Introduction
Structure 19:N1W5 (hereafter E19) is an apartment compound located near the west edge of the ancient Classic-period city of Teotihuacan (Figure 1; Millon et al. Reference Millon, Bruce Drewitt and Cowgill1973). It is only 165 m east of what has been defined as the eastern border of Tlailotlacan, the Zapotec Barrio of Teotihuacan (Figure 2; Cid Beziez Reference Cid Beziez, Brambila and Cabrera1998:321–322; Spence Reference Spence and Plunket2002: Figure 6.1). In 1990‒1991, Gómez Chávez directed an extensive series of excavations in the Zona Militar, including the almost complete excavation of E19 (Figure 3; Gómez Chávez Reference Gómez Chávez1998, Reference Gómez Chávez and Gallut2002, Reference Gómez Chávez, Charlotte Arnauld, Manzanilla and Smith2012, Reference Gómez Chávez and Robb2017; Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola and Faugère2007, Reference Gómez Chávez, Gazzola, Lauriers and Murakami2021).
Teotihuacan map, showing location of E19 (inset). Map by René Millon and Gómez Chávez.
E19 and vicinity, with 22:N1W6 and Burial 15. The east edge of Tlailotlacan extends along the east side of 5:N1W6. Figure by Gómez Chávez.
Plan of E19, showing Burials (Entierros) 25, 27, 30, and 31. Figure by Gómez Chávez.
E19 is an informative and important site for a variety of reasons, but its most striking aspect is the mortuary and ceramic evidence for the presence of people from the modern state of Michoacan. Seven architectural units have been defined for the site based on the patios, plazas, walls, and passageways that divide and connect spaces. On a larger scale, the structure is clearly separated into two major sections, an earlier northern section and a somewhat later southern section. The earliest construction dates to the Early Tlamimilolpa phase (a.d. 170‒250) but the site continued into the Metepec phase (a.d. 550‒650; Cowgill Reference Cowgill2015:Table 1.2).
E19 sample: description, crystallinity indices (CI), and oxygen isotope compositions. A, adult; YA, young adult; MA, middle adult; OA, old adult; F, female; M, male; y, years; m, months.
a Age of crown completion (Crc) stage, from median column of AlQahtani et al. (Reference AlQahtani, Hector and Liversidge2010:Tables 2–8).
b Nursing effect corrections: dM1, dM2, permanent M1, and bones of children under three years reduced by 0.7‰, C by 0.35‰.
E19 contains evidence of relationships with both Michoacan and Zapotec-related peoples, the latter surely derived from nearby Tlailotlacan. The Michoacan relationship is expressed in mortuary features, material culture associated with those features, cooking stoves different from the Teotihuacan ones, and perhaps in some biological data. In particular, there are patterns of cranial modification that do not appear elsewhere in Teotihuacan, although their foreign affiliation will require more detailed comparative analysis (Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola and Faugère2007:120). These Michoacan links appear primarily in several mortuary contexts occurring in three of the architectural units. In contrast, the evidence of Tlailotlacan influence appears in the form of architectural features, including a tomb in Architectural Unit 7 (Gómez Chávez Reference Gómez Chávez and Gallut2002:571, 602‒604).
The architectural evidence of Tlailotlacan influence appears widely in the structure. It consists of tubular ceramic drain segments (Gómez Chávez Reference Gómez Chávez1998:1465), cobblestone floors (pisos empedrados), flagstone floors (pisos enlajados), and the escapulario variant of the talud-tablero architectural facade (lacking the lower enclosing element of the tablero). These are all common features of Tlailotlacan, for the most part derived ultimately from the Valley of Oaxaca Zapotec settlements (Gómez Chávez Reference Gómez Chávez1998:1465–1466; Reference Gómez Chávez and Gallut2002:574, Photograph 2; Ortega Cabrera Reference Ortega Cabrera2014:141–145). It should be noted that cobblestone floors do appear in other areas of Teotihuacan (e.g., Reference Carballo, Hirth, Sariñana, Buckley, Mejía Ramón and KennettCarballo et al. 2019; Storey Reference Storey1992), but their frequency in Tlailotlacan coupled with the other Tlailotlacan elements in E19 leave no doubt that Tlailotlacan was the immediate source for their presence in E19.
Ritual deposits, however, have not been found in E19 despite their frequency in Tlailotlacan. Typically, such deposits consist of a ceramic vessel sitting upright on the base of a small pit, usually in a patio, with another vessel or simply some large sherds inverted over it as a cover (Spence Reference Spence and Plunket2002). These features have a long history in the Valley of Oaxaca, where they represent the long-standing Zapotec practice of burying the umbilical cord and/or afterbirth from a successful birthing in a covered jar in the family patio (Feinman et al. Reference Feinman, Nicholas and Maher2008; Lind and Urcid Reference Lind and Urcid2010:314, n4; Parsons Reference Parsons1936:76). The absence of such deposits in E19 suggests that there was no significant occupation of E19 by Tlailotlacanos despite the architectural evidence of their involvement in its construction. The one exception to this would be Architectural Unit 7, where the Zapotec tomb suggests a more substantial presence.
In order to clarify the proposed Michoacan and Tlailotlacan/Oaxacan relationships of E19, we conducted oxygen isotope analyses of dental enamel and bone samples from five of the excavated mortuary features, four of them within E19 and one a short distance beyond the apartment compound (Spence et al. Reference Spence, White, Gazzola, Chávez and Longstaffe2006). A number of projects have demonstrated the advantages of using two or more isotopes, usually oxygen and strontium (Buckley et al. Reference Buckley, Storey, Longstaffe, Carballo, Hirth and Renson2021; Manzanilla et al. Reference Manzanilla, Mejía, Jiménez, Schaaf, Lailson, Solís, Morales, Cienfuegos and Manzanilla2012; Morales Puente et al. Reference Morales Puente, Alvarado, Manzanilla Naim, Otero Trujano and Manzanilla2012; Price et al. Reference Price, Burton, Wright, White, Longstaffe, Tiesler and Cucina2007, Reference Price, Spence and Longstaffe2021; Schaaf et al. Reference Schaaf, Solís, Manzanilla, Hernández, Lailson, Horn and Manzanilla2012; White et al. Reference White, Price and Longstaffe2007). In effect, they allow the triangulation of a source area (Spence and White Reference Spence and White2009:237–239). The oxygen isotope analysis reported here, however, was done in 2004, before the development of the institutional collaborations that allowed multiple-isotope analyses. Nevertheless, single-isotope analyses like the present one can still provide reliable insight into the movements of people (e.g., Price et al. Reference Price, Manzanilla and Middleton2000; Spence et al. Reference Spence, Olsen, Cabrera Cortés and Longstaffe2020).
The oxygen isotope composition of a person's teeth and bones is derived predominantly from the isotopic composition of the water that they drink (Longinelli Reference Longinelli1984; Luz and Kolodny Reference Luz and Kolodny1985). The oxygen isotope composition of the water in turn depends on the combination of a variety of factors including temperature, humidity, distance from the ocean, and altitude, leading to distinct oxygen isotope compositions characterizing the waters of different geographic regions (Stuart-Williams et al. Reference Stuart-Williams, Schwarcz, White and Spence1996). The oxygen isotope ratio of an individual, therefore, allows us to place that person in a particular geographic location at the time of formation of the tissue from which the sample was taken, provided that: (1) baseline oxygen isotope compositions for drinking water and hence individuals from specific geographic locations are available; (2) the possible localities of interest where an individual may have resided can be inferred from other data; and (3) oxygen isotope baselines for these locations are analytically distinct within the limitations of the method.
Since dental enamel develops early in life and does not change thereafter, its isotopic composition will reflect the geographic location of an individual during the time of tooth formation. The isotopic composition of their bones, on the other hand, will reflect their more recent location because the components comprising bone will continue to turnover throughout the person's lifespan. Ideally, then, the isotopic composition of teeth and bones can allow us to identify a person's geographic relocation through time. In fact, the analysis of different teeth, which form at different ages, can show movement during the individual's childhood (e.g., White et al. Reference White, Spence, Longstaffe and Law2004a). The isotopic compositions of some of the earlier forming teeth, however, have to be corrected because of the trophic effect of breastfeeding. The values for deciduous molars and permanent first molars are adjusted downward by 0.7‰. Those for permanent canines are reduced by 0.35‰. The values for deciduous incisors, on the other hand, are not adjusted since they form in the womb and will simply match those of the mother (White et al. Reference White, Spence, Longstaffe and Law2004a:393–394). Also, bone oxygen isotope compositions of children under the age of 3 years are reduced by 0.7‰.
The burials
The five burials selected for oxygen isotope analysis include a variety of features, ranging from a burial feature that has Michoacan parallels and offerings of Michoacan items to the Zapotec-style tomb. Unfortunately, most of the burials have yet to receive a full osteological analysis. In the cases of Burial 15, a repurposed well outside E19, and of Burial 31, a cremated adult male, there is no clear archaeological evidence of either Michoacan or Tlailotlacan relationship; the isotopic analysis may offer our only clue to their affiliation. Twenty-two enamel and 19 bone samples were collected from the individuals in the five burial features.
Feature dates are based on the architectural stratigraphy and the associated ceramics. Where possible we have used the specific phase designation, e.g., the Late Tlamimilolpa phase. When that level of precision was not possible the larger period designation was used, e.g., Tlamimilolpa period. Phase and period dates follow Cowgill (Reference Cowgill2015:Table 1.2).
Burial 25
Burial 25 is a Zapotec-style tomb in Architectural Unit 7 (Figure 3; Gómez Chávez Reference Gómez Chávez1998:1476, Figure 7, 2002:602–604). It is constructed much like the numerous tombs found throughout the nearby Tlailotlacan Barrio. Material items in the tomb include small mica, obsidian, and ceramic fragments. There were no Zapotec-style or Michoacan-style ceramic items. The tomb dates to the Tlamimilolpa period (a.d. 170–350).
Also present in the tomb were the fragmented and disarticulated skeletal elements of two incomplete adults. One individual is an elderly male, as determined by the mandibular morphology and the heavy dental attrition. The other was a male of middle age (Luis Alfonso González, personal communication 1991). A dental and bone sample were taken from each individual (Table 1).
Burial 30
Burial 30, located in Architectural Unit 1 (Figure 3), is a nearly square pit, widening slightly toward the base (Figure 4; Gómez Chávez Reference Gómez Chávez1998:1479, Figures 8–10, 2002:579–582, Figures 5, 8a, Photographs 4–6). It had been sealed at two different times with wide stone covers, indicating its use on two occasions. The large offering consisted mostly of Teotihuacan items but also included three bowls and one figurine from Michoacan (Figure 5).
Profile of Burial 30 and reconstructed cover. Arrow indicates level at which covers had originally been placed. Figure by Gómez Chávez.
Burial 30 grave offering. Photograph by Gómez Chávez.
Profile and plan of B27 and “Burial” 26. Figure by Gómez Chávez.
Burial 27 grave offerings. Photograph by Gómez Chávez.
Burial 27 foreign offering items. Photograph by Gómez Chávez.
TL6 and Tlajinga 33 oxygen isotope compositions, within +14.0–16.0‰ range of Teotihuacan. Graph by Olsen.
Sites of the Michoacán Lakes Region. (1) Tzintzuntzan. (2) Tocuaro. (3) Urichu. (4) Guadalupe. (5) Milpillas. (6) El Palacio. (7) San Antonio Carupo. (8) Los Portales. (9) Los Nogales, Guanajuato. Map by Pollard.
The burial feature is similar to those that Pereira (Reference Pereira, Williams and Weigand1996, Reference Pereira1997) has designated “asymmetrical” or “niche” burials in Michoacan: a pit with one side expanded slightly or hollowed to hold a primary burial. The Michoacan examples in the Loma Alta site are in pits capped by slabs, commonly placed obliquely. They first appear in Loma Alta 2 (a.d. 0–350; Pereira Reference Pereira, Williams and Weigand1996, Reference Pereira1997). Similar features also occur at Erongaricuaro in the Patzcuaro Basin (Begun Reference Begun2013:114).
The disarticulated and burned skeletal remains of three individuals were present in the Burial 30 pit. One is an adult female (No. 3), 60 or more years of age by the auricular area and symphysis pubis methods (Lovejoy et al. Reference Lovejoy, Meindl, Pryzbeck and Mensforth1985; Suchey and Katz Reference Suchey, Katz and Reichs1998). The other adult (No. 1) is a male about 45–50 years old as determined using the same methods. The third individual (No. 2) is a child of eight to nine years by dental development (AlQahtani et al. Reference AlQahtani, Hector and Liversidge2010). A later Aztec intrusion has disturbed the feature, but the distribution of skeletal elements suggests that the adult female was the initial interment in the pit, in the Late Tlamimilolpa phase (a.d. 250–350), while the adult male and the child were buried in a later episode, in the Xolalpan period (a.d. 350–550). The stone cover of the first episode (reconstructed in Figure 4) had been originally placed at the top of the pit but was broken for the interment of the man and child. Most of the pieces were put in the bottom of the pit and a new stone cover was placed where the original one had been (Figure 4). Two samples, one bone and one dental, were taken from each individual (Table 1).
Burial 31
Burial 31 is a flexed, adult male, cremated in situ in a small pit in Architectural Unit 1 (Figure 3; Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola, Lauriers and Murakami2021:89, Figure 3.13). No Michoacan materials were present in the feature. The associated ceramics date the burial to the Late Tlamimilolpa phase (a.d. 250–350). One bone and one dental sample were taken but analysis of the dental sample failed (Table 1). The bone sample, from a left rib, was analyzed successfully. Like the Burial 30 samples, it had been selected to avoid any obvious fire effects. The crystallinity index of 3.7 (Table 1) is within the acceptable range.
Burial 27
Burial 27 is located beneath a platform in Architectural Unit 3 (Figure 3; Gómez Chávez Reference Gómez Chávez1998:1481–1485, Figures 11–15, 2002:585–597, Figures 6–7, 8b, Photographs 7–12). It is a deep pit with a stone lining in the upper part, not characteristic of Teotihuacan burials (Figure 6). Some 65 items, mostly ceramic vessels, were present in the lowest level of the B27 pit (Figure 7). Among these were several greenstone encrustations apparently intended for dental modifications, some ceramic items and two figurines of Michoacan style (Figure 8), and a blade of Zinapecuaro obsidian. The bowls are much like those from Querendaro in the Cuitzeo area of northern Michoacan (Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola, Lauriers and Murakami2021:88, Figures 3.9–3.10). Some of the crania have cranial modification of types not characteristic of Teotihuacan. They required techniques and instruments different from those used in Teotihuacan (Gómez Chávez Reference Gómez Chávez and Gallut2002:597; Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola and Faugère2007:120; Rosaura Yepes, personal communication 1998). Although possibly of West Mexico origin, more detailed comparisons will be necessary to establish their source. The offering ceramics and the architectural context of the pit place it in the interval between the Early Tlamimilolpa and Late Tlamimilolpa phases, ca. a.d. 250. The burials are among the earliest in E19.
Means and ranges of oxygen isotope compositions of E19, Patzcuaro Basin, Zacapu Basin, Tlajinga 33, and TL6. Graph by Olsen.
All levels of the pit were filled with skeletal remains. Many of these were disarticulated and isolated elements but there were also some articulated segments, including some crania with mandibles and cervical vertebrae, and some torso segments. Unfortunately, our osteological analysis of the Burial 27 remains is incomplete, covering only about one-third of the collection. Furthermore, we are unable to say whether the analyzed third is fully representative of the other two-thirds. This means that our counts of skeletal elements (MNE) will provide only a conservative estimate of the minimum number of individuals (MNI) represented in the burial. An initial count of crania showed 10 adults and one subadult, but the later partial analysis of the collection identified four subadults among the postcranial remains; there are four unfused proximal epiphyses of the right tibia and 40 thoracic vertebra bodies with unfused arches. A revised MNI for Burial 27 would then be 14, but this estimate will likely grow with a full osteological analysis.
All of the human remains and artifacts had been deposited in the pit in a single event, not added to it sequentially over time. There were also a couple of articulated segments like the foot of “Burial” 26 (Figure 6) lying on the original surface from which the Burial 27 pit was excavated. They had apparently been left where they had fallen during the interment of the Burial 27 skeletal material, in the expectation that they would be covered by the platform that was to be constructed over the feature.
The ceramics and other offering items had been placed in the bottom of the pit with the skeletal elements mostly above them. None of the analyzed skeletal elements shows cutmarks or evidence of perimortem trauma. That is not to say that some cutmarks or other evidence of dismemberment would not appear with analysis of the whole collection, but their absence in the analyzed portion suggests that many, perhaps all, of the Burial 27 individuals had been placed there after some time and decomposition in a primary context elsewhere. The burial is, in effect, an ossuary.
Burial 27 is not representative of Teotihuacan mortuary practices, in which secondary burial is not common and collective (multiple) burials are virtually absent. Nor is it representative of the Lakes Region of Michoacan, where collective secondary burials are present but different in nature from Burial 27. They occur in well-constructed, stone-walled structures, and the burials had been added sequentially to the features over years or decades (e.g.. Pereira Reference Pereira1997, Reference Pereira1999; Pollard and Cahue Reference Pollard and Cahue1999:267–269). Funerary Structure 1 of the Guadalupe site is one example. The burial structure is a square stone-walled feature, unlike the simple pit of Burial 27, but it contains an extensive set of secondary burials with only a few primary interments. The MNI is 35 and includes adults and subadults, most of them incompletely represented. Unlike Burial 27, the interments occurred as a series of events over a considerable length of time (Pereira Reference Pereira1999).
In a mixed and secondary assemblage like that of Burial 27 it is difficult to identify individuals for multiple (dental and bone) sampling. Such sampling was possible in two cases but for the most part only one sample per individual was obtained. Oxygen isotope analysis was conducted on 15 samples, 9 dental and six bone, representing at least eight individuals (Table 1).
Burial 15
Burial 15 lies in an open area outside E19, south of it and closer to site 22:N1W6 (Figure 2). The burial feature was originally a well, 83 cm in diameter at the top and slightly over 12 meters deep, that in the Early Tlamimilolpa phase (a.d. 170–250) probably provided water for a number of structures in the vicinity, including E19. At some point in the Late Tlamimilolpa phase (a.d. 250–350) it was converted into a burial feature and continued as such in the Xolalpan period (a.d. 350–550). Excavation of the feature neared but could not reach its bottom because of the danger of collapse. The absence of material in the lowest levels, however, indicates that the excavation must have reached very near the bottom of the well. Although the feature's skeletons have not yet received a comprehensive osteological analysis, an estimate suggests that there are at least 14 individuals represented. Also found were 25 canid burials, a jaguar cranium, pyrite discs, and numerous fragments of Teotihuacan theatre censers (Gómez Chávez Reference Gómez Chávez, Charlotte Arnauld, Manzanilla and Smith2012:97, n8; Pérez Ríos and Gómez Chávez Reference Pérez Ríos and Chávez2022; Velázquez González Reference Velázquez González2013:63–65). The canids include examples of the hairless Itzcuintli and short-legged Tlalchichi dogs, both of West Mexico derivation. The artifacts are mostly fill inclusions rather than burial offerings. None of the small fragments are clearly of Zapotec or Michoacan style. Its persisting use in the Xolalpan period makes Burial 15 later in time than the other burials discussed here.
Unfortunately, we are unable to say with certainty which of the nearby structures were contributing burials to the feature. As will be shown, however, the oxygen isotope compositions from Burial 15 are similar to those of E19, suggesting that either E19 was responsible for the burials or that people with Michoacan ties were more widespread in the area than just E19. Notably, the nearest structure, 22:N1W6, has been extensively excavated and its mortuary features and burial practices are much like those of Teotihuacan and unlike the Michoacan and Tlailotlacan-related burials of E19 (Cid Beziez and Torres Sanders Reference Cid Beziez, Sanders, Manzanilla and Serrano1999; Torres Sanders and Cid Beziez Reference Torres Sanders and Cid Beziez2018). This suggests that the interments in Burial 15 were more likely of E19 than 22:N1W6 residents, but a more definite conclusion is not possible with the present evidence.
Some of the bodies had been deposited in the former well as complete and articulated corpses while others were partially or fully disarticulated and often incomplete. Several were tightly flexed and had probably been lowered or carried into the well as bundles. Layers of soil intervening between the burials indicate a lapse of time between interments and may have been deposited to reduce the smell of decomposition. It was possible in a number of cases to collect both dental and bone samples from the same individual. Males and females, and adults and subadults, were present. Sex could be assessed in the six sampled adults, although most of those assessments (all male) were made based on cranial features (Buikstra and Ubelaker Reference Buikstra and Ubelaker1994:19, Figure 4). With a fuller postcranial analysis some of those assessments may change. Adult age was not precisely determined but dental and skeletal evidence (AlQahtani et al. Reference AlQahtani, Hector and Liversidge2010; Scheuer and Black Reference Scheuer and Black2000) allowed age estimates for the two subadults represented in the sample. In all, 15 samples (eight dental and seven bone) were taken from eight individuals, six male adults and two subadults (Table 1).
Analytical methods
Sample preservation
Preservation of original oxygen isotope signals in bioapatite is prerequisite to any investigation that relies on such data to explore the origin of individuals. In that regard, phosphate oxygen was chosen as the target for bioapatite isotopic analysis in this paper because, under most conditions, it is much more resistant than structural carbonate to isotopic exchange and contamination after death and burial of the individual (Schwarcz et al. Reference Schwarcz, Gibbs, Knyf, Pfeiffer and Williamson1991; Shemesh et al. Reference Shemesh, Kolodny and Luz1983). Preservation potential also varies significantly between bone and enamel, both of which were analyzed in the present study. Enamel is least likely to have undergone alteration of its original oxygen isotope composition after death and burial because it is more highly crystallized during formation and has a much lower organic content relative to bone (Quade et al. Reference Quade, Cerling, Barry, Morgan, Pilbeam, Chivas, Lee-Thorp and van der Merwe1992). Bioapatite preservation, and hence a sample's suitability for isotopic analysis, was guided in the present study using the crystallinity index (CI), as defined by Shemesh (Reference Shemesh1990). Those measurements were completed at the Laboratory for Stable Isotope Science (LSIS), the University of Western Ontario, London, Ontario, Canada, using a Bruker Vector 22 Fourier Transform Infrared (FTIR) spectrometer following procedures detailed in Webb et al. (Reference Webb, White and Longstaffe2014).
Values of CI for fresh human bone normally lie within the range ~2.8–3.0, with higher values observed for archaeological bone (3.5–4.8; Webb et al. Reference Webb, White and Longstaffe2014). Higher values for bone are indicative of recrystallization, with values greater than 4.3 diagnostic of extensive recrystallization and potential isotopic exchange. The average CI for bone samples in this study was 3.3 ± 0.4 (1σ, n = 37; all errors reported hereafter are 1σ; Tables 1–3), with no value higher than 4.0. As is the norm, the CI for enamel values was slightly higher (3.6 ± 0.2, n = 32; Tables 1 and 2), reflecting its original higher crystallinity. These data suggest that all bioapatite samples analyzed for oxygen isotope compositions were well preserved. Restriction of analyses to the phosphate component of the bioapatite gives us further confidence that original oxygen isotope compositions have been measured.
CEMCA sample: description, crystallinity indices (CI), and oxygen isotope compositions. A, adult; F, female; M, male; y, years; m, months.
Patzcuro area sample: description, crystallinity indices (CI), and oxygen isotope compositions. F, female; M, male; y, years; m, months.
Oxygen isotope analysis
The oxygen isotope compositions of bioapatite phosphate reported here were measured at LSIS in 2004. Bioapatite was first isolated from bone and enamel and converted into silver phosphate (Ag3PO4) following procedures described by Firsching (Reference Firsching1961) and Stuart-Williams and Schwarcz (Reference Stuart-Williams and Schwarcz1995). The Ag3PO4 was then reacted with bromine pentafluoride at 610°C for a minimum of 16 hours to release stoichiometrically the oxygen inherited from the bioapatite, following the method first described for silicate and oxide minerals by Clayton and Mayeda (Reference Clayton and Mayeda1963) and later adapted to silver phosphate by Crowson and colleagues (Reference Crowson, Showers, Wright and Hoering1991). The oxygen released from the silver phosphate was purified cryogenically and then converted to CO2 by reaction with red-hot carbon. The success of these procedures was first evaluated by measuring the CO2 yield produced from each Ag3PO4 sample. Theoretically, this yield should be 4.76 μmol per mg if all phosphate oxygen was recovered and no additional oxygen from contaminants added. Across all samples analyzed in the present study, an average yield of 4.64 ± 0.17 μmol per mg (n = 71) was obtained, which demonstrates quantitative recovery of oxygen without any contamination.
The oxygen isotope compositions of the CO2, and hence the bioapatite phosphate, were then measured using a Micromass Optima dual-inlet, triple-collecting, gas-source stable isotope ratio mass spectrometer. The results are reported in the normal delta (δ 18O) notation relative to Vienna Standard Mean Ocean Water in parts per thousand (‰; Coplen Reference Coplen2011). To test the accuracy of the measurements, replicate analyses of Aldrich Ag3PO4 (No. 33,738-2; accepted δ 18Op = +10.8 ± 0.3‰; White et al. Reference White, Spence, Longstaffe, Stuart-Williams and Law2002) were performed during the present study. These analyses returned average δ 18Op = +10.71 ± 0.31‰ (n = 22), which compares well with the accepted value. The average difference between duplicate analyses of samples (n = 7) was 0.29‰ (i.e., ± 0.15‰). Collectively, these results, and those for CI summarized earlier, indicate that the oxygen isotope data reported here are both accurate and precise, and are representative of the original oxygen isotope compositions of the bioapatite phosphate.
Results: The E19 samples
Moreiras Reynaga (Reference Moreiras Reynaga2019; Moreiras Reynaga et al. Reference Moreiras Reynaga, Millaire, Balderas, Román Berrelleza, Luján and Longstaffe2021) has defined five broad zones for the oxygen isotope compositions bioapatite phosphate (δ 18Op) in Mesoamerica. Only Zones 1–3 need concern us here. Zone 1, with δ 18Op typically in the +12.1–13.9‰ range, includes the Pacific Coast, West Mexico (with Michoacan), and the Valley of Oaxaca. Zone 2, characterized by δ 18Op of +14.0–16.2‰, covers the central Mexico highlands, including the Basin of Mexico, as well as Morelos, Puebla, Hidalgo, and other areas.
Teotihuacan itself, although in Zone 2, has a slightly more limited range of +14.0–16.0‰ (White et al. Reference White, Spence, Longstaffe and Law2004a). An additional factor to consider in the case of Teotihuacan, however, is the likelihood of some spatial variation within the +14.0–16.0‰ δ 18Op range typical of the city. This could be caused by a variety of factors, such as the use of distinct water sources or a difference in altitude. To test this idea, we compared the δ 18Op from site TL6 in Tlailotlacan (White Reference White, Spence, Longstaffe and Law2004a) to that from two suites of skeletal material from the Tlajinga 33 site in the lower south part of Teotihuacan (Buckley et al. Reference Buckley, Storey, Longstaffe, Carballo, Hirth and Renson2021; White et al. Reference White, Storey, Longstaffe and Spence2004b). Only enamel and bone ratios within the typical range of Teotihuacan were included in the analysis. The results show some distinctions, the TL6 δ 18Op trending higher (average +15.3 ± 0.42‰; range +14.1–16.0‰; n = 37) than those from Tlajinga 33 (average +14.8 ± 0.42‰; range +14.0–15.5‰; n = 29), though with a considerable overlap (Figure 9). The difference is not statistically significant.
Zone 3, with δ 18Op of +15.6–17.7‰, includes the southern highlands, northern Guatemala, and the eastern parts of Puebla and Hidalgo. There is some limited overlap in δ 18Op between zones 2 and 3. Also, these ranges are very broadly defined configurations. Each zone encompasses a significant variability in δ 18Op with some areas having δ 18Op above or below the typical range for that zone (White et al. Reference White, Storey, Longstaffe and Spence2004b).
Three areas are of particular interest for the identification of the external relationships of the E19 burials. One, of course, is Teotihuacan itself, in Zone 2. The other two regions of interest are the Valley of Oaxaca and the Lakes Region of northern and central Michoacan, both in Zone 1. This raises the problem of distinguishing between two such isotopically similar regions. The Valley of Oaxaca, however, may be of less relevance here. Although a number of architectural features and ceramics of Zapotec affiliation were found in E19 (Begun Reference Begun2013), they were probably derived from Tlailotlacan, the nearby Zapotec Barrio, rather than being directly traceable to the Valley of Oaxaca.
It is worth noting that after the initial settling of Tlailotlacan there was apparently very little biological exchange between Tlailotlacan and the Valley of Oaxaca. Only two of a series of 56 δ 18Op values from Tlailotlacan fall in the +12.0–14.0‰ range suggested for the Valley of Oaxaca (White et al. Reference White, Spence, Longstaffe and Law2004a). Of two separate strontium isotope studies, with a total of 45 samples tested from Tlailotlacan, none fall in the 0.7074–0.7076 range of the Valley of Oaxaca (Nado Reference Nado2017; Price et al. Reference Price, Manzanilla and Middleton2000).
Table 1 presents the available data for the E19 samples. Adult ages are, unfortunately, often recorded only as “adult” since there has been no comprehensive analysis of the E19 skeletal material. The enamel samples include a wide variety of teeth, and so of ages. We only analyzed teeth with crowns that had fully formed, at or past the “crown complete” stage. This is the stage recorded in Tables 1 and 2 for each tooth, based on data from the median columns of Tables 2–8 of AlQahtani et al. (Reference AlQahtani, Hector and Liversidge2010). Later comparative analyses by AlQahtani et al. (Reference AlQahtani, Hector and Liversidge2014) show that their system provides more accurate ages for tooth formation than the Schour and Massler, and Ubelaker, charts. Those “crown complete” ages, then, indicate the age reached by that particular individual while still living in the region characterized by the tooth's δ 18Op.
Individual 1 of Burial 25, the Zapotec-style tomb, has a bone δ 18Op of +12.2‰. On the one hand this value might suggest that he came to E19 from the Valley of Oaxaca shortly before his death. On the other hand, his enamel value (+14.2‰) suggests that he passed his early childhood in Teotihuacan. This isotopic pattern is similar to many others in the E19 series, so the region represented by the bone value of Individual 1 may be the same one as in the other samples, and not the Valley of Oaxaca. Both the enamel and bone δ 18Op of Individual 2, the other tomb occupant, are compatible with Teotihuacan residence. His enamel δ 18Op, however, is in the overlap between Zones 2 and 3 values and is 1.8‰ higher than his bone δ 18Op of +14.3‰, so it is possible that he moved within Zone 2 after his childhood.
Burial 30 is in a feature that has parallels in the Lakes Region of Michoacan. Again, there is a mix of Zone 1 and Zone 2 values for δ 18Op. Individual 1 presents both enamel (+13.6‰) and bone (+12.1‰) δ 18Op that indicate long-term residence in a Zone 1 area. Individual 3 seems to have moved from Teotihuacan to a Zone 1 location. The δ 18Op of Individual 2, a child of eight to nine years at death, suggest residence in Teotihuacan throughout that brief lifespan.
Only a bone δ 18Op (+13.0‰) is available for Burial 31. It suggests residence elsewhere before death, in a Zone 1 location, like the pattern of many other E19 individuals.
Because Burial 27 was a collective secondary burial we were able to obtain enamel and bone samples from the same individual in only two cases. The adult male represented by Cranium 7, with enamel δ 18Op of +13.5‰ and +14.1‰ for successive teeth and then of +12.6‰ for the temporal bone, seems to have passed most or all his life in a Zone 1 environment, rather than Teotihuacan. The C38 Cranium child, only 10 years old at death, has an enamel δ 18Op of +14.0‰, which could indicate residence in Teotihuacan or somewhere in Zone 1. The later frontal bone δ 18Op of +12.7‰ is more firmly in the Zone 1 range. It is, then, quite possible that the child was born and perhaps even died in that environment. There are only enamel δ 18Op values for the Cranium 1 child, but they show a clear picture of movement from Teotihuacan to a Zone 1 location sometime before the age of three, then burial in Teotihuacan after death at eight to nine years of age.
Values of bone δ 18Op for Burial 27, presumably reflecting residence within the last decade or so of life, all indicate a Zone 1 environment. Their range, +12.6–13.7‰, shows some variability, perhaps because of varying degrees of equilibration to the Teotihuacan environment. In contrast, their enamel δ 18Op are much more heterogeneous (+12.0–15.7‰), apparently showing childhood residence in a wider range of environments, including both Zone 1 and 2 locations. It seems, then, that the Burial 27 people originated in a variety of places and came together, some as children and some perhaps in marriage, to form a collective of some sort in a Zone 1 location. After some years there, at least long enough to equilibrate to the local oxygen isotope composition, they moved, or were brought, to Teotihuacan.
Burial 15, the converted well, offers a clearer understanding of the people's movements, in part because the discrete burials could provide enamel and bone samples for each individual and in part because the oxygen isotope compositions were quite homogeneous for both enamel and bone. With the possible exception of the Level 22 male (no bone isotopic data), all individuals passed some years in a Zone 1 environment (bone δ 18Op = +11.7–13.1‰). With two exceptions, their enamel δ 18Op fit tightly (+15.4–15.8‰) into the Teotihuacan range. In fact, these results conform well to the more northerly part of that locality, as can be observed for the δ 18Op of nearby site TL6 (Figure 9). One exception is the Level 22 male, with an enamel δ 18Op of +13.9‰ on a tooth formed in early childhood. The other exception is the Level 29 male whose +17.6‰ enamel δ 18Op suggests childhood in a Zone 3 location. The Teotihuacan enamel δ 18Op of the two young children in the sample (Levels 10 and 13) are from their deciduous lateral incisors which develop largely in utero and so actually reflect their mothers’ residences. Their movement to the Zone 1 location may have occurred just before or after birth.
Results: The Michoacan evidence
The archaeological data
The range of δ 18Op characteristic of Teotihuacan is +14.0–16.0‰, while a set of samples from Monte Albán suggests a +12.0–14.0‰ range for the Valley of Oaxaca (Stuart-Williams et al. Reference Stuart-Williams, Schwarcz, White and Spence1996; White et al. Reference White, Spence, Stuart-Williams and Schwarcz1998). To assess the possibility of Michoacan relationships we obtained samples from a number of sites in the north central part of Michoacan (the “Lakes Region”), a trip of some 300 kilometers to the west from Teotihuacan, and an adjacent area of southern Guanajuato (Figure 10).
There is considerable evidence in Michoacan of exchange with Teotihuacan. In some places the relationship may have been stronger and more formal, perhaps close ties between elites. Some structures have talud-tablero facades. Some of these facades, like those in Tingambato, are Epiclassic (Punzo Díaz Reference Punzo Díaz2022; Rangel Campos Reference Rangel Campos2018) and may be the result of local incorporation of Teotihuacan elite refugees fleeing the city's collapse (Pollard Reference Pollard, Foster and Gorenstein2000:63; Spence Reference Spence, Foster and Gorenstein2000:257–258), or the return to their ancestral homeland of Michoacanos who had been living in Teotihuacan but could still claim some privilege in their original communities, which they had perhaps been visiting throughout the Classic period (Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola and Faugère2007:132, Reference Gómez Chávez, Gazzola, Lauriers and Murakami2021:94; Michelet and Pereira Reference Michelet and Pereira2009:83). The examples of talud-tablero in the Lake Cuitzeo Basin sites may be of the Classic period, suggesting a relationship with Teotihuacan that in some cases extended beyond just exchange (Filini Reference Filini2004, Reference Filini, Lauriers and Murakami2021; Filini and Cárdenas García Reference Filini, García and Faugère2007; Macías Goytia and Vackimes Serret Reference Macías Goytia and Serret1988; Manzanilla López Reference Manzanilla López1988; but see Michelet and Pereira [Reference Michelet and Pereira2009:79–80]). Thin Orange ware ceramics, blades of the Cerro de las Navajas green obsidian, and other indicators of exchange with Teotihuacan have been found in several Cuitzeo area sites (but see Filini [Reference Filini, Lauriers and Murakami2021:219]). Some of the E19 Michoacan bowls match those of Querendaro, a Cuitzeo site (Gómez Chávez and Gazzola Reference Gómez Chávez, Gazzola, Lauriers and Murakami2021:88, 93–94).
There is also evidence of exchange with Teotihuacan further west, in the Zacapu area (Figure 10). Thin Orange ware is present in sites there, although Evelyn Rattray says that the sherds that she examined from the Loma Alta site are an older variety of the ware, one present in the Puebla source area but not in Teotihuacan (Rattray in Carot Reference Carot2001:33–36, Figures 31–36). Green obsidian blades that appear to be perfect examples of Teotihuacan knapping, however, make up 92 percent of the blades from Zacapu elite burial contexts (Carot Reference Carot2001:Figures 41–45; Darras Reference Darras, Arnauld, Carot and Fauvet-Berthelot1993a:169; Reference Darras, Arnauld, Carot and Fauvet-Berthelot1993b:174). There are even two green obsidian needles like those made in the obsidian workshops of Teotihuacan (Carot Reference Carot2001:Figure 46; Spence Reference Spence1996:Table 2, Figure 2D).
Prismatic blades of the green Cerro de las Navajas obsidian and Thin Orange ceramics have also been found in the Urichu and Erongaricuaro sites on the southwestern side of Lake Patzcuaro. A Thin Orange sherd, analyzed by INAA, matched the composition of samples found in Teotihuacan (Pollard Reference Pollard2008:220). The blades occur in Loma Alta 2- and 3- and Jaracuaro-phase contexts. Pollard (Reference Pollard, Williams and Weigand1996; Pollard and Cahue Reference Pollard and Cahue1999) suggests that local elites acquired them and other exotics to bolster their status. Begun (Reference Begun2008:314–316) notes that the Burial 27 figurines match those of the Patzcuaro Basin rather than the Loma Alta site (Zacapu Basin) version of that style. Also, some of the Michoacan-style ceramics of E19 analyzed by INAA match clay deposits in the Lake Patzcuaro Basin (Begun Reference Begun2013:140; Neff Reference Neff and Begun2011).
The available archaeological evidence alone does not allow us to say whether the people of E19 had their principal relations and perhaps ancestral ties with the Cuitzeo Basin, the Zacapu area, the Patzcuaro area, or even all of these localities. It does seem likely that, whatever their foreign interactions, they were not conducted as emissaries of the Teotihuacan state. E19 is a mid-level apartment compound near the western edge of the city, with no apparent role in the state apparatus (Begun Reference Begun2013:167, 172). Rather, it is probably an example of those extensive, often kin-based groups that were active in exchange networks but operated outside the state's institutions (Gómez Chávez and Spence Reference Gómez Chávez, Spence, Nichols and Pool2012:289–290). Manzanilla (Reference Manzanilla and Manzanilla2017:7, 38) has proposed a different model for Teopancazco, suggesting that caravans loaded with trade items travelled back and forth between Teopancazco and Veracruz. The E19 situation differs from this caravan model in some important respects. Virtually all of the E19 residents, including children, were involved in the movement, and sojourns in Michoacan were lengthy enough to allow the equilibration of their δ 18Op to the local environment. Probably the movements and resettlements of the E19 people were responses to some as yet unidentified social or political factors, the material exchanges developing as a by-product of the relationships that were established rather than as causes of the resettlements.
Comparative oxygen isotope data
In order to identify the source area for the Michoacanos thought to reside in E19, we obtained bone and enamel samples from a number of sites in the Lakes Region of northern Michoacan (Figure 10). There are three major lakes in the region: Cuitzeo (1,840 m above sea level [asl]), |Zacapu (1,980 m asl) and Patzcuaro (2,033–2,035 meters asl in the Classic period; Pollard Reference Pollard2008:220). Lake Zacapu is 30 km west of Lake Cuitzeo and Lake Patzcuaro is 40 km southwest of Lake Cuitzeo but only 20 km south of Lake Zacapu. Unfortunately, we have no samples from the Cuitzeo area. An exchange relationship with Teotihuacan, however, does not necessarily mean that the Cuitzeo Basin was the original homeland of the E19 residents.
Samples from excavations by the Centro de Estudios Mexicanos y Centroamericanos (CEMCA) in and north of the Zacapu area are Late Preclassic (ca. 200 b.c.) to the Middle Postclassic period (a.d. 1250–1400). Dental enamel and bone samples (Table 2) were obtained for seven individuals from sites in the Zacapu Basin (Guadalupe, Milpillas, and El Palacio; Pereira Reference Pereira1999; Puaux Reference Puaux1989), and from two individuals from the Penjamillo area some 30 kilometers to the north (San Antonio Carupo [Faugère-Kalfon Reference Faugère-Kalfon1996] and Los Portales [Pereira Reference Pereira and Faugère2006]). All these samples were obtained from the Michoacan Project excavations. Samples from two Epiclassic individuals come from Los Nogales, a Bajío settlement of southern Guanajuato excavated by the Barajas Project (Pereira Reference Pereira, Pomédio, Pereira and Fernández-Villanueva2013).
A second series of samples, all from bone, was obtained from sites in the Patzcuaro Basin (Table 3). The Urichu, Tzintzuntzan, and Tocuaro sites are clustered around the lake. All samples are Late Postclassic but for one Classic-period sample from Urichu. Although the climate in the region was somewhat wetter in the Late Postclassic period, there is no evidence that this had a significant effect on oxygen isotope compositions. The range in δ 18Op of the three Late Postclassic Urichu samples (+12.1–13.1‰) encompasses the one Classic-period value (+12.9‰) from the site.
Comments on the Michoacan series
The CEMCA series has a range of enamel δ 18Op of +14.5–16.0‰ (Table 2), excluding three, considerably higher values, most likely from outsiders who came to the area during or after their childhood: San Antonio Carupo Burial 2, a child with a deciduous second molar value of +16.5‰; El Palacio Burial 1, an adult woman with a third molar value of +17.0‰, whose cranial modification and body treatment are atypical for the area (Pereira and Barrientos Reference Pereira, Barrientos and Forest2020); and Los Portales Burial 2, another adult woman with a third molar value of +17.6‰. The fact that the two women were still in their childhood homeland when their third molar crowns had fully formed, around the age of 13.5 years, raises the possibility that they may have moved to northern Michoacan at the time of their marriage. The child, 10–12 years old at the time of death, may have moved as a child from the same foreign area at the time of development of the second molar crown, which usually occurs at about six to eight years (AlQahtani et al. Reference AlQahtani, Hector and Liversidge2010:Tables 5–6). At that time the child was either still living in the homeland or had only recently moved to San Antonio Carupo. By the time of death, some four years later, the child's bone δ 18Op (+14.0‰) had equilibrated to the new environment.
These three individuals may have come from the same or different regions. Our understanding of the δ 18Op of people across Mesoamerica is limited, but values of +16.5–17.6‰ are certainly not characteristic of either the Lakes Region of Michoacan or the Basin of Mexico and Teotihuacan. They are typical of Moreiras Reynaga's Zone 3, which includes the southern highlands of Mexico and highland Guatemala (Moreiras Reynaga Reference Moreiras Reynaga2019:98; Moreiras Reynaga et al. Reference Moreiras Reynaga, Millaire, Balderas, Román Berrelleza, Luján and Longstaffe2021; see also White et al. Reference White, Spence, Longstaffe and Law2000). Zone 3 also includes some regions to the east of the Basin of Mexico, like the eastern parts of the states of Puebla and Hidalgo (Moreiras Reynaga et al. Reference Moreiras Reynaga, Millaire, Balderas, Román Berrelleza, Luján and Longstaffe2021: Figure 4). Nevertheless, it must be remembered that each of these broadly defined zones may encompass considerable variability, so high δ 18Op values may occur in untested areas of Zone 2.
The range of bone δ 18Op in the CEMCA series is +13.5–15.0‰, slightly lower than the enamel range (excluding the three individuals described above). This, like the enamel range, encompasses some variability but that may be due to movements within the Lakes Region, use of different water sources or, in a few cases, incomplete equilibration by immigrants to the local environment. The CEMCA combined bone and enamel δ 18Op ranges that represent local values (+13.5–16.0‰) are very similar to the range characteristic of Teotihuacan (+14.0–16.0‰). This makes it difficult to distinguish individuals from the two regions using only oxygen isotope data.
The Patzcuaro series of bone δ 18Op values (Table 3) ranges from +12.1 to +13.7‰, excluding one anomalous value of +15.2‰ from the young woman of Tocuaro. She may have been an immigrant, moving into the area from Zacapu, only 20 km to the north. The small overlap in bone δ 18Op (+13.5–13.7‰) between the Patzcuaro and CEMCA samples is within the error (+0.3‰) of the method. The difference in bone δ 18Op between the two areas is somewhat surprising, given their proximity. It may be due in part to the higher elevation of Lake Patzcuaro.
Discussion and conclusions
When we started this project we anticipated, or at least hoped, that the results would be straightforward: enamel δ 18Op indicating early residence in Michoacan and bone δ 18Op indicating later residence in Teotihuacan. We should have known it wouldn't be that easy. In fact, the data seem to suggest the opposite, yet the burials are in Teotihuacan. How to explain this unexpected pattern?
One consistent aspect is the occurrence of Zone 1 δ 18Op (+12.1–13.9‰) in the bone samples of the E19 individuals. Every bone δ 18Op of the two best represented burials (Burials 15 and 27), as well as the sole Burial 31 bone δ 18Op, one of the two Burial 25 bone δ 18Op, and two of the three Burial 30 bone δ 18Op fall in this range. The Valley of Oaxaca has a similar range of δ 18Op but, as discussed earlier, it is probably not a factor in this analysis. We have thus focused our attention on the Michoacan sector of Zone 1, and on the Lakes Region.
Teotihuacan materials, particularly Cerro de las Navajas green obsidian prismatic blades and Thin Orange ware ceramics, appear widely in the northern Michoacan Lakes Region. This informs us about where Teotihuacan goods were going, and it seems likely that the residents of E19 played a role in that distribution, but it does not necessarily identify their original homeland. That is a separate question, one best investigated with stable isotope analysis. To that end we acquired dental and bone samples from a variety of locations in the Lakes Region and some sites further to the north. While we do not have samples from the Cuitzeo Basin, as discussed earlier, the available Michoacan samples indicate a local origin for the people of E19 in the Patzcuaro Basin. Some of the E19 offering artifacts, like the figurines of Burial 27, also point to a Patzcuaro connection. The nature of that connection, however, may have changed over time.
The Michoacan-related mortuary features and artifacts appear in the earlier stages of E19, in the Tlamimilolpa period. In the Xolalpan period the architectural and ceramic evidence for a Michoacan relationship dwindles and disappears, suggesting that the residents of E19 had eventually embraced a Teotihuacan identity (Begun Reference Begun2013:148–149, 163–170; Gómez Chávez Reference Gómez Chávez and Gallut2002:607–608). If the Michoacan items in E19 burials represented Michoacan beliefs or practices, something that may be particularly likely in the case of the distinctive Michoacan female figurines in Burials 30 and 27 (Figures 5, 7, and 8), those associations had evidently been eroded by the Xolalpan period. The isotopic evidence, however, adds another dimension. To judge by Burial 15, some of the people of E19 passed years in Michoacan in the Xolalpan period, even after the architectural and ceramic evidence for a Michoacan presence at E19 had disappeared. Enamel δ 18Op indicate that most of the Burial 15 individuals had probably been born and raised in Teotihuacan, in the E19/Tlailotlacan part of the city.
The Burial 27 people appear to have passed their early years in a variety of areas, which may have included Teotihuacan, the Patzcuaro Basin, or perhaps even the Zacapu Basin. In any event almost every bone δ 18Op in the E19 series indicates movement to, and long-term residence in, the Patzcuaro Basin, starting in some cases in childhood (e.g., Cranium 1 of Burial 27) and in others as adolescents or adults. Although most of the adults have been tentatively identified as males, some females were present. People, then, were probably moving as families.
Their stay in the Patzcuaro area was long enough for their bones to remodel extensively, taking on the oxygen isotope compositions characteristic of that environment. Yet they were buried in Teotihuacan and virtually none of them shows any real shift in oxygen isotope compositions toward the Teotihuacan environment. This observation suggests their return to the city not long before death, although we do not really know how long that is. Rates of bone remodelling slow with age but are variable, depending to a considerable degree on the health and nutrition of the individual. It may take a decade or more for adult bones to fully remodel.
A small group like the E19 residents would not be likely to resist assimilation for long. Even the earlier burials have far more Teotihuacan than Michoacan items among their offerings (Figures 5 and 7). Still, the residents may have retained a residual Michoacan identity for some time, particularly if it offered some advantages. It would certainly have facilitated exchange and other relationships with people in the Lakes Region. In moving to the Lakes Region, invoking that identity would have eased their integration into local communities and locked in a socially protected role in Teotihuacan–Lakes Region relationships. Their return to Teotihuacan at a late point in their lives is a further indication that their core identity and the area that they now considered their homeland was Teotihuacan. Over time their Teotihuacan identity had become more fundamental and their Patzcuaro identity more instrumental. They would have shared, perhaps from the beginning, the benefits of Teotihuacan citizenship. They would also have been required to attend to its obligations, like taxation, corvée labor, and military service.
The erosion of a Michoacan identity might have been slowed if there had been a wider community of expatriate Michoacanos in Teotihuacan. Gómez Chávez and Gazzola (Reference Gómez Chávez, Gazzola and Faugère2007:114–115) note the presence of Michoacan ceramics at a number of other Teotihuacan sites, with a particularly interesting occurrence in site 4:N2E2. The Tlajinga barrio, however, offers the best evidence of another West Mexico connection. Although it is located at the south end of the city, some 2.7 kilometers from E19, it may also have had some ties with E19. The intensive core-blade production in site 17:S3E1 (Hirth et al. Reference Hirth, Carballo, Dennison, Carr, Imfeld and Dyrdahl2019) may have supplied the green obsidian blades found in Michoacan, perhaps via E19. The use of cobblestone floors in Tlajinga sites (Carballo et al. Reference Carballo, Hirth, Sariñana, Buckley, Mejía Ramón and Kennett2019; Storey Reference Storey1992) also suggests a Tlajinga-E19 link, although they have been found elsewhere in Teotihuacan. The shaft tomb of Tlajinga 33 (Widmer Reference Widmer, de Tapia and Rattray1987:354) is much like the one for Burial 5 in E19 (Gómez Chávez Reference Gómez Chávez and Gallut2002:578, Figure 4).
The West Mexico relationships of Tlajinga 33, however, may not have been with sites in the Lakes Region of Michoacan. The foreign δ 18Op values of Tlajinga 33 include only one composition (Burial 6, +11.3 ‰ on enamel) that is compatible with Patzcuaro Basin values, but seven for enamel and two for bone lie in the +16.3–18.1‰ range (Buckley et al. Reference Buckley, Storey, Longstaffe, Carballo, Hirth and Renson2021:Table 1; White et al. Reference White, Storey, Longstaffe and Spence2004b:Table 1). These higher δ 18Op values were taken to represent the West Mexico area with which the Tlajinga people interacted for two reasons. One was the occurrence of three of these high δ 18Op in the teeth of two of the individuals buried in the Tlajinga 33 shaft tomb. The other was the enamel δ 18Op values of +16.2 and +16.9‰ for two teeth from Burial 10 in the substructure of Yácata 3 of the Main Platform in Tzintzuntzan (White et al. Reference White, Storey, Longstaffe and Spence2004b:184). Given that most of the δ 18Op values from Tzintzuntzan and the other Lakes Region sites are lower, Burial 10 was probably not a good choice to represent the region.
The E19 mean and range of δ 18Op for bone, is considerably lower than the ranges for bone determined for two other Teotihuacan sites, Tlajinga 33 (Buckley et al. Reference Buckley, Storey, Longstaffe, Carballo, Hirth and Renson2021; White et al. Reference White, Storey, Longstaffe and Spence2004b) and TL6 of Tlailotlacan (Table 4, Figure 11; White et al. Reference White, Spence, Longstaffe and Law2004a). All three sites had important foreign relationships, but apparently with different regions. To date, E19 is the only site in Teotihuacan with a large suite of low δ 18Op values. Other sites in its vicinity like 22:N1W6 (Cid Beziez and Torres Saunders Reference Cid Beziez, Sanders, Manzanilla and Serrano1999; Torres Saunders and Cid Beziez Reference Torres Sanders and Cid Beziez2018) have not produced any evidence of West Mexico ties, but it might be worthwhile to conduct oxygen isotope analyses of some of their skeletons. Burial 15, after all, is closer to 22:N1W6 than to E19 and had no definite Michoacan materials, but still showed a strong pattern of low δ 18Op.
Comparative oxygen isotope data.
This reconstruction of population movements and affiliations is tentative, and admittedly runs the risk of conflating isotopes with identities. It is a hypothesis that will require further investigation before it can be accepted (or rejected) with confidence. That investigation should include several threads. Of particular importance is a comprehensive osteological analysis of all E19 burials: sex and precise age assessments, trauma, perimortem treatment (dismemberment, defleshing, decapitation), and morphology (cranial modification and rare anomalies like persisting metopic suture or cranial-caudal shifts in the vertebrae). Also, more isotopic analysis of the E19 burials, including those not considered in this study (e.g. Burials 5, 28, and 43), is necessary. These should include the earliest burials (Early Tlamimilolpa phase) to determine whether the original occupants of E19 were Patzcuaro Basin immigrants or Teotihuacanos who later developed a relationship with Patzcuaro Basin people. It would be helpful to have more than one enamel sample from each individual, to better track movement during childhood and adolescence. Strontium isotope as well as oxygen isotope measurements should be used, as the two methods complement each other (e.g., Buckley et al. Reference Buckley, Storey, Longstaffe, Carballo, Hirth and Renson2021; White et al. Reference White, Price and Longstaffe2007). Strontium isotope ratios may help to resolve the ambiguities in the oxygen isotope data between the Valley of Oaxaca and the Patzcuaro Basin, and between Teotihuacan and the Zacapu Basin. More samples from Michoacan, including the Cuitzeo Basin, will be needed. The isotopic data presented here confirm the Teotihuacan-Michoacan connection, pointing particularly to the Patzcuaro Basin as the Michoacan terminus and demonstrating that the relationship involved something deeper than just trade, but it will take more analyses to clarify the nature of that relationship.
Open access
