昆士兰三叠纪的飞虱(半翅目:浮蛾目:浮蛾总科)

Q4 Earth and Planetary Sciences
K. Lambkin
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引用次数: 2

摘要

Fulgoromorpha亚目种类繁多,是昆士兰三叠纪以cicadomorphaa为主的半足动物群的一个小组成部分,仅从已灭绝的Surijokocixiidae科3属3种的5个被盖标本中得知。Tricrosbia minuta Evans, 1971,和Crosbixius carsburgi gen. et nov.来自Ipswich煤系晚三叠世(Norian) Mount Crosby组,Karesmina punicea gen. et nov.来自中三叠世(Anisian) Esk组。Surijokocixiidae是来自俄罗斯的四个二叠纪属和来自吉尔吉斯斯坦和中国的未命名的三叠纪种。Tricrosbia Evans, 1971,与其他属的区别在于其简单的MP1+2和非常浅的CuA叉。Crosbixius与二叠纪Surijokocixius Becker-Migdisova相似,但在其整个长度上具有等宽的沿海空间,ScP+RA和RP的更基部分叉,MP -cu在MP和CuA1之间而不是MP3+4和CuA1之间。Karesmina的特点是其较大的尺寸(花被长9毫米,其他的< 6毫米),向后倾斜的ir,和独特的RP和MP1+2结构。Tricrosbia和Crosbixius是在三叠纪末期灭绝的最后的Surijokocixiidae,在侏罗纪由更多样化和现代外观的fulgoromorph动物群取代,由许多已灭绝的Fulgoridiidae物种主导。在克罗斯比山组确认了Surijokocixiidae的存在,为伊普斯维奇煤系半足类动物群增加了另一个科,这是三叠纪典型的过渡昆虫动物群,混合了二叠纪的幸存者,这些幸存者没有持续到三叠纪(Dunstaniidae, Scytinopteridae, Surijokocixiidae)或侏罗纪(Dysmorphoptilidae),特殊的三叠纪特有物种(chilicyclidae, Mesogereonidae, Ipsviciidae)。新出现的Hylicellidae一直存活到白垩纪,最后是更现代的形式,Archijassidae,现存膜蝉科的最早记录,以及Tettigarctidae,毛蝉,至今仍然存在。昆虫亚目,半翅目,翅虫亚目,翅虫总科,刺虫科,克罗斯比山组,埃斯克组,昆虫化石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Planthoppers (Insecta: Hemiptera: Fulgoromorpha: Fulgoroidea: Surijokocixiidae) of the Queensland Triassic
The suborder Fulgoromorpha, highly diverse and speciose today, was a minor component of the Cicadomorpha-dominant hemipteran fauna of the Queensland Triassic known only from five tegmen specimens of three species in three genera of the extinct family Surijokocixiidae: Tricrosbia minuta Evans, 1971, and Crosbixius carsburgi gen. et sp. nov., from the Late Triassic (Norian) Mount Crosby Formation of the Ipswich Coal Measures, and Karesmina punicea gen. et sp. nov. from the Middle Triassic (Anisian) Esk Formation. The Surijokocixiidae are otherwise known from four Permian genera from Russia and unnamed Triassic species from Kyrgyzstan and China. Tricrosbia Evans, 1971, is distinguished from other genera of the family by its simple MP1+2, and the very shallow fork of CuA. Crosbixius is similar to the Permian Surijokocixius Becker-Migdisova, but differs in the costal space of equal width along its entire length, the more basal fork of ScP+RA and RP, and mp-cu running between MP and CuA1 rather than MP3+4 and CuA1. Karesmina is distinguished by its larger size (tegmen length 9 mm, < 6 mm in the others), backwardly inclined ir, and peculiar structure of RP and MP1+2. Tricrosbia and Crosbixius were the last of the Surijokocixiidae which were extinct by the end of the Triassic, succeeded in the Jurassic by a more diverse and modern looking fulgoromorph fauna, dominated by numerous species of the extinct Fulgoridiidae. Confirmation of the presence of the Surijokocixiidae in the Mount Crosby Formation adds another family to the Ipswich Coal Measures hemipteran fauna, a transition insect fauna typical of the Triassic, with a mix of survivors from the Permian which did not last beyond the Triassic (Dunstaniidae, Scytinopteridae, Surijokocixiidae) or Jurassic (Dysmorphoptilidae), peculiar Triassic endemics (Chiliocyclidae, Mesogereonidae, Ipsviciidae), the newly emerged Hylicellidae which survived until the Cretaceous, and lastly more modern forms, Archijassidae, the earliest record of the extant Membracoidea, and Tettigarctidae, the hairy cicadas, which still exist today.  Insecta, Hemiptera, Fulgoromorpha, Fulgoroidea, Surijokocixiidae, Tricrosbia, Mount Crosby Formation, Esk Formation, fossil insects.
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来源期刊
Memoirs of the Queensland Museum
Memoirs of the Queensland Museum Environmental Science-Ecology
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