中国长颊花天牛属及新种记述：（鞘翅目：天牛科）

天牛科,花天牛亚科Lepturinae、花天牛族Lepturini的长颊花天牛属Gnathostrang alia是由Hayashi于1985年建立的,并将条胸长颊花天牛Lepturabilineatithorax Pic,黑条长颊花天牛Strangalia rufovittata Pic,天目山长颊花天牛Strangalia tienmushana Gressitt,黑尾长颊花天牛Strangalia aurivillei Pic以及横条长颊花天牛Strangalia longiceps Aurivillus等5个种移入此属,其中,分布在越南的有3种,加里曼丹1种,中国浙江天目山1种。该属与长尾花天牛属Pygostrangalia很近似,但头前部更长,前胸背板较宽,后侧角较发达,鞘翅基部较宽,向中部收狭,端半部外侧缘较直。本文记述了在广西龙胜和四川重庆江津四面山发现的两个新种。     

中国环缘蝽属昆虫记述(半翅目:姬缘蝽科)

环缘蝽属(Stictopleurus Stal)建立于1872年,为半翅目(Hemiptera)姬缘蝽科(Rhopalidae)中的一个类群。Reuter(1885)将其降为姬缘蝽属(Corizus Fallen)的一个亚属,该意见曾被一些学者所采纳,如Puton(1886/1899),Ragusa(1907),Van Duzee(1916),Torre-Bueno(1914)等;Muzik(1904)亦曾将其作为伊缘蝽属(Rhopalus Schil-ling)的一个亚属;但后来多数学者及近代的分类学工作者均将其视为一个独立的属,如Oshanin(1906/1912),De Seabra(1927),Harris(1943),Chopra(1967),Gollner-     

发现于贵州的中国新记录科—极蚊科并记述一新种：（双翅目：长角亚目）

双翅目长角亚目的极蚊科(Axymyiidae)为中国新记录科,是极罕见的昆虫,世界只记载过5种;现报道贵州梵净山的1个新种,模式标本藏北京农业大学昆虫标本室。 极蚊体型中等,粗壮而色暗,外貌象毛蚊类,Coquillett(1909)曾将北美种包括在毛蚊科的Eupeitenus属内。McAtee(1921)建立了Axymia furcata新属种,同时由Shannon(1921)讨论了其分类地位,作为殊蚊科(Anisopodida=Rhyphidae)的1个新     

中国新记录的隐粉蛉属及一新种记述：（脉翅目：粉蛉科）

隐粉蛉属Cryptoscenea在囊粉蛉亚科(Aleuropteryginae)中是比较特殊的,其前翅中脉上缺少一般均具有的2个脉鬃。Enderlein 1914年以其1906年所描述的Helicoconis australiensis作为模式种建立了此属,至今只记载有5个种,除1种在新几内亚外,其余均分布在澳洲,本文系此属在我国的首次纪录,并增加1新种。所有模式标本均保存在北京农业大学昆虫标本室。     

中国新叶蚜属研究及新种记述：（同翅目：斑蚜科）

作者系统整理了我国新叶蚜属Neophy llaphis Takahashi,1920标本,共有2种,其一为新种。给出中国的分种检索表。新种的模式标本保存在中国科学院动物研究所。 新叶蚜属Neophy llaphis Takahashi,1920 Neophy llaphis Takahashi,1920,Can.Ent.52:20模式种Neophy llaphis podocarpi Takahashi,1920.     

警惕新外来入侵害虫——股带针蓟马Hercinothrips femoralis(缨翅目：蓟马科)

【目的】股带针蓟马,又称温室条带蓟马,是一种多食性农业害虫,寄主超过50种,在一些国家被列为检疫性生物。2020年9月,在北京发现其成虫和幼虫危害海芋叶片,本文介绍了其形态特征、分子鉴定数据、分布地区及寄主植物等数据,以期为其准确鉴定和防治提供参考。【方法】采用拍打法收集标本;采用非破坏性方法提取单头蓟马DNA,扩增线粒体细胞色素c氧化酶Ⅰ基因(COⅠ)的部分序列,进行分子鉴定和系统发育分析;制作永久玻片进行形态鉴定。【结果】结合形态和分子数据鉴定其为股带针蓟马,是中国新记录属、种,海芋是该种新记录的寄主植物。股带针蓟马与该属其他种的主要区别在于该种前翅的亚中部浅色带比端部暗带短。COⅠ分子序列分析表明,北京种群与国外种群聚集成一个分支,序列相似性高达100%。【结论】应采取进一步调查、监测和管理措施,防止该种外来有害蓟马的传播。     

中国栗米草属植物的校订

本文校订了中国粟米属植物,共有4种。国产的粟米草应是Mollugo stricta L.,而不是M.pentaphylla L.;多棱粟米草M.costataY.T.Chang et C.F.Wei是种棱粟米草M.verticillata L.的异名     

中国扁裸藻属新记录

本文报道采自哈尔滨的扁裸藻属我国新记录3种2变种,它们是Phacus balatonicus var.boglariensis Hortob.,Ph.elegans Pochm.,Ph.glaber(Defl.)Pochm.,Ph.suecicus var.invermis Nyg.,Ph.war-szewiczii Drez.     

FOUR NEW SPECIES OF COENOSIA MEIGEN (DIPTERA: MUSCIDAE) FROM YUNNAN, CHINA

Abstract  This paper describes four new species of Coenosia Meigen, 1826, namely C. angustifolia sp.nov., C. obscuriabdominis sp. nov., C. sparagmocerca sp. nov. and C. sponsa sp. nov. Type specimens are deposited in Institute of Entomology, Shenyang Normal University, Shenyang, China.     

Billingen (Lower Arenig/Lower Ordovician) acritarchs from the East European Platform and their palaeobiogeographic significance

Billingen (Lower Arenig/Lower Ordovician) sediments of the St. Petersburg region, northwest Russia and the Leba area, northern Poland of the East European Craton yield acritarch assemblages, which are largely homogenous though displaying minor compositional differences that probably reflect a gradient from inner to outer shelf environments. Comparison with coeval acritarch microflora from the Yangtze Platform, South China, shows an overall similarity between Baltoscandian and South Chinese phytoplankton. The widespread uniformity in the fossil microphytoplankton may be related to the extensive global 'evae' sea-level transgression, which characterized the Billingen time. This suggests that during the Tremadoc through early Arenig times, acritarch assemblages displayed essentially an undifferentiated cold-water and oceanic character along the whole margin of Perigondwana in the South, as well as on the South Chinese and Baltic platforms, at middle latitudes (Mediterranean oceanic Realm). Despite this overall similarity, however, some typical taxa of the high-latitude Mediterranean Province (Arbusculidium, Coryphidium and Striatotheca) occur in South China, but are absent in Baltica. This discrepancy is explained as caused by differences in climatic and physiographic conditions that prevailed at the two palaeocontinents at this time. The inferred pattern of oceanic circulation during the Lower Ordovician is consistent with the palynological evidence of a prevailing warmer climate in Baltica than in South China, although the two palaeocontinents occupied the same palaeolatitudinal position.