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Moths Described In 1883
Moths are a group of insects that includes all members of the order Lepidoptera that are not butterflies. They were previously classified as suborder Heterocera, but the group is paraphyletic with respect to butterflies (suborder Rhopalocera) and neither subordinate taxon is used in modern classifications. Moths make up the vast majority of the order. There are approximately 160,000 species of moth, many of which have yet to be described. Most species of moth are nocturnal, although there are also crepuscular and diurnal species. Differences between butterflies and moths While the butterflies form a monophyletic group, the moths, comprising the rest of the Lepidoptera, do not. Many attempts have been made to group the superfamilies of the Lepidoptera into natural groups, most of which fail because one of the two groups is not monophyletic: Microlepidoptera and Macrolepidoptera, Heterocera and Rhopalocera, Jugatae and Frenatae, Monotrysia, and Ditrysia.Scoble, MJ 1995. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Attacus Atlas
''Attacus atlas'', the Atlas moth, is a large Saturniidae, saturniid moth endemic to the forests of Asia. The species was described by Carl Linnaeus in his 1758 10th edition of Systema Naturae, 10th edition of ''Systema Naturae''. The Atlas moth is one of the largest lepidopterans, with a wingspan measuring up to and a wing surface area of about 160 cm2 (≈25 in2). It is only surpassed in wingspan by the Thysania agrippina, white witch (''Thysania agrippina'') and ''Attacus caesar'', and in wing surface area by the Coscinocera hercules, Hercules moth (''Coscinocera hercules''). As in most Bombycoidea, silk moths, females are noticeably larger and heavier than males, while males have broader antenna (biology), antennae. Description Eggs Atlas moths lay a number of spherical eggs, in diameter, on the undersides of the leaves of food plants. Larva After approximately two weeks, dusty-green caterpillars hatch and feed on their egg-shell, and then the foliage of citr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heterocera
Moths are a group of insects that includes all members of the order Lepidoptera that are not butterflies. They were previously classified as suborder Heterocera, but the group is paraphyletic with respect to butterflies (suborder Rhopalocera) and neither subordinate taxon is used in modern classifications. Moths make up the vast majority of the order. There are approximately 160,000 species of moth, many of which have yet to be described. Most species of moth are nocturnal, although there are also crepuscular and diurnal species. Differences between butterflies and moths While the butterflies form a monophyletic group, the moths, comprising the rest of the Lepidoptera, do not. Many attempts have been made to group the superfamilies of the Lepidoptera into natural groups, most of which fail because one of the two groups is not monophyletic: Microlepidoptera and Macrolepidoptera, Heterocera and Rhopalocera, Jugatae and Frenatae, Monotrysia, and Ditrysia.Scoble, MJ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Common Germanic
Proto-Germanic (abbreviated PGmc; also called Common Germanic) is the reconstructed proto-language of the Germanic branch of the Indo-European languages. Proto-Germanic eventually developed from pre-Proto-Germanic into three Germanic branches during the fifth century BC to fifth century AD: West Germanic, East Germanic and North Germanic. North Germanic remained in contact with the other branches over a considerable time, especially with the Ingvaeonic languages (including English), which arose from West Germanic dialects, and had remained in contact with the Norse. A defining feature of Proto-Germanic is the completion of the process described by Grimm's law, a set of sound changes that occurred between its status as a dialect of Proto-Indo-European and its gradual divergence into a separate language. The end of the Common Germanic period is reached with the beginning of the Migration Period in the fourth century AD. The alternative term " Germanic parent lang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumbrian Old English
Northumbrian was a dialect of Old English spoken in the Anglo-Saxons, Anglian Kingdom of Northumbria. Together with Mercian dialect, Mercian, Kentish dialect (Old English), Kentish and West Saxon dialect, West Saxon, it forms one of the sub-categories of Old English devised and employed by modern scholars. The dialect was spoken from the Humber, now within England, to the Firth of Forth, now within Scotland. In the Danelaw after the Viking activity in the British Isles, Viking invasions, Northumbrian may have been influenced by the Norse language. Some of the earliest surviving Old English texts were written in Northumbrian, such Caedmon's Hymn, Cædmon's Hymn (7th century) and Bede's Death Song (8th century). Other works, including the bulk of Cædmon's poetry, have been Lost literary work, lost. Other examples of this dialect are the Runes on the Ruthwell Cross from the ''Dream of the Rood''. Also in Northumbrian are the 9th-century Leiden Riddle and the late 10th century ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old English
Old English ( or , or ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the Early Middle Ages. It developed from the languages brought to Great Britain by Anglo-Saxon settlers in the mid-5th century, and the first Old English literature dates from the mid-7th century. After the Norman Conquest of 1066, English was replaced for several centuries by Anglo-Norman language, Anglo-Norman (a langues d'oïl, type of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during the subsequent period the English language was heavily influenced by Anglo-Norman, developing into what is now known as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic tribes traditionally known as the Angles (tribe), Angles, Saxons and Jutes. As the Germanic settlers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Modern English
Modern English, sometimes called New English (NE) or present-day English (PDE) as opposed to Middle and Old English, is the form of the English language that has been spoken since the Great Vowel Shift in England England is a Countries of the United Kingdom, country that is part of the United Kingdom. It is located on the island of Great Britain, of which it covers about 62%, and List of islands of England, more than 100 smaller adjacent islands. It ..., which began in the late 14th century and was completed by the 17th century. With some differences in vocabulary, texts that date from the early 17th century, such as the works of William Shakespeare and the King James Bible, are considered Modern English, or more specifically, Early Modern English or Elizabethan era, Elizabethan English. Through colonization, English was adopted in many regions of the world by the British Empire, such as Anglo-America, the Indian subcontinent, Africa, Australia and New Zealand. Mod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
