Available scientific evidence indicates that humanity emerged from Africa over 100,000 years ago, yet did not arrive in the Americas until less than 20,000 years ago. Current understanding of the settlement of the Americas derives from advances in four interrelated disciplines: archaeology, Pleistocene geology, physical anthropology, and DNA analysis. While there is general agreement that the Americas were first settled from Asia, the pattern of migration, its timing, and the place(s) of origin in Asia of the peoples who migrated to the Americas remain unclear.[1] In the 2000s, researchers sought to use familiar tools to validate or reject established theories, such as Clovis first.[2] The archeological evidence suggests that the Paleo-Indians' first dispersal into the Americas occurred near the end of the last glacial period or, more specifically, what is known as the Last Glacial Maximum (LGM), around 16,500–13,000 years ago.[1]

The settlement of the Americas is of intense interest to archaeologists and anthropologists. Modern biochemical techniques, as well as the accumulation of archaeological and geological evidence, have shed progressively more light on the subject; however, significant questions remain unresolved.[3]

The environment during the latest Pleistocene

For an introduction to the radiocarbon dating techniques used by archaeologists and geologists, see radiocarbon dating.

Emergence and submergence of Beringia

Figure1. Submergence of the Beringian land bridge with post-LGM rise in eustatic sea level

During the Wisconsin Glaciation, varying portions of the Earth's water were stored as glacier ice. As water accumulated in glaciers, the volume of water in the oceans correspondingly decreased, resulting in lowering of the eustatic sea level. The variation of the eustatic sea level with time has been reconstructed using oxygen isotope analysis of deep sea cores, the dating of marine terraces, and high resolution oxygen isotope sampling from ocean basins and modern ice caps. A drop of eustatic sea level by about 60 m to 120 m lower than present-day levels, commencing around 30,000 years BP, caused the revealing of Beringia as a durable and extensive geographic feature connecting Siberia with Alaska.[4] With the rise of sea level after the Last Glacial Maximum (LGM), the Beringian land bridge was again submerged. Estimates of the final re-submergence of the Beringian land bridge based purely on present bathymetry of the Bering Strait and eustatic sea level curve place the event around 11,000 years BP (Figure 1). Ongoing research reconstructing Beringian paleogeography during deglaciation could change that estimate and possible earlier submergence could further constrain models of human migration into North America.[4]


The onset of the LGM after 30,000 years BP saw the expansion of alpine glaciers and continental ice sheets that blocked migration routes out of Beringia. By 21,000 years BP, and possibly thousands of years earlier, the Cordilleran and Laurentide ice sheets coalesced east of the Rocky Mountains, closing off a potential migration route into the center of North America.[5][6][7] Alpine glaciers in the coastal ranges and the Alaskan Peninsula isolated the interior of Beringia from the Pacific coast. Coastal alpine glaciers and lobes of Cordilleran ice coalesced into piedmont glaciers that covered large stretches of the coastline as far south as Vancouver Island and formed an ice lobe across the Straits of Juan de Fuca by 15,000 14C years BP (18,000 cal years BP).[8][9] Coastal alpine glaciers started to retreat around 19,000 [Calibration of radiocarbon dates|cal years] BP [10] while Cordilleran ice continued advancing in the Puget lowlands up to 14,000 14C years BP (16,800 cal years BP)[9] Even during the maximum extent of coastal ice, unglaciated refugia persisted on present-day islands, that supported terrestrial and marine mammals.[7] As deglaciation occurred, refugia expanded until the coast became ice-free by 15,000 cal years BP.[7] The retreat of glaciers on the Alaskan Peninsula provided access from Beringia to the Pacific coast by around 17,000 cal years BP.[11] The ice barrier between interior Alaska and the Pacific coast broke up starting around 13,500 14C years (16,200 cal years) BP.[8] The ice-free corridor to the interior of North America opened between 13,000 and 12,000 cal years BP.[5][6][7] Glaciation in eastern Siberia during the LGM was limited to alpine and valley glaciers in mountain ranges and did not block access between Siberia and Beringia.[4]

Climate and biological environments

The paleoclimates and vegetation of eastern Siberia and Alaska during the Wisconsin glaciation have been deduced from high resolution oxygen isotope data and pollen stratigraphy.[4][12][13] Prior to the LGM, climates in eastern Siberia fluctuated between conditions approximating present day conditions and colder periods. The pre-LGM warm cycles in Arctic Siberia saw flourishes of megafaunas.[4] The oxygen isotope record from the Greenland Ice Cap suggests that these cycles after about 45k years BP lasted anywhere from hundreds to between one and two thousand years, with greater duration of cold periods starting around 32k cal years BP.[4] The pollen record from Elikchan Lake, north of the Sea of Okhotsk, shows a marked shift from tree and shrub pollen to herb pollen prior to 26k 14C years BP, as herb tundra replaced boreal forest and shrub steppe going into the LGM.[4] A similar record of tree/shrub pollen being replaced with herb pollen as the LGM approached was recovered near the Kolyma River in Arctic Siberia.[13] The abandonment of the northern regions of Siberia due to rapid cooling or the retreat of game species with the onset of the LGM has been proposed to explain the lack of archaeosites in that region dating to the LGM.[13][14] The pollen record from the Alaskan side shows shifts between herb/shrub and shrub tundra prior to the LGM, suggesting less dramatic warming episodes than those that allowed forest colonization on the Siberian side. Diverse, though not necessarily plentiful, megafaunas were present in those environments. Herb tundra dominated during the LGM, due to cold and dry conditions.[12]

Coastal environments during the LGM were complex. The lowered sea level, and an isostatic bulge equilibrated with the depression beneath the Cordilleran Ice Sheet, exposed the continental shelf to form a coastal plain.[15] While much of the coastal plain was covered with piedmont glaciers, unglaciated refugia supporting terrestrial mammals have been identified on Haida Gwaii, Prince of Wales Island, and outer islands of the Alexander Archipelago.[12] The now-submerged coastal plain has potential for more refugia.[12] Pollen data indicate mostly herb/shrub tundra vegetation in unglaciated areas, with some boreal forest towards the southern end of the range of Cordilleran ice.[12] The coastal marine environment remained productive, as indicated by fossils of pinnipeds.[15] The highly productive kelp forests over rocky marine shallows may have been a lure for coastal migration.[16][17] Reconstruction of the southern Beringian coastline also suggests potential for a highly productive coastal marine environment.[17]

Environmental changes during deglaciation

Pollen data indicate a warm period culminating between 14k and 11k 14C years BP (17k-13k cal years BP) followed by cooling between 11k-10k 14C years BP (13k-11.5k cal years BP).[15] Coastal areas deglaciated rapidly as coastal alpine glaciers, then lobes of Cordilleran ice, retreated. The retreat was accelerated as sea levels rose and floated glacial termini. Estimates of a fully ice-free coast range between 16k[15] and 15k[7] cal years BP. Littoral marine organisms colonized shorelines as ocean water replaced glacial meltwater. Replacement of herb/shrub tundra by coniferous forests was underway by 12.4k 14C years BP (15k cal years BP) north of Haida Gwaii. Eustatic sea level rise caused flooding, which accelerated as the rate grew more rapid.[15]

The inland Cordilleran and Laurentide ice sheets retreated more slowly than did the coastal glaciers. Opening of an ice-free corridor did not occur until after 13k to 12k cal years BP.[5][6][7] The early environment of the ice-free corridor was dominated by glacial outwash and meltwater, with ice-dammed lakes and periodic flooding from the release of ice-dammed meltwater.[5] Biological productivity of the deglaciated landscape was gained slowly.[7] The earliest possible viability of the ice-free corridor as a human migration route has been estimated at 11.5k cal years BP.[7]

Birch forests were advancing across former herb tundra in Beringia by 14.3ka 14C years BP (17k cal years BP) in response to climatic amelioration, indicating increased productivity of the landscape.[13]

Chronology and sources of migration

While most of the archaeological community is in general agreement that the Americas were settled by migrants from northeastern Asian populations, the chronology of the migrations, the source populations that contributed to the migrations, and their migration routes remain uncertain. The uncertainty is fed by a lack of archaeological evidence along migration routes that date to the periods when those migrations are proposed to have occurred; uncertainties in the dating and interpretation of the oldest proposed archaeosites in the Americas; and uncertainties of assumptions underlying chronological and source models of migration derived from studies of modern Native American genetics.


In the early 21st century, the models of the chronology of migration are divided into two general approaches.[18][19] The first is the short chronology theory, that the first migration occurred after the LGM, which went into decline after about 19k cal years BP,[10] and was then followed by successive waves of immigrants.[20] The second theory is the long chronology theory, which proposes that the first group of people entered the Americas at a much earlier date, possibly 21k–40k cal years BP,[21][22][23] followed by a much later second wave of immigrants.[19][24] Further controversy has been generated as age-dating of archaeosites in the Americas[25][26] and the timing of the opening of the ice-free corridor[5][6][7] have challenged the Clovis First theory, which dominated thinking on New World anthropology for much of the 20th century.

Archaeological evidence

Schematic illustration of maternal geneflow in and out of Beringia.Colours of the arrows correspond to approximate timing of the events and are decoded in the coloured time-bar. The initial peopling of Berinigia (depicted in light yellow) was followed by a standstill after which the ancestors of indigenous Americans spread swiftly all over the New World, while some of the Beringian maternal lineages–C1a-spread westwards. More recent (shown in green) genetic exchange is manifested by back-migration of A2a into Siberia and the spread of D2a into north-eastern America that post-dated the initial peopling of the New World.

Figure 2. Schematic illustration of maternal (mtDNA) gene-flow in and out of Beringia (long chronology, single source model).

"Maps depicting each phase of the three-step early human migrations for the peopling of the Americas. (A) Gradual population expansion of the Amerind ancestors from their East Central Asian gene pool (blue arrow). (B) Proto-Amerind occupation of Beringia with little to no population growth for ≈20,000 years. (C) Rapid colonization of the New World by a founder group migrating southward through the ice-free, inland corridor between the eastern Laurentide and western Cordilleran Ice Sheets (green arrow) and/or along the Pacific coast (red arrow). In (B), the exposed seafloor is shown at its greatest extent during the last glacial maximum at ≈20–18 kya [25]. In (A) and (C), the exposed seafloor is depicted at ≈40 kya and ≈16 kya, when prehistoric sea levels were comparable. A scaled-down version of Beringia today (60% reduction of A–C) is presented in the lower left corner. This smaller map highlights the Bering Strait that has geographically separated the New World from Asia since ≈11–10 kya."

Figure 3. Illustration of hypothetical chronology for migration through Beringia (long chronology model). Not authoritative on timing of glacial features and not constrained by archaeological data.

Pre-LGM migration across Beringia into the Americas has been proposed to explain purported pre-LGM ages of archaeosites in the Americas such as Bluefish Caves[22] and Old Crow Flats[23] in the Yukon Territory, and Meadowcroft Rock Shelter in Pennsylvania.[19][24] The earlier 14C date from a bone artifact at the Old Crow Flats site has been supplanted by an Accelerator Mass Spectrometry 14C date that indicates a Holocene age.[27] The interpretations of butcher marks and the geologic association of bones at the Bluefish Cave and Old Crow Flats sites have been called into question.[28] The ages of the earliest positively identified artifacts at the Meadowcroft site are constrained by a compiled age estimate from 14C in the range of 12k-15k 14C years BP (13.8k-18.5k cal years BP).[25][29] The Meadowcroft Rockshelter site and the Monte Verde site in southern Chile, with a date of 14.8k cal years BP,[26] are the archaeosites in the Americas with the oldest dates that have gained broad acceptance.

The Yana River Rhino Horn site (RHS) has dated human occupation of eastern Arctic Siberia to 27k 14C years BP (31.3k cal years BP).[30] That date has been interpreted by some as evidence that migration into Beringia was imminent, lending credence to occupation of Beringia during the LGM.[31][32] However, the Yana RHS date is from the beginning of the cooling period that led into the LGM.[4] But, a compilation of archaeosite dates throughout eastern Siberia suggest that the cooling period caused a retreat of humans southwards.[13][14] Pre-LGM lithic evidence in Siberia indicate a settled lifestyle that was based on local resources, while post-LGM lithic evidence indicate a more migratory lifestyle.[14]

The oldest archaeosite on the Alaskan side of Beringia date to 12k 14C years BP (14k cal years BP).[13][27] It is possible that a small founder population had entered Beringia before that time. However, archaeosites that date closer to the LGM on either the Siberian or the Alaskan side of Beringia are lacking.

Genomic age estimates

For more details on this topic, see Genetic history of indigenous peoples of the Americas.

Recent studies of Amerindian genetics have used high resolution analytical techniques applied to DNA samples from modern Native Americans and Asian populations regarded as their source populations to reconstruct the development of human Y-chromosome DNA haplogroups (yDNA haplogroups) and human mitochondrial DNA haplogroups (mtDNA haplogroups) characteristic of Native American populations.[21][31][32] Models of molecular evolution rates are used to estimate the ages at which Native American DNA lineages branched off from their parent lineages in Asia and to deduce the ages of demographic events. One model based on Native American mtDNA Haplotypes (Figure 2) proposes that migration into Beringia occurred between 30k and 25k cal years BP, with migration into the Americas occurring around 10k to 15k years after isolation of the small founding population.[31] Another model (Figure 3) proposes that migration into Beringia occurred approximately 36k cal years BP, followed by 20k years of isolation in Beringia.[32] Yet another model proposes that migration into Beringia occurred between 40k and 30k cal years BP, with a pre-LGM migration into the Americas followed by isolation of the northern population following closure of the ice-free corridor.[21] The three Native American mtDNA evolution rate models all fall within the long chronology theory of migration into the Americas.

A study of the diversification of mtDNA Haplogroups C and D from southern Siberia and eastern Asia, respectively, suggests that the parent lineage (Subhaplogroup D4h) of Subhaplogroup D4h3, a lineage found among Native Americans and Han Chinese,[33][34] emerged around 20k cal years BP, constraining the emergence of D4h3 to post-LGM.[35] Age estimates based on Y-chromosome micro-satellite diversity place origin of the American Haplogroup Q1a3a (Y-DNA) at around 10k to 15k cal years BP.[36] Greater consistency of DNA molecular evolution rate models with each other and with archaeological data may be gained by the use of dated fossil DNA to calibrate molecular evolution rates.[33]

Source populations

There is general agreement among anthropologists that the source populations for the migration into the Americas originated from an area somewhere east of the Yenisei River. The common occurrence of the mtDNA Haplogroups A, B, C, and D among eastern Asian and Native American populations has long been recognized, along with the presence of Haplogroup X.[37] As a whole, the greatest frequency of the four Native American associated haplogroups occurs in the Altai-Baikal region of southern Siberia.[38] Some subclades of C and D closer to the Native American subclades occur among Mongolian, Amur, Japanese, Korean, and Ainu populations.[37][39]

Human genomic models

The development of high-resolution genomic analysis has provided opportunities to further define Native American subclades and narrow the range of Asian subclades that may be parent or sister subclades. For example, the broad geographic range of Haplogroup X has been interpreted as allowing the possibility of a western Eurasian, or even a European source population for Native Americans, as in the Solutrean hypothesis, or suggesting a pre-LGM migration into the Americas.[37] The analysis of an ancient variant of Haplogroup X among aboriginals of the Altai region indicates common ancestry with the European strain rather than descent from the European strain.[38] Further division of X subclades has allowed identification of Subhaplogroup X2a, which is regarded as specific to Native Americans.[31][34] With further definition of subclades related to Native American populations, the requirements for sampling Asian populations to find the most closely related subclades grow more specific. Subhaplogroups D1 and D4h3 have been regarded as Native American specific based on their absence among a large sampling of populations regarded as potential descendants of source populations, over a wide area of Asia.[31] Among the 3764 samples, the Sakhalin - lower Amur region was represented by 61 Oroks.[31] In another study, Subhaplogroup D1a has been identified among the Ulchis of the lower Amur River region(4 among 87 sampled, or 4.6%), along with Subhaplogroup C1a (1 among 87, or 1.1%).[39] Subhaplogroup C1a is regarded as a close sister clade of the Native American Subhaplogroup C1b.[39] Subhaplogroup D1a has also been found among ancient Jōmon skeletons from Hokkaido[40] The modern Ainu are regarded as descendants of the Jōmon.[40] The occurrence of the Subhaplogroups D1a and C1a in the lower Amur region suggests a source population from that region distinct from the Altai-Baikal source populations, where sampling did not reveal those two particular subclades.[39] The conclusions regarding Subhaplogroup D1 indicating potential source populations in the lower Amur[39] and Hokkaido[40] areas stand in contrast to the single-source migration model.[21][31][32]

Subhaplogroup D4h3 has been identified among Han Chinese.[33][34] Subhaplogroup D4h3 from China does not have the same geographic implication as Subhaplotype D1a from Amur-Hokkaido, so its implications for source models are more speculative. Its parent lineage, Subhaplotype D4h, is believed to have emerged in east Asia, rather than Siberia, around 20k cal years BP.[35] Subhaplogroup D4h2, a sister clade of D4h3, has also been found among Jōmon skeletons from Hokkaido.[41] D4h3 has a coastal trace in the Americas.[34]

The contrast between the genetic profiles of the Hokkaido Jōmon skeletons and the modern Ainu illustrates another uncertainty in source models derived from modern DNA samples:[40]

"However, probably due to the small sample size or close consanguinity among the members of the site, the frequencies of the haplogroups in Funadomari skeletons were quite different from any modern populations, including Hokkaido Ainu, who have been regarded as the direct descendant of the Hokkaido Jomon people."

The descendants of source populations with the closest relationship to the genetic profile from the time when differentiation occurred are not obvious. Source population models can be expected to become more robust as more results are compiled, the heritage of modern proxy candidates becomes better understood, and fossil DNA in the regions of interest is found and considered.

HTLV-1 genomics

The Human T cell Lymphotrophic Virus 1 (HTLV-1) is a virus transmitted through exchange of bodily fluids and from mother to child through breast milk. The mother-to-child transmission mimics a hereditary trait, although such transmission from maternal carriers is less than 100%.[42] The HTLV virus genome has been mapped, allowing identification of four major strains and analysis of their antiquity through mutations. The highest geographic concentrations of the strain HLTV-1 are in sub-Saharan Africa and Japan.[43] In Japan, it occurs in its highest concentration on Kyushu.[43] It is also present among African descendants and native populations in the Caribbean region and South America.[43] It is rare in Central America and North America.[43] Its distribution in the Americas has been regarded as due to importation with the slave trade.[44]

The Ainu have developed antibodies to HTLV-1, indicating its endemicity to the Ainu and its antiquity in Japan.[45] A subtype "A" has been defined and identified among the Japanese (including Ainu), and among Caribbean and South American isolates.[46] A subtype "B" has been identified in Japan and India.[46] In 1995, Native Americans in coastal British Columbia were found to have both subtypes A and B.[47] Bone marrow specimens from an Andean mummy about 1500 years old were reported to have shown the presence of the A subtype.[48] The finding ignited controversy, with contention that the sample DNA was insufficiently complete for the conclusion and that the result reflected modern contamination.[49] However, a re-analysis indicated that the DNA sequences were consistent with, but not definitely from, the "cosmopolitan clade" (subtype A).[49] The presence of subtypes A and B in the Americas is suggestive of a Native American source population related to the Ainu ancestors, the Jōmon.

Physical anthropology

Paleoamerican skeletons in the Americas such as Kennewick Man (Washington State), Hoya Negro skeleton (Yucatán), Luzia Woman and other skulls from the Lagoa Santa site (Brazil), Buhl Woman (Idaho), Peñon Woman III,[50] two skulls from the Tlapacoya site (Mexico City),[50] and 33 skulls from Baja California[51] have exhibited craniofacial traits distinct from most modern Native Americans, leading physical anthropologists to the opinion that some Paleoamericans were of an Australoid rather than Siberian origin.[52] The most basic measured distinguishing trait is the dolichocephaly of the skull. Some modern isolates such as the Pericúes of Baja California and the Fuegians of Tierra del Fuego exhibit that same morphological trait.[51] Other anthropologists advocate an alternative hypothesis that evolution of an original Beringian phenotype gave rise to a distinct morphology that was similar in all known Paleoamerican skulls, followed by later convergence towards the modern Native American phenotype.[53][54] Resolution of the issue awaits the identification of a Beringian phenotype among paleoamerican skulls or evidence of a genetic clustering among examples of the Australoid phenotype.

A report published in the American Journal of Physical Anthropology in January 2015 reviewed craniofacial variation focussing on differences between early and late Native Americans and explanations for these based on either skull morphology or molecular genetics. Arguments based on molecular genetics have in the main, according to the authors, accepted a single migration from Asia with a probable pause in Berengia, plus later bi-directional gene flow. Studies focussing on craniofacial morphology have argued that Paleoamerican remains have "been described as much closer to African and Australo-Melanesians populations than to the modern series of Native Americans", suggesting two entries into the Americas, an early one occurring before a distinctive East Asian morphology developed (referred to in the paper as the "Two Components Model". A third model, the "Recurrent Gene Flow" [RGF] model, attempts to reconcile the two, arguing that circumarctic gene flow after the initial migration could account for morphological changes. It specifically re-evaluates the original report on the Hoya Negro skeleton which supported the RGF model, the authors disagreed with the original conclusion which suggested that the skull shape did not match those of modern Native Americans, arguing that the "skull falls into a subregion of the morphospace occupied by both Paleoamericans and some modern Native Americans."[55][56]

Stemmed points

Stemmed points are a lithic technology distinct from Beringian and Clovis types. They have a distribution ranging from coastal east Asia to the Pacific coast of South America.[16] The emergence of stemmed points has been traced to Korea during the upper Paleolithic.[57] The origin and distribution of stemmed points have been interpreted as a cultural marker related to a source population from coastal east Asia.[16]

Migration routes

Interior route

Map showing the approximate location of the ice-free corridor and specific Paleoindian sites (Clovis theory).

Historically, theories about migration into the Americas have centered on migration from Beringia through the interior of North America. The discovery of artifacts in association with Pleistocene faunal remains near Clovis, New Mexico in the early 1930s required extension of the timeframe for the settlement of North America to the period during which glaciers were still extensive. That led to the hypothesis of a migration route between the Laurentide and Cordilleran ice sheets to explain the early settlement. The Clovis site was host to a lithic technology characterized by spear points with an indentation, or flute, where the point was attached to the shaft. A lithic complex characterized by the Clovis Point technology was subsequently identified over much of North America and in South America. The association of Clovis complex technology with late Pleistocene faunal remains led to the theory that it marked the arrival of big game hunters that migrated out of Beringia then dispersed throughout the Americas, otherwise known as the Clovis First theory.

Recent radiocarbon dating of Clovis sites has yielded ages of 11.1k to 10.7k 14C years BP (13k to 12.6k cal years BP), somewhat later than dates derived from older techniques.[58] The re-evaluation of earlier radiocarbon dates led to the conclusion that no fewer than 11 of the 22 Clovis sites with radiocarbon dates are "problematic" and should be disregarded, including the type site in Clovis, New Mexico. Numerical dating of Clovis sites has allowed comparison of Clovis dates with dates of other archaeosites throughout the Americas, and of the opening of the ice-free corridor. Both lead to significant challenges to the Clovis First theory. The Monte Verde site of Southern Chile has been dated at 14.8k cal years BP.[26] The Paisley Cave site in eastern Oregon yielded a 14C date of 12.4k years (14.5k cal years) BP, on a coprolite with human DNA and 14C dates of 11.3k-11k (13.2k-12.9k cal years) BP on horizons containing western stemmed points.[59] Artifact horizons with non-Clovis lithic assemblages and pre-Clovis ages occur in eastern North America, although the maximum ages tend to be poorly constrained.[25][29]

Geological findings on the timing of the ice-free corridor also challenge the notion that Clovis and pre-Clovis human occupation of the Americas was a result of migration through that route following the Last Glacial Maximum. Pre-LGM closing of the corridor may approach 30k cal years BP and estimates of ice retreat from the corridor are in the range of 12 to 13k cal years BP.[5][6][7] Viability of the corridor as a human migration route has been estimated at 11.5k cal years BP, later than the ages of the Clovis and pre-Clovis sites.[7] Dated Clovis archaeosites suggest a south-to-north spread of the Clovis culture.[5]

Pre-LGM migration into the interior has been proposed to explain pre-Clovis ages for archaeosites in the Americas,[19][24] although pre-Clovis sites such as Meadowcroft Rock Shelter,[25][29] Monte Verde,[26] and Paisley Cave have not yielded confirmed pre-LGM ages.

The interior route is consistent with the spread of the Na Dene language group and Subhaplogroup X2a into the Americas after the earliest paleoamerican migration.[34]

Pacific coastal route

Possible migration routes to the Americas as predicted by the distribution of Y-DNA haplogroups: inland route (purple lines), Pacific coastal route (brown dashed line), and possible trans-Atlantic route (light blue double line).

Pacific models propose that people first reached the Americas via water travel, following coastlines from northeast Asia into the Americas. Coastlines are unusually productive environments because they provide humans with access to a diverse array of plants and animals from both terrestrial and marine ecosystems. While not exclusive of land-based migrations, the Pacific 'coastal migration theory' helps explain how early colonists reached areas extremely distant from the Bering Strait region, including sites such as Monte Verde in southern Chile and Taima-Taima in western Venezuela. Two cultural components were discovered at Monte Verde near the Pacific coast of Chile. The youngest layer is radiocarbon dated at 12,500 radiocarbon years (~14,000 cal BP) and has produced the remains of several types of seaweeds collected from coastal habitats. The older and more controversial component may date back as far as 33,000 years, but few scholars currently accept this very early component.

As the chronology of deglaciation in the interior and coastal regions of North America became better understood, the coastal migration hypothesis was advanced by Knute Fladmark as an alternative to the ice-free corridor hypothesis.[60] Debate on coastal versus interior migration for initial settlement has centered on evidence for chronology of initial settlement of Beringia,[13][27] interior North America,[5] the Pacific coast of the Americas,[26] and timing of the opening of coastal versus interior migration routes indicated by geological evidence.[5][7] Complicating the debate has been the absence of archaeological data from the coastal and interior migration routes from the periods when the initial migration is proposed to have occurred. A recent variation of the coastal migration hypothesis is the marine migration hypothesis, which proposes that migrants with boats settled in coastal refugia during deglaciation of the coast.[16][17] The proposed use of boats adds a measure of flexibility to the chronology of coastal migration, as a continuous ice-free coast (16k-15k cal years BP) would no longer be required. A coastal east Asian source population is integral to the marine migration hypothesis.[16][17]

In 2014, the autosomal DNA of a toddler from Montana, dated at 10.7k 14C years (12.5-12.7 cal years) BP was sequenced.[61] The DNA was taken from a skeleton referred to as Anzick-1, found in close association with several Clovis artifacts. The analysis yielded identification of the mtDNA as belonging to Subhaplogroup D4h3a, a rare subclade of D4h3 occurring along the west coast of the Americas, as well as geneflow related to the Siberian Mal'ta population. The data indicate that Anzick-1 is from a population directly ancestral to present South American and Central American Native American populations. Anzick-1 is less closely related to present North American Native American populations. D4h3a has been identified as a clade associated with coastal migration.[34]

The problems associated with finding archaeological evidence for migration during a period of lowered sea level are well known.[16][62] Sites related to the first migration are usually submerged, so the location of such sites is obscured. Certain types of evidence dependent on organic material, such as radiocarbon dating, may be destroyed by submergence. Wave action can destroy site structures and scatter artifacts along a prograding shoreline. Additionally, Pacific coastal conditions tend to be unstable due to steep unstable terrain, earthquakes, tsunamis, and volcanoes. Strategies for finding earliest migration sites include identifying potential sites on submerged paleoshorelines, seeking sites in areas uplifted either by tectonics or isostatic rebound, and looking for riverine sites in areas that may have attracted coastal migrants.[16][62] Otherwise, coastal archaeology is dependent on secondary evidence related to lifestyles and technologies of maritime peoples from sites similar to those that would be associated with the original migration.

Other coastal models, dealing specifically with the peopling of the Pacific Northwest and California coasts, have been advocated by archaeologists Knut Fladmark, Roy Carlson, James Dixon, Jon Erlandson, Ruth Gruhn, and Daryl Fedje. In a 2007 article in the Journal of Island and Coastal Archaeology, Erlandson and his colleagues proposed a corollary to the coastal migration theory—the "kelp highway hypothesis"—arguing that productive kelp forests supporting similar suites of plants and animals would have existed near the end of the Pleistocene around much of the Pacific Rim from Japan to Beringia, the Pacific Northwest, and California, as well as the Andean Coast of South America. Once the coastlines of Alaska and British Columbia had deglaciated about 16,000 years ago, these kelp forest (along with estuarine, mangrove, and coral reef) habitats would have provided an ecologically similar migration corridor, entirely at sea level, and essentially unobstructed.

A 2016 DNA analysis of plants and animals suggest a coastal route was feasible.[63][64]

East Asians: Paleoindians of the coast

The boat-builders from Southeast Asia (Austronesian peoples) may have been one of the earliest groups to reach the shores of North America.[65][66][67] One theory suggests people in boats followed the coastline from the Kurile Islands to Alaska down the coasts of North and South America as far as Chile [2 62; 7 54, 57]. The Haida nation on the Queen Charlotte Islands off the coast of British Columbia may have originated from these early Asian mariners between 25,000 and 12,000. Early watercraft migration would also explain the habitation of coastal sites in South America such as Pikimachay Cave in Peru by 20,000 years ago and Monte Verde in Chile by 13,000 years ago [6 30; 8 383].

"'There was boat use in Japan 20,000 years ago,' says Jon Erlandson, a University of Oregon anthropologist. 'The Kurile Islands (north of Japan) are like stepping stones to Beringia,' the then continuous land bridging the Bering Strait. Migrants, he said, could have then skirted the tidewater glaciers in Canada right on down the coast." [7 64]'

Problems with evaluating coastal migration models

The coastal migration models provide a different perspective on migration to the New World, but they are not without their own problems. One of the biggest problems is that global sea levels have risen over 120 metres (390 ft)[68] since the end of the last glacial period, and this has submerged the ancient coastlines that maritime people would have followed into the Americas. Finding sites associated with early coastal migrations is extremely difficult—and systematic excavation of any sites found in deeper waters is challenging and expensive. On the other hand, there is evidence of marine technologies found in the hills of the Channel Islands of California, circa 10,000 BCE.[69] If there was an early pre-Clovis coastal migration, there is always the possibility of a "failed colonization". Another problem that arises is the lack of hard evidence found for a "long chronology" theory. No sites have yet produced a consistent chronology older than about 12,500 radiocarbon years (~14,500 calendar years) , but research has been limited in South America related to the possibility of early coastal migrations.

Y-DNA among South American and Alaskan natives

The micro-satellite diversity and distribution of a Y lineage specific to South America suggest that certain Amerindian populations became isolated after the initial colonization of their regions.[70] The Na-Dené, Inuit and Indigenous Alaskan populations exhibit haplogroup Q (Y-DNA) mutations, but are distinct from other indigenous Amerindians with various mtDNA and autosomal DNA (atDNA) mutations.[71][72][73] This suggests that the earliest migrants into the northern extremes of North America and Greenland derived from later migrant populations.[74][75]

Other hypotheses

Other known or supposed trans-oceanic migrations and contacts are not within the scope of this article. The well-documented 10th century Viking colonies in Canada, and the Solutrean hypothesis of Palaeolithic migration from Europe to the Americas, are discussed in those articles. An examination of the many theories, myths and legends about the settlement of the Americas is found in this article about Pre-Columbian contact.

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See also

  • Bluefish Caves
  • Dené–Yeniseian languages - proposed family of languages spoken by indigenous peoples of Asia and North America
  • Early human migrations
  • Historical migration
  • History of Mesoamerica (Paleo-Indian)
  • List of countries and islands by first human settlement
  • Making North America (2015 PBS film)
  • Norse colonization of the Americas
  • Olmec alternative origin speculations
  • Origins of Paleoindians
  • Pendejo Cave
  • Paleo-Indians period (Canada)
  • Pre-Columbian trans-oceanic contact
  • Recent African origin of modern humans

External links

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