Archaeological Investigations at the Pine Snake Site, an Allen Phase Settlement on Flat Creek in Northwestern Cherokee County, Texas

The Pine Snake site is a recently discovered late 17th to early 18th century Caddo Indian archaeological site located on private land in the northwestern part of Cherokee County, Texas, in the valley of a westward flowing tributary to the Neches River. This is an area of the Pineywoods of East Texas that contains extensive numbers of Caddo archaeological sites along all major and minor streams. Post-A.D. 1400 Frankston phase and post-A.D. 1650 Historic Caddo Allen phase sites, especially cemeteries dating to either phase, are particularly abundant in this part of East Texas. This article summarizes the findings from archaeological investigations we completed at the Pine Snake site in late 2008. They have produced important information on the domestic archaeological record at a well preserved Allen phase habitation site

Luminescence Dates from the Tuinier Farm Site (41HP237), Hopkins County, Texas

The luminescence dating of ceramics has been applied with some considerable success in a variety of settings—and on different ceramic wares—in North America, but since the days of Alpha Analytic (a subsidiary of Beta Analytic) in the early to mid-1980s, there have been no luminescence dating of Caddo ceramic wares in Northeast or East Texas. Given the abundance of ceramics of several different kinds and styles at all Caddo sites, the luminescence dating of both plain and decorated sherds recovered in situ from these many sites should be explored since it is a method “that dates the manufacture and use of…ceramic objects [that] provide a closer relationship between the target event [when a site is occupied] and the dated event [the age determined by the luminescence on a sherd]. Luminescence is particularly well suited for the dating of ceramics since the method measures the time elapsed since vessels were last heated, usually corresponding to manufacture or use. In this article, we discuss the results of recent luminescence dating on a small sample of Caddo ceramic sherds at the Tuinier Farm site (41HP237)

An Unusual Late Aboriginal Assemblage from the Wilson Site (41SS186), San Saba County, Central Texas

The late aboriginal component in the Wilson Site in San Saba County is unusual in that most of the assemblage is consistent with that of Classic Toyah, but the diagnostic projectile point is an unnotched triangular arrow point instead of the typical Perdiz point. The absence of Perdiz points suggests that this component is associated with non-Toyah people and possibly dates to after 1700. Archaeological testing by the Llano Uplift Archeological Society (LUAS) to find supporting evidence for a historic date identified an Austin phase shell midden and a “Late Component” composed of triangular arrow points, end scrapers, a beveled biface and bone-tempered sherds, but no items of European manufacture. Complicating matters, the luminescence dating on a ceramic sample opens the possibility that the Late Component predates the currently accepted beginning of the Toyah phase

Radiocarbon and Luminescence Dating at Flamingo Bay (38AK469): Implications for Site Formation Processes and Artifact Burial at a Carolina Bay

This Article is brought to you for free and open access by the Archaeology and Anthropology, South Carolina Institute of at Scholar Commons. It ha

User Guide for Luminescence Sampling in Archaeological and Geological Context

Luminescence dating provides a direct age estimate of the time of last exposure of quartz or feldspar minerals to light or heat and has been successfully applied to deposits, rock surfaces, and fired materials in a number of archaeological and geological settings. Sampling strategies are diverse and can be customized depending on local circumstances, although all sediment samples need to include a light-safe sample and material for dose-rate determination. The accuracy and precision of luminescence dating results are directly related to the type and quality of the material sampled and sample collection methods in the field. Selection of target material for dating should include considerations of adequacy of resetting of the luminescence signal (optical and thermal bleaching), the ability to characterize the radioactive environment surrounding the sample (dose rate), and the lack of evidence for post-depositional mixing (bioturbation in soils and sediment). Sample strategies for collection of samples from sedimentary settings and fired materials are discussed. This paper should be used as a guide for luminescence sampling and is meant to provide essential background information on how to properly collect samples and on the types of materials suitable for luminescence dating. La datación por luminiscencia proporciona una estimación directa de la edad del último momento en el que el cuarzo o los minerales de feldespato se expusieron a la luz o al calor y que se ha aplicado exitosamente a depósitos, superficies rocosas y materiales expuestos al fuego en distintos contextos arqueológicos y geológicos. Las estrategias de muestreo son diversas y pueden ser individualizadas dependiendo de las circunstancias locales, aunque todas las muestras de sedimentos deben incluir una muestra segura que no haya sido expuesta a la luz y material para calcular la tasa de la dosis. La exactitud y precisión de los resultados de la datación por luminiscencia están directamente relacionadas con el tipo y la calidad de los materiales muestreados y los métodos de recolección de muestras en el campo. La elección del material de estudio para su datación debe incluir las siguientes consideraciones en torno a la idoneidad de poder reposicionar la señal de luminiscencia (blanqueador óptico y térmico), la capacidad de caracterizar el ambiente radiactivo que rodea la muestra (la tasa de la dosis) y el que no exista evidencia de una alteración posdeposicional (bioperturbación en suelos y sedimentos). Se discuten las estrategias de muestreo para la recolección de muestras de contextos sedimentarios y de materiales expuestos al fuego. Este artículo debe utilizarse como una guía para el muestreo por luminiscencia y tiene la intención de proveer información básica de cómo recolectar muestras y sobre los tipos de materiales apropiados para la datación por luminiscencia

Mortuary Caves and the Dammar Trade in the Towuti-Routa Region, Sulawesi, in an Island Southeast Asian context

Archaeological evidence from survey and cave excavation in the Towuti-Routa region of Sulawesi suggests the following sequence of late Holocene cultural change. Settled communities whose subsistence included an agricultural component had established themselves by the early centuries a.d. and began the use of caves for mortuary purposes. Extended inhumations are the oldest attested mortuary practice, overlapping in time with secondary burials in large earthenware jars dated to around a.d. 1000. The third, ethnohistorically described practice involved the surface disposal of the deceased, including the use of imported martavans for the elite, between approximately a.d. 1500 and 1900. This sequence of mortuary practices has not been documented elsewhere in Island Southeast Asia, although each practice has multiple parallels. The Towuti-Routa dammar trade, which was at its peak at the time of European contact, can perhaps account for the quantity of exotic items imported to the region but not the specifics of the mortuary practices.The Indonesian government’s permission for the research was granted by the Bureau of Research and Technology (Visa 278/SIP/FRP/SM/VII/2013). The fieldwork and laboratory work were facilitated by Bambang Sulistyanto (then Director) and Bagyo Prasetyo (Head of the Department of Prehistory) at the National Research Center of Archaeology in Jakarta, and by Made Sudarmika, then Director of the Makassar Archaeology Offic

Watson Brake, A Middle Archaic Mound Complex in Northeast Louisiana

Middle Archaic earthen mound complexes in the lower Mississippi valley are remote antecedents of the famous but much younger Poverty Point earthworks. Watson Brake is the largest and most complex of these early mound sites. Wry extensive coring and stratigraphic studies, aided by 25 radiocarbon dates and six huninescence dates, show that minor earthworks were begun here at ca. 3500 B.C. in association with an oval arrangement of burned rock middens at the edge of a stream terrace. The full extent of the first earthworks is not yet known. Substantial moundraising began ca. 3350 B.C. and continued in stages until some time after 3000 B.C. when the site was abandoned. All 11 mounds and their connecting ridges were occupied between building bursts. Soils,formed on some of these temporary surfaces, while lithics. fire-cracked rock. and,fired clay/loam objects became scattered throughout the mound fills. Faunal and floral remains from a basal midden indicate all-season occupation, supported by broad-spectrum foraging centered on nuts, fish, and deer All the overlying fills are so acidic that organics have not survived. The area enclosed by the mounds was kept clean of debris, suggesting its use as ritual space. The reasons why such elaborate activities first occurred here remain elusive. However some building bursts covary with very well-documented increases in El Nino/Southern Oscillation events. During such rapid increases in ENSO frequencies, rainfall becomes extremely erratic and unpredictable. It may be that early moundraising was a communal response to new stresses of droughts and flooding that created a suddenly more unpredictable food base

Glacial Lake Great Falls and the Late-Wisconsin-Episode Laurentide Ice Margin

Stratigraphic sequences containing sediments related to the glacial Lake Great Falls are exposed within the Missouri River valley in the region extending from around Helena to east of Great Falls, in west-central Montana (cf. Alden 1932; Calhoun 1906; Feathers and Hill 2011; Hill 2001; Hill and Valppu 1997; Lemke 1977; Lemke and Maughan 1977; Maughan 1961; Maughan and Lemke 1991; Montagne 1972; Robinson et al. 1969; Schmidt 1972, 1977, 1986; Stickney 1987; Vuke et al. 1995). The sediments were deposited in a lake formed when the Missouri River was blocked by a lobe of the Laurentide Ice Sheet (LIS). Direct dating of sediments using luminescence measurements appears to support a late-Wisconsin age for these stratigraphic sequences. This implies that a lobe of the LIS advanced into northern Montana and reached the present-day location of the Missouri Valley during the Last Glacial

2000 Luminescence dating of Middle Stone Age deposits at Die Kelders

Luminescence dating of sediments has not been used extensively for dating Middle Stone Age deposits in South Africa, despite its potential for contributing to a poorly dated record. Such deposits at Die Kelders cave, on the southern South African coast, consist of narrow bands of occupation debris separated by thicker layers of aeolian sands containing much less evidence of occupation. Homogeneous, aeolian sediments are usually considered ideal for luminescence dating. Here we report luminescence analyses of five samples from these sands that demonstrate sufficient bleaching prior to burial to validate dating and that yield ages of about 60-70 ka, in agreement with other evidence from sedimentology, archaeology and electron spin resonance. Lack of significant differences in the ages suggests the deposits accumulated fairly rapidly during the early part of the Last Glaciation

Applying Luminescence Dating of Ceramics to the Problem of Dating Arctic Archaeological Sites

Dating Arctic archaeological sites is challenging because of limited terrestrial bone and the high probability of old wood in northern regions. Luminescence dating of ceramic materials, abundant in western Arctic late Holocene archaeological sites, offers another potential source of chronological information. We set out to evaluate whether luminescence can provide chronological information in one particular region. We obtained luminescence ages on 14 pottery samples from seven study sites located on the coast and interior regions of northwest Alaska. Twelve of the luminescence dates are in accord with radiocarbon, tree ring, and artifact data from the study sites. Results indicate that all of the study sites may be older than previously established, suggesting previously unknown early Thule or Birnirk occupation of the coast and interior of northwest Alaska. We conclude that luminescence dating of ceramic materials from this region is possible and can complement other dating methods that are more widely accepted in the western Arctic. There is considerable potential through future applications of luminescence dating for improving northeast Asian and Arctic chronologies and expanding our understanding of circumpolar Holocene migration, cultural interaction, and change