The Jancao Site

The Jancao site (76°13′22″ E, 09°63′55″ S, 1,925 m asl), which is the present-day Amarilis district in Peru's Huánuco province, is located on the alluvial land on the southern bank of the Huallaga River. The surrounding environment belongs to the fertile yunga zone (Pulgar Vidal Reference Pulgar Vidal1987), and the neighborhood includes several key archaeological sites of the Formative period, such as Kotosh, Wairajirca, and Shillacoto (Figure 1; Inokuchi et al. Reference Inokuchi, Onuki, Tsurumi, Matsumoto and Ruiz2002; Matsumoto Reference Matsumoto2020; Onuki Reference Onuki, Millones and Onuki1993).

Figure 1.

Map of the Central Andes (left) and the Huánuco region (right) with site locations.

The earliest archaeological investigations in the Huánuco region occurred in the 1960s and focused primarily on the study of the Formative period (Izumi and Sono Reference Izumi and Sono1963; Izumi and Terada Reference Izumi and Terada1972; Izumi et al. Reference Izumi, Cuculiza and Kanō1972; Kano Reference Kano1979; see also Matsumoto Reference Matsumoto2020). These studies identified the Wairajirca phase, the local phase of the Early Formative period in this region. Onuki (Reference Onuki, Izumi and Terada1972) analyzed the ceramic assemblage at the Kotosh site and classified all unearthed sherds, mainly by their decoration technique (such as shallow incised, zoned hachure, red plain, etc.). These studies, however, did not clearly detail a chronological sequence for Wairajirca pottery.

The Jancao site, which was found by a 2001 archaeological survey of settlement patterns (Inokuchi et al. Reference Inokuchi, Onuki, Tsurumi, Matsumoto and Ruiz2002; Matsumoto Reference Matsumoto2020), is one of the largest artificial mounds dated to the Formative period in the Huánuco region. The site was badly damaged by modern activities, including road construction. As such, our 2017 excavation was conducted in limited areas (Supplemental Figure 1). We found accumulation of cultural deposit from the Initial Formative period to the Early Intermediate period by observing the site's profile and the surface collection of ceramic sherds. However, there was very little left of the accumulation's upper parts to excavate. Thus, the great majority of the cultural deposit of the excavated area appeared to belong to the Early Formative period, the Wairajirca phase.

This mound site is basically composed of artificial accumulation. In other words, layers were formed by human activities mainly associated with centuries of building construction during serial (continuous or continual) occupation. In the Wairajirca phase deposit, each layer accumulated horizontally and was several dozen centimeters thick. This accumulation's formation would have been a result of the following process: (1) the collapsing or destruction of buildings made in a period and (2) a covering with earth and rocks to make foundations for new construction. This process would be repeated various times during the Wairajirca phase, forming consequent serial accumulations for several centuries, although the limited excavation did not find direct evidence of construction. Under the Wairajirca phase layers, an earth layer emerged that did not include any ceramic sherds, making it highly possible that it belonged to the preceramic period.

To construct a highly accurate Wairajirca phase chronology, we selected two excavation units, E1N4 and E1S2–3, in which each layer remained clear without massive disturbances by later deposits (Figure 2; also see Supplemental Figure 2). We also used two approaches to clarify the ceramic sequence in a fine time scale: a typological pottery analysis and a Bayesian radiocarbon dating analysis.

Figure 2.

Stratigraphy of selected excavation units, E1N4 and E1S2–3, with plots of the carbon sample locations.

Typological Pottery Analysis

We relied on a qualitative analysis of pottery sherds, based on morphological typology, to develop a ceramic sequence of the Jancao site. The new type classification is intended to create a finer relative chronology and to facilitate comparative analyses of pottery across various sites. From the collection of ceramic sherds unearthed in E1N4 and E1S2–3, we selected for analysis a total of 371 rim sherds and a few other fragments from which we could reconstruct vessel forms. Next, the following seven kinds of vessel forms were reconstructed: neckless jars, wide-mouthed jars, carinated bowls (with convex base), closed bowls (with rounded base), open semi-spherical bowls, boat-shaped bowls, and bottles with bridged handles. We then defined the types according to certain vessel attributes, focusing on specific profile and decoration features that were notably more “time-sensitive” than other ceramic traits. For example, certain features can be used as time marks: the rim shape of neckless jars; a thickened, beveled, tapered, and decorative element; punctate lines; arc shapes; and so on. We also defined the ceramic phases by comparing types according to their stratigraphic units. Consequently, we described the site's ceramic sequence as the serial change of the type set following the stratigraphic order.

Regarding the depositional context constraints, it is necessary to consider the possibility that the sample was mixed with sherds from older layers. Thus, we only chose types that had appeared in the assemblage for the first time to represent each type for each layer. In drawing, we applied the wet-rubbed copy method (for details, see Matsumoto Reference Matsumoto2014).

Radiocarbon Dating and Bayesian Analysis

We used radiocarbon dating and a Bayesian analysis to develop an absolute time scale. A continuous and systematic radiocarbon analysis of Early Formative contexts allows researchers to assess a site's occupation sequence and reveals an accurate temporal distribution based on stratigraphic units. The samples were collected at the cross section of E1N4 and E1S2–3. There were various burnt accumulation lenses or charcoal inclusion layers within the Early Formative contexts. We selected in situ charcoal fragments from a bottom layer to the top fill of each horizontal accumulation unit and applied a Bayesian analysis by considering the stratigraphic contexts and number of samples/data points (Figure 2). The date of the unit bottom is essential for directly estimating the timing of occupations, and the fill's temporal information enables researchers to understand the duration and transition of archaeological finds. The sequential sampling was independently set at both excavation units to avoid any confusion in interpreting the stratigraphic contexts. We cross-referenced the samples with the parallel sequence, which enabled us to evaluate the radiocarbon results and helped us construct a robust and accurate age model for the pottery assemblages.

We conducted radiocarbon analyses of the collected samples at the Laboratory of Radiocarbon Dating, University Museum, University of Tokyo. Via microscopic observations, we included charred fragments that have well-preserved plant tissue (excluding unknown charred substances) in the sample. Almost all the samples appeared like young trees or small branches and had no fine width growth/tree rings, which are developed over several hundreds of years (Supplemental Figure 3). We applied an acid-base-acid pretreatment, commonly used to remove burial contaminants, to the samples and then converted to the measurement target substance for accelerator mass spectrometry (AMS). We calculated the conventional radiocarbon age with ¹⁴C measurements and obtained δ¹³C from the compact-AMS system (0.5MV 1.5SDH-1 Pelletron, National Electrostatics Corp.). Age calibrations, which were followed by Bayesian analyses, were performed with OxCal v4.3 (Bronk Ramsey Reference Bronk Ramsey2009a). These figures were calculated using the SHCal13 atmospheric curve (Hogg et al. Reference Hogg, Hua, Blackwell, Niu, Buck, Guilderson, Heaton, Palmer, Reimer, Reimer, Turney and Zimmerman2013). However, it might be necessary to consider the effect of the Northern Hemisphere air in relation to the dynamics of the Intertropical Convergence Zone or South American Summer Monsoon, given the site location in temperate latitudes. To compare the calendar dates, we also referred to the mixed atmospheric curve described by Marsh and others (Reference Marsh, Bruno, Fritz, Baker, Capriles and Hastorf2018).

We employed the Bayesian analysis to increase the accuracy of the individually calibrated dates, estimate the duration of the pottery assemblages, and assess the depositional process of the Wairajirca stratum. Bayesian constraints defined by stratigraphic contexts can refine interpretations of calibrated dates to a higher likelihood (Bronk Ramsey Reference Bronk Ramsey1995; Christen Reference Christen1994). We also used a Bayesian analysis to simulate the optimal event date, such as a transition between cultural activities. The likelihood date, which is expressed as a probability, can be extracted from convergence and variability in the radiocarbon results (Bronk Ramsey Reference Bronk Ramsey1998). The following discussion is based on the dates estimated from the boundary between pottery assemblages.

Furthermore, identifying any inconsistencies between the radiocarbon data and stratigraphic information enables an assessment of the occupation sequence. If the radiocarbon data deviate from a certain set of archaeological contexts, it is possible that extant archaeological assumptions do not match the actual analysis samples’ provenances. In other words, the degree of model agreement suggests the disturbance of stratigraphic superposition, such as a reworking of the deposits. The agreement degree is quantified by an agreement index and represented by comparisons with expectations of the calibrated and modeled dates (Bronk Ramsey Reference Bronk Ramsey1995). The Bayesian analysis for outlier estimates is used to derive the outlier probability with a priori outlier probabilities, set at 5% (Bronk Ramsey Reference Bronk Ramsey2009b). Using the two indexes, we reviewed the archaeological stratification from the standpoint of the depositional process of charcoal.

Finally, the possibility of systematic age offsets due to the old wood effect was examined by a charcoal model—one of the Bayesian outliers’ analyses (Bronk Ramsey Reference Bronk Ramsey2009b). The charcoal model gives the charred dates an arbitrary old wood effect and estimates the likelihood dates eliminated from the age offset. We assumed that the old wood effect between 0 and 100 years exists in the measured samples and compared our results with that of other age models.

Ceramic Sequence

We separated the Wairajirca ceramic sequence at the Jancao site into five phases (I–V). As discussed in more detail later, this ceramic classification strongly corresponded with the absolute dating results. Figures 3 and 4 display a set of ceramic types from each phase (see Supplemental Figures 4–9 for more detailed data).

Figure 3.

Ceramic sequence of neckless jars and wide-mouthed jars (including small-sized ones that possibly belong to the bowl category) at the Jancao site. Each fragment in a rank represents a type that is specific to one phase.

Figure 4.

Ceramic sequence of bowls and bottles at the Jancao site.

The features of pottery from the earliest phase of the Jancao site are considerably different from those of the later phases. Neckless jars are the only vessel forms that were reconstructed in this first phase, and they do not have any decorations. Their surface treatment is rather coarse, and they seem to have been fired under poorly controlled conditions. Those neckless jars are divided into two types based on rim form: one has thickened rims (like a comma shape), and the other has rims that are rather thin and flat or slightly beveled.

Pottery from Phase II was more elaborate than that of Phase I. Phase II pottery featured plenty of decorated sherds. The assemblage consisted of neckless jars, closed bowls and convex base bowls, and bottles with bridged handles. Unlike in Phase I, there were no neckless jar sherds with thin rims. The different vessel forms shared essentially the same decoration style. This style can be divided into three types: (1) a row of small punctuation below the lip, (2) a row of short incisions with a line around the rim, and (3) a combination of punctuation and incisions (which sometimes included scale-like motifs/appliqués and was often more elaborate). In addition, some closed bowls had an arc-shaped decorative motif that likely held some connection with the next phase's neckless jars. One fragment had dense, short incisions with a rope-like appearance on the lip. As for the bottles with bridged handles, we only uncovered spouts and handles with highly polished black exteriors.

There was a major change between Phase II and Phase III pottery at the Jancao site. This change is most clearly indicated by the introduction of new vessel forms and decoration techniques: the wide-mouthed jar and red slip, respectively. The neckless jar decoration featured an arc-shaped motif by shallow incision. It appears that this decorative style can be divided into two subcategories. One type is relatively simple and is associated with short incisions or punctuations; the other type features punctuations in a square and has a more elaborate impression. As in Phase II, in Phase III the thickened rim predominated among neckless jars. The wide-mouthed jars include a type that had an extremely short neck and resembled the neckless jar. This type was elaborately decorated with specific geometric motifs, including the small circle and dots. In this phase, the red slip technique was applied to some wide-mouthed jars.

The pottery assemblage of Phase IV featured two different decoration styles. One decoration style is connected to previous phases and is mainly associated with neckless jars. The other style, however, seems to have suddenly appeared in this phase and is closely related to carinated bowls. The primary decoration of neckless jars still had arc-like motifs but was rather simple, featuring shallow and thin incisions; for certain neckless jars, a burnished technique was used. In contrast to the previous phases, the red slip was often applied to the neckless jars and the tapered rim predominated. Some Phase IV neckless jars had ridged rims, with shapes and decorations that seemed to have followed the previous phase's wide-mouthed jars. Bowls featured geometric motifs with hatching-like incisions, and a postfired pigment was applied to the carinated bowls (whose surface was blackish and well polished). Some bowls contained circle-and-dot motifs and pigmented matte depressed zones. This phase's sample also included one fragment from a possible bottle body with hatching and pigmented decoration on a black polished surface. This phase's stylistic dichotomy basically matches Toshihara's (Reference Toshihara2002) description, although she described it as a feature of the entire assemblage of Wairajirca pottery.

The final phase's assemblage consists of a wide variety of vessel forms: neckless jars, carinated bowls, wide-mouthed jars, open semi-spherical bowls, and boat-shaped bowls. In this phase, most neckless jars are without decorations, both slipped and nonslipped, with a thickened rim. The carinated bowls still have hatching and pigmented decorations, although the incisions on these are denser and longer. Hatchings were also applied to the middle-sized bowls in forms that resemble the neckless and wide-mouthed jars. This phase contains two new vessel types: open semi-spherical bowls and boat-shaped bowls. The former is plain, and the latter can be divided into two types: one is plain and often red slipped, and the other is polished black and associated with broad line incisions, postfired pigment, and zoned hatching.

Absolute Chronology

Table 1 presents the radiocarbon results for the 17 charcoal samples and the Bayesian estimates. Figure 5 summarizes the modeled dates on SHCal13 with boundary distributions. The estimates of the mixed atmospheric curve and the charcoal model are shown in Supplemental Table 1. For the Bayesian models, we used the stratigraphic order defined by the actual sampling positions as a vertical relationship and assumed the five groups identified from the pottery assemblages as a horizontal relationship to combine the parallel sequences of the grid E1N4 and E1S2–3 (Supplemental Figure 10).

Table 1.

Radiocarbon Determinations of Charcoals from the Jancao Site.

Figure 5.

The modeled dates for the Jancao sequence produced using OxCal 4.3 (Bronk Ramsey Reference Bronk Ramsey2009a). The radiocarbon ages are calibrated using the Southern Hemisphere atmospheric curve SHCal13 (Hogg et al. Reference Hogg, Hua, Blackwell, Niu, Buck, Guilderson, Heaton, Palmer, Reimer, Reimer, Turney and Zimmerman2013). The model is built based on the stratigraphic order defined by the actual sampling positions (see Supplemental Figure 10 and Supplemental Note 1 for the diagram of stratigraphic relations and OxCal CQL2 codes, respectively). Lighter shaded distributions are calibrated radiocarbon likelihoods, whereas darker outline distributions are posterior probabilities after the Bayesian modeling. The 68% and 95% probability ranges are given by the horizontal brackets beneath the probability densities.

The charcoal radiocarbon measurements of the Wairajirca phase fell within about 3500 BP–2900 BP (from the eighteenth century cal BC to the twelfth century cal BC). They seem to converge into five distributions around 3400 BP, 3300 BP, 3100 BP, 3000 BP, and 2900 BP, which synchronize with the stratigraphic subdivisions. This distribution pattern would strongly underpin the pottery classification results. The chi-square test results for the radiocarbon measurements grouped in Wairajirca V, Wairajirca IV, and Wairajirca II indicate that there are no significant differences for each age (Wairajirca V T′ = 3.62, χ² = 9.49 [p = 0.05], df = 4; Wairajirca IV T′ = 0.05, χ² = 3.84 [p = 0.05], df = 1; Wairajirca II T′ = 6.05, χ² = 7.82 [p = 0.05], df = 3). These outcomes may imply that these three phases reflect snapshots formed within a limited period. However, age differences around 100 years appeared in Wairajirca III (TKA-19533, 19562, 19554, and 19582), which indicates that there were at least two occupational events in the deposition.

The Bayesian model results suggested the following calendar dates: late eighteenth century to early seventeenth century cal BC (Wairajirca I), early sixteenth century to early fifteenth century cal BC (Wairajirca II), late fifteenth century to late fourteenth century cal BC (Wairajirca III), early thirteenth century to late thirteenth century cal BC (Wairajirca IV), and early twelfth century to late twelfth century cal BC (Wairajirca V). These estimates exhibited no large differences when using either the mixed atmospheric curve or assuming the old wood effect. Compared with the modeled dates on SHCal13, the mixed curve model and the charcoal model appeared 25 years older and 15 years younger, respectively, on average (Supplemental Table 1). We should keep in mind that age may vary for a maximum of 40 years according to the respective conditions, but this had little to no impact on our phase classification.

Each phase's start and end dates are represented by the median of the calculated boundaries as the most likely estimates. The phase durations, ranging from 80 to 170 years, indicate that transitions between phases of pottery proceeded quickly. The continuance in the age model implies that the Wairajirca depositions at the Jancao site were periodic and continuous.

The agreement index and outlier probability results indicate that the defined stratigraphic subdivision is consistent with the radiocarbon results. Because each data's agreement indexes were higher than 60% for a similar discrimination to the χ² test at 5% and the outlier probabilities remained small (Table 1), it is possible that there were no disturbances over the phases in the deposits. Thus, it can be assumed that the behavior of the archaeological inclusions remained the same along the deposition process and that the provenances of the analyzed pottery shards directly corresponded to the phrase's terminus post quem.

Indication of Relationships with Other Regions’ Pottery Traditions

Certain vessel types, decorative styles, and techniques appearing in each phase are closely related to other regions’ pottery traditions. The neckless jars with thin rims that were unique to the first phase closely resemble neckless jars found in the early stages of various north-central and south-central highland sites, including the Yesopampa phase of the La Pampa site (Terada Reference Terada1979:PL.105–107), the Toril phase of the Huaricoto site (Burger Reference Burger1985:Figures 3–6), the second phase of the La Galgada site (Grieder Reference Grieder, Grieder, Mendoza, Smith and Malina1988:Figures 156q–u), the Initial period of the San Blas de Junín site (Morales Reference Morales1998:Figure 17), and the Muyu Moqo A phase of the Waywaka site (Grossman Reference Grossman1983:Figures 7–13). This similarity, however, did not continue in the following phases, in which decorated neckless jars with thickened rims flourished. The San Blas de Junín site, located in the Junín plateau only 100 km south of the Huánuco region, is one possible post–phase I connection between the Huánuco region and the highlands. At this site, the plain neckless jars changed between the first and second phases in a similar way to the changes observed in the Jancao site (Morales Reference Morales1977, Reference Morales1998). However, the decorative style that was mainly associated with the neckless jars from phases II, III, and IV is not associated with any other region. Thus, it appears that the emergence and successive change of this style are best explained by local development.

In contrast, the decorative style with hatching and postfired pigment that emerged in phase IV is related to a neighboring tropical forest's pottery traditions (Izumi and Terada Reference Izumi and Terada1972; Izumi et al. Reference Izumi, Cuculiza and Kanō1972; Kano Reference Kano1979). Lathrap (Reference Lathrap and Benson1971) indicated that Tutishcainyo pottery traditions, located in the central Ucayali basin around the modern town of Pucallpa and dated to the Early Formative period, had a specific influence on Wairajirca pottery. Similar decoration techniques featuring geometric and animal face motifs have been observed at the Cueva de las Lechuzas site, located approximately 100 km east of the Huánuco region (Lathrap and Roys Reference Lathrap and Roys1963:Figures 1–4). When exploring the resemblance of the Tutishcainyo and Cueva de las Lechuzas examples to Wairajirca pottery, however, it is important to consider that vessels found with such decorations at those sites have marked differences from the Wairajirca assemblage. For instance, Tutishcainyo pottery includes a relatively shallow, carinated bowl (e.g., Lathrap Reference Lathrap and Benson1971:Figure 10), and the Cueva de las Lechuzas pottery includes a wide-mouthed jar with a long neck and sharp bottom. Phase IV pottery from the Jancao site features specific decoration motifs and techniques that might have been selectively introduced into the local assemblage, instead of incorporating complete sets of vessel types and decorations.

The bottle with bridged handle is another vessel type that is possibly related to the eastern lowlands. We did not find any specimen that contained both sides of the vessel top, so it is impossible to determine whether this type can be included in what DeBoer (Reference DeBoer, Raymond and Burger2003) called “Asymmetric Spouts of the Upper Amazon.” However, this vessel's spout shape, with its relatively short and thick features, is similar to examples uncovered in the Upper Amazonian region.

Interpretation of the Emergence and Development of the Early Pottery Assemblage in the Huánuco Region

The Wairajirca pottery changed stepwise for several hundred years after the first appearance of pottery in the region. The features of this change can be summarized in three points: (1) diversification of vessel forms, (2) coexistence and fusion of different stylistic traditions within an assemblage, and (3) various technological innovations. In the early stages of this development track, neckless jars and simple form bowls were a fundamental component of the Wairajirca assemblage, as was the case with many highland and coastal sites, although Wairajirca pottery also included bottles with bridged handles. However, after the early fifteenth century cal BC, the variety of vessel forms increased over time, and a unique assemblage composed of various vessels consequently formed around the early thirteenth century cal BC.

The diversification of forms in the later phases of Wairajirca pottery corresponds, at least to an extent, to a stylistic change. When the wide-mouthed jar was first introduced into the Wairajirca assemblage in Phase III, it originated a different style, unique to this type of jar, that appears to have been incorporated into Phase IV's local style. This phase's neckless jar inherited characteristics of the previous phase's arc-shaped motif tradition, but it also presented some traits of Phase III's wide-mouthed jar, including small circle lines and dots under the ridged rim, the red slip technique, and so on. In contrast, the hatching style's geometric motifs that appeared in Phase IV did not mix with the local stylistic tradition. This style was limited to bowls, and the various types of decorated bowls that appeared in the last phase were all associated with this style. Consequently, such a step-by-step introduction of different stylistic traditions results in the unique features of Wairajirca pottery that contain two distinctive styles in one assemblage.

In addition, these developments were followed by technological advances. Some techniques, such as red slips, circle-and-dot stamps that require special instruments, and postfiring pigments with hatchings curved by sharp pointed tools, were adopted at the same time as new styles were introduced into the Wairajirca assemblage.

All these features of Wairajirca pottery development indicate that various sociopolitical, economic, and ideological factors were involved in the emergence and development of pottery in the Huánuco region. The increasing need over time for elaborated ceramic vessels for utilitarian/non-utilitarian purposes and an intensifying social exchange during the frontier situation likely caused rapid stylistic changes in pottery; in addition, various forms of social interaction likely promoted the “dependent invention” (Clark and Gosser Reference Clark, Gosser, Barnett and Hoopes1995) process of pottery technology.

The data for interpreting the first stage of this process—the first acceptance of pottery into previously preceramic lifestyles—are still limited, but it appears that pottery's use in the first phase was more restricted than in the later phases. This phase's ceramic assemblage only included the neckless jar, unlike in other phases, perhaps because serving various types of foods in ceramic vessels was not fully established at this time. In addition, this period's pottery did not appear to serve as a food-processing tool. Rather, people in this region possibly began to use pottery as a replacement for earlier perishable containers, such as gourds, in response to increasing needs for more durable vessels. In fact, some scholars claim that the neckless jar was originally created by mimicking precedent gourd containers; the Huaricoto site's researcher declared that pottery was experimentally invented in some Andean locations, including in this site (Burger Reference Burger1988). Although it is unclear whether this experimental phase existed in the Huánuco region, interactions with neighboring highland regions likely play an important role in this first step of pottery technology introduction, especially considering the early pottery similarities in the broad highland areas described earlier. Phase II contained other vessel forms (bowls and bottles) that represented the local stylistic tradition of the Wairajirca assemblage. Perhaps human practices related to pottery had gradually developed in various social domains as features of ceramic vessels, which were sufficiently plastic to represent various things and became durable enough for multiple purposes after firing, were further understood.

Fluid interactions with neighboring lowlands that had their own ceramic traditions before pottery emerged would have facilitated the development of pottery use in the Huánuco region. Bottles with bridged handles that appeared from Phase II were likely directly imported to this region from the lowlands and became a new component of the highlands’ neckless jar's dominant assemblage. As seen in wide-mouthed jars in Phase III, the new style's emergence, closely associated with the introduction of new technology, indicated a direct communication between local potters and foreign ones that resulted in a knowledge transfer—including that related to potters’ motor habits and the making of special tools for pottery production. This interaction with the lowlands area seems to have increased beginning with this phase; perhaps a number of people immigrated from areas where this stylistic tradition originally existed to the Huánuco region's local communities. In addition, although there is still little evidence for the utilization of food resources at this time, certain changes in local dietary habits may have prompted increased needs for new jar forms (cf. Onuki Reference Onuki, Millones and Tomoeda1982).

Such a fluid interaction among the highlands and the lowlands is closely associated with internal sociopolitical movements or social structural changes in the frontier region, and these would also play a crucial role in the process of pottery development. The set of bowls sharing an elaborated geometric style that emerged during Phases IV and V suggests a specific function, likely for non-utilitarian purposes. In two reports of the Shillacoto site excavation (Izumi et al. Reference Izumi, Cuculiza and Kanō1972; Kano Reference Kano1979), the vast majority of pottery figures associated with an altar-like tomb belonged to this group of bowls; some had jaguar and other rain forest animal motifs incorporated in their geometric style. Such a special set of bowls might reflect certain sociopolitical needs, such as ritual ceremonies. In addition, new chronology revealed that the Kotosh and Shillacoto sites, both known for preceramic monumental architectures, were not occupied at the beginning of the Wairajirca phase but appear to have been reoccupied in Phase III. Another site was also occupied from Phase IV in the southern part of the region. Considering these cases, we can argue that some social changes, stemming from both internal and external factors during this period, led to the elaboration of ceramic vessels and their use.

As briefly illustrated earlier, the emergence and development of Wairajirca pottery can be traced as the practices related to the use of ceramic vessels developed, according to the social situation of the times in the second millennium BC. From daily life communications among individuals to single or periodic migration, various forms of human and object mobility must have existed in this frontier region, and the movement of pots, potters, and pottery knowledge directly triggered changes in ceramic form, style, and technology in various ways (Heitz and Stapfer Reference Heitz, Stapfer, Heitz and Stapfer2017; Imamura Reference Imamura and Imamura2011). This region's favored natural environment, containing various types of resources in high availability, also might have affected the course of pottery improvement. In sum, in the Huánuco region, pottery technology was developed through accepting and reinterpreting various elements from other regions in its own sociopolitical context and subsequently occurring unique features of Wairajirca pottery.