Storage adaptations among hunter–gatherers: A quantitative approach to the Jomon period

Food storage economies among hunter–gatherers have been fundamentally important in research within anthropological archeology. It is well recognized that food storage was a key element in the evolution of hunter–gatherer societies. This paper examines storage facilities utilizing a digital planimeter to evaluate the volume and morphology of storage pits in the Jomon period (ca. 13,750–500 cal. BC). Quantitative analysis of Jomon storage pits shows temporal and spatial variability in terms of size. This research demonstrates that the quantitative analysis of storage pits is an effective way to improve our understanding of storage and its role in the Jomon economy in particular and subsistence adaptations in general. Thus, this approach has potential applications to other storage economies worldwide.     

Late Preceramic Peru

This paper presents a synthesis of current knowledge of Late Preceramic Peru (ca. 4450–3800 B.P.), a field of study that is less than 50 years old. A brief history of investigations and discussion of chronological systems are presented. A review of Late Preceramic achievements concentrating on subsistence economies and technology is followed by discussion of the social world of Late Preceramic Peru and current consensus and disputes regarding culture processes. Extensive long-distance exchange, farming, and social complexity are first clearly seen in the archaeological record during this time period. Nevertheless, the significance of this evidence with regard to the nature and intensity of the culture practices and processes that they represent is currently under investigation and in contention.     

Monongahela Subsistence-settlement Change?

Abstract

The Late Prehistoric (c. A.D. 1050/1100–1635) Monongahela tradition of southwestern Pennsylvania and portions of adjoining states has come to be associated with specific subsistence-settlement traits. These include a heavy dependence on maize-based agriculture, large percentages of villages in upland locales, and use of semisubterranean storage facilities. In the traditional approach, that entails the construction of a series of sequential time periods, changes in subsistence and settlement traits are most often interpreted to have occurred at the boundaries of the time periods. These periods are defined on the basis of pottery style changes and the addition of European artifacts. An accumulation of data now allows for statistical analysis of posited changes in Monongahela tradition settlement and subsistence traits. Results of this study do not support the proposed subsistence and settlement pattern shifts at time period boundaries. Rather, the results support the position of continuous variation in the settlement and subsistence traits through the entire sequence with no evidence of regional uniformity.     

Strontium isotope analysis to reveal migration in relation to climate change and ritual tooth ablation of Jomon skeletal remains from western Japan

A gradual population increase accompanying climate cooling has been evinced as having occurred in western Japan during the Middle (ca. 5000–4000 years BP) to Late-Final Jomon period (ca. 4000–2300 years BP). We test the hypothesis that this population change paralleled increasing human migration. We also test the archaeological hypothesis that types of ritual tooth ablation can be used to distinguish between locals and immigrants during the Late-Final Jomon period. We measured strontium isotope ratios in human skeletal remains from the Middle Jomon Ota and the Late-Final Jomon Tsukumo sites located in the Sanyo region of western Japan. Tooth enamel and bone were analyzed, and modern plant samples were collected in the areas surrounding the two sites to make a map of environmental strontium isotope ratios. The biosphere strontium isotope ratios correlated well with the underlying geology, enabling us to put forth a hypothesis of immigrants’ origins. There were no migration pattern differences between the Middle and Late-Final Jomon groups, indicating that the gradual population increase was caused by an increase in the indigenous population. All the Tsukumo individuals are locals, and this finding indicates that types of tooth ablation did not distinguish between locals and immigrants. Alternative hypotheses for the presence of different tooth ablation types in the Jomon society should be explored.     

Animal Resource Exploitation among the Virgin River Puebloans in the American Southwest

Abstract

A review of the literature documenting faunal remains recovered from 16 archaeological sites attributed to the Virjin River Puebloan (VRP) tradition (ca. 300 B.C.–A.D. 1200) of the American Southwest was conducted to identify the importance of wild animal resources to the subsistence strategy. The Number of Individual Specimens (NISP) was counted (NISP = 16,386) and sorted by taxa and animal size categories to explore differences in the distributions of faunal remains by archaeological recovery strategy, site type, physiographic location, and chronology. The most significant factor in the differential use of animal resources among the VRPs was physiographic location. Desert lowland sites had greater species diversity. Sites in the intermediate St. George Basin had more large mammals such as deer, and sites located on the higher plateau had more small mammals such as lagomorphs. These results indicate that the subsistence strategy varied across diverse environmental conditions, but animal resources were always an integral part of the VRP adaptation until their abandonment of the region in the early 13th century A.D.     

Strontium isotope evidence of migration and diet in relation to ritual tooth ablation: a case study from the Inariyama Jomon site,Japan

Ritual tooth ablation was extensively practiced among Jomon (Japanese Neolithic) societies in their final phase (ca. 3000-2300 BP). This tradition includes two different tooth ablation patterns, type 4I and type 2C, referring to extraction of the mandibular incisors and canines, respectively. However, the reason for this difference is unclear. Previous carbon and nitrogen stable isotope analysis of human remains from the Inariyama shell mound revealed that type 4I individuals were more dependent on terrestrial resources and type 2C individuals on marine resources. To test this hypothesis, we performed strontium (Sr) isotope (⁸⁷Sr/⁸⁶Sr) analyses on the same skeletal remains and on modern plants around the site. Because Sr isotope ratios of plants differ according to the local geology and seawater has a consistent Sr isotope ratio, the Sr isotope ratios of tooth enamel can reveal both migration and diet. Comparing Sr isotope ratios in plants and seawater with those of tooth enamel, we identified four possible immigrants. Type 4I locals had significantly higher Sr isotope ratios than type 2C locals. The ratios of the type 4I and type 2C locals were close to those of terrestrial plants and seawater, respectively, suggesting that type 4I locals had incorporated much Sr from terrestrial resources and type 2C locals from marine resources. These results support the hypothesis that ritual tooth ablation reflects dietary differences throughout an individual’s life, and they suggest possible occupational differentiation among the Jomon people.     

Pottery production on Rishiri Island,Japan: perspectives from X‐ray fluorescence studies

Energy‐dispersive X‐ray fluorescence (EDXRF) was used to determine the minor and trace element composition of 54 sherds of pottery dating from the Final Jomon to Okhotsk periods. The majority of the sherds came from Rishiri Island, Japan. Principal component (PC) scores were calculated using the log transformed concentration values, and groups were sought in the PC scores using kernel density estimates (KDEs). Two main groups were found in the data; linear and quadratic discriminant analysis classified both groups successfully. Significant differences in the concentrations of Cu, Fe, K, Nb, Pb, Rb, Th and Zr were found to exist between the two groups. The lack of correspondence between chronological ware types and geochemical groups implies that the same raw materials and paste recipes were in use during the Epi‐Jomon and Okhotsk eras on Rishiri Island. One possiblity is that the Epi‐Jomon and Okhotsk potters used the same clays and tempers, since no other alternatives were available. Alternatively, the Okhotsk potters could have adopted the same paste recipes as the Epi‐Jomon potters, or the Okhotsk pottery tradition could be descended from the Epi‐Jomon pottery tradition.     

New data and new issues for the study of origin of rice agriculture in China

China was one of the major centers for the origin of agriculture in the world. The origins of agriculture in China, especially the origin of rice agriculture, made a significant contribution not only to the occurrence of Chinese civilization but also to the development of world history. Recently, the study on the origin of rice agriculture has attracted the attention of the academic community due to the dramatic development of archaeobotanical research in China. In recent years, the flotation technique has widely implemented in archaeological excavations in China. As the result, a tremendous amount of plant remains have been recovered from archaeological sites, including those much related to the study of early rice agriculture. The new data provide direct archaeological evidence for, and raise some new issues about, the origin of rice agriculture in China. For example, the rice remains from the Shangshan site, dated to ca. 10,000 cal. B.P., suggest the beginning of rice cultivation regardless of whether that rice was domesticated or not. The quantitative analysis of plant remains recovered by floatation from the Jiahu site, dated to ca. 8,000 cal. B.P., revealed that the subsistence of the Jiahu people mainly relied on fishing/hunting/gathering, while the products of rice cultivation and animal husbandry were only a supplement to their diet. The ongoing excavation, with floatation and water-sieving, at the Tianluoshan site, dated to 6,000 to 7,000 cal. B.P., suggests that rice farming, though important, was only part of a broader subsistence pattern of the Hemudu Culture, and rice domestication culminated after 6,500 B.P and the beginning of rice domestication remain unclear.     

Hunter-gatherer cultural dynamics: Long- and short-term trends in Australian prehistory

Recent evidence indicates that a wide range of environmental sectors of Greater Australia had been peopled between ca. 30,000 and ca. 40,000 B.P. Differences in regional Pleistocene patterns of settlement, subsistence, and demography are becoming increasingly evident—such as those between central arid Australia and sub-Antarctic Tasmania. It now remains to model and explain the extremely long-term Pleistocene cultural sequences (spanning tens of thousands of years), in contrast to the more short-term cultural sequences that characterize, for example, the mid-late Holocene period of mainland Australia. While explanations remain unresolved, the latter period indicates the widest range of regional sociocultural and demographic changes.     

Diffuse idiopathic skeletal hyperostosis in Late Jomon Hokkaido,Japan

The purpose of this study is to describe and analyse the evidence for diffuse idiopathic skeletal hyperostosis (DISH) in samples of human skeletal material recovered from Late Jomon (ca. 1500–300 BCE) and Okhotsk (CE 500–900) cultural period sites, northwestern Hokkaido, Japan. Two individuals from the Jomon period assemblage (n = 14) exhibited lesions consistent with DISH, while the larger Okhotsk sample (n = 39) was free of this condition. The aetiology of this condition is reviewed with reference to the clinical and bioarchaeological literature, in addition to behavioural and environmental considerations specific to this region and these time periods. Copyright © 2006 John Wiley & Sons, Ltd.     

Late Holocene human impact on the vegetation around Mizorogaike Pond in northern Kyoto Basin,Japan: a comparison of pollen and charcoal records with archaeological and historical data

Pollen and macroscopic charcoal analyses of AMS radiocarbon-dated sediment from Mizorogaike Pond, located near Japan’s ancient capital established in AD 794, were used along with archaeological and historical data to reconstruct vegetation change in the northern Kyoto Basin since 7300 cal yr B.P. Between ca. 7300 and 3400 cal yr B.P. (Early to Late Jomon period), the site was surrounded by warm-temperate forest composed of Quercus subgenus Lepidobalanus and Q. subgenus Cyclobalanopsis with Celtis/Aphananthe trees. With the occurrence of fire disturbance, Q. subgenus Lepidobalanus increased from ca. 3400 to 1400 cal yr B.P. (Late Jomon to Kofun periods). In the early seventh century (Asuka period), Pinus started to increase, coinciding with a significant charcoal peak, probably related to the operation of roof tile kilns near the site. Pinus continued to increase and Q. subgenus Cyclobalanopsis decreased through the seventh to tenth centuries (Asuka to Heian periods). Further increase of Pinus occurred in the eleventh century, possibly reflecting the establishment of the manor of Kamigamo Shrine. From the eleventh to seventeenth centuries (Heian to medieval periods), no significant vegetational change or fire disturbance took place. In the eighteenth century, the landscape became totally open, with poor vegetation and sparse Pinus woodland. The medieval and early modern landscapes reconstructed from the palaeoecological record are rather similar to those described from studies of ancient artwork and historical documents. This study demonstrates that late Holocene vegetation change in the northern Kyoto Basin was closely tied to anthropogenic activities, such as the pottery industry and fuel wood collection.     

Pig exploitation in the southern Kanto region,Japan

This study investigates changes in past human and animal relationships by focusing on pig (Sus scrofa) remains excavated from archaeological sites in southern Kanto, Japan. Pigs and humans have had a close relationship since prehistoric times and the process of change in this relationship, including possible domestication, is one of the major issues in Japanese zooarchaeology. This study attempts to gain a better understanding of the nature of past interaction between humans and pigs by investigating their relative importance compared with other vertebrate remains, kill‐off patterns, and changes in their size and shape at these sites. The materials used for this study date from the Earliest to Final Jomon (ca. 10,000–2500 BP), Yayoi (ca. 2500–1700 BP) and Kofun (ca. 1700–1300 BP) periods. The relative proportions of pigs were calculated to show the overall trend of pig exploitation in each site. Age at death was obtained based on the state of tooth eruption. Bucco‐lingual crown measurements were taken on the third and fourth premolars and on each cusp of the first and second molars of the mandible, and the logarithmic ratio technique was then applied to these data. The age structure of Sus varies between different sites in the Jomon Period, and significant changes were observed in the Yayoi and Kofun Periods. A decrease in the relative proportion of pigs in the faunal assemblages was observed from Jomon to Kofun. Three major differences were observed in the size of pigs. The overall size of pigs significantly increased from Early to Middle Jomon, whilst a decrease in size occurred in the Yayoi Period. Finally, overall size increased significantly during the Kofun Period. Together with the archaeological evidence—such as the ritual burial of pigs accompanying human burial—we suggest that the interaction between pigs and humans became gradually stronger at some sites during the Late Jomon Period, and the relationship intensified in the Yayoi Period. Copyright © 2006 John Wiley & Sons, Ltd.     

Evaluation of carnivory in inland Jomon hunter–gatherers based on nitrogen isotopic compositions of individual amino acids in bone collagen

Archaeological studies including stable carbon and nitrogen isotope analyses of bone collagen from human remains have suggested their heavy dependence on terrestrial foods during the Jomon period in the inland central region in Japan. However, it is not easy to quantitatively evaluate the extent of carnivory for archaeological human remains based on the bulk collagen chemistry, because of variable ¹⁵N-enrichment factor along the trophic step and background isotopic variations in ecosystems. In order to overcome these problems and more precisely evaluate diets of prehistoric humans who strongly adapted to terrestrial environment, in this study we applied nitrogen isotope analysis of individual amino acids in bone collagen to two inland human populations in the Jomon period. Our results suggest that the two populations were predominantly dependent on the C₃-plant-based terrestrial ecosystem and consumed little aquatic resources. Furthermore, their mean trophic positions (2.7 for both cases) are closer to that of the fox (2.8–3.0) rather than those of pure herbivores (2.0–2.2), and show little change over time. These results are the first evidence that inland Jomon populations may have had more carnivorous diets than is traditionally considered.     

Carbon and nitrogen stable isotope analysis on the diet of Jomon populations from two coastal regions of Japan

We report on a stable isotope paleodietary reconstruction of Jomon populations in Japan during the Middle to Final Jomon period (ca. 5000–2300 years BP), focusing on dietary differences within and among populations and between regions. Carbon and nitrogen isotope analysis was performed on human and faunal bone collagen from six coastal sites along the Inland Sea in the Sanyo (Ota, Funamoto, and Tsukumo) region and along Mikawa Bay and the Pacific Ocean in the Tokai (Kawaji, Yoshigo, and Inariyama) region. We found that carbon and nitrogen isotope ratios were positively correlated, indicating that the Jomon people consumed a mixed diet of marine (shellfish and marine fish) and terrestrial (C₃ plants and terrestrial mammals) protein. In the Ota samples (n = 25, during the Middle Jomon period, 5000–4000 years BP), sex was one of the main reasons for the intra-population dietary variation. Ota males consumed greater amounts of marine food, while Ota females consumed greater amounts of terrestrial food; these dissimilar diets may have been related to the sexual division of labor. Significant inter-population dietary differences were found, which may have been related to differences in age or site location. Notably, the two coastal regions showed clear isotopic differences. Nitrogen isotope ratios of individuals from the Sanyo region were significantly higher than ratios of individuals from the Tokai region. The individuals in the Sanyo region might have consumed a diet high in aquatic foods, particularly high trophic level marine fish, whereas the individuals in the Tokai region might have consumed a lot of marine shellfish. Another possible reason for the regional isotopic difference might have been different baseline of nitrogen isotope ratios of the marine ecosystems.     

Local diversity in settlement,demography and subsistence across the southern Indian Neolithic-Iron Age transition: site growth and abandonment at Sanganakallu-Kupgal

The Southern Indian Neolithic-Iron Age transition demonstrates considerable regional variability in settlement location, density, and size. While researchers have shown that the region around the Tungabhadra and Krishna River basins displays significant subsistence and demographic continuity, and intensification, from the Neolithic into the Iron Age ca. 1200 cal. BC, archaeological and chronometric records in the Sanganakallu region point to hilltop village expansion during the Late Neolithic and ‘Megalithic’ transition period (ca. 1400–1200 cal. BC) prior to apparent abandonment ca. 1200 cal. BC, with little evidence for the introduction of iron technology into the region. We suggest that the difference in these settlement histories is a result of differential access to stable water resources during a period of weakening and fluctuating monsoon across a generally arid landscape. Here, we describe well-dated, integrated chronological, archaeobotanical, archaeozoological and archaeological survey datasets from the Sanganakallu-Kupgal site complex that together demonstrate an intensification of settlement, subsistence and craft production on local hilltops prior to almost complete abandonment ca. 1200 cal. BC. Although the southern Deccan region as a whole may have witnessed demographic increase, as well as subsistence and cultural continuity, at this time, this broader pattern of continuity and resilience is punctuated by local examples of abandonment and mobility driven by an increasing practical and political concern with water.     

我国传统村镇旅游研究进展

不同专业背景的学者纷纷从不同的角度对传统村镇旅游进行研究和探讨,涌现了许多相关研究成果。这些成果主要集中在:传统村镇旅游资源特点和价值,传统村镇旅游开发,传统村镇旅游资源保护和开发,旅游对传统村镇的影响,传统村镇旅游流和客源市场,传统村镇旅游存在问题及对策。同时,我国传统村镇旅游研究还存在着一些问题。     

Late Paleolithic and Mesolithic Coastlines of Greece and the Aegean

Abstract

Reconstructions of the late Quaternary paleogeography of Greece and the Aegean show that at 18,000 years B.P. the northern Aegean and northern Adriatic formed large coastal plains traversed by many rivers. Broad plains also existed off the coast of Elis and the present Gulf of Korinth, and along the Anatolian coast. Many islands, such as Kerkira, Euboea, and the northern Sporadhes, were connected with the mainland, and most of the Cycladic islands were joined together in a Cycladic semi-peninsula. The post-glacial rise of sea level beginning ca. 15,000 B.P. restored around 9,000 B.P. the coastal geography to approximately its present configuration. The late Quaternary paleogeography and its subsequent changes have many archeological implications that are worth serious consideration. The well-watered northern coastal plains may have furnished subsistence for a plains population quite independent of the resources of the northern mountain regions, and they constituted easy access to the Greek peninsula from the NE and NW. Loss of coastal plain land during the post-glacial rise of sea level drastically changed the resource base in many areas. The island of Melos, known source of obsidian for toolmaking since at least 10,000 B.P., may have been discovered considerably earlier when access to the island was largely over land.     

WATER, ANIMALS AND AGRICULTURAL TECHNOLOGY: A STUDY OF SETTLEMENT PATTERNS AND ECONOMIC CHANGE IN NEOLITHIC SOUTHERN GREECE

Summary. This study, based on evidence from archaeological surveys and excavations in southern Greece, demonstrates two major shifts in the subsistence economy during the Neolithic. In the EN and MN periods the presence of large villages in locations near reliable water-sources and permanently moist or seasonally flooded soils of high and sustained productivity illustrates a village farming economy concentrating on arable agriculture. The first economic shift occurred in the late MN-LN with occupation of highland caves and islands, indicating increased sheep/goat pastoralism, fishing, and perhaps hunting, with a reduced number of farming villages present in the plains. The second shift took place in the FN-EBA, when a dispersal of agricultural settlements into dry upland regions indicates expanding plough agriculture and pastoralism, important factors contributing to the development of the flourishing EBA economy. The expansion of settlement was most marked in southeastern Greece, and it is suggested here that the extensive grazing areas provided by the open vegetation and mountainous terrain of this dry region, and its relative scarcity of well-watered fertile lowlands, may have stimulated the LN-FN expansion of pastoralism.     

The Woodland and Mississippian traditions in the prehistory of Midwestern North America

Cultural developments in Midwestern North America between 5000 and 400 B.P. are reviewed and related to two overlapping, but contrasting, cultural traditions: Woodland and Mississippian. Significant changes in prehistoric subsistence systems, settlement patterns, and sociopolitical organization are reviewed within a three-division framework, beginning with a Transitional period (5000–2000 B.P.) when Late Archaic and Early Woodland societies settled into different regions, constructed regional markers (cemeteries, mounds, earthworks), and established economic and social relations with both neighboring and more distant groups. This was followed by the Middle Woodland period (2000–1500 B.P.) that is associated with the Hopewell climax of long-distance exchange of exotic materials, mound building, and ceremonial activities, although all Middle Woodland groups did not participate in this Hopewell interaction sphere. In the Late Prehistoric period (1500–400 B.P.), the Woodland tradition persisted in some areas, while the Mississippian tradition developed from local Late Woodland societies elsewhere. Finally, the patterns of interaction between the two traditions are discussed.     

Game Resources, Social Interaction, and the Ecological Footprint in Southwest New Mexico

Humans have modified their environments for millennia, but the role of these impacts on economic and social strategies among communities can be difficult to assess. This is due in part to the difficulty of quantifying impacts, which hinders our evaluations of the effects of different resource acquisition strategies and impairs attempts to understand competing demands on resources and their effects on the evolution of social relations. In this paper we employ footprint analysis, a tool used in ecology, to assess the impact of prehistoric subsistence farming communities on the environment, specifically faunal resources. We use footprint analysis to quantify the impact of various strategies of game acquisition by Classic Mimbres period (AD 1000-1130) farmers in the North American Southwest. Assessments are then employed in identifying changes in social relations among communities that may have contributed to settlement changes in the region.