Siberia

Siberia (/saɪˈbɪəriə/ sy-BEER-ee-ə; Russian: Сибирь, romanized: Sibir', IPA: [sʲɪˈbʲirʲ] ⓘ) is an extensive geographical region comprising all of North Asia, from the Ural Mountains in the west to the Pacific Ocean in the east.[2] It has formed part of the sovereign territory of Russia and its various predecessor states since the centuries-long conquest of Siberia, which began with the fall of the Khanate of Sibir in the late 16th century and concluded with the annexation of Chukotka in 1778. Siberia is vast and sparsely populated, covering an area of over 13.1 million square kilometres (5,100,000 sq mi), but home to only one-fifth of Russia's population. Novosibirsk and Omsk are the largest cities in the area.[3]

Not to be confused with Serbia.
See also: North Asia
"Siberian" redirects here. For other uses, see Siberia (disambiguation) and Siberian (disambiguation).

Siberia
Сибирь
Geographical region
Coordinates: 60°0′N 105°0′E
ContinentAsia
CountryRussia
Parts
Area
 • Total13,100,000 km2 (5,100,000 sq mi)
Population
 (2023)
 • Total36.8 million[1]
 • Density2.8/km2 (7/sq mi)
DemonymSiberians

Because Siberia is a geographic and historic concept and not a political entity, there is no single precise definition of its territorial borders. Traditionally, Siberia spans the entire expanse of land from the Ural Mountains to the Pacific Ocean, with the Ural River usually forming the southernmost portion of its western boundary, and includes most of the drainage basin of the Arctic Ocean. It is further defined as stretching from the territories within the Arctic Circle in the north to the northern borders of Kazakhstan, Mongolia, and China in the south, although the hills of north-central Kazakhstan are also commonly included.[2][4] The Russian government divides the region into three federal districts (groupings of Russian federal subjects), of which only the central one is officially referred to as "Siberian"; the other two are the Ural and Far Eastern federal districts, named for the Ural and Russian Far East regions that correspond respectively to the western and eastern thirds of Siberia in the broader sense.

Siberia is known for its long, harsh winters, with a January average of −25 °C (−13 °F).[5] Although it is geographically in Asia, Russian sovereignty and colonization since the 16th century have rendered the region culturally and ethnically European.[6] Over 85% of its population are of European descent,[7][8] chiefly Russian (comprising the Siberian sub-ethnic group), and Eastern Slavic cultural influences predominate throughout the region.[6] Nevertheless, there exist sizable ethnic minorities of Asian lineage, including various Turkic communities—many of which, such as the Yakuts, Tuvans, Altais, and Khakas, are Indigenous—along with the Mongolic Buryats, ethnic Koreans, and smaller groups of Samoyedic and Tungusic peoples (several of whom are classified as Indigenous small-numbered peoples by the Russian government), among many others.

Etymology

The origin of the name is uncertain. [9] The modern usage of the name was recorded in the Russian language after the Russian conquest of Siberian Khanate.

Some sources say that "Siberia" originates from the Siberian Tatar word for "sleeping land" (Sib ir). A further variant claims that the region was named after the Sibe people.[10] The Polish historian Chyliczkowski has proposed that the name derives from the proto-Slavic word for "north" (север, sever),[11] same as Severia. Anatole Baikaloff has dismissed this explanation. He said that the neighbouring Chinese, Turks, and Mongolians, who have similar names for the region, would not have known Russian. He suggests that the name might be a combination of two words with Turkic origin, "su" (water) and "bir" (wild land).[12] Another account sees the name as the ancient tribal ethnonym of the Sirtya (also "Syopyr" (sʲɵpᵻr)), a Paleoasiatic ethnic group assimilated by the Nenets.

Mongolist György Kara explained that "Siberia" is derived from a Mongolic word "sibir", cognate with modern Buryat "sheber" or "dense forest".[13]

History
Main articles: Prehistory of Siberia, History of Siberia, and List of Russian explorers

Prehistory
Horseman hunting, with characteristic Xiongnu horse trappings, Southern Siberia, 280–180 BCE. Hermitage Museum.[14][15][16]

Siberia in Paleozoic times formed the continent of Siberia/Angaraland, which fused to Euramerica during the Late Carboniferous, as part of the formation of Pangea.[17]

The Siberian Traps were formed by one of the largest-known volcanic events of the last 251 million years of Earth's geological history. Their activity continued for a million years and some scientists consider it a possible cause of the "Great Dying" about 250 million years ago,[18] – estimated to have killed 90% of species existing at the time.[19]

The region has paleontological significance, as it contains bodies of prehistoric animals from the Pleistocene Epoch, preserved in ice or in permafrost. Specimens of Goldfuss cave lion cubs, Yuka the mammoth and another woolly mammoth from Oymyakon, a woolly rhinoceros from the Kolyma, and bison and horses from Yukagir have been found.[20] Remote Wrangel Island and the Taymyr Peninsula are believed to have been the last places on Earth to support woolly mammoths as isolated populations until their extinction around 2000 BC.[21]

At least three species of human lived in Southern Siberia around 40,000 years ago: H. sapiens, H. neanderthalensis, and the Denisovans.[22] In 2010 DNA evidence identified the last as a separate species.[23]

Late Paleolithic southern Siberians appear to be related to paleolithic Europeans and the paleolithic Jōmon people of Japan.[24] Ancient DNA analysis has revealed that the oldest fossil known to carry the derived KITLG allele, which is responsible for blond hair in modern Europeans, is a 17,000 year old Ancient North Eurasian specimen from Siberia.[25] Ancient North Eurasian populations genetically similar to Mal'ta–Buret' culture and Afontova Gora were an important genetic contributor to Native Americans, Europeans, Ancient Central Asians, South Asians, and some East Asian groups (such as the Ainu people). Evidence from full genomic studies suggests that the first people in the Americas diverged from Ancient East Asians about 36,000 years ago and expanded northwards into Siberia, where they encountered and interacted with Ancient North Eurasians, giving rise to both Paleosiberian peoples and Ancient Native Americans, which later migrated towards the Beringian region, became isolated from other populations, and subsequently populated the Americas.[26][27]

Early history
Chukchi, one of many Indigenous peoples of Siberia. Representation of a Chukchi family by Louis Choris (1816)

During past millennia different groups of nomads – such as the Enets, the Nenets, the Huns, the Xiongnu, the Scythians, and the Yugur – inhabited various parts of Siberia. The Afanasievo and Tashtyk cultures of the Yenisey valley and Altay Mountains are associated with the Indo-European migrations across Eurasia.[28] The proto-Mongol Khitan people also occupied parts of the region. In the 13th century, during the period of the Mongol Empire, the Mongols conquered a large part of this area.[29]

With the breakup of the Golden Horde, the autonomous Khanate of Sibir formed in the late-15th century. Turkic-speaking Yakut migrated north from the Lake Baikal region under pressure from the Mongol tribes during the 13th to 15th century.[30] Siberia remained a sparsely populated area. Historian John F. Richards wrote: "... it is doubtful that the total early modern Siberian population exceeded 300,000 persons".[31]

Further information: Russian conquest of Siberia

The growing power of Russia in the West began to undermine the Siberian Khanate in the 16th century. First, groups of traders and Cossacks began to enter the area. The Russian Army was directed to establish forts farther and farther east to protect new Russian settlers who migrated from Europe. Towns such as Mangazeya, Tara, Yeniseysk, and Tobolsk developed, the last becoming the de facto capital of Siberia from 1590. At this time, Sibir was the name of a fortress at Qashliq, near Tobolsk. Gerardus Mercator, in a map published in 1595, marks Sibier both as the name of a settlement and of the surrounding territory along a left tributary of the Ob.[32] Other sources contend that the Sibe, an Indigenous Tungusic people, offered fierce resistance to Russian expansion beyond the Urals. Some suggest that the term "Siberia" is a russification of their ethnonym.[10]

Russian Empire
Coat of arms of Siberia, which was a part of the Russian Imperial Coat of Arms until 1917
Map of the Siberian Route in the 18th century (green) and the early 19th century (red)

By the mid-17th century, Russia had established areas of control that extended to the Pacific Ocean. Some 230,000 Russians had settled in Siberia by 1709.[33] Siberia became one of the destinations for sending internal exiles. Exile was the main Russian punitive practice with more than 800,000 people exiled during the nineteenth century.[34][35]

The first great modern change in Siberia was the Trans-Siberian Railway, constructed during 1891–1916. It linked Siberia more closely to the rapidly industrialising Russia of Nicholas II (r. 1894–1917). Around seven million Russians moved to Siberia from Europe between 1801 and 1914.[36] Between 1859 and 1917 more than half a million people migrated to the Russian Far East.[37] Siberia has extensive natural resources: during the 20th century, large-scale exploitation of these took place, and industrial towns cropped up throughout the region.[38]

At 7:15 a.m. on 30 June 1908 the Tunguska Event felled millions of trees near the Podkamennaya Tunguska River (Stony Tunguska River) in central Siberia. Most scientists believe this resulted from the air burst of a meteor or a comet. Even though no crater has ever been found, the landscape in the (sparsely inhabited) area still bears the scars of this event.[39]

Soviet Union
Siberian Cossack family in Novosibirsk

In the early decades of the Soviet Union (especially in the 1930s and 1940s), the government used the Gulag state agency to administer a system of penal labour camps, replacing the previous katorga system.[40] According to semi-official Soviet estimates, which did not become public until after the fall of the Soviet government in 1991, from 1929 to 1953 more than 14 million people passed through these camps and prisons, many of them in Siberia. Another seven to eight million people were internally deported to remote areas of the Soviet Union (including entire nationalities or ethnicities in several cases).[41]

Half a million (516,841) prisoners died in camps from 1941 to 1943[42] during World War II. At other periods, mortality was comparatively lower.[43] The size, scope, and scale of the Gulag slave-labour camps remain subjects of much research and debate. Many Gulag camps operated in extremely remote areas of northeastern Siberia. The best-known clusters included Sevvostlag (the North-East Camps) along the Kolyma and Norillag near Norilsk, where 69,000 prisoners lived in 1952.[44] Major industrial cities of Northern Siberia, such as Norilsk and Magadan, developed from camps built by prisoners and run by former prisoners.[45]

Geography
Further information: Geography of Russia and North Asia § Geography
View from Haiyrakan mountain, Tuva
Altai, Lake Kutsherla in the Altai Mountains
The peninsula of Svyatoy Nos, Lake Baikal
The river Vasyugan in the southern West Siberian Plain
Koryaksky volcano towering over Petropavlovsk-Kamchatsky on the Kamchatka Peninsula

Siberia spans an area of 13.1 million square kilometres (5,100,000 sq mi), covering the vast majority of Russia's total territory, and almost 9% of Earth's land surface (148,940,000 km2, 57,510,000 sq mi). It geographically falls in Asia, but is culturally and politically considered European, since it is a part of Russia.[6] Major geographical zones within Siberia include the West Siberian Plain and the Central Siberian Plateau.

Eastern and central Sakha comprises numerous north–south mountain ranges of various ages. These mountains extend up to almost 3,000 metres (9,800 ft), but above a few hundred metres they are almost completely devoid of vegetation. The Verkhoyansk Range was extensively glaciated in the Pleistocene, but the climate was too dry for glaciation to extend to low elevations. At these low elevations are numerous valleys, many of them deep and covered with larch forest, except in the extreme north where the tundra dominates. Soils are mainly turbels (a type of gelisol). The active layer tends to be less than one metre deep, except near rivers.

The highest point in Siberia is the active volcano Klyuchevskaya Sopka, on the Kamchatka Peninsula. Its peak reaches 4,750 metres (15,580 ft).

Mountain ranges

Geomorphological regions
See also: Great Russian Regions

Lakes and rivers
Main article: Rivers in Russia

Grasslands

Geology

The West Siberian Plain, consisting mostly of Cenozoic alluvial deposits, is somewhat flat. In the mid-Pleistocene, many deposits on this plain resulted from ice dams which produced a large glacial lake. This mid- to late-Pleistocene lake blocked the northward flow of the Ob and Yenisey rivers, resulting in a redirection southwest into the Caspian and Aral seas via the Turgai Valley.[47] The area is very swampy, and soils are mostly peaty histosols and, in the treeless northern part, histels. In the south of the plain, where permafrost is largely absent, rich grasslands that are an extension of the Kazakh Steppe formed the original vegetation, most of which is no longer visible.

Belukha Mountain
Verkhoyansk Range

The Central Siberian Plateau is an ancient craton (sometimes named Angaraland) that formed an independent continent before the Permian (see the Siberian continent). It is exceptionally rich in minerals, containing large deposits of gold, diamonds, and ores of manganese, lead, zinc, nickel, cobalt, and molybdenum. Much of the area includes the Siberian Traps—a large igneous province. A massive eruptive period approximately coincided with the Permian–Triassic extinction event. The volcanic event is said to be the largest known volcanic eruption in Earth's history. Only the extreme northwest was glaciated during the Quaternary, but almost all is under exceptionally deep permafrost, and the only tree that can thrive, despite the warm summers, is the deciduous Siberian Larch (Larix sibirica) with its very shallow roots. Outside the extreme northwest, the taiga is dominant, covering a significant fraction of the entirety of Siberia.[48] Soils here are mainly turbels, giving way to spodosols where the active layer becomes thicker and the ice-content lower.

The Lena-Tunguska petroleum province includes the Central Siberian platform (some authors refer to it as the "Eastern Siberian platform"), bounded on the northeast and east by the Late Carboniferous through Jurassic Verkhoyansk foldbelt, on the northwest by the Paleozoic Taymr foldbelt, and on the southeast, south and southwest by the Middle Silurian to Middle Devonian Baykalian foldbelt.[49]: 228  A regional geologic reconnaissance study begun in 1932 and followed by surface and subsurface mapping revealed the Markova-Angara Arch (anticline). This led to the discovery of the Markovo Oil Field in 1962 with the Markovo—1 well, which produced from the Early Cambrian Osa Horizon bar-sandstone at a depth of 2,156 metres (7,073 ft).[49]: 243  The Sredne-Botuobin Gas Field was discovered in 1970, producing from the Osa and the Proterozoic Parfenovo Horizon.[49]: 244  The Yaraktin Oil Field was discovered in 1971, producing from the Vendian Yaraktin Horizon at depths of up to 1,750 metres (5,740 ft), which lies below Permian to Lower Jurassic basalt traps.[49]: 244 

Climate
Main article: Climate of Russia
Siberian taiga

     polar desert      tundra      alpine tundra      taiga      montane forest
     temperate broadleaf forest      temperate steppe      dry steppe

Vegetation in Siberia mostly consists of taiga, with a tundra belt on the northern fringe, and a temperate forest zone in the south.

The climate of Siberia varies dramatically, but it typically has short summers and long, brutally cold winters. On the north coast, north of the Arctic Circle, there is a very short (about one month long) summer.

Almost all the population lives in the south, along the route of the Trans-Siberian Railway. The climate in this southernmost part is humid continental climate (Köppen Dfa/Dfb or Dwa/Dwb) with cold winters but fairly warm summers lasting at least four months. The annual average temperature is about 0.5 °C (32.9 °F). January averages about −20 °C (−4 °F) and July about +19 °C (66 °F), while daytime temperatures in summer typically exceed 20 °C (68 °F).[50][51] With a reliable growing season, an abundance of sunshine and exceedingly fertile chernozem soils, southern Siberia is good enough for profitable agriculture, as was demonstrated in the early 20th century.

By far the most commonly occurring climate in Siberia is continental subarctic (Koppen Dfc, Dwc, or Dsc), with the annual average temperature about −5 °C (23 °F) and an average for January of −25 °C (−13 °F) and an average for July of +17 °C (63 °F),[52] although this varies considerably, with a July average about 10 °C (50 °F) in the taiga–tundra ecotone. The business-oriented website and blog Business Insider lists Verkhoyansk and Oymyakon, in Siberia's Sakha Republic, as being in competition for the title of the Northern Hemisphere's Pole of Cold. Oymyakon is a village which recorded a temperature of −67.7 °C (−89.9 °F) on 6 February 1933. Verkhoyansk, a town further north and further inland, recorded a temperature of −69.8 °C (−93.6 °F) for three consecutive nights: 5, 6 and 7 February 1933. Each town is alternately considered the Northern Hemisphere's Pole of Cold – the coldest inhabited point in the Northern hemisphere. Each town also frequently reaches 30 °C (86 °F) in the summer, giving them, and much of the rest of Russian Siberia, the world's greatest temperature variation between summer's highs and winter's lows, often well over 94–100+ °C (169–180+ °F) between the seasons.[53]

Southwesterly winds bring warm air from Central Asia and the Middle East. The climate in West Siberia (Omsk, or Novosibirsk) is several degrees warmer than in the East (Irkutsk, or Chita) where in the north an extreme winter subarctic climate (Köppen Dfd, Dwd, or Dsd) prevails. But summer temperatures in other regions can reach +38 °C (100 °F). In general, Sakha is the coldest Siberian region, and the basin of the Yana has the lowest temperatures of all, with permafrost reaching 1,493 metres (4,898 ft). Nevertheless, Imperial Russian plans of settlement never viewed cold as an impediment. In the winter, southern Siberia sits near the center of the semi-permanent Siberian High, so winds are usually light in the winter.

Precipitation in Siberia is generally low, exceeding 500 millimetres (20 in) only in Kamchatka, where moist winds flow from the Sea of Okhotsk onto high mountains – producing the region's only major glaciers, though volcanic eruptions and low summer temperatures allow only limited forests to grow. Precipitation is high also in most of Primorye in the extreme south, where monsoonal influences can produce quite heavy summer rainfall.

Climate data for Novosibirsk, Siberia's largest city
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °C (°F) −12.2
(10.0)		 −10.3
(13.5)		 −2.6
(27.3)		 8.1
(46.6)		 17.5
(63.5)		 24.0
(75.2)		 25.7
(78.3)		 22.2
(72.0)		 16.6
(61.9)		 6.8
(44.2)		 −2.9
(26.8)		 −8.9
(16.0)		 7.0
(44.6)
Daily mean °C (°F) −16.2
(2.8)		 −14.7
(5.5)		 −7.2
(19.0)		 3.2
(37.8)		 11.6
(52.9)		 18.2
(64.8)		 20.2
(68.4)		 17.0
(62.6)		 11.5
(52.7)		 3.4
(38.1)		 −6
(21)		 −12.7
(9.1)		 2.4
(36.3)
Average low °C (°F) −20.1
(−4.2)		 −19.1
(−2.4)		 −11.8
(10.8)		 −1.7
(28.9)		 5.6
(42.1)		 12.3
(54.1)		 14.7
(58.5)		 11.7
(53.1)		 6.4
(43.5)		 0.0
(32.0)		 −9.1
(15.6)		 −16.4
(2.5)		 −2.3
(27.9)
Average precipitation mm (inches) 19
(0.7)		 14
(0.6)		 15
(0.6)		 24
(0.9)		 36
(1.4)		 58
(2.3)		 72
(2.8)		 66
(2.6)		 44
(1.7)		 38
(1.5)		 32
(1.3)		 24
(0.9)		 442
(17.4)
Source: [54]

Global warming

Researchers, including Sergei Kirpotin at Tomsk State University and Judith Marquand at Oxford University, warn that Western Siberia has begun to thaw as a result of global warming. The frozen peat bogs in this region may hold billions of tons of methane gas, which may be released into the atmosphere. Methane is a greenhouse gas 22 times more powerful than carbon dioxide.[55] In 2008 a research expedition for the American Geophysical Union detected levels of methane up to 100 times above normal in the atmosphere above the Siberian Arctic, likely the result of methane clathrates being released through holes in a frozen "lid" of seabed permafrost around the outfall of the Lena and the area between the Laptev Sea and East Siberian Sea.[56][57]

Since 1988, experimentation at Pleistocene Park has proposed to restore the grasslands of prehistoric times by conducting research on the effects of large herbivores on permafrost, suggesting that animals, rather than climate, maintained the past ecosystem. The nature reserve park also conducts climatic research on the changes expected from the reintroduction of grazing animals or large herbivores, hypothesizing that a transition from tundra to grassland would lead to a net change in energy emission to absorption ratios.[58]

According to Vasily Kryuchkov, approximately 31,000 square kilometers of the Russian Arctic has subjected to severe environmental disturbance.

Fauna

Birds
See also: List of birds of Russia
Capercaillies inhabit much of the Siberian taiga

Family Tetraonidae

Family Phasianidae

Mammals
See also: List of mammals of Russia

Order Artiodactyla
Two saddled Bactrian camels shedding their coats in the Altai mountain range
A muskox on Bolshoy Begichev Island in Laptev Sea

Family Canidae

Family Felidae
A Siberian tigress and cub

Family Mustelidae

Family Ursidae
Kamchatka brown bear at Kamchatka Peninsula
Polar bear on Wrangel Island

Flora
Siberian larch Larix sibirica trees in summer. Kuznetsk Alatau Nature Reserve, Kemerovo Oblast

Politics
Main article: Siberian regionalism

Notable sovereign states in Siberia

Borders and administrative division
Map of the most populated area of Siberia with clickable city names (SVG)
Comparison of the nine biggest Siberian cities' growth in the 20th century

The term "Siberia" has both a long history and wide significance, and association. The understanding, and association of "Siberia" have gradually changed during the ages. Historically, Siberia was defined as the whole part of Russia and North Kazakhstan to the east of Ural Mountains, including the Russian Far East. According to this definition, Siberia extended eastward from the Ural Mountains to the Pacific coast, and southward from the Arctic Ocean to the border of Central Asia and the national borders of both Mongolia and China.[74]

Soviet-era sources (Great Soviet Encyclopedia and others)[4] and modern Russian ones[75] usually define Siberia as a region extending eastward from the Ural Mountains to the watershed between Pacific and Arctic drainage basins, and southward from the Arctic Ocean to the hills of north-central Kazakhstan and the national borders of both Mongolia and China. By this definition, Siberia includes the federal subjects of the Siberian Federal District, and some of the Ural Federal District, as well as Sakha (Yakutia) Republic, which is a part of the Far Eastern Federal District. Geographically, this definition includes subdivisions of several other subjects of Urals and Far Eastern federal districts, but they are not included administratively. This definition excludes Sverdlovsk Oblast and Chelyabinsk Oblast, both of which are included in some wider definitions of Siberia.

Other sources may use either a somewhat wider definition that states the Pacific coast, not the watershed, is the eastern boundary (thus including the whole Russian Far East), as well as all Northern Kazakhstan is its subregion in the south-west[2] or a somewhat narrower one that limits Siberia to the Siberian Federal District (thus excluding all subjects of other districts).[76] In Russian, 'Siberia' is commonly used as a substitute for the name of the federal district by those who live in the district itself, but less commonly used to denote the federal district by people residing outside of it. Due to the different interpretations of Siberia, starting from Tyumen, to Chita, the territory generally defined as 'Siberia', some people will define themselves as 'Siberian', while others not.

A number of factors in recent years, including the fomenting of Siberian separatism have made the definition of the territory of Siberia a potentially controversial subject.[77] In the eastern extent of Siberia there are territories which are not clearly defined as either Siberia or the Far East, making the question of "what is Siberia?" one with no clear answer, and what is a "Siberian", one of self-identification.[78]

Novosibirsk is the largest city in Siberia
Federal subjects of Siberia (GSE)
Subject Administrative center
Ural Federal District
 Khanty–Mansi Autonomous Okrug Khanty-Mansiysk
 Kurgan Oblast Kurgan
 Tyumen Oblast Tyumen
 Yamalo-Nenets Autonomous Okrug Salekhard
Siberian Federal District
 Altai Krai Barnaul
 Altai Republic Gorno-Altaysk
 Irkutsk Oblast Irkutsk
 Khakassia Abakan
 Kemerovo Oblast Kemerovo
 Krasnoyarsk Krai Krasnoyarsk
 Novosibirsk Oblast Novosibirsk
 Omsk Oblast Omsk
 Tomsk Oblast Tomsk
 Tuva Kyzyl
Far Eastern Federal District
 Buryatia Ulan-Ude
 Sakha (Yakutia) Yakutsk
 Zabaykalsky Krai Chita
Amur waterfront in Khabarovsk
Vladivostok, Primorsky Krai
Yakutsk is the capital of the Sakha Republic
Federal subjects of Siberia (in wide sense)
Subject Administrative center
Far Eastern Federal District
 Amur Oblast Blagoveshchensk
 Chukotka Autonomous Okrug Anadyr
 Jewish Autonomous Oblast Birobidzhan
 Kamchatka Krai Petropavlovsk-Kamchatsky
 Khabarovsk Krai Khabarovsk
 Magadan Oblast Magadan
 Primorsky Krai Vladivostok
 Sakhalin Oblast Yuzhno-Sakhalinsk
Ural Federal District
 Chelyabinsk Oblast Chelyabinsk
 Sverdlovsk Oblast Yekaterinburg

Major cities

The most populous city of Siberia, as well as the third most populous city of Russia, is the city of Novosibirsk. Present-day Novosibirsk is an important business, science, manufacturing and cultural center of the Asian part of Russia.

Omsk played an important role in the Russian Civil War serving as a provisional Russian capital, as well in the expansion into and governing of Central Asia. In addition to its cultural status, it has become a major oil-refining, education, transport and agriculture hub.

Other historic cities of Siberia include Tobolsk (the first capital and the only kremlin in Siberia), Tomsk (formerly a wealthy merchant's town) and Irkutsk (former seat of Eastern Siberia's governor general, near lake Baikal).

Other major cities include: Barnaul, Kemerovo, Krasnoyarsk, Novokuznetsk, Tyumen.

Wider definitions of geographic Siberia also include the cities of: Chelyabinsk and Yekaterinburg in the Urals, Khabarovsk and Vladivostok in the Russian Far East, and even Petropavlovsk in Kazakhstan and Harbin in China.

Economy
Russian oil and gas pipelines in use

Novosibirsk is the largest by population and the most important city for the Siberian economy; with an extra boost since 2000 when it was designated a regional center for the executive bureaucracy (Siberian Federal District). Omsk is a historic and currently the second largest city in the region, and since 1950s hosting Russia's largest oil refinery.

Siberia is extraordinarily rich in minerals, containing ores of almost all economically valuable metals. It has some of the world's largest deposits of nickel, gold, lead, coal, molybdenum, gypsum, diamonds, diopside, silver and zinc, as well as extensive unexploited resources of oil and natural gas.[79] Around 70% of Russia's developed oil fields are in the Khanty-Mansiysk region.[80] Russia contains about 40% of the world's known resources of nickel at the Norilsk deposit in Siberia. Norilsk Nickel is the world's biggest nickel and palladium producer.[81]

Siberian agriculture is severely restricted by the short growing season of most of the region. However, in the southwest where soils consist of exceedingly fertile black earths and the climate is a little more moderate, there is extensive cropping of wheat, barley, rye and potatoes, along with the grazing of large numbers of sheep and cattle. Elsewhere food production, owing to the poor fertility of the podzolic soils and the extremely short growing seasons, is restricted to the herding of reindeer in the tundra—which has been practiced by natives for over 10,000 years. Siberia has the world's largest forests. Timber remains an important source of revenue, even though many forests in the east have been logged much more rapidly than they are able to recover. The Sea of Okhotsk is one of the two or three richest fisheries in the world owing to its cold currents and very large tidal ranges, and thus Siberia produces over 10% of the world's annual fish catch, although fishing has declined somewhat since the collapse of the USSR in 1991.[82]

Reported in 2009, the development of renewable energy in Russia is held back by the lack of a conducive government policy framework,[83] As of 2011, Siberia still offers special opportunities for off-grid renewable energy developments. Remote parts of Siberia are too costly to connect to central electricity and gas grids, and have therefore historically been supplied with costly diesel, sometimes flown in by helicopter. In such cases renewable energy is often cheaper.[84]

In 2021 the gross regional product of Siberia was ₽35.361 trillion  or around €400 billion.[85]

Sport
KHL game HC Sibir Novosibirsk vs Amur Khabarovsk

The Yenisey Krasnoyarsk basketball team has played in the VTB United League since 2011–12.

Russia's third most popular sport, bandy,[86] is important in Siberia. In the 2015–16 Russian Bandy Super League season Yenisey from Krasnoyarsk became champions for the third year in a row by beating Baykal-Energiya from Irkutsk in the final.[87][88] Two or three more teams (depending on the definition of Siberia) play in the Super League, the 2016–17 champions SKA-Neftyanik from Khabarovsk as well as Kuzbass from Kemerovo and Sibselmash from Novosibirsk. In 2007 Kemerovo got Russia's first indoor arena specifically built for bandy.[89] Now Khabarovsk has the world's largest indoor arena specifically built for bandy, Arena Yerofey.[90] It was venue for Division A of the 2018 World Championship. In time for the 2020 World Championship, an indoor arena will be ready for use in Irkutsk. That one will also have a speed skating oval.[91]

The 2019 Winter Universiade was hosted by Krasnoyarsk.

Demographics
Main article: Demographics of Siberia
See also: Siberians and Indigenous peoples of Siberia
Population of Siberia[92][93]
Ethnicity Population %
Slavic 18,235,47186.2%
Turkic 1,704,6658.1%
Mongol 454,3122.1%
Uralic 131,4300.6%
Other 637,9923.0%

According to the Russian Census of 2010, the Siberian and Far Eastern Federal Districts, located entirely east of the Ural Mountains, together have a population of about 25.6 million. Tyumen and Kurgan Oblasts, which are geographically in Siberia but administratively part of the Urals Federal District, together have a population of about 4.3 million. Thus, the whole region of Siberia (in the broadest usage of the term) is home to approximately 30 million people.[94] It has a population density of about three people per square kilometre.

Tomsk, one of the oldest Siberian cities, founded in 1604

The largest ethnic group in Siberia is Slavic-origin Russians, including their sub-ethnic group Siberians, and russified Ukrainians.[95] Slavic and other Indo-European ethnicities make up the vast majority (over 85%) of the Siberian population. There are also other groups of Indigenous Siberian and non-Indigenous ethnic origin. A minority of the current population are descendants of Mongol or Turkic people (mainly Buryats, Yakuts, Tuvans, Altai and Khakas) or northern Indigenous people. Slavic-origin Russians outnumber all of the Indigenous peoples combined, except in the Republics of Tuva and Sakha.

According to the 2002 census there are 500,000 Tatars in Siberia, but of these, 300,000 are Volga Tatars who also settled in Siberia during periods of colonization and are thus also non-Indigenous Siberians, in contrast to the 200,000 Siberian Tatars which are Indigenous to Siberia.[96] Of the Indigenous Siberians, the Mongol-speaking Buryats, numbering approximately 500,000, are the most numerous group in Siberia, and they are mainly concentrated in their homeland, the Buryat Republic.[97] According to the 2010 census there were 478,085 indigenous Turkic-speaking Yakuts.[98] Other ethnic groups Indigenous to Siberia include Kets, Evenks, Chukchis, Koryaks, Yupiks, and Yukaghirs.

About seventy percent of Siberia's people live in cities, mainly in apartments.[99] Many people also live in rural areas, in simple, spacious, log houses. Novosibirsk[100] is the largest city in Siberia, with a population of about 1.6 million. Tobolsk, Tomsk, Tyumen, Krasnoyarsk, Irkutsk, and Omsk are the older, historical centers.

Religion
See also: Shamanism in Siberia and Religion in Russia
Transfiguration Cathedral, Khabarovsk

There are a variety of beliefs throughout Siberia, including Orthodox Christianity, other denominations of Christianity, Tibetan Buddhism and Islam.[101] The Siberian Federal District alone has an estimation of 250,000 Muslims. An estimated 70,000 Jews live in Siberia,[102] some in the Jewish Autonomous Region.[103] The predominant religious group is the Russian Orthodox Church.

Tradition regards Siberia the archetypal home of shamanism, and polytheism is popular.[104] These native sacred practices are considered by the tribes to be very ancient. There are records of Siberian tribal healing practices dating back to the 13th century.[105] The vast territory of Siberia has many different local traditions of gods. These include: Ak Ana, Anapel, Bugady Musun, Kara Khan, Khaltesh-Anki, Kini'je, Ku'urkil, Nga, Nu'tenut, Num-Torum, Pon, Pugu, Todote, Toko'yoto, Tomam, Xaya Iccita and Zonget. Places with sacred areas include Olkhon, an island in Lake Baikal.

Transport

Many cities in northern Siberia, such as Petropavlovsk-Kamchatsky, cannot be reached by road, as there are virtually none connecting from other major cities in Russia or Asia. Siberia can be reached through the Trans-Siberian Railway. The Trans-Siberian Railway operates from Moscow in the west to Vladivostok in the east. Cities that are located far from the railway are reached by air or by the separate Baikal–Amur Railway (BAM).

Culture

Cuisine

Stroganina is a raw fish dish of the Indigenous people of northern Arctic Siberia made from raw, thin, long-sliced frozen fish.[106] It is a popular dish with native Siberians.[107] Siberia is also known for its pelmeni dumpling; which in the winter are traditionally frozen and stored outdoors. In addition, there are various berry, nut and mushroom dishes making use of the riches of abundant nature.

See also

References
  1. "Предварительная оценка численности постоянного населения на 1 января 2023 г." Federal State Statistics Service. Retrieved 21 February 2023.
  2. "Siberia". Encyclopædia Britannica Online. Retrieved 22 September 2021.
  3. "The Largest Cities in Siberia". August 2017.
  4. Сибирь — Большая советская энциклопедия (The Great Soviet Encyclopedia, in Russian)
  5. "Arctic Oscillation and Polar Vortex Analysis and Forecasts". Atmospheric and Environmental Research, Verisk Analytics. Retrieved 20 May 2018.
  6. Haywood, A. J. (2010). Siberia: A Cultural History. Oxford University Press. ISBN 9780199754182.
  7. "ВПН-2010". Perepis-2010.ru (in Russian). Archived from the original on 18 January 2012. Retrieved 3 April 2016.
  8. "ВПН-2010". Gks.ru (in Russian). Archived from the original on 15 March 2013. Retrieved 3 April 2016.
  9. "Siberia".
  10. Crossley, Pamela Kyle (2002). The Manchus. Peoples of Asia. Vol. 14 (3rd ed.). Wiley-Blackwell. p. 213. ISBN 978-0-631-23591-0. Retrieved 28 December 2013.
  11. Czaplicka, Marie Antoinette (1914). Aboriginal Siberia : a study in social anthropology. Oxford : Clarendon Press. p. 20.
  12. Baikaloff, Anatole (December 1950). "Notes on the origin of the name "Siberia"". Slavonic and East European Review. 29 (72): 288.
  13. "The Multilingual Far East: An Interview with Professor György Kara". Robert F. Byrnes Russian and East European Institute. Retrieved 11 September 2023.
  14. Pankova, Svetlana; Simpson, St John (21 January 2021). Masters of the Steppe: The Impact of the Scythians and Later Nomad Societies of Eurasia: Proceedings of a conference held at the British Museum, 27–29 October 2017. Archaeopress Publishing Ltd. pp. 218–219. ISBN 978-1-78969-648-6. Inv. nr.Si. 1727- 1/69, 1/70
  15. Francfort, Henri-Paul (1 January 2020). "Sur quelques vestiges et indices nouveaux de l'hellénisme dans les arts entre la Bactriane et le Gandhāra (130 av. J.-C.-100 apr. J.-C. environ)". Journal des Savants: 37.
  16. Ollermann, Hans (22 August 2019). "Belt Plaque with a Bear Hunt. From Russia (Siberia). Gold. 220-180 B.C. The State Hermitage Museum, St. Petersburg, Russia".
  17. Xu, Yan; Han, Bao‐Fu; Liao, Wen; Li, Ang (March 2022). "The Serpukhovian–Bashkirian Amalgamation of Laurussia and the Siberian Continent and Implications for Assembly of Pangea". Tectonics. 41 (3). doi:10.1029/2022TC007218. ISSN 0278-7407. S2CID 247459291.
  18. "Yellowstone's Super Sister". Archived from the original on 14 March 2005. Retrieved 17 April 2010. [...] the Siberian Traps is the prime suspect in wiping out 90 percent of all living species 251 million years ago – the most severe extinction event in Earth's history.. Discovery Channel.
  19. Benton, M. J. (2005). When Life Nearly Died: The Greatest Mass Extinction of All Time. Thames & Hudson. ISBN 978-0-500-28573-2.
  20. "Meet this extinct cave lion, at least 10,000 years old – world exclusive". siberiantimes.com. Retrieved 30 January 2016.
  21. Wang, Y; Pedersen, M.W.; Alsos, I.g.; et al. (2021). "Late Quaternary dynamics of Arctic biota from ancient environmental genomics". Nature. 600 (7887): 86–92. Bibcode:2021Natur.600...86W. doi:10.1038/s41586-021-04016-x. PMC 8636272. PMID 34671161.
  22. " DNA identifies new ancient human dubbed 'X-woman'," BBC News. 25 March 2010.
  23. Richards, Michael P. (2020). Archaeological Science. Cambridge University Press. p. 23. ISBN 9780521195225. In early 2010, researchers published a complete mitochondrial genome sequence retrieved from a hominin excavated from the Denisova cave in Siberia....The results demonstrated that the Denisovan lineage diverged early from the modern humans and Neanderthals
  24. "Jomon Culture and the peopling of the Japanese archipelago: advancements in the fields of morphometrics and ancient DNA". ResearchGate. Retrieved 18 August 2019.
  25. Evans, Gavin (2019). Skin Deep: Dispelling the Science of Race (1 ed.). Simon and Schuster. p. 139. ISBN 9781786076236.|
  26. Raff, Jennifer (9 June 2020). Origin: A Genetic History of the Americas. Twelve. ISBN 978-1-5387-4971-5.
  27. Sapiens (8 February 2022). "A Genetic Chronicle of the First Peoples in the Americas". SAPIENS. Retrieved 29 October 2022.
  28. Gibbons, Ann (10 June 2015). "Nomadic herders left a strong genetic mark on Europeans and Asians". Science. AAAS.
  29. Naumov, Igor V. (2006). "The Mongols in Siberia". In Collins, David Norman (ed.). The History of Siberia. Routledge Studies in the History of Russia and Eastern Europe. Translated by Collins, David Norman. London: Routledge. p. 44. ISBN 9781134207039. Retrieved 11 June 2019. In 1207 Chinggis Khan sent his troops north under the command of his elder son Jochi to subjugate the 'forest peoples'. Jochi was able to do so in the space of three years. The only exception was the remote northern tribes. Most of Siberia became part of the Mongol Empire.
  30. Public Domain This article incorporates text from this source, which is in the public domain: Pakendorf, B.; Novgorodov, I. N.; Osakovskij, V. L.; Danilova, A. B. P.; Protod'Jakonov, A. P.; Stoneking, M. (2006). "Investigating the effects of prehistoric migrations in Siberia: Genetic variation and the origins of Yakuts". Human Genetics. 120 (3): 334–353. doi:10.1007/s00439-006-0213-2. PMID 16845541. S2CID 31651899.
  31. Richards, 2003 p. 538.
  32. Asia ex magna Orbis terrae descriptione Gerardi Mercatoris desumpta, studio & industria G.M. Iunioris
  33. Sean C. Goodlett. "Russia's Expansionist Policies I. The Conquest of Siberia". Falcon.fsc.edu. Archived from the original on 11 May 2011. Retrieved 15 May 2010.
  34. For example: Prison without a roof
  35. Barker, Adele Marie (2010). Barker, Adele Marie; Grant, Bruce (eds.). The Russia Reader: History, Culture, Politics. The World Readers. Durham, North Carolina: Duke University Press. p. 441. ISBN 9780822346487. Retrieved 11 June 2019. Throughout Russian history there is a long-standing tradition of imprisoning and sentencing to internal exile (within the country proper) political and religious dissidents. [...] Among those sentenced to internal exile were [...] the Decembrists [...]. Several were executed; others were exiled to Siberia, the Far East, and Kazakhstan.
  36. Fisher, Raymond H.; Treadgold, Donald W. (1958). "Review: The Great Siberian Migration: Government and Peasant in Resettlement from Emancipation to the First World War". The American Historical Review. 63 (4): 989–990. doi:10.2307/1848991. JSTOR 1848991.
  37. The Russian Far East: A History. John J. Stephan (1996). Stanford University Press. p.62. ISBN 0-8047-2701-5
  38. Fiona Hill, Russia — Coming In From the Cold? Archived 24 April 2013 at the Wayback Machine, The Globalist, 23 February 2004.
  39. Farinella, Paolo; Foschini, L.; Froeschlé, Christiane; Gonczi, R.; Jopek, T. J.; Longo, G.; Michel, Patrick (2001). "Probable asteroidal origin of the Tunguska Cosmic Body" (PDF). Astronomy & Astrophysics. 377(3): 1081–1097. Bibcode:2001A&A...377.1081F. doi:10.1051/0004-6361:20011054.
  40. The Unknown Gulag: The Lost World of Stalin's Special Settlements. Lynne Viola (2007). Oxford University Press US. p.3. ISBN 0-19-518769-5
  41. Robert Conquest in "Victims of Stalinism: A Comment," Europe-Asia Studies, Vol. 49, No. 7 (Nov. 1997), pp. 1317–1319 states: "We are all inclined to accept the Zemskov totals (even if not as complete) with their 14 million intake to Gulag 'camps' alone, to which must be added four to five million going to Gulag 'colonies', to say nothing of the 3.5 million already in, or sent to, 'labour settlements'. However taken, these are surely 'high' figures."
  42. Zemskov, "Gulag," Sociologičeskije issledovanija, 1991, No. 6, pp. 14–15.
  43. Stéphane Courtois, Mark Kramer. Livre noir du Communisme: crimes, terreur, répression. Harvard University Press, 1999. p. 206. ISBN 0-674-07608-7 – "300,000 known deaths in the camps from 1934 to 1940."
  44. Courtois and Kramer (1999), Livre noir du Communisme, p.239.
  45. Chamberlain, Lesley (27 April 2003). "Dark side of the moon". Arlindo-correia.org. Retrieved 11 June 2019. Today's major industrial cities of Noril'sk, Vorkuta, Kolyma and Magadan, were camps originally built by prisoners and run by ex-prisoners.
  46. "Altai: Saving the Pearl of Siberia". Pacific Environment. Archived from the original on 22 March 2007. Retrieved 30 November 2006.
  47. Lioubimtseva E.U., Gorshkov S.P. & Adams J.M.; A Giant Siberian Lake During the Last Glacial: Evidence and Implications; Oak Ridge National laboratory Archived 13 December 2006 at the Wayback Machine
  48. C. Michael Hogan. 2011. Taiga. eds. M.McGinley & C.Cleveland. Encyclopedia of Earth. National Council for Science and the Environment. Washington DC
  49. Meyerhof, A. A., 1980, "Geology and Petroleum Fields in Proterozoic and Lower Cambrian Strata, Lena-Tunguska Petroleum Province, Eastern Siberia, USSR", in Giant Oil and Gas Fields of the Decade: 1968–1978, AAPG Memoir 30, Halbouty, M. T., editor, Tulsa: American Association of Petroleum Geologists, ISBN 0891813063
  50. "Novosibirsk climate". Worldclimate.com. 4 February 2007. Retrieved 15 May 2010.
  51. "Omsk climate". Worldclimate.com. 4 February 2007. Retrieved 15 May 2010.
  52. "Kazachengoye climate". Worldclimate.com. 4 February 2007. Retrieved 15 May 2010.
  53. Badkar, Mamta (6 February 2014). "This Tiny Town In Russia Is The Most Miserable Place In The World". Business Insider. Retrieved 28 August 2021.
  54. Гидрометцентр России (in Russian). Archived from the original on 27 June 2008. Retrieved 8 January 2009.
  55. Ian Sample, "Warming hits 'tipping point'". The Guardian, 11 August 2005.
  56. Connor, Steve (23 September 2008). "Exclusive: The methane time bomb". The Independent. Retrieved 3 October 2008.
  57. N. Shakhova, I. Semiletov, A. Salyuk, D. Kosmach, and N. Bel'cheva (2007), Methane release on the Arctic East Siberian shelf, Geophysical Research Abstracts, 9, 01071.
  58. Sergey A. Zimov (6 May 2005): "Pleistocene Park: Return of the mammoths' ecosystem" In: Science, pages 796–798. Article also to be found in www.pleistocenepark.ru/en/ – Materials. Archived 3 November 2016 at the Wayback Machine Retrieved 5 May 2013.
  59. "Northern Hazelhen (Tetrastes bonasia). Photo Gallery.Birds of Siberia". sibirds.ru. Retrieved 18 June 2020.
  60. "Siberian Grouse (Falcipennis falcipennis). Photo Gallery.Birds of Russian Far East". fareastru.birds.watch. Retrieved 18 June 2020.
  61. "Northern Black Grouse (Lyrurus tetrix). Photo Gallery.Birds of Siberia". sibirds.ru. Retrieved 18 June 2020.
  62. "Black-billed Capercaillie (Tetrao urogalloides). Photo Gallery.Birds of Siberia". sibirds.ru. Retrieved 18 June 2020.
  63. "Western Capercaillie (Tetrao urogallus). Photo Gallery.Birds of Siberia". sibirds.ru. Retrieved 18 June 2020.
  64. "Willow Ptarmigan (Lagopus lagopus). Photo Gallery.Birds of Siberia". sibirds.ru. Retrieved 18 June 2020.
  65. "Rock Ptarmigan (Lagopus muta). Photo Gallery.Birds of Siberia". sibirds.ru. Retrieved 18 June 2020.
  66. Valerius Geist (January 1998). Deer of the World: Their Evolution, Behaviour, and Ecology. Stackpole Books. p. 211. ISBN 978-0-8117-0496-0. Retrieved 30 January 2016.
  67. Nyambayar, B.; Mix, H.; Tsytsulina, K. (2015). "Moschus moschiferus". IUCN Red List of Threatened Species. 2015: e.T13897A61977573. doi:10.2305/IUCN.UK.2015-2.RLTS.T13897A61977573.en. Retrieved 12 November 2021. Database entry includes a brief justification of why this species is of vulnerable.
  68. Uphyrkina, O.; Miquelle, D.; Quigley, H.; Driscoll, C.; O'Brien, S. J. (2002). "Conservation Genetics of the Far Eastern Leopard (Panthera pardus orientalis)" (PDF). Journal of Heredity. 93 (5): 303–11. doi:10.1093/jhered/93.5.303. PMID 12547918. Archived from the original (PDF) on 4 February 2016. Retrieved 30 January 2016.
  69. Miquelle, D.; Darman, Y.; Seryodkin, I (2011). "Panthera tigris ssp. altaica". IUCN Red List of Threatened Species. 2011: e.T15956A5333650. doi:10.2305/IUCN.UK.2011-2.RLTS.T15956A5333650.en. Retrieved 12 November 2021.
  70. Garshelis, D.; Steinmetz, R. (2020). "Ursus thibetanus". IUCN Red List of Threatened Species. 2020: e.T22824A166528664. doi:10.2305/IUCN.UK.2020-3.RLTS.T22824A166528664.en. Retrieved 12 November 2021.
  71. McLellan, B.N.; Proctor, M.F.; Huber, D.; Michel, S. (2017). "Ursus arctos". IUCN Red List of Threatened Species. 2017: e.T41688A121229971. doi:10.2305/IUCN.UK.2017-3.RLTS.T41688A121229971.en. Retrieved 12 November 2021.
  72. Farjon, A. (2013). "Pinus pumila". IUCN Red List of Threatened Species. 2013: e.T42405A2977712. doi:10.2305/IUCN.UK.2013-1.RLTS.T42405A2977712.en.
  73. A. Farjon (2013). "Picea obovata". IUCN Red List of Threatened Species. 2013: e.T42331A2973177. doi:10.2305/IUCN.UK.2013-1.RLTS.T42331A2973177.en.
  74. Малый энциклопедический словарь Брокгауза и Ефрона (The Brockhaus and Efron Encyclopedic Dictionary, in Russian)
  75. Сибирь- Словарь современных географических названий (in Russian)
  76. "Siberia". Archived from the original on 24 August 2000. Retrieved 4 June 2008., The Columbia Encyclopedia, Sixth Edition
  77. "Siberian separatism: whether federal center can hold remote regions – Robert Lansing Institute". lansinginstitute.org. 27 October 2020. Archived from the original on 1 September 2022. Retrieved 22 June 2022.
  78. Douglas Causey. "Russian Far East – Siberia Class". www.siberiaclass.org. Archived from the original (Lecture) on 20 October 2021.
  79. Statistics on the Development of Gas Fields in Western Siberia, Daily Questions on Energy and Economy
  80. Schlindwein, Simone (26 August 2008). "The City Built on Oil: EU-Russia Summit Visits Siberia's Boomtown". Spiegel Online. Spiegel. Retrieved 8 August 2014.
  81. "Norilsk raises 2010 nickel output forecast". Reuters. 29 January 2010. Retrieved 8 August 2014.
  82. "FAO  National Aquaculture Sector Overview (NASO)". 16 January 2005. Retrieved 14 January 2016.
  83. Overland, Indra; Kjaernet, Heidi (2009). Russian renewable energy: The potential for international cooperation. Ashgate.
  84. Overland, Indra (2011). "The Siberian Curse: A Blessing in Disguise for Renewable Energy?". Sibirica. 9 (2): 1–20. doi:10.3167/sib.2010.090201 – via ResearchGate.
  85. "Валовой региональный продукт по субъектам Российской Федерации в 2016–2021гг" (in Russian).
  86. "Google Translate". Retrieved 14 April 2016.
  87. "Google Translate". Retrieved 14 April 2016.
  88. Photo with no context
  89. "Информация о стадионе "КЛМ стадиона "Химик", Кемерово – Реестр – Федерация хоккея с мячом России". rusbandy.ru. Retrieved 14 April 2016.
  90. "Информация о стадионе "Арена "Ерофей", Хабаровск – Реестр – Федерация хоккея с мячом России". rusbandy.ru. Retrieved 14 April 2016.
  91. "Google Translate".
  92. "Национальный состав населения". Federal State Statistics Service. Retrieved 30 December 2022.
  93. Including Siberian Federal District, Tyumen Oblast, Kurgan Oblast, Zabaykalsky Krai, Buryatia and Sakha.
  94. "Census 2010 official results (Russian) Archived 28 February 2013 at the Wayback Machine"
  95. "Ukrainians in Russia's Far East try to maintain community life". The Ukrainian Weekly. 4 May 2003. Archived 4 March 2016 at the Wayback Machine
  96. "Archived copy". Archived from the original on 27 February 2002. Retrieved 21 February 2003.{{cite web}}: CS1 maint: archived copy as title (link)
  97. World Directory of Minorities and Indigenous Peoples – Russian Federation: Buryats.
  98. World Directory of Minorities and Indigenous Peoples – Russian Federation: Yakuts.
  99. Gutman, Garik (2012). Regional Environmental Changes in Siberia and Their Global Consequences. Springer Netherlands. p. 20. ISBN 9789400745698.
  100. "Official website of the city of Novosibirsk". English.novo-sibirsk.ru. Retrieved 25 May 2022.
  101. Arnold, Thomas Walker (1896). The Preaching of Islam: A History of the Propagation of the Muslim Faith. Westminster: Archibald Constable and Company. pp. 206–207. Retrieved 11 October 2015. Of the spread of Islam among the Tatars of Siberia, we have a few particulars. It was not until the latter half of the sixteenth century that it gained a footing in this country, but even before this period Muhammadan missionaries had from time to time made their way into Siberia with the hope of winning the heathen population over to the acceptance of their faith, but the majority of them met with a martyr's death. When Siberia came under Muhammadan rule, in the reign of Kuchum Khan, the graves of seven of these missionaries were discovered [...]. [...] Kuchum Khan [...] made every effort for the conversion of his subjects, and sent to Bukhara asking for missionaries to assist him in this pious undertaking.
  102. "Planting Jewish roots in Siberia". Fjc.ru. 24 May 2004. Archived from the original on 27 August 2009. Retrieved 15 May 2010.
  103. "Why some Jews would rather live in Siberia than Israel", The Christian Science Monitor. 7 June 2010
  104. Hoppál 2005:13
  105. "Secrets of Siberian Shamanism | New Dawn : The World's Most Unusual Magazine". www.newdawnmagazine.com. 16 May 2013. Retrieved 9 January 2017.
  106. Rasputin, V.; Winchell, M.; Mikkelson, G. (1997). Siberia, Siberia. Northwestern University Press. pp. 322–323. ISBN 978-0-8101-1575-0.
  107. Motarjemi, Yasmine; Moy, Gerald; Todd, E. C. D. (2013). Encyclopedia of Food Safety. Amsterdam: Elsevier Science, Academic Press. p. 176. ISBN 978-0-12-378613-5.

Bibliography
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