Retention of hunter–gatherer economies among maritime foragers from Caleta Vitor,northern Chile,during the late Holocene: evidence from stable carbon and nitrogen isotopic analysis of skeletal remains

On the basis of stable carbon and nitrogen isotope analysis of human remains, this paper provides evidence for the retention of hunter–gatherer economies among coastal inhabitants in northern Chile during the late Holocene – at the same time that inland populations were adopting agricultural economies. Coastal diets from the Caleta Vitor region of the Atacama Desert were dominated by marine-based foods, predominantly from upper trophic levels. The focus on reliable marine food resources is interpreted as a risk minimisation strategy in this marginal arid environment. Although these coastal hunter–gatherers adopted other goods and traditions from agricultural populations, their participation in this larger interregional exchange network did not affect their basic subsistence economies.     

Isotopic Evidence for Marine Consumption and Mobility in the Atacama Desert (Quillagua,Northern Chile)

Archaeological research in the Atacama Desert has recovered evidence of considerable cultural variability. This variability seems to have increased during the Late Intermediate Period (AD 950–1400). The oasis of Quillagua, located at the margins of the Loa River in northern Chile, between the Andes and the coast (70 km from the Pacific Ocean), has shown important evidence regarding this cultural diversity. The variety in the archaeological evidence found at Quillagua has been interpreted as the result of two different cultural influences at the oasis: the Pica‐Tarapacá who occupied the coastal and inland regions to the north of Quillagua and the Atacama who occupied the oasis and fertile areas southeast of Quillagua. Here, we present the results of stable carbon, nitrogen and oxygen isotope analyses of 23 individuals recovered from the Cementerio Oriente in Quillagua, in order to test whether the observed cultural variability is also reflected in diet and mobility patterns. Results from carbon and nitrogen isotope measurements indicate the importance of marine protein, as well as a contribution of maize in the diet of some individuals. Four individuals show low δ¹⁸O values, suggesting a possible highland or non‐local origin, whereas values for the remaining individuals are consistent with lowland populations. Together, the results support the idea that the Quillagua oasis represented an important site of interaction between the Tarapacá and Atacama cultures, with close contacts with the coast but also with the presence of individuals from the highlands. Copyright © 2015 John Wiley & Sons, Ltd.     

Gastrointestinal parasites in ancient South American camelid feces from the Atacama Desert (Pampa del Tamarugal,Tarapacá, northern Chile)

Faunal remains from archeological sites worldwide, especially feces and regurgitated pellets, are usually subjected to paleoparasitological examination, allowing the identification of past animal parasites. In this study, we analyzed 10 samples of South American camelid dung, which played an important role for the ancient human groups in the South-Central Andes, dated between 341 and 1635 calCE, from the Iluga Túmulos site (Pampa del Tamarugal, Tarapacá region, Atacama Desert, Chile). Microscopy examination revealed parasite remains in seven samples, in which oocysts of Eimeria macusaniensis and eggs of Lamanema chavezi/Nematodirus lamae, Trichuris sp., Moniezia sp., capillariids, strongylids, and unidentified nematodes were found. Although some of these species pose a potential health risk to camelids, most are not considered to be of major zoonotic importance, which could explain the absence of these parasites on human coprolites from this site analyzed previously. This first paleoparasitological study on camelid fecal remains from northern Chile sheds light on the occurrence of gastrointestinal parasites and its relationship with Andean ancient human populations and the environment.     

Staple or famine food?: ethnographic and archaeological approaches to nut processing in East Asian prehistory

Recent archaeobotanical studies in East Asia show that the use of wild food plants, particularly nuts, was important for not only hunter–gatherers but also early farmers. For example, recent archaeobotanical work has identified large quantities of nut remains from early Chinese rice farming sites dating 5,000–4,500 BC. In Japan, which introduced rice farming from China around 1,000–500 BC, archaeobotanical data have shown continued exploitation of nuts even after the introduction of rice farming. Therefore, the first appearance of farming does not appear to have immediately impacted the subsistence system, although it may have changed cultural perceptions of food plants, eventually rice replacing nuts as a staple food. To explain the cultural implications of this shift in emphasis, it is necessary to investigate people’s routine subsistence activities with reference to available ethnographic information on non-mechanised plant processing. The ethnographic data provide insights into ancient nut processing, including possible methods, tools, choices of working locations and labour scales. Conceptual modelling based on ethnographic observations of the range of nut-processing practices will also aid interpretations from newly developed methods, such as starch residue analyses. The resulting archaeobotanical, archaeological and ethnographic picture may help to further explore past social organisation and social perceptions of plant foods.     

Six seasons of wild pea harvest in Israel: bearing on Near Eastern plant domestication

Harvest experiments of wild crop relatives are essential for our understanding of the biology of wild plants embodied in the economy of ancient forager communities. Most of the previous experimental harvest reports spanned a single season and therefore are unable to address questions concerning long-term yield potential. Herein we report on six consecutive harvest seasons taking place at four sites in Israel that harbour wild pea populations: three typical Pisum fulvum sites and one typical Pisum elatius site. Three out of the four sites showed no indication of a decline in grain yield as a result of repeated harvest and the removal of a considerable portion of mature seeds. Site-specific factors seem to have a strong influence on the grain yield as no seasonal yield similarity was observed between adjacent and ecologically similar sites harbouring the same wild pea taxon. The erratic year-to-year wild pea yield we observed calls for a reassessment of the presumed role of grain legume species in Near Eastern hunter–gatherers' diet. Combined with published data on cultivation of wild pea, our results are inconsistent with models suggesting protracted domestication of Near Eastern grain legumes or with the preliminary attempts to apply Niche Construction Theory to the study of plant domestication in the Near East.     

Silver lining: evidence for Inka silver refining in northern Chile

Prehistoric silver purification using lead cupellation has been documented in multiple places throughout the Andes, but direct evidence of the Inka use of this technology has remained elusive. In this study, we use X-ray fluorescence, scanning electron microscopy, and electron-microprobe analysis to document direct evidence of Inka period (AD 1400–1532) silver purification using lead cupellation in the Tarapacá Valley of northern Chile. Local metalworkers used wind-driven huayra furnaces to produce pure lead metal, sustaining temperatures of ca. 900–1100 °C to smelt lead-bearing ores that may have included galena. The lead metal was then used in open-vessel cupellation of silver-bearing ores, some of which may have been cupriferous and derived from the nearby Inka mines at Huantajaya. Phase analyses of the slagged interiors of bowl-shaped ceramic vessels used for cupellation indicate that the metalworkers maintained the oxidizing environment and temperatures between 800 and 1100 °C requisite for cupellation. We argue that the Inka introduced this technique to Tarapacá metalworkers. The absence of finished silver artifacts in local valley contexts suggests that the refined silver was removed from the valley for use elsewhere in the empire.     

The prehistory of northern Chile: A synthesis

Northern Chile, part of the south central Andes, consists of two main ecological subareas: extreme northern Chile, including the western valleys, and the Atacama Desert and oases. Different ecological conditions obtain in each subarea: puna, altiplano, and precordillera in the highlands; valleys, the desert, and oases in the intermediate zone; and coastal environments along the Pacific shores. In prehistoric times, all these environments were very interconnected. There are three different cultural traditions in the local prehistory: the early hunting and gathering tradition (10,000–4000 B.P.), the Chinchorro Tradition (7500–2500 B.P.), and the Altiplano or Andean Tradition (3000–0 B.P.). This proposed sequence is described, with emphasis on the early Chinchorro adaptations, including the important patterns of mummification, and its possible relation to tropical forest groups of the Amazon basin; and the Pre-Tiwanaku and later Tiwanaku and Inca developments, in relation to the circum-Titicaca region. The data presented in the paper are further developed to explore ideas and hypotheses for future research.     

Starch grain characterization of Prosopis chilensis (Mol.) Stuntz and P. flexuosa DC,and the analysis of their archaeological remains in Andean South America

The fruit (pods) of Prosopis (Fabaceae) are frequently recovered from pre-Hispanic Argentinian archaeological sites, suggesting that this genus was of importance in ancient economies in this region. Yet it is only recently that archaeobotanists have begun to carry out systematic research into this genus. Therefore many questions remain to be addressed concerning the food value of Prosopis fruit, and its potential contribution. This paper examines starch from the pods of two species, Prosopis flexuosa and Prosopis chilensis, for the purposes of describing and classifying their morphological features and biometrical parameters. Pods of both species were gathered from two extremes (northern and southern) of the Hualfín Valley, Catamarca, Argentina. Starch abundance is estimated and compared with that of Zea mays, an economically important plant with high concentrations of starch. This paper reveals that Prosopis pods contain very low amounts of starch compared to starch-rich edible species. Despite this, the recovery of Prosopis starch grains can be successfully used to assess archaeological tool uses. Prosopis starch grains were found to be highly variable in shape. Grain size ranged between 10 and 20 μm. Granule irregularity and the high birefringence under polarized light are two of the most important diagnostic features. No significant statistical differences were found in the structure (morphology, size and hilum) of the starch of the same species from both localities. Finally, the implications for the role of this plant in past societies are discussed.     

Andean Ores,Bronze Artifacts,and Lead Isotopes: Constraints on Metal Sources in Their Geological Context

With a focus on bronze production in the south-central Andes during the Middle Horizon, this study reports the first archaeological use of lead isotope analysis to investigate metallic ores and metal artifacts in the Andean zone of South America. Because the vast majority of metal deposits in the Andean cordillera formed in a convergent plate boundary setting, lead isotope compositions of most Andean ore sources are not unique. Lead isotope ratios of central and south-central Andean ores define four geographically distinct ore lead isotope provinces, oriented and elongated parallel or sub-parallel to the trend of the Andean cordilleras. Consequently, ore lead isotope ratios vary strongly from west to east along transects through the coast, highlands, and altiplano, but they exhibit much less variation from north to south. The strong west-to-east variation in ore lead isotope signatures allows discrimination between ore bodies, and ultimately between metal artifacts, as a function of macro-ecozone location: coast, junga-qiswa, puna, and altiplano. We present the most up-to-date database of ore lead isotope signatures for the south-central Andes including those determined for ores we sampled over an approximate 250,000-km² region within Bolivia, northern Chile, and northwest Argentina. Lead isotope signatures of Cu-As-Ni bronze artifacts from Tiwanaku (altiplano capital) and San Pedro de Atacama (desert oasis entrepôt) establish that altiplano and high sierra ore bodies provided the metal for both assemblages. Conchopata (Wari) arsenic bronze artifacts exhibit lead isotope ratios compatible with the Julcani (Huancavelica) copper sulfarsenide deposit.     

Environmental impacts around the time of Norse landnám in the Qorlortoq valley,Eastern Settlement,Greenland

Palynology, radiocarbon dating, and open-section stratigraphies from archaeological trenches are used to examine the impact of human activity around the time of Norse landnám on vegetation and landscape associated with a small farm (Ø34) in the Qorlortoq valley, Eastern Settlement, Greenland (61° N 45° W). Peat deposits from a mire abutting the Norse ruins revealed a discontinuous palaeoenvironmental record containing a possible hiatus from ca. AD 410–1020. Palaeovegetational data were recovered either side of this period. Pollen assemblages suggest that open Salix scrub dominated the landscape during the pre-settlement phase. The later phases of landnám resulted in the creation of hay fields and heavily-grazed grassy heath. Site abandonment is reflected by a re-expansion of Salix. This occurs shortly before the onset of deposition of a Sphagnum peat, dated to cal AD 1420–1630 (2σ) and reflecting an increase in mire surface wetness, probably in response to a deteriorating climate. Radiocarbon dates were obtained on peat and plant macrofossils sampled from either side of the proposed hiatus at two different but closely-spaced (<20 m) locations across the mire. These produced significantly different dates for the cessation of peat formation in the pre-landnám period (cal BC 2130–1770 and cal AD 240–410 respectively), but near-synchronous dates for the recommencement of peat growth (cal AD 890–1150 for peat and a probably more reliable interval of cal AD 1020–1190 based on plant macrofossils). It is suggested that this hiatus may represent the first direct evidence for peat cutting in Norse Greenland.     

Characterization of dyes in ancient textiles from Yingpan,Xinjiang

In this paper we analyzed the natural dyes in well-preserved, ancient textiles from Yingpan, an important archaeological site on the Silk Road, using high-performance liquid chromatography with diode array and mass spectrometric detection. Dyes were removed from textile fibers using a soft extraction method (pyridine, water and oxalic acid). Two species of madder-type plants, Rubia tinctorum and Rubia cordifolia were identified as the dye sources in red and brown samples. We also were able to detect unusual flavonoid glycosides in yellow and green woolen yarns, although we have not been able to pinpoint with certainty a specific plant that may have been used to produce this dye(s). On the other hand, we found that yellow and green silk threads had been colored with protoberberine-type dyes, probably obtained from species of cork tree, Phellodendron spp., and/or other protoberberine producing plant. We propose that the textile dyes found at Yingpan reflect a merging of Eastern and Western practices and technologies during the 800-year period (206 BCE–618 CE) encompassing the early years of the Silk Road.     

Sweet potato (Ipomoea batatas) and banana (Musa sp.) microfossils in deposits from the Kona Field System,Island of Hawaii

Analysis of plant microfossils (pollen, phytoliths, starch grains and xylem cells) was carried out on 12 soil samples from a variety of pre-contact archaeological features in South Kona within a portion of what has been termed the Kona Field System, on the Island of Hawaii. The oldest radiocarbon ages of the sampled deposits are 1300–1625 AD and 1310–1470 AD. The pollen and phytolith evidence suggests a change from more to less trees and shrubs in the area as a result of human activity. We found phytoliths of banana (Musa sp.) leaves in most and starch grains and xylem cells of tuberous roots of c.f. sweet potato (Ipomoea batatas) in all of the samples, suggesting that the sampled features were associated with these crops and that both crops were cultivated intensively within the study area. Higher concentrations (volumetric) of starch and xylem in samples from older deposits suggest that cultivation was more intensive then. The apparent absence of starch and xylem remains of other tuberous crops archaeologically identified elsewhere in Polynesia suggests that tuberous cropping within the study area was mono-specific.     

A short note on banana (Musa) phytoliths in Lapita,immediately post-Lapita and modern period archaeological deposits from Vanuatu

We present results of phytolith analysis of deposits from three prehistoric settlement sites in Vanuatu: the small islands of Vao and Uripiv off the north east coast of the main island of Malekula and at Mafilau on the west coast of Epi Island. Samples from Vao Island coarsely encompass the period from Lapita times (c. 3000 BP) to the present. The data from this site suggest deforestation by people, with a decrease in palms and increase in grasses. The data from the three sites show evidence of an introduced cultigen during different prehistoric periods. Banana (Musa) phytoliths were found in one recent Vao layer (500 BP-present) and in Mafilau layers, the latter representing the immediate post-Lapita period (c. 2800–2500 BP). This phytolith type was also found at Uripiv in Lapita layers (c. 3000–2700 BP). Banana phytoliths are diagnostic so their presence in archaeological deposits in Remote Oceania, outside their natural distribution, provides secure evidence of cultivation. This demonstrates the potential of this line of evidence for identifying both the cultigens transported by early colonists and subsequent plant introductions. The data provide the first direct evidence of banana cultivation at a Lapita site in Remote Oceania and support the contention that horticulture was an integral part of the Lapita Cultural Complex.     

Isotopic investigation of pre-Hispanic macaw breeding in Northwest Mexico

The pre-Hispanic settlement of Paquimé (ca. 1200–1450 AD) lay outside of urban Mesoamerica in arid northern Chihuahua, Mexico, yet the excavated remains of 322 scarlet macaws, tropical parrots whose northernmost habitat is 500 km to the south, suggest that Paquimé had relationships with distant communities. Here, carbon and oxygen stable isotope analysis of 30 macaw bones determines whether the Paquimeños actively bred these parrots or traded with Mesoamerican groups to obtain the birds. The δ¹³C values indicate that the macaws ate a diet of C₄ plants, foods that were unavailable to wild macaws. In addition, δ¹⁸O data suggest that the majority of the macaws spent their entire lives at Paquimé. We conclude that the ancient Paquimeños were in fact breeding scarlet macaws, although one bone with δ¹⁸O values outside the local range suggests that the breeders also maintained exchange ties with the source areas of the birds. By confirming that Paquimeños implemented a system of local macaw reproduction outside the Mesoamerican region itself, this analysis provides new evidence about the economic and ideological interdependence of pre-Hispanic societies in the Americas. It is also suggestive of the pre-industrial capabilities of humans to extend the natural ranges of animal species.     

The Unbearable Lightness of Bones: Memory,Emotion, and Pedagogy in Patricio Guzmán’s Chile,La Memoria Obstinada and Nostalgia De La Luz

Focusing on two documentary films by Patricio Guzmán, Chile, Obstinate Memory (1997) and, especially, Nostalgia of the Light (2010), this paper examines some of the relations between neoliberal violence (during and after the Pinochet dictatorship), memory, knowledge and emotionality, both historical and personal. It does so by reading and reviewing the actions, narratives and experiences of a group of astronomers, archaeologists and geologists who work in the Atacama desert of northern Chile and a group of women who search for the remains of their loved ones, victims of political violence, in the same desert within the shifting contexts of cinematic spectatorship. Attentive to the possibilities and pitfalls of empathic identifications and connections, it also considers the ethical and political implications of the interplay of cinema (Guzmán), photography (Paula Allen) and poetry, sky writing and "land art" (Raúl Zurita).     

Plant microfossil analysis reveals disturbed forest and a mixed-crop,dryland production system at Te Niu,Easter Island

Plant microfossil analysis was carried out on 12 soil samples from a variety of landscape features at three locations (100–250 m a.s.l.) along a 950 m transect at Te Niu, Easter Island. Pollen and phytolith assemblages were dominated by palms and ground ferns, and suggested disturbed forest. We identified pollen of bottle gourd (Lagenaria siceraria) and starch grains of the common yam (Dioscorea alata), sweet potato (Ipomoea batatas) and taro (Colocasia esculenta). The data suggest a mixed-crop, dryland production system at Te Niu dominated by yam and sweet potato, and supplemented by taro and bottle gourd. The data provide direct evidence of crop type and range, supporting the indirect evidence (topographic and landscape features, field and historical research, comparisons with elsewhere in the Pacific) that much of the rock covered landscape of Easter Island was used for intensive horticulture.     

Red abalone collecting and marine water temperature during the Middle Holocene occupation of Santa Cruz Island,California

Oxygen isotope values derived from prehistoric mussel (Mytilus californianus) shell calcite are used to determine whether sea-surface temperatures in the vicinity of the Punta Arena site (CA-SCRI-109) on Santa Cruz Island, California, were cooler than present between 6300 and 5300 cal BP. This site and others in the western sector of the island dating to this period are distinctive because of the presence of large red abalone (Haliotis rufescens) shells, a species that historically has been subtidal around Santa Cruz and the other northern Channel Islands. Comparison of temperature values derived from archaeological shells with those from modern mussel shells, along with water temperatures derived from satellites, indicates that waters were cooler during the 6300 to 5300 cal BP period. These results are consistent with a previous study and support the interpretation that collection of red abalone during the 6300–5300 cal BP period was partly the result of cooler water temperatures that made this large mollusk more available to foragers in the intertidal or shallow subtidal zone.     

GEOCHEMICAL ANALYSIS OF VITREOUS ROCKS EXPLOITED DURING THE FORMATIVE PERIOD IN THE ATACAMA REGION,NORTHERN CHILE*

Petrographic analysis and geochemical characterization studies were carried out on vitreous dacite and/or rhyodacite artefacts from Formative period archaeological sites in the upper Salado River Basin in the Atacama Desert, northern Chile. These were compared with samples taken from two source areas located within the subregion, named Linzor and Paniri. Source samples and archaeological specimens were analysed by inductively coupled plasma – mass spectrometry (ICP–MS) combined with optical emission plasma – mass spectrometry (ICP–OES) and atomic absorption spectroscopy (AAS). Results from the limited number of samples analysed indicate that the Linzor source seems to have been the primary source exploited during the Early and Late Formative periods in the Salado River Basin.     

Perimortem trauma in the Atacama Desert and social violence during the late Formative period (2500–1700 years BP)

This paper describes a case of a mass grave containing three naturally mummified adults with multiple traumas to the skeletal and soft tissues, buried in an isolated and informal grave in one of the valleys that traverses the Atacama Desert, north of Chile. These traumas do not appear to be indicative of post‐depositional alterations. Instead, we hypothesise that the observed marks correspond to lethal perimortem trauma, the result of acts of extreme violence brought to bear on the three individuals. Three radiocarbon dates from the site identify that the burial occurred circa 2000 BP in the Azapa Valley, which corresponds to an epoch of important cultural changes linked to the development of farming communities that broke away from an ancient marine hunter–gatherer cultural tradition. Copyright © 2009 John Wiley & Sons, Ltd.     

Ground cereal food preparations from Greece: the prehistory and modern survival of traditional Mediterranean ‘fast foods’

Archaeobotanical remains of ground cereals from prehistoric northern Greece are discussed in this paper within the context of ethnographic and textual evidence for similar food preparations encountered in countries of the Mediterranean and the Middle East. The archaeobotanical remains consist of ground einkorn and barley grain, stored in this form, from the sites of Mesimeriani Toumba and Archondiko respectively, located in the region of central Macedonia, northern Greece. The results of published pilot studies involving macroscopic, experimental, and scanning electron microscopic examination of these archaeological finds seem to suggest that these products correspond to preprocessed cereals, stored in this form. It is also likely that some at least of these finds were produced from boiled and subsequently ground cereal grains. This practice identified in the prehistoric material is similar to various forms of processing cereals still widely encountered in rural areas of modern Greece and other circum-Mediterranean countries. These products are known in Greece under the names of pligouri (bulgur) and trachanas. Through a combined examination of archaeobotanical, ethnographic, and textual evidence it is argued that the idea of pre-processing cereals for piecemeal consumption throughout the year is of considerable antiquity in this part of the world. Drawing information from food science research on similar, modern traditional preparations of the same geographical region, the paper highlights the advantages of pre-processing cereals for later consumption, which offers insights into likely prehistoric subsistence practices. Parboiling cereal grains or mixing grains with milk products in the summer would have made excellent use of seasonally available ingredients by converting them into nutritious and storable foodstuffs, which could then be consumed as part of daily meals with very little additional cooking effort and fuel. This ease of conversion into a filling meal may justify us considering them as ‘traditional fast foods’.