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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F12%3A10128053%21RIV13-GA0-11310___
rdf:type
n6:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.1002/jmor.11036
dcterms:description
Two different patterns of wing venation are currently supposed to be present in each of the three orders of Paraneoptera. This is unlikely compared with the situation in other insects where only one pattern exists per order. We propose for all Paraneoptera a new and unique interpretation of wing venation pattern, assuming that the convex cubitus anterior gets fused with the common stem of median and radial veins at or very near to wing base, after separation from concave cubitus posterior, and reemerges more distally from R 1 M stem. Thereafter, the vein between concave cubitus posterior and CuA is a specialized crossvein called ''cua-cup,'' proximally concave and distally convex. We show that despite some variations, that is, cua-cup can vary from absent to hypertrophic; CuA can re-emerge together with M or not, or even completely disappear, this new interpretation explains all situations among all fossil and recent paraneopteran lineages. We propose that the characters ''CuA fused in a common stem with R and M''and ''presence of specialized crossvein cuacup'' are venation apomorphies that support the monophyly of the Paraneoptera. In the light of these characters, we reinterpret several Palaeozoic and early Mesozoic fossils that were ascribed to Paraneoptera, and confirm the attribution of several to this superorder as well as possible attribution of Zygopsocidae (Zygopsocus permianus Tillyard, 1935) as oldest Psocodea. We discuss the situation in extinct Hypoperlida and Miomoptera, suggesting that both orders could well be polyphyletic, with taxa related to Archaeorthoptera, Paraneoptera, or even Holometabola. The Carboniferous Protoprosbolidae is resurrected and retransferred into the Paraneoptera. The genus Lithoscytina is restored. The miomopteran Eodelopterum priscum Schmidt, 1962 is newly revised and considered as a fern pinnule. In addition, the new paraneopteran Bruayaphis oudardi gen. nov. et sp. nov. is described from the Upper Carboniferous of France. Two different patterns of wing venation are currently supposed to be present in each of the three orders of Paraneoptera. This is unlikely compared with the situation in other insects where only one pattern exists per order. We propose for all Paraneoptera a new and unique interpretation of wing venation pattern, assuming that the convex cubitus anterior gets fused with the common stem of median and radial veins at or very near to wing base, after separation from concave cubitus posterior, and reemerges more distally from R 1 M stem. Thereafter, the vein between concave cubitus posterior and CuA is a specialized crossvein called ''cua-cup,'' proximally concave and distally convex. We show that despite some variations, that is, cua-cup can vary from absent to hypertrophic; CuA can re-emerge together with M or not, or even completely disappear, this new interpretation explains all situations among all fossil and recent paraneopteran lineages. We propose that the characters ''CuA fused in a common stem with R and M''and ''presence of specialized crossvein cuacup'' are venation apomorphies that support the monophyly of the Paraneoptera. In the light of these characters, we reinterpret several Palaeozoic and early Mesozoic fossils that were ascribed to Paraneoptera, and confirm the attribution of several to this superorder as well as possible attribution of Zygopsocidae (Zygopsocus permianus Tillyard, 1935) as oldest Psocodea. We discuss the situation in extinct Hypoperlida and Miomoptera, suggesting that both orders could well be polyphyletic, with taxa related to Archaeorthoptera, Paraneoptera, or even Holometabola. The Carboniferous Protoprosbolidae is resurrected and retransferred into the Paraneoptera. The genus Lithoscytina is restored. The miomopteran Eodelopterum priscum Schmidt, 1962 is newly revised and considered as a fern pinnule. In addition, the new paraneopteran Bruayaphis oudardi gen. nov. et sp. nov. is described from the Upper Carboniferous of France.
dcterms:title
Traits and evolution of wing venation pattern in paraneopteran insects Traits and evolution of wing venation pattern in paraneopteran insects
skos:prefLabel
Traits and evolution of wing venation pattern in paraneopteran insects Traits and evolution of wing venation pattern in paraneopteran insects
skos:notation
RIV/00216208:11310/12:10128053!RIV13-GA0-11310___
n6:predkladatel
n9:orjk%3A11310
n3:aktivita
n11:Z n11:S n11:P n11:I
n3:aktivity
I, P(GAP210/10/0633), S, Z(MSM0021620828)
n3:cisloPeriodika
5
n3:dodaniDat
n14:2013
n3:domaciTvurceVysledku
n15:2957523
n3:druhVysledku
n13:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n20:predkladatel
n3:idSjednocenehoVysledku
174828
n3:idVysledku
RIV/00216208:11310/12:10128053
n3:jazykVysledku
n18:eng
n3:klicovaSlova
wing venation; Hemiptera; Thripida; Psocodea
n3:klicoveSlovo
n5:wing%20venation n5:Thripida n5:Psocodea n5:Hemiptera
n3:kodStatuVydavatele
US - Spojené státy americké
n3:kontrolniKodProRIV
[47C1CAB9A001]
n3:nazevZdroje
Journal of Morphology
n3:obor
n12:EG
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
9
n3:projekt
n22:GAP210%2F10%2F0633
n3:rokUplatneniVysledku
n14:2012
n3:svazekPeriodika
273
n3:tvurceVysledku
Nel, Patricia Szwedo, Jacek Dostal, Ondrej Nel, Andre Roques, Patrick Grandcolas, Philippe Huang, Di-Ying Guilbert, Eric Prokop, Jakub
n3:wos
000301776500002
n3:zamer
n21:MSM0021620828
s:issn
0362-2525
s:numberOfPages
27
n7:doi
10.1002/jmor.11036
n16:organizacniJednotka
11310