The Redbird Focus: Cranial Evidence in Tribal Identification

Abstract

The Redbird Focus was defined in 1956, and was initially (Wood 1956) related to both Lower Loup and historic Pawnee Focus materials. Wood (1965) later took the position that Redbird was a more probable antecedent to the historic Ponca. These opposing hypotheses are tested using human crania representing the relevant populations. Samples of the following were available: Arikara from 39ST216, Pawnee from 25BU1 and 25WT1, Omaha from 25DK10 and 25DK2A, Ponca from 25KX1, and Redbird from 25KX9. Cranial measurements in a multivariate context were employed to test Wood’s suggestions regarding: (1) Ponca identification of remains from the Ponca Fort site, 25KX1, and (2) the tribal identity of the Redbird Focus crania. The Ponca Fort site is identified as historic Ponca, but with the probable presence of some Arikara females. The hypothesis that Redbird is antecedent to Ponca is found tenable on the basis of available cranial evidence.     

Theodore H. Lewis and his Northeastern Nebraska “Forts”1

Abstract

The inveterate fieldman and surveyor, T. H. Lewis, visited northeastern Nebraska in his quest for archaeological sites in the fall of 1890. He recorded four earthworks there, only one of which (Ponca Fort, 25KX1) was recorded by later workers. His field maps, published here for the first time, are accompanied by comments on the success the author has had in relocating these earthworks. Only Ponca Fort is clearly identifiable today. One enclosure, near the town of Wynot, may be part of the “Bad Village” of the Omaha; another, near Hartington, has been plowed level and yields no surface remains. The fourth earthwork, near the town of Ponca, cannot be located.     

Site 39Lm219 In The Big Bend Reservoir,South Dakota

Abstract

Site 39LM219, an earth-lodge village located in the neck of the Big Bend of the Missouri River in Lyman County, South Dakota, is assigned to the Chouteau Aspect and is presumed to date at about A. D. 1700. Probably the site is part of the Crazy Bull Site previously described in this journal.     

The Middle Missouri Tradition: the Late Stage

Abstract

Two prehistoric complexes in the northern part of the Middle Missouri area, the Thomas Riggs and Huff Foci, comprise the late stage of the Middle Missouri Tradition. Although transitional sites are as yet lacking, this late stage is regarded as an outgrowth of the early stages of the same tradition, localized further south along the Missouri River in South Dakota. The Huff Focus postdates the Thomas Riggs Focus and is a direct outgrowth of Thomas Riggs, both foci being assigned to the Fire Heart Aspect. This aspect is the prehistoric antecedent for the Heart River Focus, the protohistoric express ion of Historic Mandan culture. Brief comments are offeredon the history, or1g1ns, distribution, characteristics, dating, and relationships of the Thomas Riggs and Huff Foci.     

Physical Evidence on the Origin and Fate of the Panhandle Aspect People

Abstract

Comparison of the populations of four Panhandle Aspect sites (Alibates, Antelope Creek, Matthews Ranch, Footprint) using 28 non-metric traits of the skulls indicates generally close similarity among them, but the Panhandle groups show little similarity to Upper Republican. Antelope Creek and Matthews Ranch show some resemblance to the Fort Coffee skulls of the Fulton Aspect. The same two Panhandle site samples also resemble the Washita River people. Footpnnt is even more similar to Washita River.     

Craniometric Variation In The Northern And Central Plains

Abstract

Cranial measurements of 13 male and 12 female samples from the Central and Northern Plains region were subjected to canonical analysis. The samples include historic or protohistoric crania that can be ascribed to the Arikara, Mandan, Pawnee, Ponca and Omaha tribes. In addition, two samples belong to the archaeologically defined St. Helena Focus. Both sexes yielded five significant canonical variates, although only four were readily interpretable. The first canonical variate is clearly a Siouan-Caddoan discriminator and reflects variation in cranial vault height. St. Helena sites associate with the Arikara on this axis, supporting previous craniometric analyses which suggest a relationship between these two groups. Subsequent canonical variates deal with more particular aspects of craniometric variation among groups, but are still interpretable in historic or evolutionary terms. The classificatory analysis shows that the Arikara sites are closely related. A major exception to this is the Sully site, which frequently misclassifies with non-Arikara groups. This suggests that the Sully crania have little collective reality; and that there may be non-Arikara components represented at the Sully Site.     

Plains Apache Archaeology: A Review

Abstract

A review of the literature on the Dismal River Aspect in the light of recent additional work at Plains Apache sites has led to more specific suggestions as to probable sources of various Dismal River traits. Most of the traits that appear to have been borrowed from sedentary neighbors seem to have an eastern Plains origin. Many trade items from the Southwest may have been secured from or through the Jicarilla Apaches. Frequency of some triJ, its at Dismal River sites form a gradient from north to south. Many problems remain unsolved.     

Alaska peninsula stable isotope and radioisotope chemistry: a study in temporal and adaptive diversity

Purified bone collagen from a small suite of human remains recovered at three sites on the Alaska Peninsula (Port Moller, Brooks River, and Mink Island) were analyzed for stable carbon and nitrogen isotope chemistry and were accelerator radiocarbon dated. Because samples sizes were small and faunal isotope chemistry lacking, results should be considered preliminary. However, these data indicate that each locality was represented by a somewhat different suite of subsistence strategies and covered a distinct temporal span. Port Moller burials (n = 7) from the Hot Springs site date to a calibrated 2σ range of 3547-1388 BP. Although marine foods clearly made the greatest contribution to these diets, individuals were not as heavily reliant on high-trophic-level marine taxa as eastern Aleutian groups to the west, given their intake of salmon and evidence of caribou hunting. Brooks River burials (n = 9) expressed an inland foraging focus with significant reliance on caribou and spawning salmon and covered a calibrated 2σ range of 1484-381 BP. In contrast, individuals from Mink Island (n = 7), dating to cal. 666-292 BP, were heavily reliant on high-trophic-level marine prey similar to but not as enriched isotopically as the Aleut, perhaps a consequence of limited access to caribou and greater reliance on invertebrates. This pattern suggests that prehistoric economic strategies on the Alaska Peninsula were diverse, characterized by fine-tuned adaptations to local ecological settings, perhaps mediated by ethnic factors and territorial and social pressures.     

The Niobrara River Valley,a postglacial migration corridor and refugium of forest plants and animals in the grasslands of central North America

The Niobrara River Valley of northern Nebraska contains numerous bryophyte, vascular plant, and animal species more typical of forests far to the east, north, and west than to other forests in the grasslands that surround the Valley. Some species are probably relicts of cooler glacial and early postglacial times, when much of what is now grassland was covered by boreal and cool-temperate forests. Others entered the Valley from the east in postglacial times, and some entered from the west as the climate became semi-arid. There is a steep decline in total number of vascular plant species from the mouth of the Missouri River up through the Niobrara Valley, suggesting an environmental gradient and differential migration and extirpation of species at various times since the Pleistocene.     

An Analysis Of Four Survey Collections From Armstrong County,South Dakota 39Ar2 (No Heart Creek Site), 39Ar4, 39Ar5 And 39Ar 7

Abstract

The materials collected from four sites on the Little Bend of the Missouri River are described and analyzed. In the conclusion, these manifestations, referred to as the No Heart Creek complex, are compared to seven other sites along the river in north.-central South Dakota. The sites are related to the Le Compte Focus and are characterized by a distinetive settlement pattern.     

Uridine monophosphate kinase polymorphism in two Venezuelan populations.

A study of the uridine monophosphate kinase (UMPK) electrophoretic patterns in Venezuelan individuals from the mestizo population of Caracas and from the Warao Indians of the Nabasanuka village in the Delta of the Orinoco River are reported. Among the mestizo population, the frequency of the UMPK1, UMPK2, and UMPK3 alleles was .979, .020, and .001, respectively. A higher frequency of the UMPK3 gene was seen in the highly inbred Warao Indians than any other population studied to date.     

Site directed chromosomal marking of a fluorescent pseudomonad isolated from the phytosphere of sugar beet; stability and potential for marker gene transfer.

A plasmid-free, non-pathogenic, ribosomal RNA group 1 fluorescent pseudomonad, Pseudomonas fluorescens SBW25, was selected from the microflora of sugar beet (Beta vulgaris) and modified to contain constitutively expressed marker genes. By site directed homologous recombination a KX cassette [kanamycin resistance (kanτ) and catechol 2,3 dioxygenase (xylE)] and a ZY cassette [lactose utilization (lacZY, β-galactosidase, lactose permease)] were introduced at least 1 Mbp apart on the 6.6 Mbp bacterial chromosome. Separate sites were selected to provide sensitive detection methods and allow assessments of marker gene stability of the genetically modified micro-organism (GMM), SBW25EeZY6KX, when it colonized the leaves and roots of sugar beet plants following seed inoculation.     

Radiocarbon Dating the Wylie Focus North Central Texas

Abstract

Many archeological complexes in the Southern Plains and Texas have not been adequately dated. Many complexes in northern Texas are still dated by their association with tree-ring dated Puebloan ceramics. This paper describes recent advances in radiocarbon dating the Wylie Focus on the East Fork of the Trinity River. Based upon radiocarbon dates and associated ceramics, it is evident that these sites were occupied before A.D. 1000.     

Temporal Ordering and the Chouteau Aspect

Abstract

Temporal ordering of closely-related sites in the Oahe, Big Bend and Fort Randall Reservoirs of South Dakota may be accomplished by a simple seriation of selected traits common to, and diagnostic of, the related sites. The resultant ordering is best interpreted as three “blocks” of time within a temporal unit. The chronology inferred from the ordering reinforces the present known dates of the Chouteau Aspect as well as sites culturally and temporally marginal to the Chouteau Aspect.     

The Identity of La Salle’S Pana Slave

Abstract

In June 1682 Robert Cavelier, Sieur de La Salle, was presented with a “Pana” boy by the Illinois Michigamea Indians. The boy told La Salle of his history as a captive in four Indian tribes. He described Indian village locations and listed the tribes which had “many” horses. The significance of the information for which he was the source depends on the tribal identity of the captive. It has been suggested in anthropological literature that “Pana” indicated “Pawnee,” Ponca, Arikara, Wichita, even Apache. After examination of evidence-linguistic, cultural, historical - it seems most likely he was a Southern Pawnee, a Wichita. If this was so, then his information substantiates the theory of Kroeber, Brant and others that some Kiowa Apaches were still living in the southern Plains in the late 17th century.     

Separation and evaluation of the covalent and noncovalent interactions which contribute to the binding of pyridoxal 5'-phosphate to D-serine apodehydratase.

The equilibrium constant (KX) for the reaction D-serine dehydratase + pyridoxamine-P in equilibrium KX D-serine apodehydratase: pyridoxamine-P + pyridoxal-P was determined. At 25 degreees, pH 7.80, KX increases from 5.4 times 10-minus 5 to 21 times 10-minus 5 as T/2 is increased from 0.33 to 0.66. A value of 1.3 times 10-minus 4 M at 25 degrees, pH 7.80, T/2 0.33 for the equilibrium constant (KPMP) for dissociation of pyridoxamine-P from D-serine apodehydratase was determined from the ratio of the equilibrium constant for dissociation of pyridoxal-P from holoenzyme to KX. Pyridoxamine-P and the thiazolidine, formed from pyridoxal-P and cysteine, were found to have similar affinities for D-serine apodehydratase. Using the affinities of these derivatives as a measure of the noncovalent interactions between cofactor and protein, it was possible to estimate the contribution of the Schiff base linkage to the stability of the complex formed between pyridoxal-P and protein. The covalent Schiff base linkage in the holoenzyme was found to be no more stable than the Schiff base linkage formed between 6-aminocaproic acid and pyridoxal-P. The contribution of noncovalent interactions to the stability of the cofactor-protein complex was shown to be at least 20 to 40 times greater than the contribution of the covalent Schiff base linkage.     

Distinguishing wild and domestic wheat and barley spikelets from early Holocene sites in the Near East

Identifying morphologically domestic cereals is essential to understanding the origins of agriculture. Charred spikelet bases provide the best evidence for distinguishing wild from domestic varieties of emmer, einkorn and barley; however until now, identification criteria have not been agreed upon or well established. We examined more than 20,000 remains of charred spikelets from eleven early Holocene sites in the Near East, classing them into nine groups. We show that damage and fragmentation of wheat spikelets probably due to dehusking makes identification problematic, and only when the abscission scar is well preserved is it possible to distinguish wild spikelets which shatter from domestic spikelets which adhere and separate during threshing. Barley spikelets were found to be less damaged and more easily identified, perhaps because the processing was less damaging. Einkorn was dominant over emmer on early sites, whereas on later sites emmer was dominant. Identifications presented here from eleven sites date from approximately 13000 to 8200 cal b.p. They give an incomplete picture, but no domestic cereals were identified during the PPNA (Pre-pottery Neolithic A). Early PPNB Aswad produced domestic barley but at other sites for this period the evidence is inconclusive. Unequivocal signs of domestic emmer spikelets appear during the Middle PPNB about 10,000 years ago but wild forms continue as part of the crop after this period. These conclusions are based on limited data. Future studies will undoubtedly produce a more accurate picture.