The question of when humans first entered the Americas (the "New World") and how they arrived has been debated for centuries, and will probably continue to be for many more years to come in the anthropological community. A number of theories have been proposed over the years that explain the migration into the Americas, but as new data is recovered, these theories are continually restructured. The following is a basic look at two of the more popular models of migration to the New World.
To start things off with a simple and broad approach, the variety of models have fallen in place between two different camps. One school of thought believes in a “short chronology,” believing that the first movement into the New World occurred no earlier than 14,000 – 16,000 years ago. On the other hand, the “long chronology” camp posits that people entered the hemisphere at a much earlier date, theorizing the possibility of migration 20,000 years ago or earlier.
Their South American counterparts, on the other hand, don’t share this consistency and have a large diversity in cultural patterns. Therefore, South American archaeologists didn’t believe the Clovis model applied in the Southern Hemisphere. This brought about new theories that were developed to explain prehistoric sites that didn’t fit into the Clovis tool techno-complex in South America. However, there is now a growing effort to develop a Pan-American colonization model that integrates both North and South American archaeological records.
Recent evidence from molecular genetics suggests that the entire Amerindian population of the Americas may be derived from an effective founding population that could have been as small as 80 (Source: Hey, 2005).
A recent discovery of a very old site (pre-Clovis) indicates that migration to the Americas occurred much earlier (before the Bering Strait was exposed).
At a site named "Topper" along the Savannah River near Allendale, South Carolina by University of South Carolina archaeologist Dr. Albert Goodyear have found traces of carbon among human artifacts. The charcoal material has been radiocarbon dated by the University of California at Irvine Laboratory to be at least 50,000 years old. This indicates the presence of humans well before the last Ice Age. Other recent pre-Clovis sites have been found in South America.
The Pacific coastal model proposes that people reached South America before North America following a pacific route of water travel. Support for this argument is based on sites such as Monte Verde and Tiama-Tiama. Monte Verde consists of two cultural components. The youngest layer is radiocarbon dated at 12,500 years, while the older component possibly dates back as far as 33,000 B.P. However, the older dates associated with the site are still debated.
Some archaeologists have proposed that peoples of Oceania or southeast Asia crossed the Pacific Ocean and arrived in South America long before the Siberian hunter-gatherers. These hypothetical Pre-Siberian American Aborigines are claimed to have overspread much of South America before being nearly exterminated by the Siberian migrants coming from the north.
Other coastal models deal specifically with the peopling of the Northwest Coast. Carlson (1990 in Matson and Coupland, 1995:61-61), argues for a coastal migration from Alaska pre-10,000 B.P. that predates the migration of Clovis people moving south through an ice-free corridor located near the continental divide (Matson & Coupland, 1995:64). According to Matson and Coupland (1995) the New World was populated by a people, later known as Clovis, who moved south from Alaska through an ice free corridor located between modern British Columbia and Alberta. As the ice sheets began to melt it became possible for these riverine adapted peoples to move west to the Northwest coast (Ibid). A second migration of the Denali culture at around 10,700 b.p. brought peoples down the coast from Alaska (Matson & Coupland, 1995). Carlson (Ibid.) hypothesizes that a population with a maritime adaptation would have travelled south from Alaska down the coastal islands by watercraft, settling as the ice receded, then moving up rivers to the interior. Carlson argues that this would account for the earliest components at Ground Hog Bay in SE Alaska and Namu, about 800 km south of Ground Hog Bay near modern Bella Colla. The earliest component at Ground Hog Bay dates to 10,180 +/- 800 b.p. and contains mostly biface fragments (Matson & Coupland, 1995:62). Namu's earliest component dates from around 9700 b.p. and contains remains of a pebble tool tradition (Ibid). However compelling the Namu and Ground Hog Bay data is, the dates recovered do not discount Matson and Coupland's (1995) ice free corridor hypothesis. According to the Matson and Coupland (1995) dual migration hypothesis, Namu and Ground Hog bay represent a second migration while the initial migration route south was through the ice free corridor. Part of the difficulty is the lack of site data prior to 10,000 b.p. as well as the limited number of archaeological investigations into the coastal migration model. Other factors affecting migration models are sea level changes and the question of available land mass. Was there enough ice free land to support migrating groups of people prior to 10,000 years b.p.? What resources if any would be available and what were the technological capabilities of the migrating populations?
Evidence from Haida Gwaii, also known as the Queen Charlotte Islands in British Columbia, provides some data about food and land resources during the last glacial maximum. Fedje and Christensen (1999) have identified several sites on Haida Gwaii that date to post 9000 b.p. (642). Their data suggests that there are a number of submerged sites just beyond the shorelines of Haida Gwaii (Fedje & Christensen, 1999). Paleoecological evidence suggests that travel along the coast would have been possible between 13000 and 11000 b.p. as the ice sheets began retreating (Matson & Coupland, 1995:64). Between 13000 and 10500 b.p. Haida Gwaii had more than double its current landmass (Fedje & Christensen, 1999:638). This area was flooded as the ice sheets began to melt between 11000 and 9000 b.p. (Ibid). Therefore any evidence of human occupation would now be below sea level. Conversely, older sites that are located near modern shorelines would have been approximately 15m from the coast (Ibid). The antiquity of the lithic scatters that Fedje and Christensen (1999) have reported finding in intertidal zones along the Haida Gwaii coast is suggestive of early human occupation of the area.
Fedje and Christensen (1999) support Carlson (1990), and Fladmark's (1975, 1979 &1989) initial coastal migration model rather than the ice free corridor model proposed by Matson and Coupland (1995) through their investigations of intertidal zones on Haida Gwaii (in Fedje & Christensen, 1999:648). The coastal region was quite hospitable by 13000 b.p. to peoples with watercraft and a maritime adaptation (Fedje & Christensen, 1999:648). Furthermore, Fedje and Christensen (1999) argue that the coast was likely colonized before 13000 b.p. (648). This assertion is based largely on watercraft evidence from Japan and Australia before 13000 b.p. (Fedje & Christensen, 1999:648). It is speculated that if peoples elsewhere at 13000 b.p. could build boats then the possibility exists that migrating human groups could have produced watercraft to travel south from Beringia. There have been no water vessels recovered along the Northwest coast from this time. This may be due to poor preservation of organic materials or the fact that there were no boats built 13000 years ago. We can only infer water travel based on the presence of stone tools manufactured by humans found on island sites.
Other evidence comes from zooarchaeological finds along the Northwest coast. Goat remains as old as 12000 b.p. have been found on Vancouver Island, British Columbia as well as bear remains dating to 12,500 b.p. in the Prince of Whales Archipelago, British Columbia (Ibid.). This means that there were enough land mass and floral resources to support large land mammals. Therefore, human occupation was possible at this time. Fedje and Christensen (1999) state that further intertidal and underwater investigations will produce sites older than 11000 b.p. Coastal occupation prior to 13000 b.p. would allow for people to migrate further south and account for the early South American sites.
More compelling evidence comes from Bella Bella oral tradition recorded by Franz Boas in 1898. "In the beginning there was nothing but water and ice and a narrow strip of shoreline" (Boas, 1898:883 in Fedje & Christensen, 1999:635). This story most likely describes the Northwest coast during the last glacial maximum. It is interesting that this description survived in Bella Bella oral history up to Boas' time. This suggests that colonization of the Northwest coast occurred during the last ice age. Obviously the ice sheets left a significant impression if their description became part of the Bella Bella origin stories.
Works Cited Matson and Coupland. The Prehistory of the Northwest Coast. Academic Press. New York. 1995.
Fedje, & Christensen. Modeling Paleoshorelines and Locating Early Holocene Coastal Sites in Haida Gwaii. American Antiquity, Vol. 64, #4, 1999. Pp. 635-652.
Human migration | Modern human genetic history | History of North America | History of Central America | History of South America | Besiedlung Amerikas | Llegada del hombre a América | Théories du premier peuplement de l'Amérique | Intiaanien alkuperä
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"Models of migration to the New World".
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