Permian insects

The Auchenorrhyncha suborder of the Hemiptera contains most of the familiar members of what was called the "Homoptera" – groups such as cicadas, leafhoppers, treehoppers, planthoppers, and spittlebugs. The aphids and scale insects are the other well-known "Homoptera", and they are in the suborder Sternorrhyncha.

Meganisoptera is an extinct order of large dragonfly-like insects, informally known as griffenflies or (incorrectly) as giant dragonflies. The order was formerly named Protodonata, the "proto-Odonata", for their similar appearance and supposed relation to modern Odonata (damselflies and dragonflies). They range in Palaeozoic (Late Carboniferous to Late Permian) times. Though most were only slightly larger than modern dragonflies, the order includes the largest known insect species, such as the late Carboniferous Meganeura monyi and the even larger early Permian Meganeuropsis permiana, with win

The Palaeodictyoptera are an extinct order of medium-sized to very large, primitive Palaeozoic paleopterous insects. They are informative about the evolution of wings in insects.

The Diaphanopterodea or Paramegasecoptera are an extinct order of moderate to large-sized Palaeozoic insects. They are first known from the Middle Carboniferous (late Serpukhovian or early Bashkirian in age), and include some of the earliest known flying insects.

Meganeuropsis, from Ancient Greek μέγας (mégas), meaning "large", νεῦρον (neûron), meaning "nerve", and ὄψις (ópsis), meaning "appearance", is an extinct genus of griffenfly, order Meganisoptera, known from the Early Permian Wellington Formation of North America, and represents the largest known insect of all time. Meganeuropsis existed during the Artinskian age of the Permian period, 290.1–283.5 mya. The genus includes two described species by Frank Morton Carpenter, fossil insect curator at the Museum of Comparative Zoology at Harvard University:

The Paleodictyopterida or Palaeodictyopteroidea are an extinct superorder of Palaeozoic beaked insects, characterised by unique mouthparts consisting of 5 stylets. They represent the first important terrestrial herbivores, and the first major group of herbivorous insects. They appear during the Carboniferous (Serpukhovian stage) and continue through to the Late Permian. This large and diverse group includes 50% of all known Paleozoic insects. Palaeodictyopteroidea nymphs possessed movable wing pads and appear to have been able to perform simple flapping flight.

Coleopsis is an extinct genus of stem-group beetles. It contains a single species, Coleopsis archaica, and is the only member of the family Coleopsidae and superfamily Coleopsoidea. It is known from a single specimen from the Early Permian of southwestern Germany, estimated to be about 297 million years old. It is currently the oldest known beetle.

Paoliida is an extinct order of winged insects that lived in the late Paleozoic. Historically, both their systematic position and composition were controversial – for instance they had been considered as palaeodictyopterans, as basal Neoptera, or as stem-group of Pterygota – but recent studies have resolved them as the sister group of Dictyoptera.

Protodiptera is an extinct suborder of mecopteran insects containing the two families Permotanyderidae and Permotipulidae with a total of four genera Choristotanyderus, Permila, Permotanyderus and Permotipula. ==References==

Tshekardocoleidae is an extinct family of stem group beetles, known from the Early Permian. They represent some of the earliest known beetles. They first appeared during the Cisuralian, before becoming extinct at the beginning of the Guadalupian. A claimed Jurassic record is doubtful. Like other primitive beetles, they are thought to have been xylophagous. The oldest known beetle, Coleopsis, was originally assigned to this family, but is now assigned to its own family Coleopsidae.

thumb|A phylogeny of Dermaptera and related groups Protelytroptera is an extinct order of insects thought to be a stem group from which the modern Dermaptera evolved. These insects, which resemble modern Blattodea, or cockroaches, are known from the Permian of North America, Europe and Australia, from the fossils of their shell-like forewings and the large, unequal anal fan. None of their fossils are known from the Triassic, when the morphological changes from Protelytroptera to Dermaptera presumably took place.