Artinskian

System/ Period	Series/ Epoch	Stage/ Age	Age (Ma)
Triassic	Lower/ Early	Induan	younger
Permian	Lopingian	Changhsingian	252.2–254.1
	Lopingian	Wuchiapingian	254.1–259.8
	Guadalupian	Capitanian	259.8–265.1
		Wordian	265.1–268.8
		Roadian	268.8–272.3
	Cisuralian	Kungurian	272.3–283.5
		Artinskian	283.5–290.1
		Sakmarian	290.1–295.0
		Asselian	295.0–298.9
Carboniferous	Pennsylvanian	Gzhelian	older
Subdivision of the Permian system according to the ICS (Geologic Time Scale 2013).^[1]

Jimbacrinus bostocki Arkisitan of Australia. (Found near Jimba Jimba Station )

In the geologic timescale, the Artinskian is an age or stage of the Permian. It is a subdivision of the Cisuralian epoch or series. The Artinskian lasted between 290.1 ± 0.26 and 283.5 ± 0.6 million years ago (Ma). It was preceded by the Sakmarian and followed by the Kungurian.^[2]

Stratigraphy

The Artinskian is named after the small Russian city of Arti (formerly Artinsk), situated in the southern Ural mountains, about 200 km southwest of Yekaterinburg. The stage was introduced into scientific literature by Alexander Karpinsky in 1874.

The base of the Artinskian stage is defined as the place in the stratigraphic record where fossils of conodont species Sweetognathus whitei and Mesogondolella bissell first appear. As of 2009, there was no agreement yet on a global reference profile (a GSSP) for the base of the Artinskian. The top of the Artinskian (the base of the Kungurian) is defined as the place in the stratigraphic record where fossils of conodonts Neostreptognathodus pnevi and Neostreptognathodus exculptus first appear.

Popular culture

"Nothing Happened in the Artinskian Age" is a short story by author Tom Offland.^[3]

References

Notes

↑ "Chronostratigraphic chart 2013". ICS. Retrieved 27 March 2013.
↑ See Gradstein et al. (2004) for a detailed geologic timescale
↑ http://theneweryork.com/nothing-happened-in-the-artinskian-age-tom-offland/

Literature

Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press

External links

GeoWhen Database - Artinskian
Upper Paleozoic stratigraphic chart at the website of the subcommission for stratigraphic information of the ICS

Preceded by Proterozoic Eon	Phanerozoic Eon
	Paleozoic Era						Mesozoic Era			Cenozoic Era
	Cambrian	Ordovician	Silurian	Devonian	Carboniferous	Permian	Triassic	Jurassic	Cretaceous	Paleogene	Neogene	4ry

Geologic history of Earth

Cambrian
supereon
(Present–541.0 Mya)

Phanerzoic eon
(Present–541.0 Mya)

Cenozoic era
(present–66.0 Mya)

Quaternary (present–2.58 Mya)

Holocene (present–11.7 kya)	Holocene (present–11.7 kya)

Pleistocene (11.7 kya–2.58 Mya)	Tarantian (11.7 kya–126 kya) Ionian (126 kya–781 kya) Calabrian (781 kya–1.80 Mya) Gelasian (1.80 Mya–2.58 Mya)

Neogene (2.58–23.03 Mya)

Pliocene (2.58–5.333 Mya)	Piacenzian (2.58 Mya–3.600 Mya) Zanclean (3.600 Mya–5.333 Mya)

Miocene (5.333–23.03 Mya)	Messinian (5.333 Mya–7.246 Mya) Tortonian (7.246 Mya–11.62 Mya) Serravallian (11.62 Mya–13.82 Mya) Langhian (13.82 Mya–15.97 Mya) Burdigalian (15.97 Mya–20.44 Mya) Aquitanian (20.44 Mya–23.03 Mya)

Paleogene (23.03–66.0 Mya)

Oligocene (23.03–33.9 Mya)	Chattian (23.03 Mya–28.1 Mya) Rupelian (28.1 Mya–33.9 Mya)

Eocene (33.9–56.0 Mya)	Priabonian (33.9 Mya–38.0 Mya) Bartonian (38.0 Mya–41.3 Mya) Lutetian (41.3 Mya–47.8 Mya) Ypresian (47.8 Mya–56.0 Mya)

Paleocene (56.0–66.0 Mya)	Thanetian (56.0 Mya–59.2 Mya) Selandian (59.2 Mya–61.6 Mya) Danian (61.6 Mya–66.0 Mya)

Mesozoic era
(66.0–252.17 Mya)

Cretaceous (66.0–145.0 Mya)	Late (66.0–100.5 Mya) Early (100.5–145.0 Mya)

Jurassic (145.0–201.3 Mya)	Late (145.0–163.5 Mya) Middle (163.5–174.1 Mya) Early (174.1–201.3 Mya)

Triassic (201.3–252.17 Mya)	Late (201.3–237 Mya) Middle (237–247.2 Mya) Early (247.2–252.17 Mya)

Paleozoic era
(252.17–541.0 Mya)

Permian (252.17–298.9 Mya)	Lopingian (252.17–259.8 Mya) Guadalupian (259.8–272.3 Mya) Cisuralian (272.3–298.9 Mya)

Carboniferous (298.9–358.9 Mya)	Pennsylvanian (298.9–323.2 Mya) Mississippian (323.2–358.9 Mya)

Devonian (358.9–419.2 Mya)	Late (358.9–382.7 Mya) Middle (382.7–393.3 Mya) Early (393.3–419.2 Mya)

Silurian (419.2–443.8 Mya)	Pridoli (419.2–423.0 Mya) Ludlow (423.0–427.4 Mya) Wenlock (427.4–433.4 Mya) Llandovery (433.4–443.8 Mya)

Ordovician (443.8–485.4 Mya)	Late (443.8–458.4 Mya) Middle (458.4–470.0 Mya) Early (470.0–485.4 Mya)

Cambrian (485.4–541.0 Mya)	Furongian (485.4–497 Mya) Series 3 (497–509 Mya) Series 2 (509–521 Mya) Terreneuvian (521–541.0 Mya)

Precambrian
supereon
(541.0 Mya–4.567 Gya)

Proterozoic eon
(541.0 Mya–2.5 Gya)

Neoproterozoic (541.0 Mya–1 Gya)	Ediacaran (541 Mya–1000 Mya) Marinoan glaciation (635 Mya–650 Mya) Cryogenian (635 Mya–720 Mya) Sturtian glaciation (660 Mya–720 Mya) Tonian (720 Mya–1000 Mya)

Mesoproterozoic (1–1.6 Gya)	Stenian (1000 Mya–1200 Mya) Ectasian (1200 Mya–1400 Mya) Calymmian (1400 Mya–1600 Mya)

Paleoproterozoic (1.6–2.5 Gya)	Statherian (1600 Mya–1800 Mya) Orosirian (1800 Mya–2050 Mya) Rhyacian (2050 Mya–2300 Mya) Siderian\| (2300 Mya–2500 Mya)

Archean eon
(2.5–4 Gya)

Hadean eon
(4–4.567 Gya)

kya = thousands years ago. Mya = millions years ago. Gya = billions years ago.
Source: (2015/01). International Commission on Stratigraphy. Retrieved 13 July 2015. Divisions of Geologic Time—Major Chronostratigraphic and Geochronologic Units USGS Retrieved 10 March 2013.

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