An early Indian cranium from the Medicine Crow site, (39BF2), Buffalo County,South Dakota

Artifacts of Paleoindians have been found in most if not all of the Plains states; however, documented human skeletal remains from this early period are rare. The Medicine Crow cranium dates by stratigraphy and by the amount of absorbed alpha and beta radiation at between 5,000 and 2,000 B.C. This places this young adult male in the Archaic period and represents the earliest documented human skeletal material from South Dakota. It compares favorably in age with other well documented human skeletons from the Plains area, such as Lansing Man (Kansas) (3579 B.C.). Metrically, (with a cranial index of 76.7) and morphologically the Medicine Crow cranium falls well within the range of other early or middle Archaic skeletons.     

Inferring History From Crania: Biological Distance Comparisons Of Mill Creek And Early Middle Missouri Tradition Crania With Mandan And Arikara Population Samples

Abstract

Craniometric data are used to compare available human crania from Mill Creek and early Middle Missouri Tradition sites with a pooled Mandan sample and Coalescent Tradition samples from Crow Creek, Mobridge and Rygh(inferred proto-Arikara). Discriminant functions are computed for the reference samples, and test cases are classified according to their proximity to each population centroid. With one exception, early Middle Missouri Tradition site crania compare most favorably with Mandan. Mill Creek site specimens are unlike the Mandan, most closely resembling early Coalescent samples.     

The morphometric relationship of Upper Cave 101 and 103 to modern Homo sapiens

Since the discovery of the Homo sapiens crania from the Upper Cave of Zhoukoudian in northern China (UC 101, UC 102, and UC 103), no clear consensus has arisen regarding their affinities with modern populations. We use linear craniofacial measurements to compare UC 101 and UC 103 to a worldwide sample of H. sapiens that includes Paleoamericans and Archaic Indians, and employ Mahalanobis distance analysis and associated unweighted, unrestricted canonical variate analysis for the comparisons. Analyses indicate that UC 101 has consistent affinities with Easter Island and European populations, whereas UC 103 has more tenuous similarities with Australo-Melanesian groups. Both fossils exhibit some similarities to certain Paleoamerican and Archaic Indian individuals, but rarely cluster together. Upper Cave 103 is more of an outlier to modern populations than is UC 101. The fossils are not representative of any group to which they have been compared, but may be part of the generalized population that was ancestral to Paleoamericans.     

Notes On the Crow-Hidatsa Schism

Abstract

Three lines of evidence bearing on the Crow-Hidatsa separation provide different dates for that separation, but dates which are consistent with the following generalizations: (1) The Crow began to diverge linguistically from the various Hidatsa groups no less than five centuries ago, and perhaps even earlier. (2) The Crow movement onto the Northwestern Plains was accomplished gradually, perhaps by band-by-band movement, rather than as one precipitous migration away from the Hidatsa. (3) Archaeological evidence from sites of the Mandan/Hidatsa continuum in the Missouri Valley suggest that the Hagen site, at least, probably dates at about A.D. 1675 – although alternative explanations for related sites suggest that the Crow moved into the Northwestern Plains several centuries earlier. (4) Ethnohistorical data suggest that the Crow separation dates from the mid-1700s. Rather than dating the initial separation of the two groups, the ethnohistorical data probably reflect the final severing of ties with the Hidatsa – a separation made final by the adoption of the horse.     

Archaic Skeletal Remains from the Central Plains: Demography and Burial Practices

Abstract

Recently a number of reports on Plains Archaic skeletal material have been published which quadruple the number of burials described and analyzed in the literature. Although the total number of burials is still relatively small, it is large enough to allow research to begin in paieodemographic aspects of the central part of thePlains and the suggestion of burial patterns for these materials. By combining all Archaic burials from the Plains a demographic profile has been developed. It is compared with other Archaic populations from the eastern United States, and with a Plains population dating after A.O. 1000. The results of the analysis show that with few exceptions burial patterns and the demographic picture of the Plains are quite stable over time, although differences are found in metric and non-metric variations in both the time and space continua. The analysis further shows that certain anomalous conditions in the skeleton appear to be much more prevalent inArchaic material than in recent material from the same area. The results finally suggest that Archaic people in the demographic and burial practice continua are quite similar to later populations, at least through Middle Mississippian populationsin the Plains.     

The Gore Pit Site: An Archaic Occupation in Southwestern Oklahoma and a Review Of the Archaic Stage in the Southern Plains

Abstract

The Gore Pit site (34CM131), which is within the city limits of Lawton, Comanche County, Oklahoma, has been revealing evidence of Archaic occupation through excavation and surface collection since 1963. The site is contained in the bottom of a large borrow pit which was sera ped to a depth of 15 to 20 feet by he Highway Department.The pit is on the active flood plain of East Cache Creek and borders the creek a few feet to the east. The artifacts recovered by surface collection include projectile points, scrapers, scraper planes, Clear Fork gouges, andgrinding stones and basins. Three burned rock middens were excavated, one of which yielded radiocarbon dates, 6030 + 300 B.P. (Bastian 1964) and 6145+ 130 B.P. (GX1558). In the spring of 1968, a partially preserved, semiflexed human burial was discovered in the pit. There were no associated artifacts. A radiocarbon date obtained from the apatite fraction of the bone resulted in a determination of 7100+350 B.P. (GX2009). The earliest Archaic on the Southern Plains is presently dated around 6000 B.P. However, there is a paucity of dated and documented sites for the preceding 2000 years. Archaic subsistence patterns occur at least 2000 years earlier in areas to the west and east. The origin and age of the earliest Archaic in the Southern Plains remains undetermined. The Archaic must ultimately be identified on the basis of subsistence patterns and not on the basis of projectile point styles.     

More lingual surface attrition of the maxillary anterior teeth in American Indians: prehistoric Panamanians

Lingual surface attrition of the maxillary anterior teeth (LSA-MAT) has been found in additional prehistoric Latin American Indian skeletons. LSAMAT was first observed in crania from an Archaic Brazilian site. This second finding occurs in teeth from Venado Beach, a late prehistoric site in Panama. LSAMAT is also present in some fragmentary specimens from the Archaic Cerro Mangote site in Panama. LSAMAT at Venado Beach is present in 57% of 28 adult crania. As in the Brazilian study, LSAMAT is associated with a high caries rate (82% of 50 adults; 11.7% of 852 permanent teeth). As first suggested, eating and processing of some type of abrasive carbohydrate food, such as manioc, is the possible cause of LSAMAT. However, other possible causes relating to habitation on or near marine coasts cannot be totally ruled out.     

A re-evaluation of the metric diversity within Homo erectus

Previous work by several researchers has suggested that the cranial sample from Zhoukoudian possesses a unique metric pattern relative to the African and Asian specimens assigned to Homo erectus. The current study readdresses this issue with an expanded fossil sample and a larger and more comprehensive set of cranial measurements. To test the patterns present in the assemblage, canonical variates analysis was performed using a covariance matrix generated from the Howells data set. From this, interindividual Mahalanobis distances were computed for the fossils. Random expectation statistics were then used to measure statistical significance of the Mahalanobis distances. The results show that the Zhoukoudian hominids exhibit a unique metric pattern not shared by the African and Indonesian crania sampled. In these tests the Hexian calvaria resembled the African and Indonesian specimens and differed significantly from the craniometric pattern seen in the Zhoukoudian fossils. The Zhoukoudian specimens are characterized by a wide midvault and relatively narrow occipital and frontal bones, while the African and Indonesian crania (including Hexian) have relatively broad frontal and occipital dimensions compared to their midvaults. These results do not suggest that a multiple-species scenario is necessary to encompass the variation present in the sample. Based on the current evidence it is more probable that this variation reflects polytypism influenced by environmental adaptation and/or genetic drift.     

New evidence on the spatiotemporal distribution and evolution of the Uto-Aztecan premolar

Uto-Aztecan premolar (UAP) is a rare morphological feature of the maxillary first premolar that occurs in Native American populations with frequencies ranging 0-16.7%. A recent summary of UAP by Delgado-Burbano et al. (2010) suggests the trait evolved around 4,000 BP in the American Southwest where the earliest cases occur and where the trait exists at the highest frequencies among contemporary populations. In this article, we present new data on UAP prevalence from an Archaic North American sample from Buckeye Knoll, Texas (circa 7,500-6,200 cal BP). Buckeye Knoll preserves a single case of UAP, and a sample frequency of 3.6%. In addition, we confirm the presence of UAP in other eastern North American Archaic skeletal samples from the Windover and Harris Creek at Tick Island sites in Florida. We also review the dental morphological literature to assess: 1) whether UAP prevalence is limited to New World populations, and 2) whether the trait's antiquity can be extended further into the Early Holocene Paleoindian period. Additional cases of UAP are presented from the Pacific coast of South America, Europe, Asia, and Australia. Combined, these data greatly expand the spatial and temporal distribution of UAP and suggest the trait evolved considerably earlier than previously thought.     

Neogene Fallout Tuffs from the Yellowstone Hotspot in the Columbia Plateau Region,Oregon, Washington and Idaho,USA

Sedimentary sequences in the Columbia Plateau region of the Pacific Northwest ranging in age from 16–4 Ma contain fallout tuffs whose origins lie in volcanic centers of the Yellowstone hotspot in northwestern Nevada, eastern Oregon and the Snake River Plain in Idaho. Silicic volcanism began in the region contemporaneously with early eruptions of the Columbia River Basalt Group (CRBG), and the abundance of widespread fallout tuffs provides the opportunity to establish a tephrostratigrahic framework for the region. Sedimentary basins with volcaniclastic deposits also contain diverse assemblages of fauna and flora that were preserved during the Mid-Miocene Climatic Optimum, including Sucker Creek, Mascall, Latah, Virgin Valley and Trout Creek. Correlation of ashfall units establish that the lower Bully Creek Formation in eastern Oregon is contemporaneous with the Virgin Valley Formation, the Sucker Creek Formation, Oregon and Idaho, Trout Creek Formation, Oregon, and the Latah Formation in the Clearwater Embayment in Washington and Idaho. In addition, it can be established that the Trout Creek flora are younger than the Mascall and Latah flora. A tentative correlation of a fallout tuff from the Clarkia fossil beds, Idaho, with a pumice bed in the Bully Creek Formation places the remarkably well preserved Clarkia flora assemblage between the Mascall and Trout Creek flora. Large-volume supereruptions that originated between 11.8 and 10.1 Ma from the Bruneau-Jarbidge and Twin Falls volcanic centers of the Yellowstone hotspot in the central Snake River Plain deposited voluminous fallout tuffs in the Ellensberg Formation which forms sedimentary interbeds in the CRBG. These occurrences extend the known distribution of these fallout tuffs 500 km to the northwest of their source in the Snake River Plain. Heretofore, the distal products of these large eruptions had only been recognized to the east of their sources in the High Plains of Nebraska and Kansas.     

Artificial cranial deformation and fossil Australians revisited

Based on cranial characters shared by Homo erectus in Java and Homo sapiens in Australia, Australasia is widely considered the strongest case for a regional origin of modern humans. However, artificial vault deformation has been suggested to be the cause of "archaic" characters such as frontal recession in key fossil Australian crania. We use log-log plots of cranial arc versus chord measurements and we score nonmetric traits often thought to be associated with artificial deformation to make systematic comparisons across groups and deformation types to identify universal consequences of artificial deformation. Based on our large comparative sample (n = 588) apparatus-deformed crania have flatter frontals and occipitals and usually more angulated parietals in the sagittal plane than undeformed crania, regardless of deformation type. Fossil Australian samples exhibit evidence of both undeformed and deformed individuals. The sample from Coobool Creek provides evidence that undeformed individuals had more rounded frontals than recent Australians. However, many individuals from Coobool Creek, Kow Swamp, and Nacurrie exhibit modification of one or more cranial contours. The Kow Swamp individuals in particular plot with deformed crania from all regions. In addition, the frequency of hyperostotic traits such as bregmatic eminence, metopic and sagittal keels in H. sapiens is influenced by both artificial deformation and pathological hypervascularity/hyperostosis. Thus it is unwise to use cranial contours and these nonmetric traits to infer genetic relatedness between Fossil Australians and Indonesian H. erectus.     

The Late Prehistoric Human Ecology of Birch Creek Valley,Northeastern Oklahoma

Abstract

A multi-disciplinary study of the archaeological sites in Birch Creek Valley examined the valley’s paleoenvironment, prehistoric economy, and demography. The study indicates that during the Plains Village Period (ca. A.D. 800-1,500) the local environment was stable and similar to that of the area today with the valley being occupied during the late summer through winter by dispersed groups containing from 10 to 15 people. The Late Prehistoric occupants of the valley apparently relied on a broad-spectrum foraging economy and did not engage in horticulture.     

New craniodental fossils of papionin monkeys from Cooper's D,South Africa

Papionin monkey fossils are common in the Plio‐Pleistocene aged karst cave deposits northwest of Johannesburg in South Africa. These deposits have yielded important primate and other vertebrate fauna since their discovery in the early part of the 20th century. In this article, we describe new primate cranial and dental specimens from excavations at the site of Cooper's D in the Sterkfontein Valley that date to around 1.5 million years ago. Unlike other localities in southern Africa, most of the new fossils are referred to Theropithecus oswaldi oswaldi, an extinct gramnivorous monkey related to the living gelada. Diagnostic features of T. o. oswaldi crania and teeth include large, thickly enameled molars with tall, columnar cusps, and high molar relief, an upright mandibular ramus, postorbital constriction, and anterior fusion of temporal lines. Also present in the new sample are teeth referred to Papio sp., which show low crowned bunodont molars, and a number of indeterminate papionin teeth and skull fragments. The presence of T. o. oswaldi at Cooper's D extends the list of known localities where the taxon is found, and may indicate the presence of an open, grassland environment in the area during the early Pleistocene. The abundance of theropith fossils at Cooper's suggests that Papio was not consistently the most common papionin in southern Africa over the past three million years. Am J Phys Anthropol 151:613–629, 2013. © 2013 Wiley Periodicals, Inc.     

Middle Pleistocene Human Remains from Tourville-la-Rivière (Normandy,France) and Their Archaeological Context

Despite numerous sites of great antiquity having been excavated since the end of the 19th century, Middle Pleistocene human fossils are still extremely rare in northwestern Europe. Apart from the two partial crania from Biache-Saint-Vaast in northern France, all known human fossils from this period have been found from ten sites in either Germany or England. Here we report the discovery of three long bones from the same left upper limb discovered at the open-air site of Tourville-la-Rivière in the Seine Valley of northern France. New U-series and combined US-ESR dating on animal teeth produced an age range for the site of 183 to 236 ka. In combination with paleoecological indicators, they indicate an age toward the end of MIS 7. The human remains from Tourville-la-Rivière are attributable to the Neandertal lineage based on morphological and metric analyses. An abnormal crest on the left humerus represents a deltoid muscle enthesis. Micro- and or macro-traumas connected to repetitive movements similar to those documented for professional throwing athletes could be origin of abnormality.     

Paleoamerican morphology in the context of European and East Asian late Pleistocene variation: implications for human dispersion into the New World

Early American crania show a different morphological pattern from the one shared by late Native Americans. Although the origin of the diachronic morphological diversity seen on the continents is still debated, the distinct morphology of early Americans is well documented and widely dispersed. This morphology has been described extensively for South America, where larger samples are available. Here we test the hypotheses that the morphology of Early Americans results from retention of the morphological pattern of Late Pleistocene modern humans and that the occupation of the New World precedes the morphological differentiation that gave rise to recent Eurasian and American morphology. We compare Early American samples with European Upper Paleolithic skulls, the East Asian Zhoukoudian Upper Cave specimens and a series of 20 modern human reference crania. Canonical Analysis and Minimum Spanning Tree were used to assess the morphological affinities among the series, while Mantel and Dow-Cheverud tests based on Mahalanobis Squared Distances were used to test different evolutionary scenarios. Our results show strong morphological affinities among the early series irrespective of geographical origin, which together with the matrix analyses results favor the scenario of a late morphological differentiation of modern humans. We conclude that the geographic differentiation of modern human morphology is a late phenomenon that occurred after the initial settlement of the Americas.     

Craniofacial diversity in earlyHomo and the affinities of the Sterkfontein Valley

The Sterkfontein Valley specimens SK 847 (Swartkrans Member 1) and Stw 53 (Sterkfontein Member 5) provide important evidence of earlyHomo in southern Africa. However, specific identity has been disputed, with that of SK 847 especially contentious. Opinions differ markedly as to whether the specimens are conspecific or not, whether they should be referred to East African earlyHomo species, or whether they represent new species. Morphometric analysis of facial dimensions reveals contrasting affinities for the two South African fossils, and so does not support claims for their conspecifity. Stw 53 is very like smaller East African crania referred toH. habilis, whereas SK 847 has a distinctive facial pattern. In some respects it resembles early AfricanH. erectus (=H. ergaster), but with a markedly more projecting mid-face, prominent zygomatic and unexpanded frontal region, all of which militate against inclusion in that species. The taxonomic implications of these contrasting facial affinities are briefly discussed.     

The Neanderthal "chignon": variation, integration, and homology

The occipital bun ("chignon") is cited widely as a Neanderthal derived trait. It encompasses the posterior projection/convexity of the occipital squama and is associated with lambdoid flattening on the parietal. A 'hemibun' in some Upper Paleolithic Europeans is thought by some authors to indicate interbreeding between Neanderthals and early modern Europeans. However, 'bunning' is difficult to measure, and the term has been applied to a range of morphological patterns. Furthermore, its usefulness in phylogenetic reconstruction and its homologous status across modern and fossil humans have been disputed. We present a geometric morphometric study that quantitatively evaluates the chignon, assesses its usefulness in separating Neanderthals from modern humans, and its degree of similarity to Upper Paleolithic 'hemibuns.' We measured the three-dimensional coordinates of closely spaced points along the midsagittal plane from bregma to inion and of anatomical landmarks in a large series of recent human crania and several Middle and Late Pleistocene European and African fossils. These coordinate data were processed using the techniques of geometric morphometrics and analyzed with relative warps, canonical variates, and singular warps. Our results show no separation between Neanderthals and modern humans, including early modern Europeans, when the shape of the occipital plane midsagittal-profile is considered alone. On the other hand, Neanderthals are well separated from both recent and fossil modern humans when information about the occipital's relative position and relative size are also included. Furthermore, the occurrence of a highly convex and posteriorly projecting midline occipital profile (interpreted as the occipital bun) is highly correlated (>0.8) with a flat parietal midsagittal profile and with antero-superiorly positioned temporal bones across both our recent and our fossil human samples. We conclude that the shape of the occipital profile alone should not be considered an independent trait, as it is very tightly integrated with braincase shape. Our analysis does not support differences in integration of the posterior midsagittal profile and the cranial base in Pleistocene and recent humans.     

Human cranial diversity and evidence for an ancient lineage of modern humans

This study examines the genetic affinities of various modern human groupings using a multivariate analysis of morphometric data. Phylogenetic relationships among these groupings are also explored using neighbor-joining analysis of the metric data. Results indicate that the terminal Pleistocene/early Holocene fossils from Australasia exhibit a close genetic affinity with early modern humans from the Levant. Furthermore, recent human populations and Upper Paleolithic Europeans share a most recent common ancestor not shared with either the early Australasians or the early Levantine humans. This pattern of genetic and phylogenetic relationships suggests that the early modern humans from the Levant either contributed directly to the ancestry of an early lineage of Australasians, or that they share a recent common ancestor with them. The principal findings of the study, therefore, lend support to the notion of an early dispersal from Africa by a more ancient lineage of modern human prior to 50 ka, perhaps as early as OIS 5 times (76-100 ka).     

Within-group human variation in the Asian Pleistocene: the three Upper Cave crania

Numerous studies on Pleistocene samples have shown that within-group cranial variation was greater than that seen today. The three anatomically modern Upper Cave crania (UC 101, UC 102, and UC 103) from Zhoukoudian, China provide one of the best samples available for addressing the issue of the antiquity of the modern pattern of within-group cranial variability because archaeological evidence indicates that they are spatially and temporally restricted. Research on the Upper Cave fossils usually only includes UC 101 and UC 103 because of postmortem damage to UC 102's cranial vault. However, the face of UC 102 is undamaged, allowing for most facial measurements to be performed accurately. In this study we use facial dimensions to compare all three Upper Cave specimens, and we evaluate whether the variation seen among them is larger than that observed in extant populations.Using a worldwide sample of modern populations to establish a baseline, the three Upper Cave crania were compared to each other. Since there is disagreement over the sex of UC 102, this specimen is treated alternately as a female and as a male. Results show that the Upper Cave specimens exhibit significantly more variation than do individuals within more recent human populations, especially if UC 102 is considered male. Furthermore, results indicate that the fossils never fall into the same modern human group, and that each specimen is significantly atypical of its nearest modern neighbor in multivariate space.We conclude that the three Upper Cave crania do not represent a family group but are representative of the larger contemporaneous heterogeneous Asian Pleistocene population. Our results support the contention that today's within-group homogeneity is a relatively recent phenomenon, and is likely the result of a Neolithic population expansion and its many effects.