Stroinolepis Temporal range: | |
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Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Infraphylum: | Agnatha |
Class: | † Thelodonti |
Order: | † Thelodontiformes |
Family: | † Loganelliidae |
Genus: | † Stroinolepis Märss & Karatajūtē-Talimaa, [1] 2002 |
Species | |
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Stroinolepis is an extinct genus of thelodontid that lived during the Middle and Late Ordovician period in what is now October Revolution Island, Severnaya Zemlya archipelago of Russia. It is known by scales of 0.2 to 1 mm in length. [1]
Generic name refers to the Strojnaya River where the holotype was found, while the specific epithet is given after Dr. P. Männik, who found and gave the specimen for study. [1]
Severnaya Zemlya is a 37,000 km2 (14,000 sq mi) archipelago in the Russian high Arctic. It lies off Siberia's Taymyr Peninsula, separated from the mainland by the Vilkitsky Strait. This archipelago separates two marginal seas of the Arctic Ocean, the Kara Sea in the west and the Laptev Sea in the east.
Komsomolets Island is the northernmost island of the Severnaya Zemlya group in the Russian Arctic, and the third largest island in the group. It is the 82nd largest island on earth. About 65% of the island is covered with glaciers, including Russia's largest, the Academy of Sciences Glacier.
October Revolution Island is the largest island of the Severnaya Zemlya group in the Russian Arctic. It is named after the October Revolution which led to the former Russian Empire becoming a Socialist country.
Pioneer Island is part of the Severnaya Zemlya group in the Russian Arctic. It measures 1,527 km2 (590 sq mi) in area. The island was discovered by Georgy Ushakov and Nikolay Urvantsev during their 1930-32 expedition.
Schmidt Island is one of the islands of the Severnaya Zemlya group in the Russian Arctic. It was named after Soviet scientist and first head of the Chief Directorate of the Northern Sea Route, Otto Schmidt. Located at the far northwestern end of Severnaya Zemlya, it lies slightly south of the Arctic Cape on Komsomolets Island.
Baltica is a paleocontinent that formed in the Paleoproterozoic and now constitutes northwestern Eurasia, or Europe north of the Trans-European Suture Zone and west of the Ural Mountains. The thick core of Baltica, the East European Craton, is more than three billion years old and formed part of the Rodinia supercontinent at c. 1 Ga.
Bolshevik Island is an island in Severnaya Zemlya, Krasnoyarsk Krai, Russian Arctic. The island is named after the political faction of the same name.
Nikolay Nikolayevich Urvantsev was a Soviet geologist and explorer. He was born in the town of Lukoyanov in the Lukoyanovsky Uyezd of the Nizhny Novgorod Governorate of the Russian Empire to the family of a merchant. He graduated from the Tomsk Engineering Institute in 1918.
Georgy Alexeyevich Ushakov was a Soviet explorer of the Arctic.
Maly Taymyr Island is an island in the Laptev Sea, Russian Arctic.
Karpinsky Glacier or Karpinsky Ice Cap, also known as Mount Karpinsky, is a large ice cap on October Revolution Island, Severnaya Zemlya, Russian Federation.
Cape Unslicht is a headland in Severnaya Zemlya, Russia.
The Academy of Sciences Glacier is a large ice cap on Komsomolets Island, Severnaya Zemlya, Russian Federation.
Cape Baranov is a headland in Severnaya Zemlya, Russia.
Cape October is a headland in Severnaya Zemlya, Russia.
Dianulites is an extinct genus of bryozoans from the early Ordovician period, belonging to the family Dianulitidae. Its colonies can be turbinate, horn-shaped, conical, or massive and hemispherical. Individual zooecia take the form of long, thin-walled polygonal tubes. It lacks styles (acanthopores), which helps differentiate it from similar genus Nicholsonella.
Ozyornaya is a river in the Krasnoyarsk Krai of Russia on the island of October Revolution, belonging to Severnaya Zemlya archipelago. The river originates in the Fiordovoye lake, for the most part flows in a south-westerly direction and meet the Kara sea with the formation of a delta. In the middle reaches, it goes around the Vavilov ice dome along its southeastern border, where several tributaries from the glacier flow into the river.