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1.
James T. Pokines 《International Journal of Osteoarchaeology》2013,23(4):475-484
This research reports the herpetological (reptile and amphibian) remains from Khonkho Wankane, an urban and ceremonial centre in the southern Lake Titicaca region of the Bolivian Altiplano, which fluoresced during the Late Formative period. The total n = 1710, including a minimum of six taxa and representing a significant portion of the relatively depauperate modern herpetofauna recorded for the Lake Titicaca area. A lizard of the genus Liolaemus (Tropiduridae) was identified. Amphibians are represented by Andean toad Rhinella spinulosa (Bufonidae) and by at least four taxa of frogs: [cf. Gastrotheca marsupiata (Hylidae) and Pleurodema marmorata or P. cinerea and Telmatobius spp. (Leptodactylidae)]. The latter genus does not include members of the giant variants (T. culeus) that dwell in Lake Titicaca. The question of how these remains were incorporated into the site deposits is examined taphonomically. No indicators of human or small carnivore predation were detected. Significant spatial clustering of amphibian remains was detected, with two clusters contributing n = 1562 or 92.4% of the amphibian total (n = 1690). These concentrations also are characterised by a depressed ratio of cranial versus postcranial elements, which cannot be explained by recovery methods. These concentrations of herpetofaunal remains likely represent in‐burrow deaths of species sheltering for thermoregulatory benefits away from this harsh Altiplano environment, with the lowered recovery of cranial elements hypothesised to have resulted from a lack of ossification. The bulk of herpetofaunal remains recovered therefore likely were recent intrusions into the site deposits and do not represent the residue of human exploitation during the occupation of Khonkho Wankane. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
2.
J. T. Pokines 《International Journal of Osteoarchaeology》2013,23(6):746-756
The urban and ceremonial center Khonkho Wankane flourished in the southern Lake Titicaca Altiplano region during the Late Formative prior to the rise of Tiwanaku as a dominant urban center. This site yielded an avifaunal number of identified specimens (NISP) = 631, with a minimum of 26 taxa represented among 539 skeletal elements or fragments. A total of 92 egg shell fragments also were recovered. The avifauna inhabited two major ecological zones: Lake Titicaca, its margins/wetlands and other water margins; and the dry Altiplano grassland (or puna). Lake/wetland taxa include Phoenicopterus chilensis (Chilean flamingo), Nycticorax nycticorax (night heron) and multiple taxa in the Order Anseriformes (ducks, geese, etc.) including Chloephaga melanoptera (Andean goose), Anas georgica (yellow‐billed pintail), A. flavirostris (speckled teal) and Oxyura jamaicensis (Andean ruddyduck). Also present are Fulica ardesiaca (Andean coot), Gallinago andina (puna snipe), Himantopus mexicanus (black‐necked stilt) and Charadrius alticola (puna plover). Puna taxa include Nothoprocta cf. ornata (ornate tinamou), Nothura cf. darwinii (Darwin's nothura), Metropelia sp. (ground doves), Athene cunicularia (burrowing owl), and multiple Passeriformes (songbirds, etc.). Taxa with a cosmopolitan distribution include Falco cf. femoralis (aplomado falcon) and Tyto alba (barn owl). Taphonomic analysis indicates that the avifauna were used in ceremonial contexts, including multiple Falco cf. femoralis burials, and for dietary and possibly tool‐making purposes. Other sources of introduction into the site deposits likely include natural mortality of taxa directly inhabiting the site area. These findings are compared to the avifauna recovered from the Formative site of Chiripa along the Lake Titicaca margin, which included a much higher proportion of lake bird fauna. At Khonkho Wankane, the importance of wetland avifauna may have been enhanced by the alteration of the local environment to include qochas, or artificial reservoirs/ponds, and continued despite reliance upon multiple domesticated plant and mammal species. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
3.
Khonkho Wankane is a ceremonial center located in the southern Lake Titicaca Basin, Bolivia. During the Late Formative period (AD 1–500), its residents practiced agropastoral lifeways and participated in the rise of the state at Tiwanaku. Like at many Andean sites, bones from the family Camelidae are the most abundant large mammal in domestic contexts. Identifying camelid morphotypes represented by these bones carries far‐reaching implications for understanding past hunting, herding, and caravanning practices, and their roles in larger social and economic webs. Identifications were based on a locally focused reference collection, including llamas (Lama glama) from the immediate vicinity of the site, as well as Andean guanacos (Lama guanicoe), a much smaller morphotype than the Patagonian guanacos used in many osteometric studies. Multivariate statistical analyses and incisor morphology identified all four camelid. Different analyses suggest that the crux of osteometry lies in the reference collection, not the statistical test. An additional, very large morphotype likely corresponds to a castrated llama, the preferred cargo animal among modern drovers. The presence of these animals is interpreted as evidence that groups hunted vicuña (Vicugna vicugna) and guanaco, which are not currently present around the site, herded llamas and alpacas (Vicugna pacos), and perhaps organized caravans with castrated llamas. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
4.
John W. Janusek 《Journal of Archaeological Research》2004,12(2):121-183
The Lake Titicaca Basin provides a fascinating case study for examining the prehistoric rise of complexity and archaic state development. The development of the Tiwanaku state and preceding polities involved conjunctions of regional environmental, socioeconomic, and ideological transformations. Significant social, economic, and ideological diversity characterized each major phase, indicating that the creation of inclusive domains of shared values, practices, and identities was critical to the formation of polities in the region. Tiwanaku and its precursors were, in great part, incorporative sociopolitical phenomena in which social diversity remained vital throughout their histories. 相似文献
5.
Maria Daniela Sanchez‐Lopez 《对极》2019,51(4):1318-1339
The Uyuni salt flat (Salar de Uyuni) in Bolivia possesses the largest lithium deposit in the world. Over the past 40 years, this location has been commodified and radically transformed. This paper examines how a landscape, understood from its material attributes and qualities, shapes and is shaped by social relations unfolding in a process of commodification and mining expansion. Based on primary qualitative data, the paper explores two elements: (1) how the symbolic meaning of this landscape has changed over time for the surrounding indigenous communities; and (2) how the different materialities of the salt flat as landscape, as ulexite and as lithium allow understanding of the drivers of socio‐environmental change and conflict in this region. The paper argues that social relations and governance frameworks are interlinked with changing symbolic meanings and the different materialities of the Uyuni salt flat. 相似文献
6.
Tiwanaku influence significantly affected the lifestyle of the prehistoric peoples of the Atacama Desert as it represented an important period of social and economic change. Such intense changes as social stratification and new religious and ideological influences have always been characterized as peaceful ones. Palaeopathological studies based on the violence‐induced traumatic lesions of 64 well‐preserved human skeletons from an excavated funerary site named Solcor‐3 have facilitated a comparison between Pre‐Tiwanaku and Tiwanaku periods. Results show an increase in violence between males represented by low‐intensity skull traumas, arrow wounds and a high mortality rate between 20 and 30 years of age during the Tiwanaku period. The interpretation of this data is contrary to the model of peaceful acceptance of the changes that followed the Tiwanaku influence into the Atacama. At least for Solcor‐3, economic and political factors should be re‐considered in order to explain the emergence of social tension during the Tiwanaku period. In the future, more detailed studies will probably help to clarify if conflicts had also extended to other sites in San Pedro de Atacama under Tiwanaku influence. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献
7.
F. Rivals A. Testu A.‐M. Moigne H. de Lumley 《International Journal of Osteoarchaeology》2006,16(3):249-268
The argali (Ovis ammon antiqua) assemblages from the Middle Pleistocene site of the Caune de l'Arago (Tautavel, southern France) were studied in terms of zooarchaeology and taphonomy. It is possible to discern palaeobiological information lost during fossilisation, as well as the palaeoethology of the bone collector, by the observation of taphonomic details preserved on the bone assemblages. The observations leave no doubt that both humans and carnivores were involved in the accumulation of argali carcasses in the cave. In some assemblages, the type of bones found in articulation and the gnawing marks observed are characteristic of carnivores. In other levels, the intense fracturing of the major limb bones in relation to their marrow content and mineral density, and butchering marks found on specimens in the earlier levels, are in favour of human accumulation, the modalities of which are discussed. The results suggest that the degree of carnivore activity seems to have been higher in levels M, N and O than in level F. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
8.
The consumption of hallucinogenic substances is a long-standing tradition in the Americas. San Pedro de Atacama (SPA) in Northern Chile is the archaeological zone with the highest incidence of snuffing implements in the world. Snuff trays from SPA have been studied under a variety of prisms but their provenience, in particular that of the wood used in their manufacture, has not yet been addressed. The delicate nature of trays and their excellent state of preservation call for the use of non-invasive analytical methods. Wood density was used to demarcate a possible range of species and hence as a broad provenience marker, and its value determined for 169 trays from the museum at San Pedro de Atacama. The results showed that although some of the SPA snuff trays studied may have been manufactured with local wood, most of them used exogenous wood as raw material. At this point, it is not possible to ascertain the precise origin of such wood, but Bolivia and NWA appear as likely candidates. Three distinct styles have been defined for SPA trays: Tiwanaku, San Pedro, and Circumpuneño (encompassing the area around the Puna de Atacama and including SPA). The effect of style on density points to different sources of wood in Tiwanaku style trays and trays in San Pedro and Circumpuneño styles. As expected from geographically and temporally dynamic patterns of interaction of SPA with neighboring regions, diachronic differences in wood density distributions were found. Tray manufacturing technique was not dependent on wood density, suggesting that the skill of artisans and the quality of their tools allowed them to use any type of wood for their art work, independent of its complexity. 相似文献
9.
Charles Stanish Edmundo de la Vega Michael Moseley Patrick Ryan Williams Cecilia Chvez J. Benjamin Vining Karl LaFavre 《Journal of Anthropological Archaeology》2010,29(4):524-532
This paper provides data and analysis from an intensive settlement survey in the southwestern Titicaca Basin. This research was designed to assess the nature of Tiwanaku (AD 600–1100) long-distance trade. The survey area was placed between the prehistoric urban capital of Tiwanaku and its primary colony in Moquegua, a valley located on the Pacific watershed approximately 325 km away. The survey was specifically placed in an area where GIS analysis indicated a least-cost transit route between Tiwanaku and Moquegua. Field adjustments to the survey area were made based upon informant data about the historic location of caravan routes. The results of the survey indicate that there is a light but virtually continuous string of Tiwanaku occupation along the trails and roads in the area sampled between Tiwanaku and Moquegua. However, in contrast to the later Inca (AD 1450–1532) period pattern, Tiwanaku did not maintain way stations or build any kind of formal road system. The data indicate that Tiwanaku had indeed relied upon camelid caravans utilizing the least-cost pathways, but it did so in a more decentralized and informal way than the later Inca state. 相似文献
10.
《Journal of Field Archaeology》2013,38(4):397-405
AbstractArcheological and ethno-historical data from the coastal, transitional, and lower sierra variants of the Chillon Valley, Central Coast of Peru, have led to a new understanding of the nature of Inca political and economic control of one subjugated region. The data reveal that the region was settled unevenly by the Cuzqueños; a more intensive state occupation of the lower sierra is indicated. It is suggested that control of the valley was managed by choice from a geographical-political locus in the highland zone because of certain cultural and environmental circumstances in each valley variant that posed advantages and disadvantages for state operations. Major sites yielding evidence of integration into the Inca state are discussed within the context of such a settlement pattern. 相似文献
11.
Frequencies of maxillary sinusitis in the population of the medieval town Sigtuna, Sweden, were examined. The first aim was to explore the occurrence of sinus conditions in this urban population, and the second was to investigate the effects of preservation in relation to these changes. The skeletal sample consisted of 274 adolescent and adult individuals buried ca 970–1530 AD. The maxillary sinuses were examined for different types of skeletal change related to sinusitis. The severity and location of these changes were recorded, together with the preservation of the sinus. When the diagnostic criteria for bone preservation from previous studies was used, i.e. the preservation of at least one complete antral floor, the results showed that 97.7% (n = 157) of the individuals were affected, with older individuals showing more severe bone changes. In the entire (i.e. more fragmented) sample, 94.5% (n = 259) showed signs of sinusitis. Again, older individuals showed more severe bone changes, and males were more frequently affected. Also, an increased frequency over time was found. The maxillae were subdivided into groups of bone preservation, and the results showed that there was a significant relation between preservation and the registered presence and severity of sinusitis. The results may be used as a cautionary note against investigating the occurrence of maxillary sinusitis without considering the skeletal preservation factor. There was no correlation between preservation and sex or age groups. This suggests that the differences between younger and older and male and female were not a result of preservation alone and could be considered as trustworthy. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
12.
Hermann M. Niemeyer Víctor Zapata Paulina Cantillana Alejandra Missene José Aguilera Arturo Torres 《Journal of archaeological science》2013
Wooden snuff trays from San Pedro de Atacama (SPA) in northern Chile are objects of particular museological value. Computed tomography (CT), a non-destructive analytical technique useful in the analysis of archaeological objects in which physical tampering is not desirable, was used to study provenience of wood, quality of craftmanship, taphonomic processes and nature of gemstone inlays in a group of snuff trays. While wood used in the manufacture of trays was mostly exogenous to SPA, gemstones used in inlays were likely of local origin. These findings support the active exchange of goods proposed for the south-central Andes region. Several features revealed in the trays support the view that craftsmen producing them were skillful artisans. 相似文献
13.
Sampling of deposits at the Queens Hotel site, York, produced a substantial number of small terrestrial vertebrate remains from the Anglo–Scandinavian features. By studying bone surface modification, fragmentation and skeletal completeness as taphonomic indicators, it was possible to demonstrate that the assemblage had resulted from two very different modes of accumulation and deposition. Refuse pits situated within the boundaries of the tenements had acted as accumulators of the fragmented and abraded small mammal and amphibian bones that existed as a sub‐surface death assemblage within the local environment. In contrast, the excellent preservation and skeletal completeness of numerous frogs recovered from the basal fill of a wooden well could be accounted for by their direct entry into the burial environment as a result of pit‐fall trapping. This paper also discusses the implications that the temporal and spatial variation in deposition demonstrated by the micro‐faunal remains has for the reconstruction of local ecological and environmental conditions within this site, and for other such sites. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
14.
Gregory J. Retallack 《Alcheringa: An Australasian Journal of Paleontology》2013,37(3):215-240
Retallack, G.J., September, 2007. Growth, decay and burial compaction of Dickinsonia, an iconic Ediacaran fossil. Alcheringa 31, 215-240. ISSN 0311-5518. Dickinsonia is a Neoproterozoic, Ediacaran fossil, variously considered a polychaete, turbellarian or annelid worm, jellyfish, polyp, xenophyophoran protist, lichen or mushroom. Its preservation as unskeletonized impressions in quartz sandstones has been attributed to a Neoproterozoic regime of aerobic decay less effective than today, microbial pyritization much nearer the surface than today, or agglutinate-mineralization as in xenophyophorans. However, the great variation in thickness independent of width or length of South Australian Dickinsonia is evidence of decay like the wilting of a fossil leaf, lichen or mushroom, but unlike clotting and distortion during decay, wilting or osmotic shrinkage of modern and fossil worms and jellyfish. Decayed specimens of Dickinsonia arrayed in arcs have been interpreted as slime trails or tumble tracks, but can also be interpreted as rhizinous bases of decayed crustose lichens or mushrooms arranged in fairy rings. Dickinsonia is interpreted to be sessile because adjacent specimens show reaction rims indicative of competitive interaction, and because no overlapping well-preserved specimens have ever been found. Folded and bent Dickinsonia reveal firm attachment and limited flexibility, but no brittle deformation indicative of pyritic, sideritic or calcitic ‘death masks’ or xenophyophoran agglutinate skeletons. Dickinsonia was resistant to compaction by overburden, like fossil lichens such as Spongiophyton and Thucomyces, and more compaction-resistant than fossil logs, jellyfish or worms. Dickinsonia also shows indeterminate growth like lichens, fungi, plants, xenophyophorans and colonial animals. Growth, decay and burial compaction of Dickinsonia were more like those of plants, lichens and fungi, than of worms, jellyfishes or anemones. G.J. Retallack [gregr@uoregon.edu], Department of Geological Sciences, University of Oregon. Eugene, OR 97403-1272, USA; received 18.11.05, revised 23.3.06. 相似文献
15.
Hans Huisman Bertil van Os 《Conservation and Management of Archaeological Sites》2013,15(1-3):372-386
Preservation in situ and the monitoring of archaeological sites have become important themes since the acceptance and implementation of the Valletta Treaty. In the last few decades, our knowledge of degradation processes has increased manyfold, and a range of techniques have been tested and applied for use in both assessment and monitoring. Despite these successes, all is not well. First, we have little notion of the speed of the decay processes involved. This makes it difficult to distinguish between acute and protracted degradation. Apart from that, many assessments and subsequent monitoring projects rely (too?) heavily on complex and costly specialist technology. For any future preservation — in situ — projects low-tech observations together with best estimates of decay rates and archaeological site information should be combined to make an accurate assessment of the effects of decay on the archaeological record. Monitoring for preservation purposes is only appropriate if (1) decay processes occur within a relevant and measurable time scale, and (2) if mitigating actions can be taken or preservation ex situ can be performed (i.e. a rescue excavation) if significant degradation takes place. 相似文献
16.
Herv Guy Claude Masset Charles-Albert Baud 《International Journal of Osteoarchaeology》1997,7(3):221-229
In almost all living creatures, in Primates as well as in seventeenth–eighteenth century human populations, a high infant mortality is the rule; therefore, the scarcity of children's bones in cemeteries is suspicious from a demographic point of view. Though possible in some cases, sociological causes appear less important than the peculiar behaviour of infants' bones in the tomb. This paper examines the physico-chemical properties of infants' bones and their consequences for the preservation of archaeological samples; it proposes a new way of approaching distributions at death in the past. © 1997 John Wiley & Sons, Ltd 相似文献
17.
Haijing Sun Loren E. Babcock Jin Peng Jessica M. Kastigar 《Alcheringa: An Australasian Journal of Paleontology》2017,41(1):79-100
Sun, H., Babcock, L.E., Peng, J. &; Kastigar, J.M., July 2016. Systematics and palaeobiology of some Cambrian hyoliths from Guizhou, China, and Nevada, USA. Alcheringa 41, xxx–xxx. ISSN 0311-5518.Hyoliths constitute one of the most important groups of early biomineralized metazoans. Abundant hyolith specimens, comprising both hyolithides and orthothecides, from the Balang Formation (Cambrian Stage 4), Guizhou, China, and the Poleta Formation (Cambrian Stages 3–4), Pioche Formation (Stages 4–5) and Emigrant Formation (Stages 4–5) Nevada, USA, add to the early Palaeozoic record of hyoliths from South China and Laurentia, and provide new taxonomic, taphonomic and palaeoecologic information about this group. Hyoliths from the Balang Formation include the hyolithides ‘Ambrolinevitus’ maximus Jiang, 1982, Galicornus seeneus? Val’kov, 1975, Haplophrentis reesei Babcock &; Robison, 1988, ‘Linevitus’ guizhouensis sp. nov., Meitanovitus guanyindongensis Qian, 1978, undetermined forms, and undetermined orthothecides. Hyoliths from Nevada include the hyolithides Haplophrentis carinatus (Matthew, 1899), Nevadotheca whitei (Resser, 1938), an undetermined form, and undetermined orthothecides. In the Balang Formation, eocrinoids have been found attached to hyolithide conchs, which supports the view that hyolithides were benthic animals.Haijing Sun* [hjsun1987@163. com], Resources and Environmental Engineering College, Guizhou University, Guiyang 550025, PR China; Loren E. Babcock? corresponding author [babcockloren@gmail. com], School of Earth Sciences, The Ohio State University, Columbus, OH 43210, USA; Jin Peng corresponding author [gzpengjin@126. com], Resources and Environmental Engineering College, Guizhou University, Guiyang 550025, PR China; Jessica M. Kastigar [kastigar. 2@osu. edu], School of Earth Sciences, The Ohio State University, Columbus, OH 43210, USA. *Also affiliated with Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, PR China. ?Also affiliated with Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden. 相似文献
18.
Dolores R. Piperno 《Journal of archaeological science》1985,12(4):247-267
This paper presents the results of research into the nature, distribution and significance of phytoliths in archeological sediments from Panama. Four sites are investigated that span a time period dated by radiocarbon from 6600 BC to AD 500, and which encompass a range of human adaptations and ecological settings. The strengths and limitations of phytolith analysis are evaluated in relation to a diverse set of paleoecological issues. The results indicate that Panamanian archeological deposits contribute silicified structures from a large number of plant taxa. Phytoliths appear to be horizontally and vertically stable after deposition. There are problems in human paleoecology, such as the evolution of root cropping systems, that are not amenable to study with phytolith data. However, a considerable amount of information can be generated about some components of prehistoric seed cropping systems, wild plant usage, and landforms. 相似文献
19.
Burger Richard L. Chávez Karen L. Mohr Chávez Sergio J. 《Journal of World Prehistory》2000,14(3):267-362
Recent discovery of the major geological sources of Central Andean obsidian permits a new understanding of the patterns of obsidian procurement and exchange by the Prehispanic societies of southern Peru and northern Bolivia. Based on the trace element analysis of obsidian artifacts from 160 archaeological sites, it can be established that the two major deposits of obsidian were being exploited by 9400 BP, and that volcanic glass was being transported over long distances throughout Andean prehistory. Inhabitants of the Cuzco region acquired most obsidian from the Alca source in central Arequipa, while those in the high plateau surrounding Lake Titicaca obtained most obsidian from the Chivay source in southern Arequipa. Obsidian evidence suggests close ties between the Cuzco and Circum-Titicaca regions throughout prehistory, except during the Middle Horizon (ca. 1400–1050 BP), when the expansion of the Huari and Tiahuanaco states disrupted this pattern. 相似文献
20.
Olivia Saunders 《国际历史评论》2016,38(3):551-572
This article analyses the relationship between Britain, the United States, and Bolivia in the context of the tin nexus after the Second World War. While the connection between Britain and Bolivia was long-standing - Bolivian tin had been shipped to Britain since the nineteenth century - it extended far beyond simple bilateralism. Such was the intricate web of connections in the global tin industry that any rupture in the Anglo-Bolivian relationship would have fundamental ramifications on the equilibrium of the industry, and, in turn, Britain's predominant position within it. The United States had overtly challenged Britain's dominance during the Second World War by constructing a smelter to be supplied by Bolivian ores. Despite the financial exigencies of the post-war period, the profound upheavals in the domestic Bolivian tin industry, and the contentious, destabilising tin-procurement policy pursued by the United States, Britain was determined to confront this threat. By actively seeking to preserve its long-term contract for Bolivian tin, Britain was able to maintain its predominance in the post-war global tin industry. At the same time, Bolivia deftly utilised Anglo-American rivalry to ensure more than one outlet for its most critical export commodity. 相似文献