Pre-Finno-Ugric substrate in the context of "Paleo-Laplandic"

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⭐ Core Definition: Pre-Finno-Ugric substrate

Pre-Finno-Ugric substrate refers to substratum loanwords from unidentified non-Indo-European and non-Uralic languages that are found in various Finno-Ugric languages, most notably Sámi. The presence of Pre-Finno-Ugric substrate in Sámi languages was demonstrated by Ante Aikio. Janne Saarikivi [fi] points out that similar substrate words are present in Finnic languages as well, but in much smaller numbers. The proposed substrate influence in Finnic may have been related either by borrowing or a direct genetic relationship to the languages that influenced Sámi.

Borrowing to Sámi from Paleo-Laplandic probably still took place after the completion of the Great Sámi Vowel Shift. Paleo-Laplandic likely became extinct about 1500 years ago.

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Pre-Finno-Ugric substrate in the context of Lake Saimaa

Saimaa (/ˈsmɑː/ SY-mah, Finnish: [ˈsɑi̯mɑː]; Swedish: Saimen) is a lake located in the Finnish Lakeland area in southeastern Finland. With a surface area of approximately 4,279 square kilometres (1,652 sq mi), it is the largest lake in Finland, and the fourth-largest natural freshwater lake in Europe.

The name Saimaa likely comes from a non-Uralic, non-Indo European substrate language. Alternatively, it has been proposed that the name may be connected to the Sami word sápmi.

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