Jason Eshleman

Distribution of mtDNA haplogroup X among Native North Americans.

Mitochondrial DNA (mtDNA) samples of 70 Native Americans, most of whom had been found not to belong to any of the four common Native American haplogroups (A, B, C, and D), were analyzed for the presence of Dde I site losses at np 1715 and np 10394. These two mutations are characteristic of haplogroup X which might be of European origin. The first hypervariable segment (HVSI) of the non-coding control region (CR) of mtDNA of a representative selection of samples exhibiting these mutations was sequenced to confirm their assignment to haplogroup X. Thirty-two of the samples exhibited the restriction site losses characteristic of haplogroup X and, when sequenced, a representative selection (n = 11) of these exhibited the CR mutations commonly associated with haplogroup X, C --> T transitions at np 16278 and 16223, in addition to as many as three other HVSI mutations. The wide distribution of this haplogroup throughout North America, and its prehistoric presence there, are consistent with its being a fifth founding haplogroup exhibited by about 3% of modern Native Americans. Its markedly nonrandom distribution with high frequency in certain regions, as for the other four major mtDNA haplogroups, should facilitate establishing ancestor/descendant relationships between modern and prehistoric groups of Native Americans. The low frequency of haplogroups other than A, B, C, D, and X among the samples studied suggests a paucity of both recent non-Native American maternal admixture in alleged fullblood Native Americans and mutations at the restriction sites that characterize the five haplogroups as well as the absence of additional (undiscovered) founding haplogroups.

The Structure of Diversity within New World Mitochondrial DNA Haplogroups: Implications for the Prehistory of North America

The mitochondrial DNA haplogroups and hypervariable segment I (HVSI) sequences of 1,612 and 395 Native North Americans, respectively, were analyzed to identify major prehistoric population events in North America. Gene maps and spatial autocorrelation analyses suggest that populations with high frequencies of haplogroups A, B, and X experienced prehistoric population expansions in the North, Southwest, and Great Lakes region, respectively. Haplotype networks showing high levels of reticulation and high frequencies of nodal haplotypes support these results. The haplotype networks suggest the existence of additional founding lineages within haplogroups B and C; however, because of the hypervariability exhibited by the HVSI data set, similar haplotypes exhibited in Asia and America could be due to convergence rather than common ancestry. The hypervariability and reticulation preclude the use of estimates of genetic diversity within haplogroups to argue for the number of migrations to the Americas.

Implications of the Distribution of Albumin Naskapi and Albumin Mexico for New World Prehistory

The known distributions of two mutational variants of the albumin gene that are restricted to Mexico and/or North America, Albumin Mexico (AL*Mexico) and Albumin Naskapi (AL*Naskapi), were expanded by the electrophoretic analysis of sera collected from more than 3, 500 Native Americans representing several dozen tribal groups. With a few exceptions that could be due to recent, isolated cases of admixture, AL*Naskapi is limited to groups that speak Athapaskan and Algonquian, two widely distributed language families not thought to be related, and to several linguistically unrelated groups geographically proximate to its probable ancestral homeland. Similarly, AL*Mexico is limited to groups that speak Yuman or Uto-Aztecan, two language groups in the American Southwest and Baja California not thought to be closely related to each other, and to several linguistically unrelated groups throughout Mexico. The simultaneous consideration of genetic, historical, linguistic, and archaeological evidence suggests that AL*Naskapi probably originated on the northwestern coast of North America, perhaps in some group ancestral to both Athapaskans and Algonquians, and then spread by migration and admixture to contiguous unrelated, or distantly related, tribal groups. AL*Mexico probably originated in Mexico before 3,000 years BP then spread northward along the Tepiman corridor together with cultural influences to several unrelated groups that participated in the Hohokam culture.

Use of DNase to eliminate contamination in ancient DNA analysis

Using polymerase chain reaction (PCR) amplification, it is possible to analyze DNA from limited source template. This method has proved especially valuable in studies of ancient DNA and in forensic investigations. However, PCR reactions containing minimal or damaged source template are prone to contamination by DNA from a number of other sources. While standard protocols to prevent and/or detect contamination do exist, methods of eliminating contamination are needed to ensure the validity of results obtained. We present a method to eliminate sources of contamination in reagents and labware through the use of a DNase prior to PCR amplification without damaging even the minimal amounts of template present in ancient DNA samples. This method, suggested previously for forensics applications, appears to be effective in eliminating contamination without interfering with the amplification of ancient template.

Mitochondrial DNA and Prehistoric Settlements: Native Migrations on the Western Edge of North America

We analyzed previously reported mtDNA haplogroup frequencies of 577 individuals and hypervariable segment 1 (HVS1) sequences of 265 individuals from Native American tribes in western North America to test hypotheses regarding the settlement of this region. These data were analyzed to determine whether Hokan and Penutian, two hypothesized ancient linguistic stocks, represent biological units as a result of shared ancestry within these respective groups. Although the pattern of mtDNA variation suggests regional continuity and although gene flow between populations has contributed much to the genetic landscape of western North America, some evidence supports the existence of both the Hokan and Penutian phyla. In addition, a comparison between coastal and inland populations along the west coast of North America suggests an ancient coastal migration to the New World. Similarly high levels of haplogroup A among coastal populations in the Northwest and along the California coast as well as shared HVS1 sequences indicate that early migrants to the New World settled along the coast with little gene flow into the interior valleys.

Mitochondrial DNA of Protohistoric Remains of an Arikara Population from South Dakota: Implications for the Macro-Siouan Language Hypothesis

Abstract Mitochondrial DNA (mtDNA) was extracted from skeletal remains excavated from three Arikara sites in South Dakota occupied between AD 1600 and 1832. The diagnostic markers of four mtDNA haplogroups to which most Native Americans belong (A, B, C, and D) were successfully identified in the extracts of 55 (87%) of the 63 samples studied. The frequencies of the four haplogroups were 42%, 29%, 22%, and 7%, respectively, and principal coordinates analysis and Fishers exact tests were conducted to compare these haplogroup frequencies with those from other populations. Both analyses showed closer similarity among the Mohawk, Arikara, and Sioux populations than between any of these three and any other of the comparison populations. Portions of the first hypervariable segment (HVSI) of the mitochondrial genome were successfully amplified and sequenced for 42 of these 55 samples, and haplotype networks were constructed for two of the four haplogroups. The sharing of highly derived lineages suggests that some recent admixture of the Arikara with Algonquian-speaking and Siouan-speaking groups has occurred. The Arikara shared more ancient lineages with both Siouan and Cherokee populations than with any other population, consistent with the Macro-Siouan language hypothesis that Iroquoian, Siouan, and Caddoan languages share a relatively recent common ancestry.