RESUMO
The timing of Tiwanaku's collapse remains contested. Here we present a generational-scale chronology of Tiwanaku using Bayesian models of 102 radiocarbon dates, including 45 unpublished dates. This chronology tracks four community practices: residing short- vs. long-term, constructing monuments, discarding decorated ceramics, and leaving human burials. Tiwanaku was founded around AD 100 and around AD 600, it became the region's principal destination for migrants. It grew into one of the Andes' first cities and became famous for its decorated ceramics, carved monoliths, and large monuments. Our Bayesian models show that monument building ended ~AD 720 (the median of the ending boundary). Around ~AD 910, burials in tombs ceased as violent deaths began, which we document for the first time in this paper. Ritualized murders are limited to the century leading up to ~AD 1020. Our clearest proxy for social networks breaking down is a precise estimate for the end of permanent residence, ~AD 1010 (970-1050, 95%). This major inflection point was followed by visitors who used the same ceramics until ~AD 1040. Temporary camps lasted until roughly ~AD 1050. These four events suggest a rapid, city-wide collapse at ~AD 1010-1050, lasting just ~20 years (0-70 years, 95%). These results suggest a cascading breakdown of community practices and social networks that were physically anchored at Tiwanaku, though visitors continued to leave informal burials for centuries. This generation-scale chronology suggests that collapse 1) took place well before reduced precipitation, hence this was not a drought-induced societal change and 2) a few resilient communities sustained some traditions at other sites, hence the chronology for the site of Tiwanaku cannot be transposed to all sites with similar material culture.
Assuntos
Sepultamento , Cerâmica , Humanos , Teorema de Bayes , Homicídio , Arqueologia/métodosRESUMO
Radiogenic strontium isotopes (87Sr/86Sr) have long been used in analyses of paleomobility within Mesoamerica. While considerable effort has been expended developing 87Sr/86Sr baseline values across the Maya region, work in central Mexico is primarily focused on the Classic period urban center of Teotihuacan. This study adds to this important dataset by presenting bioavailable 87Sr/86Sr values across central Mexico focusing on the Basin of Mexico. This study therefore serves to expand the utility of strontium isotopes across a wider geographic region. A total of 63 plant and water samples were collected from 13 central Mexican sites and analyzed for 87Sr/86Sr on a Thermo-Finnigan Neptune multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS). These data were analyzed alongside 16 published 87Sr/86Sr values from two additional sites within the region of interest. A five-cluster k-means model was then generated to determine which regions of the Basin of Mexico and greater central Mexico can and cannot be distinguished isotopically using 87Sr/86Sr values. Although the two clusters falling within the Basin of Mexico overlap in their local 87Sr/86Sr ranges, many locations within the Basin are distinguishable using 87Sr/86Sr values at the site-level. This study contributes to paleomobility studies within central Mexico by expanding knowledge of strontium isotope variability within the region, ultimately allowing researchers to detect intra-regional residential mobility and gain a greater understanding of the sociopolitical interactions between the Basin of Mexico and supporting outlying regions of central Mexico.
Assuntos
Paleontologia/métodos , Isótopos de Estrôncio/análise , Estrôncio/análise , Monitoramento Ambiental/métodos , Monitoramento Ambiental/normas , México , RadioisótoposRESUMO
In the decades since Verano (1997) published his foundational piece on Andean paleopathology, scholars have recognized the importance of the bioarchaeology of childhood. Yet, scholarship on ancient childhood in the Andes deemphasizes paleopathology. Nonadult paleopathological data are often employed in large-scale, biocultural studies focused on environmental or political adaptations; however, they can also elucidate children's individual lived experiences and roles in society. To generate culturally-meaningful paleopathological data, we must take a contextualized approach to our analyses and interpretations. Disparate use of chronological age in published datasets makes synthesis across studies problematic, and ethnohistorical and ethnographic data on Andean children demonstrate that developmental age categories, rather than chronological age ranges, are most appropriate. Further, paleopathological data can best inform our investigations when they are combined with related datasets such as those on sex, diet, activity, and mobility. With that in mind, we use the theoretical framework of "local biologies" (and the related "situated biologies"), where biology is viewed as heavily contingent on culturally-specific beliefs and practices and local physical, sociocultural, and political environments (Lock, 1993, 2001; Niewöhner and Lock, 2018). Local biologies approaches can enrich social bioarchaeology and paleopathology to by specifically situating children and their experiences within the ancient Andean world.
Assuntos
Doença/história , Paleopatologia , Projetos de Pesquisa , Fatores Etários , Criança , Características Culturais , Difusão de Inovações , Doença/etnologia , Feminino , Previsões , História Antiga , Humanos , Masculino , Paleopatologia/tendências , Projetos de Pesquisa/tendências , América do SulRESUMO
OBJECTIVES: Stable carbon and nitrogen isotope analysis is used to reconstruct diet among a pre-Hispanic population from the Peruvian Andes to evaluate whether local foodways changed with Wari imperial influence in the region. This study also compares local diet to other Wari-era sites. MATERIALS AND METHODS: Samples derive from the site of Beringa in Peru and correspond primarily to pre-Wari (200-600 CE) and Wari (600-1,000 CE). We examine stable carbon isotopes from enamel (n = 29) and bone apatite (n = 22), and stable carbon and nitrogen isotopes from bone collagen (n = 29), and we present stable carbon and nitrogen isotope data on archaeological and modern fauna (n = 37) and plants (n = 19) from the region. RESULTS: There were no significant differences in either δ13 C or δ15 N from the pre-Wari to Wari era, indicating that those measurable aspects of diet did not change with Wari influence. There were no sex-based differences among juveniles (as inferred from δ13 C from enamel carbonates) nor among adults (based on δ13 C and δ15 N from adult bone collagen). Comparisons to other Wari era sites show that Beringa individuals exhibited significantly lower δ13 C values, suggesting that they consumed significantly less maize, a socially valued food. Further, the Froehle et al. (2012) stable isotope model suggests that the majority of the Beringa individuals consumed more C3 than C4 plants, and dietary protein was derived primarily from terrestrial animals and some marine resources. CONCLUSIONS: The similar diets from pre-Wari to Wari times hint at strong local dietary traditions and durable food trade networks during the period of Wari imperial influence. The presence of limited marine foods in the diet suggests a trade network with coastal groups or sojourns to the coast to gather marine resources.
Assuntos
Isótopos de Carbono/análise , Dieta/história , Indígenas Sul-Americanos/estatística & dados numéricos , Isótopos de Nitrogênio/análise , Adolescente , Adulto , Exoesqueleto , Animais , Arqueologia , Osso e Ossos/química , Criança , Pré-Escolar , Colágeno/química , Esmalte Dentário/química , Feminino , História Antiga , História Medieval , Humanos , Lactente , Masculino , Pessoa de Meia-Idade , Peru , Adulto JovemRESUMO
OBJECTIVES: The goal of this article is to assess the scale of human paleomobility and ecological complementarity between the lowlands and highlands in the southern Andes during the last 2,300 years. By providing isotope results for human bone and teeth samples, we assess a hypothesis of "high residential mobility" suggested on the basis of oxygen isotopes from human remains. METHODS: We develop an isotopic assessment of human mobility in a mountain landscape combining strontium and oxygen isotopes. We analyze bone and teeth samples as an approach to life-history changes in spatial residence. Human samples from the main geological units and periods within the last two millennia are selected. RESULTS: We present a framework for the analysis of bioavailable strontium based on the combination of the geological data with isotope results for rodent samples. The 87 Sr/86 Sr values from human samples indicate residential stability within geological regions along life history. When comparing strontium and oxygen values for the same human samples, we record a divergent pattern: while δ18 O values for samples from distant regions overlap widely, there are important differences in 87 Sr/86 Sr values. CONCLUSIONS: Despite the large socio-economic changes recorded, 87 Sr/86 Sr values indicate a persisting scenario of low systematic mobility between the different geological regions. Our results suggest that strontium isotope values provide the most germane means to track patterns of human occupation of distinct regions in complex geological landscapes, offering a much higher spatial resolution than oxygen isotopes in the southern Andes.
Assuntos
Antropologia Física/métodos , Migração Humana/história , Isótopos de Estrôncio/análise , Adulto , Animais , Argentina , Osso e Ossos/química , Chile , Feminino , História Antiga , Humanos , Masculino , Pessoa de Meia-Idade , Isótopos de Oxigênio/análise , Roedores , Dente/químicaRESUMO
OBJECTIVES: Hypothetical models of socioeconomic organization in pre-Columbian societies generated from the rich ethnohistoric record in the New World require testing against the archaeological and bioarchaeological record. Here, we test ethnohistorian Maria Rostworowski's horizontality model of socioeconomic specialization for the Central Andean coast by reconstructing dietary practices in the Late Intermediate Period (c. AD 900-1470) Ychsma polity to evaluate complexities in social behaviors prior to Inka imperial influence. MATERIALS AND METHODS: Stable carbon and nitrogen isotope analysis of archaeological human bone collagen and apatite (δ13 Ccol[VPDB], δ15 Ncol[AIR] , δ13 Cap[VPDB] ) and locally available foods is used to reconstruct the diets of individuals from Armatambo (n = 67), associated ethnohistorically with fishing, and Rinconada Alta (n = 46), associated ethnohistorically with agriculture. RESULTS: Overall, mean δ15 Ncol[AIR] is significantly greater at Armatambo, while mean δ13 Ccol[VPDB] and mean δ13 Cap[VPDB] are not significantly different between the two sites. Within large-scale trends, adult mean δ13 Cap[VPDB] is significantly greater at Armatambo. In addition, nearly one-third of Armatambo adults and adolescents show divergent δ15 Ncol[AIR] values. DISCUSSION: These results indicate greater reliance on marine resources at Armatambo versus Rinconada Alta, supporting the ethnohistoric model of socioeconomic specialization for the Central Andean coast. Deviations from large-scale dietary trends suggest complexities not accounted for by the ethnohistoric model, including intra-community subsistence specialization and/or variation in resource access.
Assuntos
Isótopos de Carbono/análise , Dieta/história , Comportamento Alimentar/etnologia , Isótopos de Nitrogênio/análise , Adolescente , Adulto , Antropologia Física , Apatitas/química , Osso e Ossos/química , Criança , Pré-Escolar , Colágeno/química , Feminino , História Antiga , Humanos , Lactente , Recém-Nascido , Masculino , Peru , Adulto JovemRESUMO
OBJECTIVES: To assess the relationship between the Tiwanaku polity and the individuals buried at the Middle Horizon (â¼AD500-1000) cemetery of Larache in northern Chile, a site that has been singled out as a potential elite foreign enclave. MATERIALS AND METHODS: We explore this association through the skeletal remains of 48 individuals interred at the cemetery of Larache using bioarchaeological, biogeochemical, and artifactual evidence. Data from cranial modification practices, violent injury, and the mortuary assemblage are used to explore culturally constructed elements of status and identity, radiogenic strontium isotope analyses provide us with a perspective on the geographic origins of these individuals, and stable carbon and nitrogen analyses allow discussion of paleodiet and access to resources. RESULTS: Radiogenic strontium isotope values show the presence of multiple first generation migrants at Larache. Stable carbon and nitrogen isotope data reveal significant differences among individuals. The mortuary context reveals a standard pattern for the oases but also includes a series of unusual burials with abundant gold and few other objects. Interestingly, both local and nonlocal individuals with different head shapes had access to the differentiated burial context; however nonlocal individuals appear to be the only ones with a heavily maize-based diet. CONCLUSIONS: Our evidence shows that Larache served as a burial place for a diverse, yet culturally integrated and potentially elite segment of the Atacameño population, but not a foreign enclave as had been postulated.
Assuntos
Cemitérios/história , Isótopos de Estrôncio/análise , Adolescente , Adulto , Arqueologia , Arte , Osso e Ossos/química , Cerâmica , Criança , Pré-Escolar , Chile/etnologia , Colágeno/química , Feminino , História Medieval , Humanos , Lactente , Recém-Nascido , Masculino , Pessoa de Meia-Idade , Crânio/patologia , Adulto JovemRESUMO
OBJECTIVES: Gender and other facets of social identity play important roles in the organization of complex societies. This study reconstructs dietary practices within the Middle Horizon (AD 500-1000) Tiwanaku colonies in southern Peru to increase our knowledge of gendered patterns of consumption within this early expansive state. METHODS: We use stable isotope analysis of 43 human bone samples representing 14 females, 20 males, 8 juveniles, and 1 indeterminate individual recovered from burial excavations at the sites of Rio Muerto and Omo in the Moquegua Valley. Data are contextualized by comparisons with previously published Tiwanaku isotope data from the period. RESULTS: Our results find mean values of δ(13) Capatite = -7.3 ± 1.6% (N = 36, 1SD), δ(13) Ccollagen = -12.3 ± 1.5% (N = 43, 1SD), and δ(15) Ncollagen = 8.4 ± 1.6% (N = 43, 1SD). Between the sexes, Mann-Whitney U tests demonstrate significant differences in δ(13) Ccollagen (U = 74, P = 0.021), but no differences in δ(13) Capatite (U = 58, P = 0.095) or δ(15) Ncollagen (U = 116, P = 0.755) values. CONCLUSIONS: These data indicate relatively high C4 plant consumption among the Tiwanaku colonies, and support paleobotanical and archaeological evidence that maize (Zea mays) was the staple crop. Dietary values are similar overall between the sexes, but significantly higher δ(13) Ccollagen values in males is consistent with a model of gendered norms of consumption similar to that of the later Inca (AD 1438-1533), where males consumed more maize than females, often in the form of beer (chicha). Results provide new insights on social dynamics within the Tiwanaku colonies and suggest the increased importance maize consumption for males during the Tiwanaku expansion.
Assuntos
Apatitas/análise , Osso e Ossos/química , Isótopos de Carbono/análise , Colágeno/análise , Dieta/etnologia , Isótopos de Nitrogênio/análise , Adolescente , Adulto , Antropologia Física , Criança , Pré-Escolar , Feminino , Humanos , Masculino , Pessoa de Meia-Idade , Peru , Comportamento Social , Adulto JovemRESUMO
Bioarchaeological approaches are well suited for examining past responses to political and environmental changes. In the Andes, we hypothesized that political and environmental changes around AD 1100 resulted in behavioral changes, visible as shifts in paleodiet and paleomobility, among individuals in the San Pedro de Atacama oases and Loa River Valley. To investigate this hypothesis, we generated carbon and oxygen isotope data from cemeteries dating to the early Middle Horizon (Larache, Quitor-5, Solor-3), late Middle Horizon (Casa Parroquial, Coyo Oriental, Coyo-3, Solcor-Plaza, Solcor-3, Tchecar), and Late Intermediate Period (Caspana, Quitor-6 Tardío, Toconce, Yaye-1, Yaye-2, Yaye-3, Yaye-4). Carbon isotope data demonstrate a greater range of carbon sources during the late Middle Horizon compared with the Late Intermediate Period; while most individuals consumed largely C3 sources, some late Middle Horizon individuals consumed more C4 sources. Oxygen isotope data demonstrate greater diversity in drinking water sources during the late Middle Horizon compared with the Late Intermediate Period. Water samples were analyzed to provide baseline data on oxygen isotope variability within the Atacama Desert, and demonstrated that oxygen isotope values are indistinguishable in the San Pedro and Loa Rivers. However, oxygen isotope values in water sources in the high-altitude altiplano and coast are distinct from those in the San Pedro and Loa Rivers. In conclusion, instead of utilizing a wider variety of resources after environmental and political changes, individuals exhibited a wider range of paleodietary and paleomobility strategies during the Middle Horizon, a period of environmental and political stability.
Assuntos
Cemitérios/história , Dieta/história , Migração Humana/história , Adulto , Antropologia Física , Arqueologia , Osso e Ossos/química , Isótopos de Carbono/análise , Chile , Esmalte Dentário/química , Meio Ambiente , Feminino , História Antiga , História Medieval , Humanos , Masculino , PolíticaRESUMO
Paleomobility has been a key element in the study of the expansion of ancient states and empires, including the Tiwanaku polity of the South Central Andes (AD 500-1000). We present radiogenic strontium and oxygen isotope data from human burials from three cemeteries in the Tiwanaku-affiliated Middle Horizon archaeological site complex of Rio Muerto in the Moquegua Valley of southern Peru. At Rio Muerto, archaeological human enamel and bone values range from (87) Sr/(86) Sr = 0.70657-0.72018, with a mean of (87) Sr/(86) Sr = 0.70804 ± 0.00207 (1σ, n = 55). For the subset of samples analyzed for oxygen isotope values (n = 48), the data ranges from δ(18) Ocarbonate(VSMOW) = +18.1 to +27.0. When contextualized with other lines of archaeological evidence, we interpret these data as evidence for an archaeological population in which the majority of individuals had "local" origins, and were likely second-generation, or more, immigrants from the Tiwanaku heartland in the altiplano. Based on detailed life history data, we argue a smaller number of individuals came at different ages from various regions within the Tiwanaku polity. We consider whether these individuals with isotopic values consistent with "nonlocal" geographic origins could represent first-generation migrants, marriage exchange partners, or occupationally mobile herders, traders or other travelers. By combining isotopic life history studies with mortuary treatment data, we use a person-centered migration history approach to state integration and expansion. Isotopic analyses of paleomobility at the Rio Muerto site complex contribute to the role of diversity in ancient states by demonstrating the range of geographic origins rather than simply colonists from the Lake Titicaca Basin.