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Concept
Maykop culture
Summary
The Maykop culture (майкоп, mɐjˈkop, scientific transliteration: Majkop,), c. 3700 BC–3000 BC, was a major Bronze Age archaeological culture in the western Caucasus region.
It extends along the area from the Taman Peninsula at the Kerch Strait to near the modern border of Dagestan and southwards to the Kura River. The culture takes its name from a royal burial, the Maykop kurgan in the Kuban River valley.
According to genetic studies on ancient DNA published in 2018, the Maykop population came from the south, from Imereti, and was descended from the Chalcolithic farmers known as Darkveti-Meshoko who first colonized the north side of the Caucasus. Maykop is therefore the "ideal archaeological candidate for the founders of the Northwest Caucasian language family".
In the south, the Maykop culture bordered the approximately contemporaneous Kura-Araxes culture (3500—2200 BC), which extends into the Armenian Plateau and apparently influenced it. To the north is the Yamna culture, including the Novotitorovka culture (3300—2700), which it overlaps in territorial extent. It is contemporaneous with the late Uruk period in Mesopotamia.
The Kuban River is navigable for much of its length and provides an easy water-passage via the Sea of Azov to the territory of the Yamna culture, along the Don and Donets River systems. The Maykop culture was thus well-situated to exploit the trading possibilities with the central Ukraine area.
New data revealed the similarity of artifacts from the Maykop culture with those found recently in the course of excavations of the ancient city of Tell Khazneh in northern Syria, the construction of which dates back to 4000 BC.
Radiocarbon dates for various monuments of the Maykop culture are from 3950 - 3650 - 3610 - 2980 calBC.
After the discovery of the Leyla-Tepe culture in the 1980s, some links were noted with the Maykop culture.
The Leyla-Tepe culture is a culture of archaeological interest from the Chalcolithic era. Its population was distributed on the southern slopes of the Central Caucasus (modern Azerbaijan, Agdam District), from 4350 until 4000 B.
Official source
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