(geology) Lower Middle Triassic geologic time.
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(geology) Lower Middle Triassic geologic time.
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| System | Series | Stage | Age (Ma) | |
|---|---|---|---|---|
| Jurassic | Lower | Hettangian | younger | |
| Triassic | Upper | Rhaetian | 199.6–203.6 | |
| Norian | 203.6–216.5 | |||
| Carnian | 216.5–228.0 | |||
| Middle | Ladinian | 228.0–237.0 | ||
| Anisian | 237.0–245.0 | |||
| Lower | Olenekian | 245.0–249.7 | ||
| Induan | 249.7–251.0 | |||
| Permian | Lopingian | Changhsingian | older | |
| Subdivision of the Triassic system according to the IUGS, as of July 2009. | ||||
In the geologic timescale, the Anisian is the lower stage or earliest age of the Middle Triassic series or epoch and lasted from 245 million years ago until 237 million years ago, approximately.[1] The Anisian age succeeds the Olenekian age (part of the Lower Triassic epoch) and precedes the Ladinian age.
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The stage and its name were established by Austrian geologists Wilhelm Heinrich Waagen and Carl Diener in 1895. The name comes from Anisus, the Latin name of the river Enns. The original type locality is at Großreifling in the Austrian state of Styria.
The base of the Anisian stage (also the base of the Middel Triassic series) is sometimes laid at the first appearance of conodont species Chiosella timorensis in the stratigraphic record. Other stratigraphers prefer to use the base of magnetic chronozone MT1n. The global reference profile for the base (the GSSP or golden spike) is at a flank of the mountain Deşli Caira in the Romanian Dobruja.[2]
The top of the Anisian (the base of the Ladinian) is at the first appearance of ammonite species Eoprotrachyceras curionii and the ammonite family Trachyceratidae. The conodont species Neogondolella praehungarica appears at the same level.
Sometimes (especially in Central Europe) the Anisian stage is subdivided into four substages: Aegean, Bythinian, Pelsonian and Illyrian.
The Anisian contains six ammonite biozones:
The earliest potential dinosaur fossil to date is a partial pubis from Anisian-age rocks of the Moenkopi Formation, Arizona. It may have come from a herrerasaurid.[3]
Examples of vertebrates from this age are:
| †Non-archosaurian Archosauromorphs of the Anisian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| †Non-mammalian Therapsids of the Anisian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Nothosauroids of the Anisian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Guizhou and Hubei, China | ||||
| Placodonts of the Anisian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Northern Italy | ||||
| Thalattosauria of the Anisian | ||||
|---|---|---|---|---|
| Taxa | Presence | Location | Description | Images |
| Italy | A very thin, elongated creature (about 2 meters long) that probably swam like an eel, that was probably a fish eater and hunted in deep waters, based on its large eyes (which would allow it to see better in dark water) and the protective bony ring around them (also seen in ichthyosaurs), which prevented them from getting squashed in by the immense water pressure at great depths. | |||
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Ananorites Arthaberites Beyrichites Bosnites Buddhaites Bukowskiites Caucasites Danubites Gangadharites Japonites Laboceras Longobarditoides Mesocladiscites Noetlingites Parapinacoceras Parasageceras Phyllocladiscites Proavites Pseudodanubites Psilocladiscites Salterites Tropigymnites Xiphogymnites Pararcestes Sageceras
Alloptychites Anagymnites Grambergia Groenlandites Gymnites Lenotropites Pearylandites Silberlingites Isculites Stenopopanoceras
Acrochordiceras Alanites Anagymnotoceras Arctohungarites Balatonites Bulogites Cuccoceras Czekanowskites Epacrochordiceras Hollandites Huishuites Inaigymnites Ismidites Kiparisovia Malletophychites Nicomedites Phillipites Platycuccoceras Pronoetlingites Reiflingites Discoptychites Intornites Nevadisculites Paraceratites Parapopanoceras Proarcestes Longobardites Ptychites
Amphipopanoceras Aplococeras Arctogymnites Eudiscoceras Eutomoceras Gymnotoceras Halilucites Judicarites Kellnerites Metadinarites Nevadites Parakellnerites Proteusites Repossia Semiornites Serpianites Stoppaniceras Ticinites Tozerites Tropigastrites Joannites Epigymnites Ceratites Flexoptychites Frechites Norites Gevanites Hungarites
Spinoleiophyllites Ussurites Monophyllites
Trachynautilus Thuringionautilus Styrionautilus
Indonautilus Sibyllonautilus
Paranautilus
Holconautilus Proclydonautilus
Crassiatractites Breviatractites
| Triassic period | ||
|---|---|---|
| Lower/Early Triassic | Middle Triassic | Upper/Late Triassic |
| Induan | Olenekian | Anisian | Ladinian | Carnian | Norian Rhaetian |
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| Ladinian (geology) | |
| Middle Triassic | |
| Anarosaurus |
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