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| Physical Anthropology The scientific study of the mechanisms of biological evolution, human adaptability and variation, and the fossil record of human evolution. |
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Found here
Quote:
Interesting comments in the same thread about the genetic relations: Quote:
http://forum.skadi.net/showthread.php?t=43269 and The Imazighen (Berbers)
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relationship between Guanches, "Blond" riffian berbers and UP Europe Cro magnonids seems to be well known from long date. Coon said that Isolated Borreby & Brunn populations still remained in North Africa and Canary Islands. BTW and just for info seems that the hair colour in mummies is not always the original one (though in the case of the guanche mummies it is most likely to have been the life colour). I read in several articles that human hair contains both peoh and eumelanin but eumelanin is less stable in front of environmental, humidity and climatic canches and is the first to go, the most lingering/enduring being the melanin responsible of red hair. That would the reason why why might found redheadmummies even in places where it would be the less spected (seem that several inca mummies with andid features presented a reddish hair tone) |
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I assume that Guanches and riffian berberes come from Europe into N Africa at the turn of the last glaciar period.Then they sailed at a moment to Canary islands. What I wander is if there has been any genetic drift/differenciation between W Europe cro magnonids and N AFRCAN-Canarian ones and how developped where their sailing skills when they passed through the Canary Islands; did they have a quite specialized shipping knowledge, more or less as the more recent megalithics had as it is usually assumed, or rather they come in a patera like vessel? one must bear in mind that Australia was populated much before the Canary Islands and at a time were homo sapiens intelectual faculties were less developped for a similar distance to cross by sea, in spite of the lower sea level of the epoch (well that rather depends if the mean population stream arrived during a glaciar period or during an interglaciar one) |
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