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Prehistory of Siberia
The Prehistory of Siberia is marked by several archaeologically distinct cultures. In the Chalcolithic, the cultures of western and southern Siberia were pastoralists, while the eastern taiga and the tundra were dominated by hunter-gatherers until the Late Middle Ages and even beyond. Substantial changes in society, economics and art indicate the development of nomadism in the Central Asian steppes in the first millennium BC.
Scholarly research of the archaeological background of the region between the Urals and the Pacific began in the reign of Peter the Great (1682-1725), who ordered the collection of Scythian gold hoards and thereby rescued the contents of several robbed graves before they were melted down. During his reign, several expeditions were charged with the scientific, anthropological and linguistic research of Siberia, including the Second Kamchatka Expedition of the Danish-born Russian Vitus Bering (1733-1743). Scholars also took an interest in archaeology and carried out the first archaeological excavations of Siberian kurgans. After a temporary reduction of interest in the first half of the nineteenth century, archaeological research in Siberia reached new heights in the late nineteenth century. Excavations were particularly intense in South Siberia and Central Asia. The results of the October Revolution 1917 created different, often restricted, conditions for archaeological research, but led to even larger projects, especially rescue excavations as a result of gigantic building projects. Eventually, even remote areas of the Soviet Union such as Sakha and Chukotka, were archaeologically explored. After the Second World War, these developments continued. Following the Collapse of the Soviet Union in 1991, much more intensive collaboration with the west became possible.
Siberia is characterised by a great deal of variety in climate, vegetation, and landscape. In the west, it is bordered by the Ural Mountains. From there, the west Siberian lowlands extend to the east, all the way to the river Yenisei. Beyond this are the central Siberian highlands which are bordered on the east by the basin of the Lena River, beyond that are the northeast Siberian highlands. Siberia is bordered on the south by a rough chain of mountains and to the southwest by the hills of the Kazakh border. The climate is very variable. Yakutia, northeast of the Lena, is among the coldest places on Earth, but every year temperatures may vary for more than 70°C, from as low as −50°C in winter to over +20°C in summer. The rainfall is very low. This is true of the southwest as well, where steppes, deserts and semi-deserts border on one another.
Agriculture is only possible in Siberia without artificial irrigation today between 50° and 60° north. The climatic situation is responsible for the different biomes of the region. In the northernmost section, there is tundra with minimal vegetation. The largest part of Siberia, aside from the mountainous regions, is taiga, northern coniferous forests. In the southwest this becomes forested steppe, and even further south it transitions to grass steppes and the central Asian desert. Before the beginning of the Holocene about 12,000 years ago, the situation was different. During the Weichselian glaciation (from before 115,000 years ago until 15,000 years ago), the tundra extended much further south and an ice sheet covered the Urals and the area to the east of the lower Yenisei.
Late Paleolithic southern Siberians appear to be related to Paleolithic Europeans and the Paleolithic Jōmon people of Japan. Various scholars point out similarities between the Jōmon and Paleolithic and Bronze Age Siberians. A genetic analyses of HLA I and HLA II genes as well as HLA-A, -B, and -DRB1 gene frequencies links the Ainu people and some Indigenous peoples of the Americas, especially populations on the Pacific Northwest Coast such as Tlingit, to Paleolithic southern Siberians.
Finds from the Lower Paleolithic appear to be attested between east Kazakhstan and Altai. The burial of a Neanderthal child found in 1938 shows similarities with the Mousterian of Iraq and Iran. In the Upper Palaeolithic, by contrast, most remains are found in the Urals, where, among other things, rock carvings depicting mammoths are found, in Altai, on the upper Yenissei, west of Lake Baikal and around 25,000 on the shore of the Laptev Sea, north of the Arctic Circle. The remains of huts have been found in the settlement of Mal'ta near Irkutsk. Sculptures of animals and women (Venus figurines) recall the European Upper Palaeolithic. The Siberian Palaeolithic continues well into the European Mesolithic. In the postglacial period, the taiga developed. Microliths, which are common elsewhere, have not been found.
In North Asia, the Neolithic (c. 5500–3400 BC) is mostly a chronological term, since there is no evidence for agriculture or even pastoralism in Siberia during the central European Neolithic. However, the Neolithic cultures of North Asia are distinguished from the preceding Mesolithic cultures and far more visible as a result of the introduction of pottery.
Southwest Siberia reached a Neolithic cultural level during the Chalcolithic, which began here towards the end of the fourth millennium BC, which roughly coincided with the introduction of copper–working. In the northern and eastern regions, there is no detectable change.
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Prehistory of Siberia
The Prehistory of Siberia is marked by several archaeologically distinct cultures. In the Chalcolithic, the cultures of western and southern Siberia were pastoralists, while the eastern taiga and the tundra were dominated by hunter-gatherers until the Late Middle Ages and even beyond. Substantial changes in society, economics and art indicate the development of nomadism in the Central Asian steppes in the first millennium BC.
Scholarly research of the archaeological background of the region between the Urals and the Pacific began in the reign of Peter the Great (1682-1725), who ordered the collection of Scythian gold hoards and thereby rescued the contents of several robbed graves before they were melted down. During his reign, several expeditions were charged with the scientific, anthropological and linguistic research of Siberia, including the Second Kamchatka Expedition of the Danish-born Russian Vitus Bering (1733-1743). Scholars also took an interest in archaeology and carried out the first archaeological excavations of Siberian kurgans. After a temporary reduction of interest in the first half of the nineteenth century, archaeological research in Siberia reached new heights in the late nineteenth century. Excavations were particularly intense in South Siberia and Central Asia. The results of the October Revolution 1917 created different, often restricted, conditions for archaeological research, but led to even larger projects, especially rescue excavations as a result of gigantic building projects. Eventually, even remote areas of the Soviet Union such as Sakha and Chukotka, were archaeologically explored. After the Second World War, these developments continued. Following the Collapse of the Soviet Union in 1991, much more intensive collaboration with the west became possible.
Siberia is characterised by a great deal of variety in climate, vegetation, and landscape. In the west, it is bordered by the Ural Mountains. From there, the west Siberian lowlands extend to the east, all the way to the river Yenisei. Beyond this are the central Siberian highlands which are bordered on the east by the basin of the Lena River, beyond that are the northeast Siberian highlands. Siberia is bordered on the south by a rough chain of mountains and to the southwest by the hills of the Kazakh border. The climate is very variable. Yakutia, northeast of the Lena, is among the coldest places on Earth, but every year temperatures may vary for more than 70°C, from as low as −50°C in winter to over +20°C in summer. The rainfall is very low. This is true of the southwest as well, where steppes, deserts and semi-deserts border on one another.
Agriculture is only possible in Siberia without artificial irrigation today between 50° and 60° north. The climatic situation is responsible for the different biomes of the region. In the northernmost section, there is tundra with minimal vegetation. The largest part of Siberia, aside from the mountainous regions, is taiga, northern coniferous forests. In the southwest this becomes forested steppe, and even further south it transitions to grass steppes and the central Asian desert. Before the beginning of the Holocene about 12,000 years ago, the situation was different. During the Weichselian glaciation (from before 115,000 years ago until 15,000 years ago), the tundra extended much further south and an ice sheet covered the Urals and the area to the east of the lower Yenisei.
Late Paleolithic southern Siberians appear to be related to Paleolithic Europeans and the Paleolithic Jōmon people of Japan. Various scholars point out similarities between the Jōmon and Paleolithic and Bronze Age Siberians. A genetic analyses of HLA I and HLA II genes as well as HLA-A, -B, and -DRB1 gene frequencies links the Ainu people and some Indigenous peoples of the Americas, especially populations on the Pacific Northwest Coast such as Tlingit, to Paleolithic southern Siberians.
Finds from the Lower Paleolithic appear to be attested between east Kazakhstan and Altai. The burial of a Neanderthal child found in 1938 shows similarities with the Mousterian of Iraq and Iran. In the Upper Palaeolithic, by contrast, most remains are found in the Urals, where, among other things, rock carvings depicting mammoths are found, in Altai, on the upper Yenissei, west of Lake Baikal and around 25,000 on the shore of the Laptev Sea, north of the Arctic Circle. The remains of huts have been found in the settlement of Mal'ta near Irkutsk. Sculptures of animals and women (Venus figurines) recall the European Upper Palaeolithic. The Siberian Palaeolithic continues well into the European Mesolithic. In the postglacial period, the taiga developed. Microliths, which are common elsewhere, have not been found.
In North Asia, the Neolithic (c. 5500–3400 BC) is mostly a chronological term, since there is no evidence for agriculture or even pastoralism in Siberia during the central European Neolithic. However, the Neolithic cultures of North Asia are distinguished from the preceding Mesolithic cultures and far more visible as a result of the introduction of pottery.
Southwest Siberia reached a Neolithic cultural level during the Chalcolithic, which began here towards the end of the fourth millennium BC, which roughly coincided with the introduction of copper–working. In the northern and eastern regions, there is no detectable change.