High-Tech Foragers? Folsom and Later Paleoindian Technology on the Great Plains

Archaeologists generally argue that early (ca. 11,000–8000 B.P. populations on the North American Great Plains moved over very large areas, relying on sophisticated, biface-based flaked stone technology and on extensive resharpening and recycling of tools to cope with unpredictable access to raw material sources. This paper reviews the development of this reconstruction and considers the degree to which data from assemblages of Paleoindian flaked stone tools support it. Published information implies that patterns of raw material use vary greatly over the Plains, that bifaces were not the centerpiece of Paleoindian technology, that there are no published efforts to document an unusual degree of resharpening or recycling, and that the data that are available on these topics do not suggest that either was important. Detailed analysis of one assemblage, from the Allen site in southwestern Nebraska, carried out with these issues in mind, shows similar patterns. The great difference between what the literature says about Paleoindian technology and the documented character of that technology suggests that Paleoindian lifeways were far more variable than current discussions suggest.     

Stratigraphy and geochronology of La Playa archaeological site,Sonora, Mexico

La Playa archaeological site in northern Sonora, Mexico contains a long record of human activity that includes the Paleoindian period (terminal Pleistocene) and much of the Holocene. The size and complexity of La Playa has discouraged a systematic characterization of its stratigraphy and geochronology, a deficiency we redress in the study. We distinguished seven stratigraphic units ranging in age from >44,570 to 400 cal yr B.P. using ¹⁴C dates from charcoal and terrestrial gastropods found mostly in archaeological features. All of the buried (in situ) cultural remains are contained in Units B (4690–1580 cal yr B.P.) and C (1010–400 cal yr B.P.) and represent overbank deposition from the nearby Rio Boquillas. Occupation at the site peaks in Units B₄ and B₅, corresponding to the Cienega phase (2800–1800 cal yr B.P.) of the Early Agricultural period. This period coincides with the growth of early agricultural villages in the region and is marked at La Playa by thousands of archaeological features including roasting pits, human burials, and extensive canal irrigation systems. The presence of semi-aquatic and aquatic snails demonstrates that water was present year round in the canal systems constructed during this period. Stable and radiometric isotopic evidence suggests that early agriculturalists diverted ground water over several kilometers from the nearby Rio Boquillas. The extensive Cienega phase occupation ended after about 1700 cal yr B.P. with deep erosion of the site, an event also visible in alluvial records in southern Arizona that marked the end of the Early Agricultural period and significant changes in settlement organization in the region.     

Clovis,Folsom, and Midland components at the Debra L. Friedkin site,Texas: context,chronology, and assemblages

The archaeological transition from Clovis to Folsom and Midland in the North American Great Plains coincides with the end of the Pleistocene and onset of the Younger Dryas. Comparisons exploring the adaptive changes that took place during this period frequently employ regional-scale approaches. The focus on regional-scale analyses largely results from the dearth of sites repeatedly visited by multiple early Paleoindian groups. However, regional-scale comparisons have the potential to overlook smaller-scale differences. The Debra L. Friedkin site, Texas offers an opportunity to study Midland, Folsom, and Clovis technology and site-use at a single site. This paper presents the context and chronology of the Midland, Folsom, and Clovis assemblages and a site-scale analysis of lithics from the Friedkin site. It is argued that point production and late-stage reduction were primary activities, and the use of bifacial cores for flake tools was important throughout these occupation periods. Site use at Friedkin differs from early Paleoindian occupation at the nearby Gault site and expands our understanding of settlement and technological organization in the region.     

Molecular evidence of changing foodways across the Mississippian transition at the George Reeves site (11S650)

ABSTRACT

The George Reeves site (11S650) is a multicomponent village on the bluffs in the central American Bottom, Illinois. The site was occupied from the Late Woodland Rosewood phase through the Mississippian Lohmann phase. Pottery use and dietary variation between the Late Woodland and Emergent Mississippian occupations at the site were explored through stylistic analysis, pottery residue analysis, and compound-specific carbon isotopic analysis of pottery residues. Although more samples should be analyzed, diet and pottery use at George Reeves seems to have been varied, with maize present by cal AD 900–1000, but comprising a relatively small portion of lipid residues in pottery. Residue analysis indicates a C₄ presence in 5 of 16 sampled pots from the early Emergent Mississippian deriving from either maize or from meat from animals consuming maize. Pottery residues were mixed, showing C₃ and C₄ plants as well as meat and fish or shellfish. One residue showed a high incidence of C₄ contribution, most likely from Portulaca oleracea (common purslane), as well as large amounts of fish or shellfish and another C₃ plant. Residue from a ceramic pipestem indicates that maize may have been smoked, probably in the form of maize silk mixed with other nontobacco plants.     

Early Mesoamerican Garbage: Ceramic and Daub Discard Patterns from Cuauhtémoc, Soconusco, Mexico

Formation processes are all too infrequently addressed by archaeologists excavating in Mesoamerica. This paper examines refuse disposal patterns from the site of Cuauhtémoc on the Pacific coast of Chiapas, Mexico, to provide insight into how the site formed and how artifacts accumulated. This analysis uses materials dating between 1600–800 BCE which encompass the centuries before, during and after the late Early Formative or Early Olmec period (i.e., 1250–900 BCE). First, I employ sherds and daub from shared open-air middens and trash-filled pits to explore trash deposit formation through the 800 years that the site was occupied. Next, I use these same classes of data to make synchronic comparisons between five different depositional contexts dating to the Conchas phase (900–800 BCE). For all phases, these analyses demonstrate that pit features received more debris than open-air middens and that material in the latter contexts were more broken up. Further, the low density of daub from late Early Formative period contexts suggests that distinctive architectural customs may have been practised during this time. Conchas phase refuse indicates that waste disposal locations physically separated an elite residential zone from the rest of society and that elite contexts were more intensively used. Accounting for the formation of archaeological deposits allows for more nuanced interpretations of this early Mesoamerican village.

Great white shark teeth used as pendants and possible tools by early‐middle Holocene terrestrial mammal hunter‐gatherers in the Eastern Pampas (Southern South America)

Two great white shark (Carcharodon carcharias) teeth recovered in a terrestrial mammal hunter‐gatherers context in the Pampas are described. Associated lithic (mainly quarzite) tools, and the predominant exploitation of the Lama guanicoe relate the ancient inhabitants of the site with those of the early‐middle Holocene sites of the Area Interserrana of the Provincia de Buenos Aires. According to the stratigraphic context and the terrestrial fauna, the age of the deposit seems to be constrained to the early‐middle Holocene. The root tips of the shark teeth are marked by an artificial transvers groove fitted to tie a thread. Tooth edge serrations are strongly eroded, suggesting they were used as tools. We favour the hypotheses that the fish could have stranded on the beach or a small estuary in the neighbourhood, or that the teeth were obtained from the body of a pinniped attacked by a shark and sobsequenty found by humans. Copyright © 2003 John Wiley & Sons, Ltd.     

Investigating the peopling of North America through cladistic analyses of Early Paleoindian projectile points

The initial colonization of North America remains a controversial topic. There is widespread agreement that Clovis and related cultures of the Early Paleoindian period (∼11,500–10,500 BP) represent the first well-documented indications of human occupation, but considerable differences of opinion exist regarding the origins of these cultures. Here, we report the results of a study in which data from a continent-wide sample of Early Paleoindian projectile points were analyzed with cladistic methods in order to assess competing models of colonization as well as several alternative explanations for the variation among the points, including adaptation to local environmental circumstances, cultural diffusion, and site type effects. The analyses suggest that a rapidly migrating population produced the Early Paleoindian projectile point assemblages. They also suggest that the population in question is unlikely to have entered North America from either the Isthmus of Panama or the Midatlantic region. According to the analyses, the Early Paleoindians are more likely to have entered North America via either the ice-free corridor between the Laurentide and Cordilleran ice sheets that is hypothesized to have opened around 12,000 BP, or the Northwest Coast.     

Holocene paleoshorelines,water levels and submerged prehistoric site potential of Rice Lake (Ontario,Canada)

Rice Lake, located in the eastern Great Lakes of North America, has a high density of prehistoric (11–0.5 ka BP) terrestrial archaeological sites. It has been speculated that a large number of sites are submerged on the lakebed, as lake levels have risen >9 m since the arrival of Early Paleoindian peoples (∼11 ka BP). In order to better understand the submerged landscape and its archaeological potential, a detailed bathymetric survey and sediment-coring program was conducted across a 30-km² area of northeastern Rice Lake. Changes in Holocene water levels and shoreline positions were reconstructed by integrating core data with a digital elevation and bathymetric model (DEBM) that accounted for differential isostatic uplift and basin sedimentation. The DEBM was used to generate a series of maps showing changes in the lake paleobathmetry and paleogeography and areas of prehistoric archaeological potential.     

PHOSPHORUS ANALYSIS AT ARCHAEOLOGICAL SITES: AN OPTIMIZATION OF THE METHOD AND INTERPRETATION OF THE RESULTS

The application of phosphorus analysis to archaeological contexts can be considerably improved through ultrasonic extraction and the statistical evaluation of results through an analysis of variance. Such tools make the archaeological application of phosphorus analysis faster as well as more economical and coherent. This paper describes the features of these tools and provides a practical case: the Late Neolithic—Early Copper phase of the site ‘Polideportivo’in Martos, southern Spain.     

Evaluation of Fe isotope values as a provenance tool for chert artefacts from the north-eastern United States

Iron (Fe) isotope compositions of prehistoric stone tools and geological sources were compared to evaluate the robustness of this isotopic fingerprinting technique. Artefacts and source materials were collected from the Hatch site in central Pennsylvania, United States, where both veined chert (Bald Eagle chert) and stone tools coexist within several metres. Yellow artefacts (δ⁵⁶Fe = 0.38 ± 0.1, n = 7) and source materials (δ⁵⁶Fe = 0.42 ± 0.1, n = 8) isotopically matched within error. The source values also overlap yellow chert samples from three other Bald Eagle chert locations in the area. These values are different from six other chert locations in the north-eastern United States. These data suggest that the Fe isotope composition of chert artefacts reflect distinct geological sources. To enhance the mechanical characteristics of the stone tools, the chert experienced heat treatment, which induced a phase shift of the Fe oxide mineral goethite to hematite. This phase shift changes the colour of the chert to red. The red chert artefacts and source material also have overlapping Fe isotope values, but are 0.2‰ higher than the initial yellow chert. Experimental work where cherts were heated with different clays shows that Fe exchange with site soils induces the +0.2 fractionation. These data demonstrate that predictable Fe isotope fractionation occurs during heating, resulting in isotopically distinct artefacts.     

10,000 Years in the Rocky Mountains: The Helen Lookingbill Site

Abstract

Located in a spring-fed meadow at 2620 masl, Helen Lookingbill is a stratified, high-altitude open site in the Washakie Range of the Absaroka Mountains in NW Wyoming. The site contains cultural material ranging in age from Paleoindian through Late Prehistoric periods. Although the densest cultural deposits date to the Early Archaic (8000–5000 b.p., uncalibrated), other time periods are well represented. A 10,400 year old layer comprises the earliest component (Haskett/Hell Gap) in the main excavation area; above it is a series of Late Paleoindian, Early Archaic, later Archaic, and Late Prehistoric components. The major materials at the site are chipped stone and bone, while a deer bone bed dating between 6500 and 6800 b.p. is contained within the main excavation block. In addition to deet; the site contains the remains of mountain sheep, bison, porcupine, and other mammals. Located on and near both quartzite and chert stone sources, the mountain meadow served as a prehistoric camp site and yielded evidence of tool production, heat treatment, refurbishing, and use. Interdisciplinary research provides much information pertinent to understanding the nature of site occupation with implications for regional cultural dynamics, high altitude hunter-gatherer adaptations, and site formation processes.     

MATHEMATICAL MODELLING OF THE RELATIONSHIP BETWEEN NEOLITHIC SITES AND THE RIVERS IN XI’AN (SHAANXI PROVINCE,CHINA)*

Based on analyses of the ecological environments of the Neolithic sites along the Chan and Ba Rivers in the Xi’an area (Shaanxi Province, China), it was found that the characteristic factors of the sites had a very close relationship with the nearby river. The characteristic factors of Neolithic sites have been analysed and defined as mathematical parameters by statistical methods. A mathematical model of the human–land relationship between Neolithic sites and rivers has been established using the stepwise regression procedure REGRESS in SPSS^®. The mathematical model is Y = 496.153 – 4.833X₁ + 113.692X3 + 725.097X₅ – 27.683X₃X₄. It shows that the distance (Y) from a site to a river has a marked relationship with the site area (X₁), the river flux (X₃), the site location (X₅) and river ratio drop (X₄). The model shows that the relationship between the sites and the river is in accordance with the conclusions of archaeological research. The mathematical model not only offers theoretical guidance for the archaeological excavation of Neolithic sites in Xi’an, but also contributes to the archaeological environmental research of Xi’an Neolithic sites.      

Akhalkalaki: The Taphonomy of An Early Pleistocene Locality in the Republic of Georgia

As part of our investigations into the potential of the Republic of Georgia for providing information on early hominin occupation of Eurasia, we report here on Akhalkalaki, a large late Early Pleistocene locality located along the lower slopes of a Miocene andesitic cone. Originally excavated in the 1950s as a palaeontological site, it was re-opened in the 1990s and stone tools were found associated with the fauna, suggesting that it is also an archaeological occurrence. Excavations in the 1950s and 1990s uncovered thousands of bones of an early Galerian fauna, including the remains of new species of Hippopotamus,Equus , and Canis (Vekua, 1962, 1987) and dominated by the remains of Equus süssenbornensis. We present the stratigraphy of the site, which together with faunal correlations and reversed paleomagnetics indicates an age most likely in the late Matuyama Chron, probably between 980,000 and 780,000 years ago. Taphonomic analysis suggests that the fauna was deposited and buried over a short time period, and was heavily modified by carnivores, but we cannot demonstrate involvement by hominins. Based on evidence of abundant krotovina (animal burrows filled with sediment) and the lack of definitive evidence for hominin modification to the bones, the stone tools at the site may have been mixed in with the older fauna. The taphonomic characteristics of the Akhalkalaki bone assemblage are not readily explained with reference to assemblage formation processes developed with actualistic studies that have been mostly conducted in Africa, including carnivore dens, predator arenas, human hunting and scavenging, mass deaths, or attritional bone deposition. Because of extreme anthropogenic modification of the present environments, the temperate setting, and the presence of mainly extinct taxa, local models based on actualistic studies cannot approximate the mammalian ecology reflected in the Akhalkalaki bone assemblage. A few comparisons are made with preliminary taphonomic observations from Dmanisi, an Early Pleistocene Homo ergaster site not far away.     

Schooling the Quantum Generations: Textbooks and Quantum Cultures from the 1910s to the 1930s

Ever since Thomas Kuhn's influential The Structure of Scientific Revolutions (1962), textbooks have suffered a bad reputation. They have been accused of distorting—at times purportedly—history and of feeding students with an unacceptably simplified and optimistic view of science. This attitude started to change only in recent times. With the increase of attention paid not only to how theories are conceived, but also how they are practiced, disseminated, and appropriated, historians have rehabilitated textbooks as a legitimate site of knowledge production. In this paper, I adopt textbooks as an instrument to unfold multiple facets of the culture that allowed quantum physics to flourish between 1900 and the early 1930s. I organize the article around two stories about two major textbooks, i.e., Sommerfeld′s Atombau und Spektrallinien and Dirac′s Principles of Quantum Mechanics. I explore the complex pedagogical cultures underlying these two masterpieces and how they intersect local agendas.     

Plants and Technology: Current and Future Directions

Abstract

Located within the driftless area of southwestern Wisconsin, the Withington site provides a unique opportunity to examine the adaptive responses of Early Paleoindians exploiting this region. With a lithic assemblage dominated by Hixton Silicified Sandstone from sources over 170km to the north, chipped stone technological attributes and raw material diversity suggest that the occupants of the site were highly mobile, employed a mixed organizational strategy of toolstone transport, and possessed a wide knowledge of the lithic and social landscape. While our recent understanding of the early archaeological record of this region has progressed, a lack of published reports continues to hinder the incorporation of data from this area into larger models of Early Paleoindian subsistence and settlement. As part of an on-going research effort to address this, I present here a report and analysis of lithic material recovered from the site.     

Clovis Blades at Paleo Crossing (33ME274), Ohio

Abstract

This paper describes the previously undocumented Paleoindian lithic blade assemblage from the Paleo Crossing Site, Ohio (33ME274). Qualitative and quantitative comparisons of the Paleo Crossing blade assemblage to blade assemblages from other Paleoindian sites demonstrates its fragmented and utterly exhausted nature, but support its designation as Clovis. This is significant given that a majority of the Paleo Crossing toolstone outcrops 600 km southwest of the site in southern Indiana and western Kentucky, a prominent locale for Clovis prismatic blade manufacture. We propose that blade reduction was practiced for prolonging the use-life of distally retouched endscrapers, a prominent tool form at Paleo Crossing. Since use-wear and ethnographic evidence often show that endscrapers were used for hide-working, Paleo Crossing may be an appropriate venue to test for the presence of intense caribou hide-working.     

The oldest handaxes in Europe: fact or artefact?

Hominin presence is well documented in a number of Early Pleistocene and early Middle Pleistocene European localities. However, the evidence currently available indicates that Acheulean handaxes spread in the fluvial basins of Western Europe during MIS 11, ～400 kyr ago, associated with Homo heidelbergensis, although a number of early Middle Pleistocene Acheulean assemblages have been dated from MIS 16 onwards. For this reason, the magnetostratigraphic dating in Southeast Spain of two archaeological localities, the open-air site of Solana del Zamborino (SZ) and the rock-shelter site of Cueva Negra del Estrecho del Quípar (EQ), that put back the appearance of handaxes to the Early-Middle Pleistocene limit (Scott and Gibert, 2009) is of particular interest, as the new ages suggest that H. heidelbergensis was a contemporary of H. antecessor that had the ability to produce Levallois debitage and to control fire during the Early-Middle Pleistocene transition. However, we have detected a number of errors in the interpretation of the archaeological assemblage from the first site as well as striking discrepancies with the original faunal lists published for both localities, with several large mammal species that are omitted or arbitrarily changed to make the assemblages consistent with the new ages deduced from magnetostratigraphy. For this reason, we suggest that: (1) the finding of reverse polarity in the sediments sampled for paleomagnetism in SZ may simply record one of the polarity reversals that took place during the Brunhes Chron, although the use by Scott and Gibert (2009) of a composite stratigraphic column precludes correlating these levels with a specific reversal; and (2) the fauna and tools of EQ correspond to the late Middle Pleistocene sedimentary infillings of this karst site, while the samples taken for paleomagnetism belong to a previous sedimentary cycle during the Matuyama Chron. Such interpretations would be in better agreement with the age estimates provided by biostratigraphy and also with the currently accepted chronology for the appearance of Acheulean industries in Western Europe.     

Marking Identity through Cultural Cranial Modification within the First Sedentary Communities (Ninth to Eighth Millennium BCE) in the Near East: Tepe Abdul Hosein,Iran

This paper explores bioarchaeological evidence for cultural cranial modification (CCM; a.k.a. headshaping) in early Neolithic Near East and at Tepe Abdul Hosein (TAH), Iran, in particular. Skeletal remains from 12 Neolithic individuals (n  = 12) recovered from eight mortuary contexts were analysed for evidence of intentional CCM. The TAH remains are among the earliest Neolithic human skeletal remains in the world, dated to around 10 000 years ago. Five adult individuals have sufficient cranial remains to allow assessment of CCM. Of the remaining seven individuals, three are foetuses or perinates, for which no in vivo CCM was expected to be observed, two are subadults with no assessible cranial remains, and two adults have no associated cranial remains. Of the five adult individuals, which could be assessed for CCM, four display circumferential CCM, instigated by the use of two bands. Three are male, while the sex of the fourth cannot be estimated. The fifth individual displays no modification and is female. While all the modified individuals that can be sexed at TAH are male, the sample size is too small to draw extensive inferences as to the potential connection of CCM with any gendered sociocultural practices. Other possible motivations for CCM at TAH include elaboration of status differentiation or group affinity, the former of which can most likely be ruled out based on current understandings of early Neolithic societies in the region. The extent of the two‐band circumferential modification at TAH is significantly more pronounced than at Ganj Dareh, a contemporaneous site located within the same watershed. The discovery of different extents of headshaping within the same watershed, in relatively close proximity to each other, has a bearing on the understanding of the first sedentary Neolithic communities in southwest Asia and the elaboration of bodily difference and identity. Copyright © 2017 John Wiley & Sons, Ltd.     

A computerized system to determine the provenance of finds in archaeological sites using acoustic signals

Some archaeological excavations require the accurate determination of the provenance of finds (three-dimensional location and orientation) for a subsequent spatial analysis. The traditional manual measurement using a grid reference is not a very efficient registration method. Some proposed computerized solutions based on total stations, photogrammetry and DGPS, are more effective but have some limitations. This paper presents a new acoustic localization system (3D-LOCUS) for measuring the three-dimensional position of finds in archaeological sites. The system can also be used for registering the size, shape and orientation of artifacts. 3D-LOCUS basically consists of a set of wireless rod-like pointing devices that are localized with a network of intelligent nodes installed above the excavation site. Archaeologists use the pointing device as a stylus to locate and outline the object under study. The main technological characteristics of the system are: omnidirectional wideband acoustic transducers, Bidirectional Time-Of-Arrival (BTOA) estimation, redundant ranging and robust trilateration. 3D-LOCUS achieves an accurate registration, even if used simultaneously to the digging labor, or in noisy or turbulent airflow conditions. We tested the system in the Gran Dolina archaeological site (Atapuerca, Spain). The typical location accuracy is below 10 mm in natural conditions, and the achieved resolution is 5 mm, which allows us sketching objects with enough detail.