luo gen. nov.

简述早寒武世关山动物群的研究现状及重要意义。重点描述该动物群中一三叶形虫新属PanlongiaLiuetLuogen.nov.及其两个新种:即个体小、拥有等大的头甲和尾甲、边缘没有明显突出刺状物的PanlongiatetranodusaLiuetLuogen.etsp.nov.及头甲后侧和尾缘具刺的PanlongiaspinosaLiuetLuogen.etsp.nov.。三叶形虫在关山动物群中的首次发现为寒武纪生命大爆发以及古地理、古板块恢复的研究提供了有益的证据。     

原狭蚌虫属一新种（鳃足纲：介甲目）

作者于1987年6月自山东省兖州县淡水养殖试验场鱼池中发现原狭蚌虫属的一个新种——兖州原狭蚌虫Eoleptestheria yanchowensis sp.nov.作者对新种的形态特征进行了详细描述,并与中国原狭蚌虫Eoleptestheria chinensis Daday 1923,及东平原狭蚌虫Eoleptestheria dongpingensis Hu 1987。作了比较。     

A NEW PARASEMIONOTID-LIKE FISH FROM THE LOWER TRIASSIC OF JURONG, JIANGSU PROVINCE, SOUTH CHINA

Abstract:  Based on a well-preserved specimen from the Early Triassic Lower Qinglong Formation exposed at Qingshan Quarry, Jurong, Jiangsu Province of China, the new taxon Peia jurongensis gen. et sp. nov. is named and described with anatomical details of its dermal skull, neurocranium and postcranial skeleton. The new taxon is characterized by the following set of characters: shallow V-shaped, tuber-like rostral; anterior part of frontal widened to roughly same width as its posterior part; roughly squared parietal; supraorbital absent; wide and slightly posteriorly inclined preopercle; five small ossifications present in dorsal half of preopercle; preopercular canal shifting anteriorly in ventral half of the preopercle, and reaching the anteroventral corner of this bone; dermosphenotic joining the skull roof and with a descending lamina; numerous branchiostegal rays. Comparisons are made between the new taxon and several parasemionotids from the same locality; a discussion is carried out on the distribution and evolution of several characters in halecomorphs and other closely related neopterygians.     

云南省蚱科一新属新种(直翅目:蚱科)

本文报道蚱科一新属一新种。新属,微翅蚱属Alulatettix gen nov.的主要特征是前胸背板强烈隆起呈屋脊形,前胸背板侧片后缘具二凹陷,前、后翅甚微小。其模式种为云南微翅蚱Alulatettix yunnanensis sp.nov.     

RHYTIDOSTEID TEMNOSPONDYLS IN GONDWANA: A NEW TAXON FROM THE LOWER TRIASSIC OF BRAZIL

Abstract:  A new South American Early Triassic stereospondyl is described and considered to represent a new taxon, Cabralia lavinai gen. et sp. nov. The material consists of two well-preserved skull fragments. According to recent phylogenetic analyses of rhytidosteids and related taxa, the new taxon is referred to the Rhytidosteidae based on the presence of orbits that are located close to the skull margins, an otic notch that is reduced to an embayment, tabular horns that are reduced and broad based, a straight posterior margin of the palate, skull sculpture with nodules and pustules, and a 'twisted' quadrate ramus of the pterygoid. The presence of a prominent lacrimal bone suggests a basal position within Rhytidosteidae for C. lavinai , and possibly a close relationship with the Indian Indobrachyops , because all other known rhytidosteids exhibit the derived condition of an absence of the lacrimal. The presence of a basal rhytidosteid in the Paraná Basin of South America strongly supports previous hypotheses of a Gondwanan origin and radiation of stereospondyl temnospondyls during the Early Triassic, but leaves unresolved the question of where exactly they arose within that region.     

MORPHOLOGY OF PLACENTOPHORA (SOLIERIACEAE,GIGARTINALES: RHODOPHYTA), A NEW GENUS BASED ON SARCODIOTHECA COLENSOI FROM NEW ZEALAND1

The only member of the red algal family Solieriaceae known from New Zealand is the endemic Sarcodiotheca colensoi (Hook. & Harv.) Kylin. This study shows that it differs in several respects from the type S. furcata (Setch. & Gard.) Kylin; thus a new genus Placentophora is created for the New Zealand alga. Although P. colensoi nov. comb. is retained in the Solieriaceae on the basis of vegetative, spermatangial, tetrasporangial, carpogonial-branch and early gonimoblast features, it differs from typical members of that family in its pattern of later carposporophyte development. After a single gonimoblast initial is cut off from the auxiliary cell towards the center of the thallus, further gonimoblasts develop from the initial as ramifying, radiating filaments. These filaments enter an extensive “nutritive-cell” region surrounding the auxiliary cell, form, numerous connections to the “nutritive” cells, and incorporate most of them into a central placenta of interconnected, and variously-fused vegetative and gonimoblast cells. Carpo-sporangia then form in short chains around the periphery of the placenta. The cystocarp lacks both a central fusion cell and a sterile-celled investment, or “Faserhülle.” The distinctive carposporophyte of Placentophora is compared to patterns of gonimoblast development, known in other members of the Solieriaceae.