北京延庆地区雾迷山组燧石相微体古生物研究

本文报道的微体化石产于北京延庆地区雾迷山组中的燧石相岩层中,共鉴定出10个属19个种,其中含1个新种,3个未定种,以及2个相似种。化石类型以蓝细菌中的颤藻科、念珠藻科和色球藻科属种为主,还保存有少量绿藻和大量分类位置未定的藻类。新的化石资料必将进一步丰富燕山雾迷山组的微化石群的内容,并为进一步评价雾迷山组微化石的生物演化和多样性的水平,及其生物地层意义提供更充分的依据。     

广西隆林祥播中二叠世生物礁的钙藻化石

本文描述了广西隆林祥播中二叠世茅口期生物礁中的钙藻化石17属18种,其中新属5个:Paralithoporella gen. nov., Guangxilamina gen. nov., Favoporella gen. nov., Sinophyllum gen. nov.,和Monostysisyrinx gen. nov.; 新种9个:Solenopora guangxien sis sp. nov., Paralithoporella sincrisis gen. et sp. nov., Guangxilamina incompta gen. et sp. nov., Favoporella hexagona gen. et sp. nov., Ivanovia permica sp. nov., Anchicodium expressum sp. nov., Sinophyllum hexagonum gen. et sp. nov., Sphaeroporella minima gen. et sp. nov., Monostysisyrinx circula ris gen. et sp. nov.。本文还建立一新科——Monostysi sy rinaceae。在当前生物礁中,钙藻是重要的造礁生物,可以起造架、粘结、障积等作用,也可作为居礁生物或造粒生物     

高于庄古生物学

距今14～16亿年的华北地区高于庄组黑色层状、结核状和透镜状燧石与叠层石的黑色硅质部分中保存着极丰富的原核和真核生物微化石.宏观藻类在该组的页岩中亦已发现.本组为评估中元古代生命状况、古环境和前显生宙生物地层提供了重要的生物信息.迄今为止在高于庄组地层中已有百余个化石种被人们认识.根据古植物和古环境的特征这些生物种类可分为三个不同的组合,即:1.颤藻和色球藻组合,出现在高于庄组一段,代表浅水藻席建造者和居住者与一些可能的外来浮游生物的种类;2.念珠藻组合,仅发生在该组的二段,还含一些底栖藻席建造者或居住者的种类;3.第四段的色球藻组合,它代表了潮间带至亚潮带的藻席建造者和外来的种类.元古代燧石中的微化石,尤其是蓝藻化石,尽管在元古代它们就已不断趋向于多样化,但由于它们形态上的保守性,对环境的指示比对地质时代的指示更有价值.高于庄组微化石的特点和大多数链状念珠藻垂直层理保存的事实表明:1.高于庄组微化石的个体大小随时间趋向于增大;2.高于庄组的沉积可能是处于一个淡水环境,且沉积率可能等于或少于微生物的生长率;3. 高于庄组织沉积模式可能是从潮间带至亚潮带或深海,然后再至潮间带或潮上带;4.当高于庄组沉积时真核生物亦已出现.     

高于庄古生物学(英)

距今 14～ 16亿年的华北地区高于庄组黑色层状、结核状和透镜状燧石与叠层石的黑色硅质部分中保存着极丰富的原核和真核生物微化石。宏观藻类在该组的页岩中亦已发现。本组为评估中元古代生命状况、古环境和前显生宙生物地层提供了重要的生物信息。迄今为止在高于庄组地层中已有百余个化石种被人们认识。根据古植物和古环境的特征这些生物种类可分为三个不同的组合 ,即 :1.颤藻和色球藻组合 ,出现在高于庄组一段 ,代表浅水藻席建造者和居住者与一些可能的外来浮游生物的种类 ;2 .念珠藻组合 ,仅发生在该组的二段 ,还含一些底栖藻席建造者或居住者的种类 ;3.第四段的色球藻组合 ,它代表了潮间带至亚潮带的藻席建造者和外来的种类。元古代燧石中的微化石 ,尤其是蓝藻化石 ,尽管在元古代它们就已不断趋向于多样化 ,但由于它们形态上的保守性 ,对环境的指示比对地质时代的指示更有价值。高于庄组微化石的特点和大多数链状念珠藻垂直层理保存的事实表明 :1.高于庄组微化石的个体大小随时间趋向于增大 ;2 .高于庄组的沉积可能是处于一个淡水环境 ,且沉积率可能等于或少于微生物的生长率 ;3.高于庄组织沉积模式可能是从潮间带至亚潮带或深海 ,然后再至潮间带或潮上带 ;4 .当高于庄组沉积时真核生物亦已出现。     

中国三江平原产新鞭毛藻

本文论述了采自中国三江平原(黑龙江省宝清县)的新鞭毛藻,共1新属6新种1新变种.新属为Cercobodoides gen. nov.; 6新种为Tranguillus pyriformis sp. nov., Cercobodo obliqua. sp. nov., Cercobodoides heilongjianica sp. nov.; Oicomonas ovata Sp. nov., Rhizomastix borealis sp. nov., Trigonomonas papillata sp. nov.; 1新变种为Tranguillus pyriformis var, obovata var. nov.     

中国甘肃和青海省叶蜂类六新种记述(膜翅目:叶蜂科)(英文)

记述了叶蜂科采自甘肃的3个新种:Tenthredo(Tenthredo)sinotemula sp.nov.,Tenthredo(Tenthredella)labrangensis sp.nov.和Tenthredo(Tenthredella)sinosimplex sp.nov.;采白青海的3个新种:Tenthredo(Tenthredella)rolleri sp.nov.,Tenthredo(Tenthredella)qinghaiensis sp.nov.和Tenthredo(Tenthredella)yunningsiensis sp.nov.     

高于庄古生物学

距今14～16亿年的华北地区高于庄组黑色层状、结核状和透镜状燧石与叠层石的黑色硅质部分中保存着极丰富的原核和真核生物微化石。宏观藻类在该组的页岩中亦已发现,本组为评估中元古代生命状况,古环境和显生宙生物地层提供了重要的生物信息。迄今为止在高于庄组地层中已有百余个化石种被人们认识,根据古植物和古环境的特征这些生物种类可分为三个不同的组合,即：1.颤藻和色球藻组合,出现在高于庄组一段,代表浅水藻席建造和居住与一些可能的外来浮游生物的种类;2.念珠藻组合,仅发生在该组的二段,还含一些底栖藻席建造或居住的种类;3.第四段的色球藻组合,它代表了潮间带至亚潮带的藻席建造和外来的种类。元古代燧石中的微化石,尤其是蓝藻化石,尽管在元古代它们就已不断趋向于多样化,但由于它们形态上的保守性,对环境的指示比对地质时代的指示更有价值。高于庄组微化石的特点和大多数链状念珠藻垂直层理保存的事实表明：1.高于庄组藻化石的个体大小随时间趋向于增大;2.高于庄组的沉积可能是处于一个淡水环境,且沉积率可能等于或少于微生物的生长率;3.高于庄组织沉积模式可能是多潮间带至亚潮带或深海,然后再至潮间带或潮上带;4.当高于庄组沉积时真核生物亦已出现。     

秦巴山区竹子上的瘿螨三新种记述(蜱螨亚纲,瘿螨总科,瘿螨科)

记述了采自陕西秦巴山区竹子上的瘿螨科3新种:纹股新波羽瘿螨Neocymoptus ornapodus sp.nov.,寄主慈竹Neosinocalamus affinis (Rendle) Keng;刚竹背槽瘿螨Aculochetus phyllostacher sp.nov.,寄主刚竹属Phyllostachys sp.;尖嘴四瘿螨Tetra spicrostrae sp.nov.,寄主刚竹属Phyllostachys sp..     

毛蚊科九新种记述：双翅目：长角亚目

本文记述了双翅目毛蚊科3属9新种,其中棘毛蚊属3种:长喙棘毛蚊 Ditophus macrosiphonius sp.nov.,吉林棘毛蚊 D.jilinensis sp.nov.和膜棘毛蚊 D.membranaceus sp.nov.;叉毛蚊属2种:异角叉毛蚊 Penthetria aberrans sp.nov.和甘肃叉毛蚊 P.gansuensis sp.nov.;襀毛蚊属4种:裂襀毛蚁 Plecia dilacerabilis sp.nov.,峨眉襀毛蚊 P.emeiensis sp.nov.,钳襀毛蚊 P.forcipiformis sp.nov.和长叶襀毛蚊 P.longifolia sp.nov.。所有模式标本均保存在北京农业大学昆虫标本室。     

中国竹类中的新分类等级及一新组合

本文在大明竹属Pleioblastus下发表1新组,2新种,即Pl.sect.Amari sect.nov.及Pl.incarnatus sp.nov.,Pl.sanmingensis sp.vov.。在矢竹属Pseudosasa下发表新亚属Ps.subgen.Sinicae subgen.nov.;2新组Ps.subgen.Sinicae sect.Sinicae sect.nov.及sect.Cantorisect.nov.;2新系Ps.subgen.Sinicae sect.Sinicae ser.Amabiles er.nov.ser.Maculiferae ser.nov.;4新种Ps. rirta sp nov.,Ps. truncatula sp. nov. Ps. wuyiensis sp. nov. viridula sp. nov.; 3新变种及一新组合Ps. amabilis var. farinosa var. nov., Ps. nanunica var. angustifotis var. nov., Ps. maculi fera var. hirsute var. nov.,及Ps. pallidiflora (Meclure) comb. nov.     

New Microorganisms from the Gaoyuzhuang Formation of Northern Taihang Mountains,China

A new diverse assemblage of microorganisms has been discovered in black bedded, nodular and lenticular cherts and dark chert of domical stromatolites in dolostone of the Gaoyuzhuang Formation in Lingqiu County, northern Taihang Mountains. The geologic relationships, biostratigraphic correlations, and available radiometric age determinations place the age of the Gaoyuzhuang Formation at approximately 1 400-1 600 million years in age. Eight new species, three unnamed species, and two emended genera of oscillatoriacean, nostocacean, and chroococcacean cyanobacteria are described. These data coupled with reports of others indicate that the diversity of taxa in the Gaoyuzhuang Formation reaches 100 species. The Gaoyuzhuang Formation contains one of the richest Mesoproterozoic communities of microfossils. The following new and emended taxa are described: Oscillatoriaceae: Eophormidium orculiformis sp. nov., E . sp., Siphonophycus caudataceous sp. nov., Palaeolyngbya complanata sp. nov., P. capitata sp. nov., P . sp. and Oscillatoriopsis sp..Nostocaceae: Veteronostocale vaginata sp. nov.. Chroococcaceae: Maculosphaera giganta sp. nov. and Gloeotheceopsis grandis sp. nov. Incertae sedis: Myxococcoides limpida sp. nov.     

Early Silurian(Telychian)rugose coral fauna of Daguan area, northeast Yunnan Province,China

Study on rugose coral fauna of the Sifengya Formation(early Telyehian)and Daluzhai Formation (mid-late Telychian)in Daguan area,northeast Yunnan Province,China was carded out.Rugose coral fauna of the Sifengya Formation included 18 genera and 34 species,while Daluzhai Formation with nine genera,ten species.We described rugose coral fauna(12 genera,19 species)including one new genus and five new species,i.e.Protoketophyllum daguanense gen.et sp.nov..Crassilasma huanggexiense sp.nov.,Pseudophaulactis heae sp.nov.,P.convolutus sp.nov.,and Shensiphyllum minor sp.nov..The characteristics and geological significance of rugose coral fauna of Sifengya Formation and Daluzhai Formation were analyzed.Particularly,mgose coral fauna of the Sifengya Formation represent early Telychian rugosan fauna in the Upper Yangtze region and improve the sequences of early Silurian(Llandovery)mgose coral assemblages in Yangtze region.It is therefore very meaningful to further analyze radiation period of rugose coral fauna in such epoch.     

河北和辽宁晚侏罗世古蝉化石(同翅目:头喙亚目)(英文)

本文描述古蝉科化石2新属、6新种,即Liaocossushuegen.etsp.nov.,L.beipiaoensisgen.etsp．nov,L．exiguusgen．etsp．nov,L．fengningensisgen．etsp．nov,L．Pingquanensisgen.etsp.nov.,Miracossusingentiusgen．etsp．nov.。这批化石保存有完整的虫体标本,使作者能够进一步研究古蝉类化石的虫体特征。化石采于冀北和辽西晚侏罗世义县组地层中,保存在中国地质博物馆。     

Mallomonadaceae (Chrysophyceae) from Malaysia and Australia

The Mallomonadaceae (Chrysophyceae) of Malaysia and Australia are described by scanning and transmission electron microscopy. Thirty taxa are reported from Malaysia, twenty eight for the first time. Eighteen taxa are reported from Australia, twelve for the first time. Twelve taxa are reported for the first time from the tropics. Four new taxa, Mallomonas ocellata sp. nov., M. tropica sp. nov., M. favosa f. gemina f. nov. and Chrysosphaerella astrea sp. nov. are described and the diagnosis of Mallomonas adamas Harris et Bradley is emended.     

New Middle Permian foraminifers (Chitralinidae) from the Karakaya Complex,in northwestern Turkey

One new foraminiferal genus, Rectoformata gen. nov., with two new species, has been described from a Permian limestone block in the Karakaya Complex in the South of the Balya district (Balikesir, northwestern Turkey). The type species of Rectoformata, Rectoformata tekini sp. nov., is characterized by a quadrangular transverse section having a calcareous microgranular wall with fine alveolar structures, whereas Rectoformata acari sp. nov. is recognized by a pentagonal transverse section having a calcareous microgranular wall with fine alveolar structures. The age of the described taxa is assigned as Midian ( = Capitanian) based on the association with small foraminifers and fusulinids. These new taxa are included in the family Chitralinidae, which is emended herein.     

中国内蒙古中侏罗世脉翅目昆虫化石—新科(英文)

建立脉翅目昆虫化石新科———Grammolingiidaefamnov .,并描述该科化石 3新属 6新种 :Grammolingiaboigen .nov .ofsp .nov .,Litholingiarhoragen .nov .ofsp .nov .,Litholingiaeumorphagen .nov .ofsp .nov .,Litholing iapolychotomagen .nov .ofsp .nov .,Leptolingiajurassicagen .nov .ofsp .nov .,Leptolingiatianyiensisgen .nov .etsp .nov ..给出了新科的属级检索表 ,描述的所有模式标本均采自于内蒙古自治区宁城县中侏罗世九龙山组地层中。标本分别保存在义县博物馆和首都师范大学生物系。本次发现再次表明目前关于脉翅目昆虫的认识仍然十分贫乏。     

New radiolaria of the family Pseudodictyomitridae from the Coniacian-Santonian of the Perapedhi Formation of southern Cyprus

A new genus of Late Cretaceous radiolarians, Cyprodictyomitra gen. nov., comprising two new species, C. longa sp. nov., C. elegantissima sp. nov., and a new species, Pseudodictyomitra crassa sp. nov. are described. These new taxa come from rich Coniacian-Santonian radiolarian associations of the Perapedhi Formation of Southern Cyprus.     

New fossil mantidflies (Insecta: Neuroptera: Mantispidae) from the Mesozoic of north‐eastern China

Abstract:  Three new genera and four new species of the extinct mantidfly subfamily Mesomantispinae (Insecta: Neuroptera: Mantispidae) are described from the Lower Cretaceous Yixian Formation of Liaoning and the Middle Jurassic Jiulongshan Formation of Inner Mongolia: Archaeodrepanicus nuddsi gen. et sp. nov., A. acutus gen. et sp. nov., Sinomesomantispa microdentata gen. et sp. nov., (Yixian Formation) and Clavifemora rotundata gen. et sp. nov. (Jiulongshan Formation). The specimens described herein represent the first Mesozoic mantidfly compression fossils to have body parts preserved, including the specialized raptorial forelegs articulated to the prothorax anteriorly, an autapomorphy of the family. These new taxa further confirm the placement of the subfamily Mesomantispinae within the family Mantispidae; however, the monophyly of Mesomantispinae has not been confirmed, and it is likely that it will prove to be paraphyletic.     

New mesozoic diving beetles (Coleoptera,Dytiscidae) from China

A new subfamily of predaceous diving beetles, Liadytiscinae subfam. nov., including two genera and four species, Liadytiscus gen. nov. (L. cretaceus sp. nov., L. longitibialis sp. nov., and L. latus sp. nov.) and Liadroporus gen. nov. (L. elegans sp. nov.), from the Late Tithonian-Berriasian (Huangbanjigou, Yixian Formation) of China is described. Two new genera, Mesoderus gen. nov. with two species, M. magnus sp. nov. and M. ventralis sp. nov., and Sinoporus gen. nov. with one species, S. lineatus sp. nov., are also described; their position in the system of Dytiscidae remains uncertain. Relationships of the taxa described with Recent and fossil taxa of the same rank and some presumable ecological features of the new taxa are discussed.     

ORDOVICIAN NAUTILOID FAUNA FROM LUNSHAN, JURONG, JIANGSU

The fossil nautiloids described in this paper were collected in 1984 and 1985 from Lunshan, Jurong in Jiangsu; there the Ordovician strata are well developed and may be divided in descending order into seven formations as follows:Upper Ordovician: Wufeng Formation Tangtou FormationMiddle Ordovician Pagoda Formation Lower OrdovicianKuniutan FormationDawan FormationHunghuayuan FormationLunshan FormationThese nautiloids comprise 36 species belonging to 13 genera (including one new genus and 11 new species), namely,Middle OrdovicianPagoda FormationSinoceras chinense (Foord), Michelinoceras changjiangense Chen, densn (Y), M. paraelongatum Chang.Lower OrdovicianKuniutan FormationRhynchorthoceras jurongense sp. nov., R. lunshanense sp. nov., Dideroceras wahlenbergi (Foord), D. holmi Flower, Michlinoceras irregulare sp. nov., Kotoceras gaoluncunense sp. nov.Dawan Formation.Cochlioceras yantzeense Chang, Chisiloceras ichangense Wang, C. yaoshanense Qi, C. changyangense (Chang), Protocycloceras deprati Reed, P. hupehcnse (Shimizu and Obata), P. sichuanense Wang, P. remotum Lai, P. gangshanense sp. nov., P. siphosedimentum Pan, P. chaoi sp. nov., P.shishantouense sp. nov., P. gaojiabianense sp. nov., Changyangoceras gaojiabianense sp. nov., Gangshanoceras jurongense gen. et sp. nov., G. densum gen. et sp. nov., Michelinoceras cf. dayongense Lai, Troedssonella lunshanensis sp. nov., Mesosendoceras leei (Y), Vaginoceras peiyangense malukonense Chen, Dideroceras mui (Chang), D. gaoluncunense sp. nov.