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Citation: Andrushko, Valerie A., Michele R. Buzon, Arminda M. Gibaja, Gordon F. McEwan, Antonio Simonetti, and Robert A. Creaser. 2011. Investigating a Child Sacrifice Event from the Inca Heartland. Journal of Archaeological Science 38:323-333.
aDepartment of Anthropology, Southern Connecticut State University, 501 Crescent Street, New Haven, CT 06515
bDepartment of Anthropology, Purdue University, 700 West State Street, West Lafayette, IN 47907
cInstituto Nacional de Cultura-Cusco, Calle San Bernardo S/N, Cusco Peru
dDepartment of Sociology and Anthropology, Wagner College, One Campus Road, Staten Island, NY
eDepartment of Civil Engineering and Geological Sciences, University of Notre Dame, Notre Dame, IN
fDepartment of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB T6G 2R3, Canada
Human sacrifice in the Inca Empire at times took the form of the capacocha, a sacrificial rite involving the most beautiful children in the empire. In this study, we investigate a possible capacocha at the pre-Columbian site of Choquepukio in the Cuzco Valley of Peru. During excavations at Choquepukio in 2004, seven children (aged 3 to 12 years) were discovered buried together; accompanying them was an elaborate assemblage of high status artifacts similar to those from other recent archaeological finds that are believed to be capacocha sacrifices. Since colonial documents indicate that capacocha children were selected from diverse regions of the empire, we initiated a radiogenic strontium isotope analysis to determine the origins of the children found at Choquepukio. Our analysis showed that, indeed, two children in the assemblage had non-local origins. When considered together, the osteological, archaeological, and isotopic evidence
suggest that a capacocha event occurred at Choquepukio, representing the only lower- elevation capacocha to have been found in the Cuzco region
Human sacrificial practices of the Inca Empire (AD 1400–1532) have received attention in recent years due to the discovery of well-preserved child mummies on a number of Andean peaks (Reinhard, 1996, 1997, 1999, 2005). These mummies appear to represent the Inca capacocha, a sacrificial rite involving children in honor of the Sun and other deities (Benson, 2001; Duviols, 1976; Salomon, 1995:332; Verano, 2008). The term capacocha has been translated alternatively as “solemn sacrifice” (Betanzos, 1996 :132) or “royal obligation” (McEwan and van de Gutche, 1992:359).
For this ritual, children of great physical beauty were chosen from locations throughout the empire and brought to the capital city of Cuzco, where they were dressed and adorned, treated to ceremonial rites and feasts, and then redistributed throughout the Inca realm for sacrifice at major shrines (Molina, 1943 ). Miniature objects buried with the children, as symbolic gifts from the Inca ruler, established a connection between the community supplying the sacrifice and the divine monarchy of the Inca (McEwan and van de Gutche, 1992:364). Capacocha rituals were performed in response to catastrophes such as earthquakes, droughts, and volcanic eruptions, as well as to mark historic events in the life of the emperor, such as succession to the throne (Cobo, 1979 :237; 1990 :112).
The selection of girls and boys from the far reaches of the Inca domain was essential, a stipulation imposed by the Inca to ideologically unify the empire (Rowe,1982). The names of the sacrificed children were remembered by their local ayllus (kin- based corporate groups) and their tombs revered, a system that provided a “network holding the great Inca realm together” (Rowe, 1982:110).
Such characteristics of the capacocha allow us to set up a framework for investigating a possible capacocha discovery. A ritual of this nature should result in: (1) an archaeological assemblage of child burials, (2) varied geographic origins of the sacrificed children, and (3) elaborate Inca artifacts accompanying the burials. Though the geographical origins may be impossible to determine using material culture alone, chemical analysis of radiogenic strontium isotopes in human skeletal material can be used instead (Price et al., 2007). Local individuals may be distinguished from foreigners by analyzing the strontium isotope ratio (87Sr/86Sr) present in an individual’s dental enamel—a marker of early-childhood locale—and comparing it to ratios from the local environment.
In this paper, we investigate a possible capacocha at the site of Choquepukio, in the Inca heartland of the Cuzco Valley, Peru. We first describe the capacocha ritual based on Spanish colonial documents and archaeological discoveries. Next, we describe seven children found buried together at Choquepukio, using the archaeological and osteological findings. Following these descriptions, we present strontium isotope data to ascertain whether these children were local residents of the Cuzco Valley region or foreigners. Finally, we synthesize and interpret the data in light of Inca religious practices to better understand the role of child sacrifice in the Inca Empire.
2. Ethnohistoric and Archaeological Evidence of the Inca Capacocha
2.1 Colonial Documents
Information on the Inca capacocha can be found in several Spanish colonial documents. One of these, Bernabe Cobo’s Historia del Nuevo Mundo (Cobo, 1979
, 1990 ), is considered amongst the most reliable of the Spanish chronicles and presents a comprehensive description of Inca myths, religious beliefs, and ceremonies (Urton, 1990:31). According to Cobo (1990 :111-114, 156), children— ranging from infants to 16-year-olds—were selected for sacrifice throughout the Inca realm based on their physical perfection. Parents could also volunteer their children as part of the annual tribute under the Inca system of taxation, an offering that was met with great rewards and social prestige. While both sexes were chosen for the ritual, it appears that females were sacrificed more often than males.
Those children selected for the capacocha were brought to Cuzco, lavished with feasts and ceremonies, and then taken to the place of sacrifice, sometimes thousands of kilometers from the capital city (Cobo, 1990 ). Upon arrival at their final destination, additional feasts and rituals were held before the children were sacrificed, usually through strangulation, exsanguination, or interment while alive (though probably drugged with alcohol). The bodies of the children were then buried together with elaborate objects of gold, silver, Spondylus shell, wood, bone, textile and ceramic (Cobo,1990 ).
The Spanish chronicler Juan de Betanzos (1996 :132) described a capacocha event performed at the request of the Emperor Pachacuti as part of his planned funerary rites. Pachacuti ordered that exactly one thousand children be chosen from across the empire and brought to Cuzco, paired ritually as married couples, and buried with the traditional gold and silver “table service” of a wedded couple. Betanzos noted that the sacrificed children were to serve the emperor in his afterlife.
Several chroniclers mentioned capacocha rituals that occurred in and around the imperial capital of Cuzco (Betanzos, 1996 ; Cobo, 1990 ; Molina, 1943 ; Sarmiento de Gamboa, 2007 :119, 140). Betanzos (1996 :46) described a capacocha at the Temple of the Sun in the heart of Cuzco, where “well dressed and adorned” children were buried alive to consecrate the new temple. Also, Cobo (1990 :156) wrote of a capacocha in which “the children were strangled and buried with gold and silver on the hill of Chuquichanca, which is a half league from [Cuzco] city above San Sebastian” and other rituals performed near the Angostura, southeast of Cuzco city, in which “a greater quantity of children were sacrificed here than anywhere else” (Cobo, 1990 :72).
2.2 Archaeological Discoveries
A remarkable capacocha discovery was made in 1995 when Johan Reinhard and colleagues found “Juanita,” a frozen Inca child mummy, on the summit of Cerro Ampato in the Colca Canyon region of southern Peru (Reinhard, 1996, 2005). The child was wrapped in a belted dress, shawl, and tupu (shawl) pin, with leather slippers on her feet; around her lay artifacts including a Spondylus female figurine, classic Inca-style ceramics, and a coca bundle. Laboratory analysis revealed that the 13- to 15-year-old Juanita died from a blow to the head, as evidenced by a skull fracture on the right temple (Reinhard, 1997). Three other children were found on Cerro Ampato, including a 9- to 10-year-old boy (though badly charred by lightening) and a 12- to 14-year-old girl with a headdress of macaw feathers and tiny sandals (Bray et al., 2005; Reinhard, 1996). Many of the associated artifacts, such as twin wooden cups and two bird-headed plates, were found in pairs (Reinhard, 1996:76), with the fine Inca ceramics originating from the imperial centers of Cuzco and Tiwanaku (Bray et al., 2005:96).
In 1999, three child mummies were found on Cerro Llullaillaco in northwestern Argentina (Reinhard, 1999, 2005). With them was a diverse assemblage of artifacts, including more than 20 clothed statues that mimicked the apparel of the sacrificed children (Reinhard, 2005:309). While the exact cause of death could not be determined, radiographs of the teeth and long bones provided the ages-at-death for the three individuals: a 6-year-old girl, a 7-year-old boy, and a 15-year-old female (Previgliano et al., 2003:1474).
While these two capacocha discoveries—and additional ones found on Cerro Chañi, Cerro Quechuar, and other peaks in the Andean range—were in high-altitude contexts, the ritual was not limited to the Andean peaks. Capacochas have also been discovered at lower altitudes, including at Tiwanaku along the Bolivian shore of Lake Titicaca, Túcume on the Peruvian north coast, and on La Plata Island off the coast of Ecuador (Bray et al., 2005:87; Knudson et al., 2006; McEwan and Silva, 1989; McEwan and van de Gutche, 1992:362). Given these archaeological discoveries, along with the ethnohistoric descriptions of capacochas performed in and around Cuzco, high altitude should not be a defining criterion for the identification of a capacocha context, as this would limit our understanding of the ritual and its significance within the Inca Empire.
3. Child Sacrifice at Choquepukio, Cuzco Valley, Peru
3.1 Archaeological Evidence
The assemblage of seven child burials was discovered in 2004 at Choquepukio, a stratified site in the Cuzco Valley occupied continuously from the Early Intermediate Period (~400 BC–AD 540) through the Late Horizon (AD 1476–1532) (McEwan, 2006; McEwan et al., 2002; McEwan et al., 1995) (Fig. 1). During excavations of this site, Choquepukio field directors Gordon McEwan and Arminda Gibaja uncovered an imperial Inca building with an intact floor, dated to AD 1410–1520 using radiocarbon samples of burned roofing material and wooden columns (Gibaja et al., 2005).
Adjacent to the ceramic jars, six additional individuals—all juveniles—were found near a bedrock outcrop that protruded through the floor and back wall of the building (Fig. 2). As opposed to the secondary interment of the adult skeletons, the child burials were undisturbed primary interments representing a single burial event.
Approximately three meters from the group burial, an additional child was uncovered with the most elaborate artifact of all—a silver figurine approximately 25 cm in height with a Spondylus shell headdress and fragments of cloth (Gibaja et al., 2005) (Fig. 5). The figurine was modeled with male anatomy and its hands positioned across its chest. Around this artifact were miniature gold, silver, and Spondylus figurines of human males and llamas (Fig. 6), with even more rich offerings found nearby, including
miniature silver and gold headdress ornaments, gold and silver llama figurines, Spondylus
shell male human figures, a miniature bracelet, and pieces of gold foil (Fig. 7).
3.2 Osteological Evidence
The osteological analysis provided chronological ages-at-death of the children, based on dental development and eruption rates (Moorrees et al., 1963; Ubelaker, 1999). The ages were as follows: one individual of 3-4 years, one of 4-5 years, two of 5-6 years, one of 6-7 years, one of 8-9 years, and one of 11-12 years. The sex of the individuals could not be determined because of their juvenile status. While some methods have been proposed for determining the sex of pre-pubescent skeletal remains (e.g., Cardoso, 2008; Schutkowski, 1993; Weaver, 1980), there is no consensus regarding the reliability of these methods.
The skeletal analysis of these seven individuals did not reveal evidence of physical trauma that would indicate a violent death. However, the bones were found in a poor state of preservation—exhibiting cortical damage, exfoliation, and flaking—which could have obscured indications of trauma. Along with an absence of trauma, no pathological conditions were found aside from slight dental wear on the deciduous teeth of five children, a condition also observed in two sacrificed children from Cerro Llullaillaco (Previgliano et al., 2003:1476).
4. Strontium Isotope Evidence from Child Burials
4.1 Principles of Strontium Isotope Analysis
Strontium isotope analysis has emerged as an important tool for investigating residential mobility and geographical origins (e.g., Ericson, 1985; Knudson et al., 2005; Price et al., 2002; Price et al., 2004; Price et al., 2006; Sealy et al., 1991). This type of analysis is based on the premise that an individual’s teeth can reflect the geographic area of childhood residence.
Radiogenic strontium isotope ratios (87Sr/86Sr) in soils and groundwater vary based on the local geological conditions, specifically, the age and composition of subsurface bedrock (Faure, 1986). These ratios are then reflected in the tissues of plants and animals of each region and remain constant throughout incorporation. When these local sources of strontium are consumed by humans, their dental and skeletal tissues reflect the ratios of the local region (Bentley, 2006; Burton et al., 2003; Ericson, 1985).
For strontium isotope analysis, tooth enamel is preferred over bone because it is less susceptible to contamination. Teeth absorb strontium isotopes until tooth crown formation has completed, from fetal stages through the first 12 years of life, depending on the type of tooth. Deciduous tooth crown development begins in utero while most permanent tooth crowns begin developing during the first year of life (Hillson, 1996:123-
When individuals of a population relocate to another area, strontium isotope ratios of their teeth may differ from local residents (Price et al., 1994; Price et al., 2004; Wright,
2005). A comparison of these ratios can reveal the presence of foreigners through deviations from the local isotope signature. This local signature is often determined by sampling local fauna that consumed only locally grown foods; for the Andean region, guinea pigs (cuy, Cavia porcellus) are frequently used.
Despite the clear utility of strontium isotope analysis for determining residential mobility, the technique does have some limitations. Strontium isotopic variability throughout the Andes is not well understood on both a macro- and micro-regional level, and the areas with known 87Sr/86Sr values represent only a fraction of the geologically variable regions of the Andes (see Andrushko et al., 2009, Conlee et al., 2009, Knudson and Buikstra, 2007, and Slovak et al., 2009 for a review of strontium isotope analysis in the Andes). Moreover, many areas may overlap in their signatures due to similar geology; as a result, it is far easier to classify individuals as non-local than to determine, with certainty, their original residence. These limitations—as well as concerns regarding contamination and diagenesis—must be taken into account when initiating a strontium isotope analysis.
4.2 Strontium Isotope Ratio Range for the Cuzco Region
The Cuzco Valley and the adjacent Vilcanota Valley constitute an inter-Andean basin separating the Andean hills to the south and west and the higher-range slopes to the north and east. The valley floor, formed by the Quaternary Pleistocene-aged San Sebastián Formation, consists of sedimentary gravels, alluvial fan sands, mud flows, extended diatomite, loams, clays, and peats. Within the district of Cuzco, igneous intrusive plutonic bodies of Paleocene origin have been identified. One such complex located north of the city of Cuzco, the Stock of Sacsayhuaman, is characterized by medium-to-coarse fractured gray-green quartz diorite (Salvador and Davila, 1994). Although no strontium isotope values have been published on geologic material from the Cuzco region, 87Sr/86Sr values for the Arequipa volcanics located just to the south range from 0.70714 to 0.70794 (James et al., 1976:Table 1; Lebti et al., 2006). While
geological sources may be used to determine the 87Sr/86Sr value of a region, faunal sources are preferred (Price et al., 2002; Sillen et al., 1995). Faunal sources more accurately measure biologically available 87Sr/86Sr values, while water and soil sample 87Sr/86Sr values do not always have a direct 1:1 relationship with animal tissue.
A preliminary range of strontium isotope ratios (87Sr/86Sr ) was identified for the Cuzco region as part of an adult strontium study at Choquepukio (Andrushko et al.,2009). The study used dental samples from 59 adults, along with the teeth of eight guinea pigs from Choquepukio and the site of Tipón, located five kilometers from Choquepukio. The four Choquepukio archaeological guinea pig teeth produced an average 87Sr/86Sr value of 0.70795 (std. dev. = 0.00013), while the four modern guinea pig teeth from Tipón yielded an average 87Sr/86Sr value of 0.70826 (std. dev. = 0.00027). Using these faunal values along with a data-outlier approach to the human strontium values, the Cuzco-region 87Sr/86Sr range was determined to be 0.70728 to 0.70906 (Andrushko et al.,2009).
Certain foods likely contributed to the 87Sr/86Sr values seen in all sampled individuals at Chokepukio. Diets rich in plant sources such as seeds, nuts, and legumes contribute to 87Sr/86Sr levels in humans (Price et al., 1994:323). The native Andean diet included maize, potatoes and other tubers, quinoa, camelid and cuy meat, peppers, and beans (Rowe, 1946:210). Of these foods, beans constitute the most important source for strontium, because legumes have a high calcium and strontium content (Burton and Wright, 1995:278). Although individuals at Chokepukio may have consumed non-locally grown imported maize, maize consumption does not influence human 87Sr/86Sr values, as the crop contains little calcium and strontium (Aufderheide and Allison, 1995). Additionally, while certain marine resources can affect strontium values (Burton, 1996), these resources did not constitute a substantial portion of the local Cuzco diet (Rowe,
5. Materials and Methods
The strontium analysis of the seven Choquepukio child burials was conducted at the Radiogenic Isotope Facility, Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton. The samples were prepared for analysis in the Class 100 cleanroom facility and sonicated for 15 minutes in Millipore water (MQ) followed by 5% acetic acid for 15 minutes. After an overnight leaching in 5% acetic acid, the acid was removed and samples were rinsed with MQ prior to transfer to vials. After adding a Rb-Sr spike, the samples were digested in a microwave oven in 4 ml 16N HNO3 and 1 ml~10 N HCl. Digested samples were dried overnight on a hot plate (80C).
Trace element analysis was conducted on the same samples at the same facility to check for possible contamination. In addition, laboratory preparation for the strontium isotope analysis followed standardized protocol with steps taken to ensure that contamination did not affect the results. Although tooth enamel is much less susceptible to contamination than bone or dentine, we further decreased the possibility of post- depositional contamination by chemically and mechanically cleaning and abrading the tooth surfaces, techniques shown to reduce some diagenetic contamination (Nielsen- March and Hedges, 2000). This study utilized the solution mode for isotopic analysis, which appears to offer a more accurate method for detecting historical migrations than laser ablation (Simonetti et al., 2008). Diagenetic contamination from the burial environment was monitored through uranium concentrations, which should be below the detection limit of the Inductively Coupled Plasma – Mass Spectrometer (ICP-MS). For a complete description of these methods, see Andrushko et al. (2009), Buzon et al. (2007), and Simonetti et al. (2008:373-374).
Strontium isotope measurements were determined using a NuPlasma MC-ICP-MS instrument. Subsequent to ion chromatographic treatment of the samples, the Sr-bearing aliquots were diluted in a 2% HNO3 solution and aspirated into the ICP torch using a desolvating nebulizing system (DSN-100 from Nu Instruments Inc.). Strontium isotope data were acquired in static, multicollection mode using five Faraday collectors for a total of 400 seconds, consisting of 40 scans of 10 second integrations. The ‘wash-out’ period following the analysis of a sample was approximately 5 minutes. Prior to the aspiration of
a sample, a 30 seconds measurement of the gas (+ acid) blank was conducted, which is critical for the correction of the 86Kr and 84Kr isobaric (plasma-based) interferences. The isobaric interference of 87Rb was also monitored and corrected for using the 85Rb ion signal; however, the latter was negligible for all of the results reported here. Accuracy
and reproducibility of the analytical protocol were verified by the repeated analysis of a
100 ppb solution of the NIST SRM 987 Sr isotope standard during the course of this study; this yielded an average value of .710242 ± .000041 (2 standard deviation; n = 13 analyses) and is indistinguishable compared to the accepted value of .710245 (Faure and Mensing, 2005:78). The typical internal precision (‘error’) associated with an individual Sr isotope analysis varies from .00001 to .00003 (2 level).
6. Results of the Choquepukio Child Burial Strontium Analysis
Based on the 87Sr/86Sr range for the Cuzco region (0.70728 to 0.70906), two of the seven children were identified as non-local (Table 1). The first individual (CHO 141) exhibited a 87Sr/86Sr value of 0.70910, just above the Cuzco-region range and within the range of the Tiwanaku region of Bolivia (0.7087 to 0.7105) (Knudson, 2004). The second individual (CHO 142) yielded a 87Sr/86Sr value of 0.70638, well below the Cuzco range. Instead, this 87Sr/86Sr ratio fell into the range observed for Wari individuals from the Ayacucho region (0.7054 to 0.7067) (Tung, 2003:80).
The 87Sr/86Sr values of the other five children were within the local range, suggesting that they originated from the area around Choquepukio (or a geologically similar area). Two individuals had values resembling the Choquepukio faunal average (CHO 140, 87Sr/86Sr =0.70796; CHO 144, 87Sr/86Sr =0.70783), while another individual yielded a value slightly below the average (CHO 152, 87Sr/86Sr =0.70768). The final two individuals had values similar to the Tipón faunal average (CHO 143, 87Sr/86Sr =0.70827; CHO 146, 87Sr/86Sr =0.70809).
The sampled teeth were a mixture of deciduous and permanent teeth (Table 1). For three individuals, the second deciduous molar was used, which resulted in a strontium ratio reflecting the geographic place of in utero development, birth, and the first 11 months of life (Hillson, 1996:124). In another case, the first permanent molar was used, representing the individual’s geographic origins from birth to age three. For two more children, the sampled teeth were permanent central incisors; the resulting values corresponded to their residences during ages three months to four years. Finally, for the single child whose first premolar was analyzed, the 87Sr/86Sr ratio related to the geographic residence during the first to sixth years of life (Hillson, 1996:123).
Trace element data indicated that the results were not influenced by contamination, with the possible exception of one enamel sample (Table 1). The sample from local individual CHO 140 contained 0.04 ppm of uranium, just above the allowable limit of 0.03 ppm (detection limit for the MC-ICP-MS). Uranium, which is not normally found in skeletal tissues, can reflect the uptake of groundwater and may influence
87Sr/86Sr ratios (Hedges and Millard, 1995). Contamination of this sort could cause a non-local strontium value to resemble the local signature, but is unlikely to change a local value into a non-local value. As such, CHO 140 could have been a non-local child whose 87Sr/86Sr value matched the local signature due to contamination.
When considered together, the osteological, archaeological, and isotopic evidence suggest that a capacocha event occurred at Choquepukio. First, the ages of the Choquepukio children closely match the ages reported in colonial accounts of capacocha sacrifices. At Choquepukio, the children ranged in age from 3 to 12 years, with a mean age of 6.5 years. Meanwhile, the Spanish chronicler Betanzos (1996 :132) noted that for the capacocha demanded by the Emperor Pachacuti, “[a]ll these children should be from five to six years of age.” Another Spanish chronicler, Rodrigo Hernández Principe, described a capacocha in which children aged 10 to 12 years were brought in from the four corners of the empire (Hernández Principe, 1923).
The mortuary treatment also provides evidence for a capacocha event. These seven children represent a single interment episode—a significant deviation from the normal burial treatment of children at Choquepukio during Inca times (Andrushko et al.,2006).
In addition, the artifacts found with the grouped children bear a striking similarity to those found at the Ampato capacocha. For both sites, gendered human figurines and tiny llama figurines feature prominently (Bray et al., 2005). At Choquepukio, some children were buried with female figurines, while the last child recovered had a 25 cm silver male figurine with a Spondylus headdress. At Ampato, Juanita had a female figurine buried with her and the 10-year-old boy had a male statue. Similar gendered figurines were also recovered at capacocha contexts on Cerro el Plomo and Cerro Copiapó in Chile and other sites (Benson, 2001:16; McEwan and van de Gutche,1992:363).
Of particular interest are the origins of the Choquepukio children—strontium results reveal that two of the children originated from outside of the Cuzco region, possibly from the Tiwanaku region of Bolivia and the Ayacucho region of Peru. As the colonial documents note that capacocha children were selected throughout the empire, the inclusion of non-local children is not surprising. Perhaps more surprising is the presence of five sacrificed children at Choquepukio who do not appear foreign based on their strontium isotope values. However, some accounts note that children were returned to their homelands for sacrifice after traveling to Cuzco (McEwan and van de Gutche,1992:360; Reinhard, 2005:30), in which case the presence of local children in the sacrificial context is understandable.
With the totality of evidence for the seven child burials—the ages of the children, the mass grave and exclusion of adults, the elaborate artifacts resembling those from other capacocha events, and the strontium results pointing to the inclusion of non-local children—we believe these burials represent a capacocha event. In fact, the Choquepukio context mirrors the archaeological expectations put forth by McEwan and van de Guchte (1992:362):
The presence of a child’s body accompanied by suites of miniature offerings in precious metals, sea shell, and textiles is convincing proof that the final act of sacrifice was carried out at carefully selected locations…
If so, this is a significant discovery that allows us to increase our understanding of the capacocha ritual apart from what is known in ethnohistoric documents. Our findings at Choquepukio, along with those from recent archaeological discoveries, show that a capacocha could vary by number and age of victims, type of grave goods, and location. Such variability may relate to the fact that some capacocha rituals were initiated at the village level, while others were enacted at the level of the state (McEwan and van de Gutche, 1992:362). The discovery at Choquepukio illustrates that capacocha events were not restricted to high-altitude environments, but rather were carried out at a variety of elevations throughout the Inca Empire.
The osteological evidence does not indicate how the children died. This may be due to the poor preservation of the skeletal remains, masking any indication of trauma, or it may be due to the specific way in which the children were sacrificed. Children were frequently strangled as part of the capacocha ritual (Cobo, 1990 ), which would not have left any mark on the bones. The hyoid bone, which is often fractured when adults are strangled, rarely fractures in children because it is unfused (O’Halloran and Lundy, 1987). Consequently, children in Inca sacrificial contexts rarely show physical evidence for cause of death (Verano, 2001:168).
Why was Choquepukio chosen as a site for the capacocha? One possible explanation lies in the historical importance of the site. Prior to the rise of the Inca Empire, during the Late Intermediate Period (AD 1000–1476), the Pinagua ethnic group had their center of political power at Choquepukio. Together with another group, the
Ayarmaca, they controlled the Lucre Basin and territory to the east of Cuzco as well as territories to the north (Hiltunen and McEwan, 2004:246; McEwan et al., 2002:292). The Pinagua constructed monumental niched temples at Choquepukio for purposes of feasting and forming alliances, as inferred from architecture and associated luxury items (McEwan et al., 1995). In later Inca times, Choquepukio’s distinction as a powerful ancient site would have imbued it with ceremonial value, since the Inca venerated locations of historic significance (Bauer, 1998; Bray et al., 2005:87). Such ceremonial value may have contributed to Choquepukio’s selection for the capacocha event.
A second possible explanation lies in Choquepukio’s geographical location on the sacred landscape (Swenson, 2003:276). For the Inca, points of intersection (tinkuy) held symbolic importance, such as the confluence of two roads or two rivers. Choquepukio lies close to the intersection of the Huatanay River and the Collasuyu Road, one of four Inca roads originating in Cuzco—and both the Huatanay River and the Collasuyu Road were associated with the supreme Inca deity Viracocha. It is therefore possible that Choquepukio’s geographical position as a point of intersection conferred a ritual significance to the site.
A third explanation concerns the warm natural spring that flows out from beneath the hill on which Choquepukio sits. A warm spring would have been an important and powerful huaca, a sacred object or place on the landscape (Bauer, 1998; Van de Gutche,
1999). The Incas would have desired to propitiate the supernatural spirit embodied by the spring and this could explain the location of the sacrifice. Given the profound significance of the capacocha ritual, the occurrence at Choquepukio suggests an important religious event in the history of the site.
Our study investigates a possible capacocha, the Inca ritual of child sacrifice, at the site of Choquepukio in the Valley of Cuzco, Peru. The 2004 discovery consists of seven children buried together with a large assemblage of luxury artifacts, including gold and silver miniature human figurines, red Spondylus shell figurines, gold, silver, and bronze tupu pins, and several sets of Inca imperial ceramic vessels. This type of mortuary treatment deviates from other child burials at Choquepukio, suggesting that the burial assemblage does not represent local children who died of natural causes. The strontium isotope results further indicate that two of these children were non-local. When considered together, the osteological, archaeological, and isotopic evidence suggest that a capacocha event occurred at Choquepukio.
The findings at Choquepukio accord with descriptions from Spanish chronicles regarding the sacrifice of children at lower-elevation locations, such as at the Temple of the Sun in Cuzco. However, our recent knowledge of capacochas has derived mainly from the spectacular high-altitude findings on several Andean mountain peaks.
This study reinforces that the capacocha was an important aspect of Inca religion and further illustrates the variability within this ritual regarding the number and ages of children sacrificed, location of sacrifice, and types of offerings included in the graves. The study also challenges the supposition that sacrificed children always originated from diverse regions of the empire. Our study suggests that local children were mostly sacrificed, although two non-local children were included in this ritual.
Finally, this study highlights the importance of isotope analysis in investigating archaeological contexts of human sacrifices. A growing number of studies (Fernández et al., 1999; Knudson et al., 2006; Price et al., 2007; Tung and Knudson 2010; White et al. 2007; White et al., 2002; Wilson et al., 2007, among others) have contributed significant information regarding the geographic origins and pre-death treatment of sacrificial victims. In the case of Wilson and colleagues’ (2007) study, hair samples from four mummies—including the 15-year-old "Llullaillaco Maiden" and the 7-year-old "Llullaillaco Boy"—indicate that the children’s diets changed markedly in the twelve months before their deaths, suggesting they were fed more “elite” foods in preparation for sacrifice. In addition, isotopic changes found in their hair samples indicate that the children began their pilgrimage to the mountains three to four months before they died.
As evident from these studies, archaeological chemistry techniques now enable us to document with detail an intriguing phenomenon—the practice of human sacrifice—that held great importance for many ancient civilizations.
The authors wish to gratefully acknowledge the Bernard Selz Foundation whose funding has made possible all excavations and artifact analyses of the Selz Foundation Excavations at Choquepukio, Peru. We extend our deep gratitude to the Wenner-Gren Foundation for Anthropological Research (Individual Research Grant #7283) and the National Science Foundation (Doctoral Dissertation Improvement Grant #0424213) for providing funding for this project. The Radiogenic Isotope Facility at the University of Alberta is supported, in part, by an NSERC Major Resources Support Grant. Elva Torres Pino is gratefully acknowledged as the Director of Physical Anthropology at the INC- Cusco. We would also like to thank Melissa Chatfield, Paul Steele, Katharina Schreiber, Viviana Bellifemine, Tiffiny Tung, Kelly Knudson, Bethany Turner, Nicole Slovak, and Barbara Hewitt. Special thanks to Froilan Itturiaga Guzman from the Choquepukio Project. Additional thanks to Jaime Donnelly for sample preparation and GuangCheng Chen for assistance with the MC-ICP-MS analyses. Finally, we are grateful to the editors and anonymous reviewers for their helpful and insightful comments.