Карта западно сибирского моря

Особенности древнего Западно-Сибирского моря и его карта

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Ancient West Siberian Sea Features

The ancient West Siberian Sea was a lake formed during the last (Zyryan) glaciation, approximately 40.1 thousand years ago [2] . It reached a height of about 125 meters above the contemporary sea level and disappeared during the Karginsk (middle Zyryan) interglacial period, around 31-32 thousand years ago [2] . The ancient West Siberian Sea was divided into two parts: the Jurassic and Cretaceous periods, each of which was further divided into several stages [4] .

West Siberian Sea Map

The map of the West Siberian Sea consists of 15 maps, which are included in the Atlas of Lithologic-Paleogeographic Maps of the USSR [4] . These maps cover various time periods and stages, such as the Bajos, Bath, and Callovian periods [4] .

West Siberian Plain

The West Siberian Plain extends from the shores of the Kara Sea to the steppes of Kazakhstan and from the Ural Mountains in the west to the Central Siberian Plateau in the east [5] . In Russia, there are no more extensive plains with such a weakly intersected relief and such small fluctuations in relative heights [5] . The elevation above sea level reaches more than 200 meters, with about half of the territory lying below the level of 100 meters [5] . The weak drainage of the area in its central part led to the formation of the ancient West Siberian Sea [5] .

Seima-Turbino Phenomenon

The Seima-Turbino phenomenon refers to a trade network, primarily consisting of weaponry, which developed as the Abashevo and Sintashta cultures interacted with the populations of the Taiga [6] . This network played a crucial role in the interaction between Uralic-speaking peoples and Indo-Iranian-speaking peoples, as well as other groups across Eurasia [6] .

West Siberian Glacial Lake

The West Siberian Glacial Lake was situated on the West Siberian Plain, with a maximum surface area of more than 750,000 km² [9] . The lake formed when the Arctic Ocean outlets for the Ob and Yenisei rivers were blocked by the Barents-Kara Ice Sheet [9] . The lake’s drainage patterns have been postulated, and it is possible that water from the Selenga River and Lake Baikal may have drained to the Mediterranean Sea through a circuitous route [9] . The lake existed in two phases, with dates of 90-80 ka and 60-50 ka, and elevations of 60 m and 45 m, respectively [9] .

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Source: «West Siberian Glacial Lake — Wikipedia» (from web, en.wikipedia.org)

• West Siberian Glacial Lake
  • Situated on the West Siberian Plain
  • Maximum extent of the lake’s surface area was more than 750,000 km2
  • Postulated drainage patterns exist
  • Formed when the Arctic Ocean outlets for each of the Ob and Yenisei rivers were blocked by the Barents-Kara Ice Sheet
  • Water from the Selenga River and Lake Baikal may have drained to the Mediterranean Sea through a circuitous route
  • Date: 90-80 ka, 60-50 ka
  • Elevation: 60 m, 45 m
  • Area: 610,000 km2, 881,000 km2
  • Volume: 15,000 km3, 32,000 km3
  • Average depth: 24 m, 36 m
  • Baikal seal
  • Turgai Sea or West Siberian Sea
  • Paratethys

  Source: «What is the Seima-Turbino phenomenon? Is this c. » (from reddit, r/IndoEuropean)

  • The Seima-Turbino phenomenon was not a material culture, but a trade network
    • The core region is essentially just a bunch of burials which contain the distinct Seima-Turbino weaponry
    • There is a wide distribution of the weapons outside of that core region
    • It developed as the Abashevo and Sintashta cultures started to interact with the populations of the Taiga
    • It was a trade network mainly consisting of weaponry, and during the period there was significant militarization and conflicts
    • It is the most likely explanation for how early Uralic speaking peoples reached Europe and had interactions with Indo-Iranian speaking peoples
    • West Siberian ancestry is mostly direct ANE ancestry
    • Uralic speakers have a lot of said ANE ancestry
    • It was not just traded between Uralic and Indo-Iranian peoples, a plethora of other peoples had these weapons
    • West Siberian peoples had ST weaponry as well
    • The Altai region was one of the hotspots and artefacts have been found in Greece all the way to Central China
    • People had more reasons and resources to migrate or expand, likely travelling down south via rivers in Russia, and from there to other directions
    • It is too late to be formative to PIE
    • Steppe culture might have been a sort of cline given the geography of Eurasia and mobility of the people

    Source: «All West Russian regional and superregional foc. » (from reddit, r/TNOmod)

    • Komi regional and superregional focus trees
      • Link to a Reddit post containing all Komi paths
      • Link to a Reddit post containing all West Siberian regional and superregional paths
      • Link to a Reddit post containing all Central Siberian regional and superregional paths
      • Link to a Reddit post containing all Far Eastern regionals and superregionals
      • User suggests England could be great
      • Link to a Discord attachment of a map
      • Comment about Tukhachevsky being cringe

      Source: «West Siberian Glacial Lake — Wikiwand» (from web, www.wikiwand.com)

      Source: «Paleogene events in Central Eurasia: their role. » (from web, www.researchgate.net)

      What is the significance of the 15 maps of the West-Siberian Sea in the Atlas of Lithology-Paleographic Maps of the USSR?

      What are the environmental impacts of the West-Siberian Sea during the Pleistocene period?

      What are the main features of the ancient West-Siberian Sea?

      What were the climatic conditions during the Ermakovsky (early Zyrjan) glaciation?

      What assumptions about the paleogeography of the West-Siberian Sea are made in this paper?

      Source: «Osobennosti razvitiia rel’efa Zapadno-Sibirskoi. » (from web, otherreferats.allbest.ru)

      • Особенности развития рельефа Западно-Сибирской равнины
        • Равнина простирается от берегов Карского моря до степей Казахстана и от Урала на западе до Среднесибирского плоскогорья на востоке
        • В России нет больше таких обширных равнин со столь слабо пересеченным рельефом и такими небольшими колебаниями относительных высот
        • Отметки над уровнем моря достигают более 200 м; около половины ее территории лежит ниже уровня 100 м
        • Слабой дренированности территории в ее преде

        Source: «15 kart Zapadno-Sibirskogo moria (mezozoi): kod. » (from web, kodeam.livejournal.com)

        • Особенности древнего Западно-Сибирского моря
          • Древнее Западно-Сибирское море было озером во времена последнего (зырянского) оледенения.
          • Оно было разделено на две части: юрский и меловой периоды.
          • Каждый период был дальше разделен на несколько ярусов.
          • Карта Западно-Сибирского моря включает в себя 15 карт.
          • Они представлены в Атласе литолого-палеографических карт СССР.
          • Включают в себя байосский, батский, ке

          Source: «Zapadno-Sibirskoe ozero — Vikipediia» (from web, ru.wikipedia.org)

          • Западно-Сибирское озеро-море
            • Образовалось во время ермаковского (раннезырянского) оледенения 40,1 тыс. лет назад
            • Достигало высоты примерно 125 м над современным уровнем моря
            • Исчезло в период каргинского (среднезырянского) межледниковья ориентировочно 31—32 тыс. лет назад
            • Впервые Енисейский приледниковый внутриконтинентальный бассейн был отмечен в 1952 году
            • Концепцию одновременного существования трёх самостоятельных ледниково-подпрудных о

            Source: «(PDF) PALEOGEOGRAFIIa ZAPADNO-SIBIRSKOGO OSADOC. » (from web, www.researchgate.net)

            Source: «15 kart Zapadno-Sibirskogo moria (mezozoi) | Ka. » (from web, ru.pinterest.com)

            What are the features of the Ancient West Siberian Sea and what does its map look like?

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