Situating the Ik'hubil Ceramic Complex: Approaches to the analysis

Elsewhere, I suggest that the Ik'hubil Complex is best characterized as a mix or hybridized assemblage of local and “foreign” traits introduced during the Terminal Classic in an area of north-central Belize (Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013). Scholars have long noted the increased regionalization of ceramic traditions during the ninth-century Terminal Classic. Willey and colleagues (Reference Willey, Patrick Culbert and Adams1967:311) attributed the “proliferation of [ceramic] spheres” defined by ceramicists for this time period as a result of this high degree of local differentiation in many areas of the southern Maya Lowlands. To understand this ceramic regionalization for the ninth-century Terminal Classic transition, Demarest and colleagues (Reference Demarest, Rice, Rice, Demarest, Rice and Rice2004:558–559) have called for “systematic site-by-site, subregion-by-subregion comparison and correlation of data … [with] alignment of chronologies and typologies and collaborative construction of subregional culture-histories.” As noted above, the development of fixed culture histories in archaeology has long been critiqued for privileging the diffusion of traits and external influence over local innovation as an explanatory model and, in many ways, belies the movement and mixing of people evident in the Terminal Classic. Despite the weaknesses of the culture-historical “explanatory” model, the approach remains foundational in Maya archaeology, specifically with ceramic studies (Gándara Reference Gándara, Nichols and Pool2012).

Rather than a clear theoretical persuasion, the culture-historical approach in ceramic studies is perhaps best viewed as one aspect of the archaeologist's tool kit that serves as a “first step” for understanding regional and subregional differences in ceramic assemblages. The type-variety method as a culture-historical approach is considered among the most efficient for achieving intersite ceramic comparisons (Forsyth Reference Forsyth1983:241). Type-variety is a mode of classification in which archaeologists “[have] established a common language for the description of ancient pottery by organizing pottery hierarchically into wares, groups, types, and varieties based on stylistic similarity” (Aimers and Graham Reference Aimers, Graham and Aimers2013:92). A ceramic group is a discrete collection of ceramic types grouped together based on a suite of shared attributes. The ceramic types within the group share “a distinctive homogeneity in range of variation concerning form, base color, technological, and other allied attributes” (Gifford Reference Gifford1963:23, cited in Forsyth Reference Forsyth1983:9). The variety further subdivides individual types, usually based on specific stylistic elements (e.g., plain versus incised). As Aimers and Graham (Reference Aimers, Graham and Aimers2013:96) observe, type-variety as an analytical approach tends to privilege stylistic choices over those of production, but it remains a useful mode of classification for addressing specific questions regarding consumption and—of importance for this study—intersite and interregional comparisons.

A typological approach such as type-variety is a classification system that groups ceramics based on select sets of attributes, usually a specific suite of surface treatments, whereas a modal approach can crosscut individual types and varieties (Forsyth Reference Forsyth1983:9). The latter classifies ceramics using single features or attributes, most commonly vessel form or technological modes of manufacture (Forsyth Reference Forsyth1983:3). Scholars such as Donald Forsyth (Reference Forsyth1983) advocate for the use of a combination of approaches to ceramic studies—what is often referred to as a type-variety-mode classification system. Although my approach here emphasizes the type-variety system of classification, I do consider select modal attributes in terms of certain vessel forms and functions, as well as paste and other technological aspects of manufacture. Additionally, there are some distinctive and chronologically significant modes found in select ceramics that I describe as “horizon markers” (Forsyth Reference Forsyth1983:9; Willey et al. Reference Willey, Patrick Culbert and Adams1967:305–306), because they are widely shared across space and between complexes. Like the northern-style circular architecture, these distinctive modes found in Terminal Classic ceramics mark broader regional changes taking place during this transitional time in the Maya Lowlands.

Defining a ceramic complex using type-variety offers an effective means for not only making typological comparisons but also constructing a general chronological framework that can be compared with other sites across the Maya Lowlands. In the type-variety system of classification, a ceramic “complex” is defined as “the sum total of the ceramic content of an archaeological unit or phase” (Forsyth Reference Forsyth1983:9). The ceramic complex provides “a means for categorizing the contents of individual site assemblages and for exploring and expressing the degree of similarity between assemblages from different sites” (Bill Reference Bill and Aimers2013:29). In its strictest definition, a ceramic complex is only applicable to one site (Willey et al. Reference Willey, Patrick Culbert and Adams1967:292). The Ik'hubil Complex presented here deviates from this strict definition of a ceramic complex because it is defined based on my own quantitative and qualitative type-variety analyses of ceramics from two neighboring sites in the Sibun Valley—Oshon and Obispo. These sites are located across the river from one another about 2.5 km apart (see Figure 1; Harrison-Buck Reference Harrison-Buck2007). The site of Pechtun Ha in the middle reaches of the Sibun Valley around 20–25 km away also shares a majority of the ceramic content of the Ik'hubil Complex, so it is appropriately referred to as a member of a larger ceramic “sphere” (see discussion below).

All three sites in the Sibun Valley share not only ceramic content but also a distinctive circular architectural complex indicative of a similar occupational history and chronological framework. I relied most heavily on these three sites for defining the primary ceramic groups of the Ik'hubil Sphere (see Table 1). I compared the ceramic content with two other sites in the Sibun Valley—Pakal Na and Hershey—which lack circular architecture. Although all five sites generally share similar ceramic content, the distributions vary somewhat (see Table 2). Pakal Na and Hershey, located in the middle and upper reaches of the Sibun Valley (respectively), show greater affinities with the upper Belize/Peten region to the west in terms of both material culture and architecture (see Harrison-Buck et al. Reference Harrison-Buck2007). Although both Pakal Na and Hershey have a stronger Late Classic occupation than the other three sites, there is also clear evidence of Terminal Classic construction with stratified deposits.

Table 1.

Primary ceramic types for the Spanish Lookout, Ik'hubil, and Rancho Ceramic Spheres

Table 2.

Total percentages of primary ceramic groups from sites in the Sibun and Upper Belize Valley^a

^a Percentages generated from Aimers Reference Aimers2004a:Appendices B–D; Gifford Reference Gifford1976; Harrison-Buck Reference Harrison-Buck2007; LeCount Reference LeCount1996:Table 5.9.

The Ik'hubil Ceramic Complex was defined based on ceramic data collected from a series of test excavations carried out at Oshon and Obispo and compared with assemblages from multiple sites as part of a valley-wide settlement survey. Normally, ceramic complexes are defined based on a large quantity of ceramic data derived from years of excavations at a single site. For instance, most of the ceramic complexes described by Willey and colleagues (Reference Willey, Patrick Culbert and Adams1967:Figure 1) provide seminal examples, one of which is the Spanish Lookout Complex defined at Barton Ramie (see Gifford Reference Gifford1976). In valley-wide settlement studies, such as the Sibun, test excavations tend to be more limited in scope and as such have less chance of finding intact deposits with whole ceramic pots. However, the benefits of such valley-wide studies are that they provide more comprehensive areal coverage and offer greater information about the occupational histories for many different sites across a larger region. Moreover, they allow the same analyst to make firsthand intersite comparisons, enabling a better understanding of how ceramic typologies and modes vary through time and also across space.

Below I provide an overview of the primary ceramic types of the Ik'hubil Complex. I compare the assemblage alongside published ceramic studies, including the type-variety analysis of the Spanish Lookout Complex, considered one of the best documented ceramic complexes from the site of Barton Ramie in the upper Belize Valley (see Gifford Reference Gifford1976). While I did not do a first-hand analysis of any of the ceramics from the upper Belize Valley, Dr. Jim Aimers was kind enough to spend several weeks with me in the Sibun Lab during the summer of 2004 and was instrumental in helping me to identify ceramic types that resembled those from his own first-hand studies of the ceramics from Barton Ramie, Baking Pot, and Tipu. Through the course of my analysis, it became clear that many of the primary ceramic types found at sites in the upper Belize Valley were noticeably absent or underrepresented at sites in the lower Sibun Valley, namely at Oshon and Obispo where I defined the Ik'hubil Complex. Below I describe in more detail both the similarities and differences of these two ceramic complexes.

Comparing the Ik'hubil and Spanish Lookout Ceramic Complexes

The primary ceramic types of the Ik'hubil Sphere are presented in Table 1. In defining the Ik'hubil Complex, one general observation I gleaned from my analysis of the ceramics from the Sibun Valley is that the most common ceramic types typically represent the least common types in the Spanish Lookout Complex (Harrison-Buck Reference Harrison-Buck2007). Conlon and Ehret (Reference Conlon, Ehret and Lucero2002) made a similar observation in their analysis of the Terminal Classic ceramics at Saturday Creek in the middle Belize Valley despite this site being in close proximity to Barton Ramie (see also Lucero Reference Lucero1999a, Reference Lucero1999b, Reference Lucero2002). The site of Barton Ramie is located just 20km overland to the west of Saturday Creek in the middle Belize Valley, or roughly 40 km if paddling the sinuous Belize River (refer to Figure 1).

The Spanish Lookout Complex is divided into an early facet (generally dating to Late Classic II) and a late facet (dating to the Terminal Classic) that was originally defined by James Gifford (Reference Gifford1976) based on his analysis of the ceramic assemblages from Barton Ramie. Because many Late Classic II ceramics continue to be used through Terminal Classic times, it is almost impossible to parse these two time periods neatly with the existing published data on ceramic counts. For this reason, the comparative calculations presented in Table 2 (given as relative percentages) are based on the combined total percentage of all early and late-facet Spanish Lookout ceramic types recorded from Barton Ramie. For the sake of intersite comparison, counts of both Late Classic II and Terminal Classic ceramics from other sites are also combined in Table 2 (see Aimers Reference Aimers2004a:Appendices B–D; LeCount Reference LeCount1996:Table 5.9). For the most part, percentages are calculated based on raw counts (total rim and body sherds) for ceramics recovered from the sites in the Sibun and Upper Belize Valley. The one exception is Xunantunich, where rim counts are used to generate percentages of Late Classic II and Terminal Classic assemblages (see LeCount Reference LeCount1996:Table 5.9). Because the Xunantunich counts are based on rims, the percentages of each ceramic group and type may be a more conservative calculation than the others. But when charted alongside Barton Ramie, Baking Pot, and Tipu, I believe a shared Spanish Lookout Ceramic Sphere is clearly demonstrated (Table 3).

Table 3.

Percentage of shared primary ceramic types of the Spanish Lookout Sphere at sites in the Upper Belize Valley^a

^a Percentages generated from Aimers Reference Aimers2004a:Appendices B–D; Gifford Reference Gifford1976; LeCount Reference LeCount1996:Table 5.9.

A ceramic ”sphere” is defined “when two or more [ceramic] complexes share a majority of their most common types” (Willey et al. Reference Willey, Patrick Culbert and Adams1967:306). Full membership in a specific ceramic sphere is traditionally defined based on the percentage (at least 60 percent or more) of shared ceramic content found among the various ceramic complexes that have been reported from sites (Rice and Sharer Reference Rice and Sharer1987; Willey et al. Reference Willey, Patrick Culbert and Adams1967:306). Willey and colleagues (Reference Willey, Patrick Culbert and Adams1967:Figure 3) defined the Spanish Lookout Complex as a ceramic sphere, and others have subsequently suggested that this sphere may extend from Barton Ramie west throughout much of the upper Belize Valley, where similar Late Classic II and Terminal Classic ceramics have been found at the sites of Baking Pot, Tipu, and Xunantunich (see Tables 2 and 3). Belize Red is the primary shared type for the Spanish Lookout Sphere (Gifford Reference Gifford1976). However, scholars have shown that Mount Maloney Black, although less common at Barton Ramie, is also a widely shared primary ceramic type at sites in the upper Belize Valley and might be considered a primary diagnostic of the Spanish Lookout Ceramic Sphere (Aimers Reference Aimers2004a, Reference Aimers and Garber2004b; Gifford Reference Gifford1976; LeCount Reference LeCount1996, Reference LeCount, López Varela and Foias2005).

Willey and colleagues (Reference Willey, Patrick Culbert and Adams1967:302) suggest that the late facet of the Spanish Lookout Complex shows “some modal similarities to Eznab at Tikal [but] the total complex does not articulate well with the Petén.” However, more recent analysis suggests that ceramics associated with the early and late facets of the Spanish Lookout Complex show strong stylistic and modal connections with the Peten-affiliated Tepeu/Eznab Ceramic Sphere (Figure 1). Prudence Rice and Donald Forsyth (Reference Rice, Forsyth, Demarest, Rice and Rice2004:37) even question whether the Spanish Lookout Sphere should be considered a distinct sphere or simply a peripheral Tepeu/Eznab Sphere (sensu Ball Reference Ball and Gifford1976), highlighting the fuzziness of sphere boundaries. Lisa LeCount (Reference LeCount, López Varela and Foias2005:101–102) concludes, “The Petén influence in pottery styles was unwavering within the Upper Belize Valley during the Terminal Classic even though this region was experiencing considerable internal turmoil.” There are strong similarities in their ritual and serving vessels along with the presence of volcanic ash paste commonly found in the Peten-style Tinaja Red ceramics (LeCount Reference LeCount, López Varela and Foias2005:102, Figures 5 and 7; see also intersite comparisons of Tinaja and other Eznab ceramics in Culbert and Kosakowsky Reference Culbert and Kosakowsky2019).

The distribution patterns of ceramic groups (representing the total percentage from Late and Terminal Classic assemblages) shown in Table 2 derive from James Gifford's (Reference Gifford1976) ceramic study of Barton Ramie; subsequent studies by James Aimers (Reference Aimers2004a, Reference Aimers and Garber2004b) and Lisa LeCount (Reference LeCount1996, Reference LeCount, López Varela and Foias2005) carried out at Baking Pot, Tipu, and Xunantunich; as well as my own analyses of the Sibun Valley ceramics (Harrison-Buck Reference Harrison-Buck2007). One pattern that emerges from the differential distribution patterns visible in Table 2 is that some of the most common ceramic groups associated with sites in the Sibun Valley represent the least common ceramic groups at sites in the upper Belize Valley. For instance, Belize Red (closely related to the Peten Eznab Tinaja Red) is the most common red slipped ceramic group in the upper Belize Valley, but this volcanic ashware is relatively rare in the Sibun, especially at the three sites in the middle and lower reaches with circular architecture—Oshon, Obispo, and Pechtun Ha. Inversely, Table 2 shows that the Vaca Falls ceramic group is relatively rare in the Spanish Lookout Complex at Barton Ramie and throughout the upper Belize Valley, but it is the most common red slipped ceramic group identified throughout the Sibun Valley during the Terminal Classic (see Table 4 for a breakdown of Vaca Falls ceramic types).

Table 4.

Total percentages of ceramic types from the Vaca Falls group from sites in the Sibun and Upper Belize Valley^a

^a Percentages generated from Aimers Reference Aimers2004a:Appendices B–D; Gifford Reference Gifford1976; Harrison-Buck Reference Harrison-Buck2007; LeCount Reference LeCount1996:Table 5.9.

Similarly, Sibun Red Neck jars (defined as part of the Sibun Group) are prevalent in the Sibun Valley but appear to be virtually absent at sites in the upper Belize Valley (Table 2). Although this is a ceramic group and type name that postdates the type-variety studies from the upper Belize Valley, a careful read of the ceramic reports from Barton Ramie, Baking Pot, Tipu, and Xunantunich show that jars slipped red on the neck are exceedingly rare at these sites (see Cayo Unslipped: Variety Unspecified [Red-slipped] in Gifford [Reference Gifford1976:282] for a possible analogous type at Barton Ramie, as well as two other possible examples of Sibun Red Neck jars lumped in with the Vaca Falls Red type by Gifford [Reference Gifford1976: Figure 144j–k] at Barton Ramie).

Other unslipped types belong to the Tu Tu Camp and Cayo Ceramic Groups, both of which appear in the Spanish Lookout and Ik'hubil Spheres (Table 1). Because the studies of ceramics at sites in the upper Belize Valley do not consistently present the ceramic types with variety designations (e.g., Aimers Reference Aimers2004a:Appendices B–D and LeCount Reference LeCount1996:Table 5.9), I am only able to compare counts and percentages of ceramic types (Table 1) and groups (Table 2). This only presents an issue with Cayo Unslipped, given that significant differences at the variety level are noted between the Upper Belize Valley and the Sibun Valley sites (described further below). In such circumstances, I am unable to accurately calculate these differences because I only have exact counts and percentages for the Upper Belize Valley down to the type level.

Table 5.

Percentage of primary Spanish Lookout ceramic types in the Sibun Valley^a

^a Percentages generated from Harrison-Buck Reference Harrison-Buck2007.

In terms of the Dolphin Head ceramic group, no clear differential distribution patterns could be drawn between the Sibun and upper Belize Valley—the numbers are relatively low but generally equivalent across these two regions (see Table 2). Mount Maloney Black bowls, on the other hand, are virtually absent in the Sibun Valley, but they are ubiquitous at most sites in the upper Belize Valley, with the exception of Barton Ramie. Given its abundance elsewhere in the upper Belize Valley, Mount Maloney is generally considered a primary ceramic group for the Spanish Lookout Sphere (see Tables 1–3).

When cross-examining the ceramic types present at Oshon, Obispo, and Pechtun Ha in the Sibun Valley, it is clear that, for the most part, these sites cannot be considered full or even peripheral members of the Spanish Lookout Sphere given that they share less than 40 percent of the same primary ceramic types (Table 5 [see Ball Reference Ball and Gifford1976:323]). Pakal Na and Hershey, on the other hand, share greater ceramic and architectural affinities with the upper Belize Valley and Peten region to the west. Hershey is the only site in the Sibun Valley that might be considered a full member of the Spanish Lookout Sphere. Pakal Na also may be a peripheral member, with just over 50 percent of shared ceramic content (see Ball Reference Ball and Gifford1976:323). However, when comparing the total percentages of primary ceramic types found at the three sites with circular architecture in the Sibun Valley—Oshon, Obispo, and Pechtun Ha—the frequencies suggest that these three sites are full members of the Ik'hubil Ceramic Sphere, sharing roughly 60 percent of the same primary ceramic content (Table 6). Pechtun Ha falls slightly below this number and might be considered a peripheral member, but more likely, this reflects the lack of preservation at the site. When compared to Oshon and Obispo, Pechtun Ha had the highest percentage of unidentified ceramics as a result of severe erosion of the sherds, which made solid identifications down to the type level more difficult to ascertain.

Table 6.

Percentage of Ik'Hubil primary ceramic types in the Sibun Valley.^a

^a Percentages generated from Harrison-Buck Reference Harrison-Buck2007.

The diagnostic ceramic types associated with the Ik'hubil Complex described herein provide ceramic data for an area of north-central Belize that has up until now remained poorly documented. The ceramic typology is grouped below more generally in terms of broader modal categories, including slip (or lack thereof), and discussed in terms of surface treatment and—to some extent—form. In addition to the Sibun Valley, I make note of similar ceramic types identified in my more recent studies of archaeological sites in the eastern half of the Belize Valley, including Saturday Creek, Chikin’ Chi'Ha, Hum Chaak, Ik'nal, Chulub, and Jabonche, which may be part of a larger peripheral Ik'hubil Sphere (see Figure 1). While comparable calculations have not yet been carried out at sites outside of the Sibun Valley, I have observed similar trends with the ceramic distribution patterns for sites in the eastern half of Belize River watershed (Harrison-Buck Reference Harrison-Buck2010; Harrison-Buck, ed. Reference Harrison-Buck2011, Reference Harrison-Buck2013, Reference Harrison-Buck2015a, Reference Harrison-Buck2015b, Reference Harrison-Buck2018, Reference Harrison-Buck2020). I present these and other heuristic comparisons to prompt researchers to further cross-examine the aerial extent of the proposed Ik'hubil Sphere. Below, I discuss the different ceramic types, grouping them by modal categories of surface treatment.

Unslipped types

The most common unslipped jar form found in both the Spanish Lookout and Ik'hubil Complexes is Cayo Unslipped. However, there are important stylistic and modal differences in the paste, surface treatment, and lip form of Cayo Unslipped that Gifford (Reference Gifford1976) differentiated at the varietal level. In the upper Belize Valley during the Terminal Classic period, unslipped jars tend to have an elaborate lip treatment: either pinched and flared downward or upward, grooved, given “pie crust” treatments, or bolstered and rolled (Aimers Reference Aimers2004a:79; LeCount Reference LeCount1996:159; LeCount Reference LeCount1999:251, Figure 6). Aimers (Reference Aimers2004a:79–80) notes that these jars with such fancy rim treatment tend to be a buff variety, defined by Gifford (Reference Gifford1976:179–180, Figure 181) as Cayo Unslipped: Variety Unspecified (Buff).

There were only a select few examples of the Cayo Unslipped: Variety Unspecified (Buff) type recorded in the Sibun Valley, and none with the fancy rim treatment. There was a slightly higher number of examples of Alexanders Unslipped, another Cayo Group type defined at Barton Ramie, which is a significantly larger jar form (Figure 2). Both types make up most of the Terminal Classic Cayo Group assemblages at sites in the upper Belize Valley (Aimers Reference Aimers2004a; Gifford Reference Gifford1976; LeCount Reference LeCount1996). In the Sibun Valley, the Cayo Unslipped: Cayo Variety defined by Gifford (Reference Gifford1976) at Barton Ramie is the most common type of unslipped jar. This outflaring jar form ranges from smudged brown to brick red and contains plain rims that tend to be thicker walled and more crudely made than the Cayo Unslipped: Variety Unspecified (Buff) type. Gifford (Reference Gifford1976) placed these two unslipped ceramics under the same group (Cayo) and type name (Cayo Unslipped) and only distinguished them at the varietal level. However, the stark differences in paste color, firing, and decorative treatment suggest they should probably be given two separate type names and, perhaps, even be separated at the group level.

Figure 2.

Cayo group types from the Sibun Valley, Belize: (a–e) Cayo Unslipped: Cayo Variety; (f–h) Cayo Unslipped: Variety Unspecified (Buff); (i–k) Alexanders Unslipped: Alexanders Variety. Illustrations by the author and C. Cesario.

LeCount (Reference LeCount1996) proposed separate ceramic groups and type names for some unslipped types at Xunantunich based on their paste color and other modal characteristics, which might apply here provisionally. She notes that “paste colors [that] range from light gray or pale brown to brown 10YR 4/3; 5/2-4; 6/2-6; 7/2; to 7.5 YR 4/2; 5/3-6; and 6/3-6) – [are] exemplary of the Cayo Ceramic Group,” whereas those that “exhibit more red or reddish brown pastes (7.5 YR, 5 YR, or 2/5 YR hues within 5/4-8 value and chroma)…are defined as members of the Cambio Ceramic Group” (LeCount 1996:374). At Xunantunich, most of the Cambio Group ceramics (which are rare) include “large flaring bowls, lids, and censers” (LeCount Reference LeCount1996:274) and in the Sibun and eastern Belize Valley, the unslipped forms are predominantly large, flaring jars. Most analysts tend to view Cayo and Cambio Groups as roughly equivalent (see Culbert and Kosakowsky Reference Culbert and Kosakowsky2019:345; Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:25–26). Because I have not carried out firsthand analytical comparisons, for now, I have retained Gifford's (Reference Gifford1976) Cayo Unslipped type-variety designations in Table 2, distinguishing the two types at the varietal level. However, because the studies of ceramics at sites in the upper Belize Valley do not consistently quantify the ceramic types at the varietal level (e.g., Aimers Reference Aimers2004a:Appendices B–D; LeCount Reference LeCount1996:Table 5.9), I am unable to compare exact counts and percentages of the different varieties. My assessments of the more common buff variety of Cayo Unslipped in the upper Belize Valley are based on various qualitative discussions provided in the ceramic reports.

In the Ik'hubil Complex, the most abundant unslipped jar type is referred to as Sibun Red Neck (Table 2). The Sibun Red Neck jars have short, outflaring necks that are slipped red on the interior and exterior rim extending down to the neck of the vessel, with the remainder of the jar unslipped (Figure 3). In some cases, the unslipped portion has a “wash” and is lightly striated on the exterior (Figure 3d–e). To my knowledge, similar-style jars are not common in the upper Belize Valley Spanish Lookout Sphere or farther west in the Peten (Tepeu Sphere). As noted above, I have identified in Gifford's (Reference Gifford1976) Barton Ramie report only a few isolated examples of red-necked jars that Gifford (Reference Gifford1976:282, Figure 144j–k) placed under the late facet Spanish Lookout Complex.

Figure 3.

Sibun Red Neck jars from the Sibun Valley, Belize. Illustrations by the author.

Graham (Reference Graham, Rice and Sharer1987:78–79) notes a red-neck jar at sites such as Lamanai (see Pierce Reference Pierce2016:Figure A.13-LA640/3) and San Jose (Thompson Reference Thompson1939:138–139, Plate 21c) that resembles the form and surface treatment of the Sibun Red Neck type. In addition, a similar striated type referred to as Red Neck Mother Striated jars has been found farther north in the Ikilik Complex at Nohmul, which is defined as part of the Rancho Sphere (D. Chase Reference Chase1982a:75; Table 1). Although there may be a plain variant, the Red Neck Mother Striated name suggests this is the predominant variant. In the Ik'hubil Complex, there is a striated variety that occurs, but it is less common. Firsthand analysis is necessary to determine if all of these similar-style ceramics should be considered the same type.

Red slipped types

Both Roaring Creek Red and Dolphin Head Red are red slipped types that are considered primary ceramic types of the Ik'hubil Complex/Sphere (Figures 4 and 5, Tables 1 and 6). The Roaring Creek Red type is part of the Vaca Falls group, and in the Sibun Valley, it consists primarily of outflaring dishes that are slipped red on the interior and exterior of the vessel and that have a basal break with sometimes a fairly pronounced basal ridge. They are supported by either a low ring base or somewhat elevated pedestal base. Gifford (Reference Gifford1976:227–230, 240–243, Figures 137–139, 149–151) defined the Roaring Creek Red and Dolphin Head Red types at Barton Ramie, but both are relatively rare at this site and elsewhere in the Upper Belize Valley compared to other red slip types, such as Belize Red (see Tables 1–3; LeCount Reference LeCount, López Varela and Foias2005).

Figure 4.

Roaring Creek Red type from the Sibun Valley, Belize. Illustrations by the author.

Figure 5.

Dolphin Head Red type from the Sibun Valley, Belize. Illustrations by the author and C. Cesario.

LeCount (Reference LeCount1996:Table 5.9) notes that Dolphin Head Red is predominantly a Late Classic I–II type at Xunantunich but does carry through to the Terminal Classic. Aimers (Reference Aimers2004a) observed the presence of collared jars in the Dolphin Head Red type at Baking Pot dating to the Terminal Classic. Although no jars were identified in the Sibun Valley, the Dolphin Head Red type occurs in the Late Classic II and is fairly well represented in stratified Terminal Classic contexts. The types in the Ik'hubil Complex most closely align with the forms and type descriptions for the Dolphin Head Group presented by LeCount (Reference LeCount1996:183–386, Figure E7) for Xunantunich. The forms, paste, and slip resemble the earlier Silver Creek Impressed variety that is also found in the Sibun Valley but strictly in Late Classic II contexts. It is notable that, at Xunantunich, the few Roaring Creek Red types that were identified were mostly shouldered bowls and jar forms (LeCount Reference LeCount1996:388, Figure E.9a), which are exceedingly uncommon in the Ik'hubil Complex (see Figure 4e–g for some rare examples of jar forms). Given the abundance of Roaring Creek Red, it is surprising that the Vaca Falls Red type is largely absent in the Sibun Valley (see Table 4). It does occur to some extent in the upper Belize Valley (see Table 4).

Belize Red is a red slip type that can be considered the primary ceramic type of the Spanish Lookout Complex at Barton Ramie, but it is significantly less common in the Ik'hubil Complex (Tables 3 and 5). From my own excavations (see contributions in Harrison-Buck, ed. Reference Harrison-Buck2015a, Reference Harrison-Buck2015b) and preliminary analysis of the ceramics at Saturday Creek (Harrison-Buck Reference Harrison-Buck2010), I observed a much heavier frequency of Roaring Creek Red and Dolphin Head Red types, with relatively few examples of Belize Red when compared to the ceramics from Barton Ramie. I would agree with the observations made by Conlon and Ehret (Reference Conlon, Ehret and Lucero2002) of what they refer to as “reversed redware frequencies” at Saturday Creek: Roaring Creek Red and Dolphin Head Red predominate, and Belize Red is exceedingly rare. This trend is also reflected when comparing the distribution patterns between sites in the Sibun Valley and upper Belize Valley (see Tables 2, 3, 5).

Belize Red—the most common of all the red slipped types in the Spanish Lookout Complex—has a distinctive volcanic-ash paste (see full description in Gifford Reference Gifford1976). Only a few examples of the Belize Red type were found in the Sibun Valley (Table 2), and of these as many as half were “imitation” ash wares made from a fine, calcite-based paste (Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013). One example was found in a burial context at the site of Pakal Na in the Sibun Valley (Figure 6e) that is virtually indistinguishable from a “real” volcanic-ash-paste version found at Xunantunich (Figure 6f). Only through a combination of petrographic analysis and chemical testing were we able to confirm that this was not a volcanic ash ware (Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013).

Figure 6.

Belize Red type (a–e) from the Sibun Valley, Belize; and (f) from Xunantunich (redrawn after LeCount Reference LeCount1996:Figure E.14a). Illustrations by the author.

The outflaring dish form of Roaring Creek Red (Table 4, Figure 4) is one of the most common types found at sites in the eastern Belize and Sibun Valleys (Conlon and Ehret Reference Conlon, Ehret and Lucero2002; Harrison-Buck Reference Harrison-Buck2007, Reference Harrison-Buck2010). Shirley Mock (Reference Mock1994:280–281) also notes that Roaring Creek Red dishes are found in abundance at sites along the north-central coast of Belize, such as Northern River Lagoon (NRL) and Saktunja, during the Terminal Classic period (see also Masson and Mock Reference Masson, Mock, Demarest, Rice and Rice2004). Although they have not been identified using type-variety, similar-style ceramics also appear illustrated in ceramic reports from Altun Ha (Pendergast Reference Pendergast1990:357, Figures 46e, 46j, 97h, 152e), Lamanai (Howie Reference Howie2006, Reference Howie2012), San Jose (Thompson Reference Thompson1939:Figures 76a–n, 76s, 78), Mayflower, T'au Witz, and other sites in the Stann Creek District (Graham Reference Graham, Rice and Sharer1987:78–79; see also Graham Reference Graham, Chase and Rice1985, Reference Graham1994). Firsthand analysis is necessary to determine if all of these similar-style ceramics should be considered the same type.

Black slipped types

At Saturday Creek, Conlon and Ehret (Reference Conlon, Ehret and Lucero2002:11) observed that “even more lacking than Belize Red is Mount Maloney Black.” The Mount Maloney Black type consists of black-slipped utilitarian bowl and jar forms that are ubiquitous at sites such as Xunantunich, particularly the bowl form (LeCount Reference LeCount1996, Reference LeCount, López Varela and Foias2005). In my own analyses, I have found that Mount Maloney Black types are rare at sites in the mid-to-lower Belize Valley east of Saturday Creek, and they are also exceedingly rare throughout the Sibun Valley (Table 2). When found, it is never the bowl form; invariably, it is the jar form (Figure 7), which is much less common in the upper Belize Valley, even at sites such as Xunantunich, where the Mount Maloney ceramic group is most heavily represented (see Table 2). This seems to be another reverse modal frequency—in this case, with ceramic forms: jars of Mount Maloney (along with Roaring Creek Red jars described above) are reversed in frequency between the Spanish Lookout and Ik'hubil Spheres.

Figure 7.

Mount Maloney Black jars from the Sibun Valley, Belize, showing overhanging, angled profiles typical of the Terminal Classic. Illustrations by the author.

When they are found in the upper Belize Valley during the Terminal Classic, LeCount (Reference LeCount1996:160) notes that Mount Maloney jars typically have overhanging, angled profiles (see Figure 7), whereas the Late Classic II jars generally have smooth contours (see LeCount Reference LeCount1996:Figure 5.6 for illustrations of this lip microseriation). LeCount (Reference LeCount1996:245–246) concludes that narrow-necked jars such as Mount Maloney Black, with a collar diameter of less than 13 cm, were probably used for transporting and serving liquids. These utilitarian jars were probably not the product of any formal exchange between elites. Rather, their value as an “import” in the Sibun and eastern Belize Valleys was probably in what they carried (water, chocolate, chicha, balche, or some other precious liquid). Very few Mount Maloney bowls have been identified in the Ik'hubil Complex; the more common are Dolphin Head Red and Garbutt Creek Red bowls (Gifford Reference Gifford1976:230–231, Figures 140 and 141; Harrison-Buck Reference Harrison-Buck2007:Figure 6.8a–f, Plate 3a). The Dolphin Head Red tends to have a brighter “velvety” red slip as opposed to the darker red-brown slip on the interior of Garbutt Creek bowls. The latter type also appears to be fairly common at Barton Ramie, but the Garbutt ceramic group decreases in frequency to the west at places such as Xunantunich, where bowls from the Mount Maloney group predominate (Table 2).

In the Ik'hubil Complex, the most common black-slipped vessel is a stamp-impressed variety of Achote Black (Figure 8e, g–i). Unlike Mount Maloney, Achote group ceramics are not utilitarian ceramics but more finely crafted specialty serving vessels. The Achote group was originally defined in Peten ceramic studies and is found in the Terminal Classic Eznab Complex at Tikal (Culbert and Kosakowsky Reference Culbert and Kosakowsky2019:350–351) among other Peten sites in Guatemala (e.g., Chase Reference Chase1984). Achote group ceramics, including a type known as Cubeta Incised, is also reported from northwestern Belize at sites such as Ka'kabish and La Milpa, where they become increasingly common during the Terminal Classic period (Sagebiel Reference Sagebiel2014; Sagebiel and Haines Reference Sagebiel and Haines2015:364). Achote Black is also found at Nohmul and Santa Rita Corozal and is considered a primary type of the Rancho Sphere in this far northern part of Belize (Chase Reference Chase1982a; Figure 1, Table 1). In her study of the Terminal Classic Ikilik ceramics from Nohmul, Diane Chase (Reference Chase1982b:507) noted differences between Achote group ceramics in the Peten and those in northern Belize, and she went so far as to propose a new ware designation—“San Pablo Gloss”—to distinguish them from the Peten Gloss Wares.

Figure 8.

Achote group ceramics from the Sibun Valley, Belize: (a–b) annular bases; (c–d) Chilar Fluted; (e, g–i) Achote Black: Stamp-Impressed Variety bowls; (f) Cubeta Incised. Illustrations by the author and C. Cesario.

Although this ware designation has never been widely applied, other analysts working in northern Belize agree that the Peten Achote group ceramics are somewhat different from the black slipped types in northern Belize, which are mottled and fire clouded and have a somewhat soapy to waxy surface rather than a pure, hard, glossy black surface (Kerry Sagebiel, personal communication 2022). Shirley Mock (Reference Mock, López Varela and Foias2005:124) provides a similar description of the northern Belize Achote types at Northern River Lagoon (NRL) and notes a northern Yucatec influence. She concludes that these black slipped types “show the influence of thin slate wares in northern Belize and perhaps even imitation of Ticul slate ware bowls by local potters as the gray, fire-clouded slip on some bowls is slightly waxy or soapy.” Both Mock (Reference Mock1994:242–244) and Ball (Reference Ball1977:34–36) observe that the Achote Black in northern Belize as well as Quintana Roo typically have a very pale brown paste with calcite inclusions, but they also describe a less common pink paste variant that also occurs. Both paste variants have been identified in the Sibun Valley, displaying a similar waxy or soapy black exterior slip.

Kosakowsky and colleagues (Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:26) observe that types in the Achote group, like Cubeta Incised, become the predominant serving vessel during the Terminal Classic at sites in northern Belize (see also Sagebiel Reference Sagebiel2014; Walker Reference Walker1990): “These black types are often incised, fluted, gouged-incised, impressed, modeled, or stamped” (Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:Figure 7g–h). According to these scholars, the most common forms of the Achote group in northern Belize include outflared and round bowls and cylinder vases. Although it is not considered a “primary” ceramic group in the Ik'hubil Sphere (Table 2), these same forms—especially the rounded bowl form with a slightly outflaring neck—have been identified at sites in the Sibun and eastern Belize Valleys (see Figure 8e, g–i).

In both the Sibun and eastern Belize River Valleys, types in the Achote group are found in trash heaps and other “domestic” contexts, but they are also found associated with burials and other special ritual deposits. The Achote group ceramics are described as an important serving vessel and tradeware throughout north-central Belize (Chase and Chase Reference Chase and Chase2020:38; Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020; Sagebiel Reference Sagebiel2014:129, 132; Sagebiel and Haines Reference Sagebiel and Haines2015; see also Culbert and Kosakowsky Reference Culbert and Kosakowsky2019:351 for other intersite comparisons). Achote types in the Sibun and eastern Belize Valleys have less diverse styles when compared to the types from sites in northeastern Belize (such as NRL) and southern Quintana Roo (such as Becan), where they incorporate a wide range of surface treatments—including appliquéd, impressed, incised, modeled, and composite surface attributes—and, in rare cases, resist slip decoration (Ball Reference Ball1977:34–36; Mock Reference Mock, López Varela and Foias2005:124).

In the Sibun and eastern Belize Valleys, the most common forms of Achote Black include a round-sided bowl, as well as a squat rounded bowl with a high neck that has slightly outflaring sides. Incising and stamped-impressed designs in the form of circles and ovals frequently occur on these bowl forms (Figure 8e–i). Similar examples of squat and round-sided bowls with black slip are recorded as San Jose IV Black Ware at San Jose (Thompson Reference Thompson1939:Figure 73a, e–f, h–j, l), and other similar-looking vessels are found at Lamanai (Pierce Reference Pierce2016:Figure A13) and Altun Ha (Pendergast Reference Pendergast1990:Figures 19m, 64a, 64c, 90d, 90f, 163n, 163q). Is it noteworthy that the squat bowls from Lamanai, Altun Ha, and San Jose share nearly identical forms and surface treatment, with incised lines and postslip-prepolish unit-stamped circular or oval designs as found at sites in the Sibun and eastern Belize Valleys (compare Figure 8e–i with Pendergast Reference Pendergast1990:Figures 106n, 163q; Pierce Reference Pierce2016:Figure A.13-LA640/1; Thompson Reference Thompson1939:Figure 73e–f). Firsthand analysis is necessary to determine if all of these similar-style ceramics should be considered the same type.

Other special types

Like Achote Group ceramics, Daylight Orange: Darknight Variety is another special type associated with the Ik'hubil Complex. The outflaring dish form is virtually identical to Roaring Creek Red and is also comparable to the San Jose V vessels from the site of San Jose (Thompson Reference Thompson1939; Figure 9). What distinguishes the Daylight Orange: Darknight dishes are blocks of smudged black or dark reddish-brown blotches that form intentional decorative patterns across the interior of the reddish-orange slipped vessel. The black smudged designs consist of humanoid faces, monkey motifs, spirals, and other abstract designs. Figure 10d shows an example of a Daylight: Darknight vessel from a Terminal Classic burial deposit found at Saturday Creek. The Saturday Creek dish shows a pair of monkeys, which is a frequent motif found on this ceramic type and in Terminal Classic iconography, in general (Harrison-Buck Reference Harrison-Buck2010; Mock Reference Mock1997; Rice and South Reference Rice and South2015). At the nearby site of Chikin Chi'Ha’, a similar vessel was found in another Terminal Classic burial inverted over the head of the primary interment. It was associated with an Achote Black squat bowl form with oval stamp impressions that rested on the left arm of the main interment (Harrison-Buck et al. Reference Harrison-Buck, Craig and Murata2017; for similar examples, see Figures 8e, 8g–8i).

Figure 9.

Daylight Orange: Darknight Variety from (a–c) the Sibun Valley; and (d) Saturday Creek, Belize Valley. Illustrations by the author and C. Cesario; photograph by the author.

Figure 10.

Terminal Classic Palmar-Orange Polychromes from (a–b) the Sibun Valley; and (c–f) Northern River Lagoon (redrawn after Mock Reference Mock1997:Figures 4, 12, 15). Illustrations by C. Cesario and the author.

In the Sibun and eastern Belize Valley, Daylight Orange: Darknight appears to be generally found in elite ritual contexts, such as burials. It does not constitute a primary ceramic type of the Ik'hubil Complex, but it appears to have been an important serving vessel like the Achote group vessels. The distribution of Daylight Orange: Darknight seems to be widespread beginning in the late Late Classic and increases in distribution during Terminal Classic times (Sagebiel Reference Sagebiel2005, Reference Sagebiel2014; Valdez Reference Valdez1987). During the ninth and tenth centuries, it is found across a broad area of north-central Belize and along the eastern Caribbean coast (Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:27). Examples have been reported as far away as the Maya port of Vista Alegre on the northeastern tip of the Yucatan peninsula (Jeffrey Glover, personal communication 2012).

At Barton Ramie, Gifford (Reference Gifford1976:300–302) suggested that Daylight Orange: Darknight was an Early Postclassic (New Town Complex) type, but scholars now widely accept that this type dates no later than the Terminal Classic (Graham Reference Graham, Rice and Sharer1987). At La Milpa, Caye Coco, and other sites in Belize, both Daylight Orange: Darknight and Roaring Creek Red have been identified in Late Classic contexts (Kosakowsky, personal communication July 2016; Masson and Mock Reference Masson, Mock, Demarest, Rice and Rice2004:387; Sagebiel Reference Sagebiel2014:126). However, these two types are usually considered strong “horizon markers” of the Terminal Classic period (Aimers Reference Aimers2004a:73; Gifford Reference Gifford1976:240; Graham Reference Graham, Rice and Sharer1987:78; Harrison-Buck Reference Harrison-Buck2007:Table 5.1; Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:27; LeCount Reference LeCount1996:388).

Polychrome types

A distinctive polychrome type is found in the Ik'hubil Complex that appears to be equivalent to what other analysts in northern Belize refer to as Palmar Orange Polychrome (Mock Reference Mock1997; Pierce Reference Pierce2016:414; Valdez Reference Valdez1987; Walker Reference Walker1990). In the Sibun and eastern Belize Valleys, these polychrome dishes, plates, and platters are considerably eroded and fragmentary, and they are not considered a primary ceramic type, but this type seems to have had a broad distribution throughout north-central Belize during the Terminal Classic (Figure 10). This type is reported at NRL and Colha in northern Belize (Mock Reference Mock1997, Reference Mock, López Varela and Foias2005:126–128; Valdez Reference Valdez1987). Analysts also suggest that it occurs at Lamanai, where similar-style polychrome dishes, plates, and platters are described as “common” in the Terminal Classic period. When she visited Lamanai, ceramicist Debra Walker was able to examine these ceramics firsthand, and she noted that they are equivalent to what many analysts call Palmar Orange Polychrome (Pierce Reference Pierce2016:414). Given their abundance, Elizabeth Graham dubbed them “Lamanai Polychromes” (Graham Reference Graham2004:235; see also Pierce Reference Pierce2016:84, 414). Both Lamanai and the nearby site of Ka'kabish have this distinctive local polychrome (see Graham Reference Graham2004; Sagebiel and Haines Reference Sagebiel and Haines2015). It is described as having “a matte rather than glossy finish and very little red decoration, consisting mostly of black-on-orange. The decoration, which is not as finely executed as Petén polychromes, evolves throughout the Late to Terminal Classic” (Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:26–27).

Like the Achote group types, the Palmar Orange Polychrome type was initially defined in Peten ceramic studies, and scholars frequently attribute them as both Peten imports and evidence of trade ties with this area in the Late Classic (Aimers Reference Aimers2004a:108–110; Ball Reference Ball, Sabloff and Henderson1993:260; Gifford Reference Gifford1976:192–193). More recently, scholars have concluded that types dubbed “Lamanai Polychromes” are a local variant in northern Belize that are distinct from the Peten Palmar Orange Polychrome types (Kosakowsky et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:26–27; see also discussion in A. Chase and D. Chase Reference Chase and Chase2020:40). At Lamanai and Kichpanha, scholars use the name “Lamanai Polychrome” to distinguish them from the upper Belize Valley and Peten Palmar Orange Polychromes (Pierce Reference Pierce2016:129; Sagebiel and Haines Reference Sagebiel and Haines2015:364). The form of these late Terminal Classic vessels are mostly large dishes, plates, and platters, whereas the upper Belize Valley and Peten Palmar Orange Polychromes are primarily bowl and vase forms (see A. Chase and D. Chase Reference Chase, Chase, Rice and Sharer1987; LeCount Reference LeCount, López Varela and Foias2005). Their surface treatment also varies.

The Lamanai Polychromes have a loose painterly style, with designs that are less refined than Palmar Orange Polychrome designs, which is why they are often described as “sloppy” or “cartoonish” (Kosakowski et al. Reference Kosakowsky, Robertson, Sagebiel and Aimers2020:27; Pierce Reference Pierce2016:126). Pierce (Reference Pierce2016:129) notes “‘Lamanai polychromes’ are red and black on orange, usually with encircling stripes around the rim interior. The interior base is commonly decorated with a cartoon-like jaguar or other animal” (see Pierce Reference Pierce2016:Figure 6.28). Other common designs rendered in this loose painterly style include floral elements, cacao, monkeys, deer, and other animals; more abstract imagery, such as “X” and mat motifs; as well as lines, dots, and triangles (Figure 10; Ball Reference Ball1977:Figure 28e; Graham Reference Graham2004:Figure 7; Mock Reference Mock1997; Pendergast Reference Pendergast1990:Figure 106a, 163o; Pierce Reference Pierce2016:Figures A.37–A.39, A.49–A.51). In sum, it is clear that the Lamanai Polychrome type takes on very different forms and surface treatments and should probably be given its own type name in the future.

At least two other polychrome types have been identified in the Ik'hubil Complex and are assigned to the Kik Polychrome group: Indian Creek Polychrome and Fat Polychrome (Figure 11). In my original ceramic analysis (Harrison-Buck Reference Harrison-Buck2007), I followed Shirley Mock's assignment, placing the Fat Polychrome type in the Kik group. This type was originally defined in her study of the ceramics from the site of Northern River Lagoon (NRL) on the northern Belize coast (Mock Reference Mock1994:106–107, Figure 51; Mock Reference Mock, López Varela and Foias2005:128, Figure 7; Masson and Mock Reference Masson, Mock, Demarest, Rice and Rice2004:387, Figure 17.7d–e). I subsequently defined the more diminutive Indian Creek Polychrome based on my studies of the ceramics from the Sibun Valley (Harrison-Buck Reference Harrison-Buck2007:265–270). The Kik group, first defined by Diane Chase (Reference Chase1982b:495–501) as part of the Ikilik Complex at the site of Nohmul consists of a wide variety of red slipped ceramic types, including Kik Red and Campbells Red (see Chase Reference Chase1982b:495–501; see also Pring Reference Pring1976). These Kik Group types have a reddish-orange monochrome slip. Types such as Campbells Red are characteristic of the Rancho Sphere (see Table 1). A few possible examples of Campbells Red may be present in the assemblages from the Sibun and eastern Belize Valleys, becoming more frequent at sites farther to the north, such as Jabonche and Chulub (see Harrison-Buck et al. Reference Harrison-Buck, Hutson and Ardren2020:Figure 9g). Mock (Reference Mock1994) also reported some examples from NRL, but they appear to be rare. Kik Red is also present at NRL (Masson and Mock Reference Masson, Mock, Demarest, Rice and Rice2004). Although the form looks very similar to Roaring Creek Red, the slip is described as more of an orange color. To my knowledge, no polychrome varieties have been reported in the Kik Group at Nohmul or elsewhere in the northern Rancho Sphere, although Chase and Chase (Reference Chase and Chase2020:Figure 4e) report one possible example from Santa Rita Corozal. In the type-variety system, polychromes are normally placed in ceramic groups that are separate from redwares. Therefore, I have tried to distinguish these types from those of the Kik group by provisionally using the new ceramic group name Kik Polychrome.

Figure 11.

Kik Polychromes from the Sibun Valley, Belize: (a–b) Indian Creek Polychrome; (c–f) Fat Polychrome. Illustrations by C. Cesario and the author.

Both Indian Creek Polychrome and Fat Polychrome are found in moderate frequencies at sites in the Sibun and eastern Belize Valleys, although the former type (at least in the Sibun Valley) has a somewhat higher frequency than Fat Polychrome. The paste and surface decoration of Fat Polychrome is very similar to Indian Creek Polychrome, but the polychrome designs around the exterior vary somewhat between the two types. In both cases, the rounded bolster rim and interior of the vessels contain a hard, waxy, deep red slip that is generally well preserved, but rarely does the polychrome paint on the vessel exterior survive. On the best-preserved examples, a reddish-orange paint is found on the exterior just below the rounded lip and is covered with black and red polychrome painted designs. On the Fat Polychromes, faint traces of bold, black and red painted designs include lines; dots; s-, u-, and c-shaped designs; spirals; and other abstract motifs (Figure 11c–f). On a larger, better-preserved example from the Cara Blanca site in Belize, Joanne Baron recorded a jaguar and a sky band element with possible ak'bal (“darkness”) and k'an (“yellow” or “precious”) signs (Lucero and Kinkella Reference Lucero and Kinkella2015:171). On the Indian Creek Polychromes, designs include human, deer, and monkey imagery, as well as triangles and crosshatched areas separated by panels with angular and curvilinear vertical elements (Figure 11a–b).

No complete vessels of Indian Creek Polychrome bowls were recovered from the Sibun and eastern Belize Valley excavations. However, I have been able to reconstruct several partially reconstructable vessels from both the Sibun and eastern Belize Valley excavations (Figure 11). Other similar examples may be found at Altun Ha (Graham Reference Graham, Rice and Sharer1987:Figure 2g) and Lamanai (Pierce Reference Pierce2016:Figure A.54e), which show similar diminutive basal-break bowls with polychrome designs that contain ring bases. No complete Fat Polychrome basins were found in the assemblages that I studied, but the large, bulbous rim fragments are easily identifiable. The thick bolstered rim of the Fat Polychrome basins can vary significantly in size, but they are consistently larger than the rounded P-shaped lip of the Indian Creek Polychrome bowls (see Figure 11).

I have observed ceramics illustrated in various reports that bear a strong resemblance to Fat Polychrome and Indian Creek Polychrome types at a number of sites in north-central Belize, including Lamanai (Howie Reference Howie2006, Reference Howie2012; Pierce Reference Pierce2016:Figure A.54e), San Jose (Thompson Reference Thompson1939:124–125, Figures 5 and 65a, b, d–h), Cara Blanca (Lucero and Kinkella Reference Lucero and Kinkella2015:171), Altun Ha (Graham Reference Graham, Rice and Sharer1987:Figure 2g; Pendergast Reference Pendergast1990:Figure 46c, f), and along the coast of Belize at the sites of NRL, Saktunja, and the Salt Creek sites (Mock Reference Mock1994:106–107, Figure 51; Mock Reference Mock, López Varela and Foias2005:128, Figure 7; Masson and Mock Reference Masson, Mock, Demarest, Rice and Rice2004:387, Figure 17.7d–e [refer to Figure 1]). Kik group Polychromes also bear a strong resemblance to Thompson's (Reference Thompson1939:124–125, Figure 65) San Jose IV Red-and-Black-on-Orange polychrome “craters.” Firsthand analysis and quantification are needed to determine type assignments and how prevalent such polychrome types are across north-central Belize.

The Kik group type name did not exist when James Gifford (Reference Gifford1976) originally defined the Spanish Lookout Complex at Barton Ramie, but Thompson's (Reference Thompson1939) study of the San Jose ceramics was well known, and there is no mention of ceramics at Barton Ramie that resemble his San Jose IV Red-and-Black-on-Orange polychrome “craters.” Moreover, subsequent ceramic studies have been carried out at sites in the upper Belize Valley since Diane Chase (Reference Chase1982a) defined the Kik group types and Shirley Mock (Reference Mock1994) defined the Fat Polychrome type, but none mention any types that resemble these large red-slipped and polychrome-style bolster-rimmed basins (e.g., Aimers Reference Aimers2004a, Reference Aimers and Garber2004b; LeCount Reference LeCount1996). The pronounced P-shaped lip of the Kik Polychromes is very distinctive and is not easily missed even in circumstances of exceptional erosion, as was the case with the ceramics from Pechtun Ha. It is notable that although I identified Kik Polychromes at sites in the middle and lower reaches of the Sibun Valley, I did not find any of these ceramic types in the assemblages of Terminal Classic deposits at the Hershey site in the upper reaches of the Sibun Valley (Table 2). This site has relatively high quantities of Belize Red and Mount Maloney Black and comparably low quantities of Sibun Red Neck and Roaring Creek Red types, suggesting a stronger affiliation with the Spanish Lookout / Tepeu Spheres to the west.

Overall, the larger Fat Polychrome basin forms represent a smaller percentage of the Ik'hubil Complex compared to the more diminutive Indian Creek bowls (Table 7). The basins also represent a smaller percentage when compared to other wide-mouthed storage vessels, such as the Sibun Red Neck jars; the latter were eight times more prevalent at sites across the Sibun Valley (refer to Table 2). The relatively low quantity of Fat Polychrome basins combined with the presence of polychrome paint on the exterior of these pots suggests that these containers were probably not used for general-purpose storage but that they may have held a more specific purpose. The distribution patterns in the Sibun Valley suggest that the polychrome basins are more often associated with elite midden deposits, circular shrines, and other special ritual contexts, although they are notably absent in cave contexts (Peterson Reference Peterson2006). Based on their distribution, it is possible these vessels played a role in the presentation of bulk foods and/or public feasting and hosting events, as opposed to individual household consumption.

Table 7.

Total percentages of ceramic types from the Kik Polychrome Group from sites in the Sibun Valley^a

^a Percentages generated from Harrison-Buck Reference Harrison-Buck2007.

Stylistic and technological changes in the Terminal Classic

Stylistically, the Kik Polychrome ceramics present a marked disjunction from earlier materials, exhibiting new forms and painterly styles that have no known Late Classic precursors in the Tepeu 2 / early facet Spanish Lookout ceramic tradition that characterizes the Late Classic II ceramics from the upper and lower Sibun and Belize Valleys. The basin form and pronounced P-shaped bolster rim of the Fat Polychrome type are uncommon features in the ceramics of the southern Maya Lowlands, but they have a long history in the northern Maya Lowlands and are common forms in the Cehpech and Sotuta Ceramic Complexes, namely the Puuc and Chichen slate wares (Brainerd Reference Brainerd1958:52–53, Figures 41d, 41f, 43a–c, 73d; Smith Reference Smith1971:Figures 16d, 16g, 27h–i). Both Diane Chase (Reference Chase1982b:72) and Shirley Mock (Reference Mock1994, Reference Mock, López Varela and Foias2005) observed that the basin form and pronounced bolster rim of the Kik group types bear a strong resemblance to the Florescent Medium Puuc and Chichen slate ware basins from northern Yucatan. The quantity and distribution of the northern-style Kik Polychrome ceramics, coupled with petrographic and chemical studies of the paste characteristics, suggest that most were produced locally (Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013; Mock Reference Mock, López Varela and Foias2005:128). The surface finish of the Kik Polychrome ceramics found in Belize differs from the distinctive “soapy” slip of the Yucatecan slate wares. The Fat Polychrome and Indian Creek Polychrome are red slipped and usually contain a bichrome or polychrome design. The loose painterly style of the black painted motifs (abstract s- and u-shaped elements, cross-hatching, and monkey motifs) of the Kik Polychromes, as well as the Lamanai Polychromes, bear some resemblance to the motifs and loose painterly style found on some of the painted ceramics from Chichen Itza and Uxmal in northern Yucatan (Brainerd Reference Brainerd1958:Figures 72e and 72i, 76c, 9-10; Smith Reference Smith1971:Figure 20h).

The basin and bowl forms of the Kik Polychrome ceramics found in the Terminal Classic Ik'hubil Complex reflect vessel forms and painterly styles characteristic of northern Yucatan (Harrison-Buck Reference Harrison-Buck2007; Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013). Beyond a merely stylistic emulation, however, the basin form may have been functionally significant and indicative of specific changes in foodways. The basin form is reminiscent of the large tureens or soup dishes that were predominantly represented in the archaeological assemblage of San Pedro Siri, a colonial Caste War Maya site in the middle Belize Valley occupied by refugees from Yucatan. Jason Yaeger and colleagues (Reference Yaeger, Church, Dornan and Leventhal2004:8–9) concluded that dish forms represented only 10 percent of the ceramic assemblage, and bowl forms comprised the majority of the historic pottery, likely indicative of their suitability for Yucatec Maya cuisine, which traditionally includes stews, brines, and chilmole—a soup made of black mole–type sauce traditionally served with turkey roasted in a subterranean pib, or pit oven. It is notable that a subterranean pib dating to the Terminal Classic was identified at Nohmul in association with Yucatec-style architecture, including a circular shrine dating to the same time period (Chase and Chase Reference Chase and Chase1982). Additionally, an influx of ladles are reported from Terminal Classic deposits in the southern Maya Lowlands, which Flynn-Arajdal and colleagues (Reference Flynn-Arajdal, Halperin, Freiwald, Wolf and Salas2023) argue is indicative of a shift in cooking assemblages that derives from the Gulf Coast lowlands and shows influence from the north (see LeCount Reference LeCount1996:Figure E4b for an example from Xunantunich).

This influx of ladles, bolster-rimmed basins and small bowl forms of the Kik Polychromes during the Terminal Classic period may be congruent with increased feasting using more forms of traditional Yucatecan cuisine, including soups and stews. It is important to note that during this period of time, we also see comales—round pottery griddles for cooking corn tortillas—introduced in north-central Belize and elsewhere in the Maya Lowlands (Aimers Reference Aimers2004a; Bill Reference Bill and Braswell2014:96; Fry Reference Fry and Aimers2013:89; Harrison-Buck Reference Harrison-Buck2007:322–323; LeCount Reference LeCount1996:Figure 7.4; Rice Reference Rice2007:24; Taube Reference Taube1989). Although comales originally derived from Central Mexican cooking traditions, tortillas are a common accompaniment with Yucatecan cuisine. The introduction of these utilitarian wares in the Maya Lowlands signal marked changes in the habits of food preparation traditionally made by women in the domestic sphere.

Although the comales, ladles, and basin and bowl forms could be interpreted as merely local emulation of “foreign” styles (Fry Reference Fry and Aimers2013:89), alternatively, they could point to the physical migration of “foreigners” from northern Yucatan and/or the Gulf lowlands into places such as north-central Belize at this time, intermarrying with local individuals and bringing their foodways with them—what anthropologists characterize as core elements of social identity. Anthropologists have long argued that foodways (and their associated utilitarian wares) can often serve as core markers of “ethnic” or social identity because they relate to “central value orientations” (Barth Reference Barth1969:120)—certain social conventions or ways of doing things (Hegmon Reference Hegmon and Stark1998:272; see also Stark, ed. Reference Stark1998). Whereas emulation implies intentionality and often embodies politically informed action, the construction, maintenance, and negotiation of social identity is not a “self-conscious process of communication” (Gosselain Reference Gosselain2000:188) but a socially informed action, often embodying the mundane “every day” choices (Stark Reference Stark and Stark1998, Reference Stark2003).

Other northern traits introduced during the Terminal Classic period include distinctive Yucatec-style architectural structures, which have been interpreted elsewhere as wind shrines associated with the Mexican feathered serpent cult, where feasting as well as collective male bloodletting and ceremonial initiation took place (Harrison-Buck and Pugh Reference Harrison-Buck and Pugh2020; Harrison-Buck et al. Reference Harrison-Buck, Runggalider and Gantos2018; Ringle et al. Reference Ringle, Negrón and Bey1998). Terminal Classic circular shrines are found at sites in the eastern Sibun and Belize Valleys, including Pechtun Ha, Oshon, Obispo, Hum Chaak, and Ik'nal (Figure 1). These buildings bear a strong resemblance to one another and also to others found across a broad area of the Maya Lowlands, found as far apart as Lamanai, Nohmul, Chichen Itza, Uxmal, El Tigre, Ucanal, and Seibal (D. Chase and A. Chase Reference Chase and Chase1982; Halperin and Garrido Reference Halperin and Garrido2019; Harrison-Buck Reference Harrison-Buck2012a; Harrison-Buck and McAnany Reference Harrison-Buck and McAnany2013; Harrison-Buck and Pugh Reference Harrison-Buck and Pugh2020; Pendergast Reference Pendergast1986:11; Pierce Reference Pierce2016:179–180, Figure 5.7).

Local and regional spheres of interaction: Trading diasporas and intermarriage

Yucatec and Gulf lowland traits, including circular architecture and marked changes in foodways, strongly suggest more than just local emulation and trade. They point to the possibility of northern migrants entering places such as north-central Belize during the Terminal Classic. Yet the hybridized ceramic forms and maintenance of certain local ceramic traditions do not suggest a wholesale population replacement as a result of colonization. Elsewhere, I have suggested the possibility of trading diasporas and more intimate social relations such as intermarriage to explain this mix of local and hybrid forms of material culture introduced during Terminal Classic times (Harrison-Buck and McAnany Reference Harrison-Buck and McAnany2013; Harrison-Buck and Pugh Reference Harrison-Buck and Pugh2020; Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013). Trading diasporas may have involved the circular migration of northern merchants who intermarried with the local inhabitants in places such as north-central Belize. A trading diaspora model helps to explain the sudden influx of Terminal Classic settlement across the Maya Lowlands with circular architecture, which appears to be positioned at strategic points along the coast and rivers and connected to both the Gulf Coast and the Caribbean Sea (Harrison-Buck Reference Harrison-Buck2012a:Figure 1). The distribution pattern of settlement suggests an important connection between shrine centers and the movement of goods and people, either on foot or via canoe, and it may be tied to a long-distance trade network fueled by northern Maya groups during this time (Harrison-Buck and McAnany Reference Harrison-Buck and McAnany2013; Harrison-Buck and Pugh Reference Harrison-Buck and Pugh2020; Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013).

Jeff Kowalski and colleagues (Reference Kowalski, Rubio, Más, Herrera, Macri and McHargue1994:7–8) suggest that “the round structure form was disseminated by the Itzá,” a branch of Chontal-speaking Maya people who appear to have their origins in the Gulf lowlands (Harrison-Buck and McAnany Reference Harrison-Buck and McAnany2013; Scholes and Roys Reference Scholes and Roys1968:23–24). Kowalski (Reference Kowalski, Diehl and Berlo1989:173–177) and others have suggested that Chontal–Itza factions established themselves at Chichen Itza and developed a long-distance, circum-peninsular trade network that stretched from the Gulf Coast around the Yucatan peninsula, running along the east coast of Belize as far south as the Bay of Honduras and into the Guatemalan highlands (e.g., Ball and Taschek Reference Ball, Taschek, Diehl and Berlo1989; Kowalski Reference Kowalski, Diehl and Berlo1989; Sabloff and Willey Reference Sabloff and Willey1967; Vargas Reference Vargas1997, Reference Vargas2001). The archaeological evidence cited in support of this long-distance trade network includes the widespread appearance of certain “horizon markers” often described as “non-Classic” or “Mexicanized-Maya” elements found in the epigraphy, iconography, molded-carved ceramics, and new types of architecture, including circular shrines (e.g., Ball and Taschek Reference Ball, Taschek, Diehl and Berlo1989; Chase Reference Chase, Robertson and Fields1985; Kowalski Reference Kowalski, Diehl and Berlo1989; Proskouriakoff Reference Proskouriakoff1950; Sabloff Reference Sabloff and Culbert1973, Reference Sabloff, Bishop, Harbottle, Rands and Sayre1982; Sabloff and Willey Reference Sabloff and Willey1967; Thompson Reference Thompson1970; Vargas Reference Vargas2001).

Circular shrines have been found as far inland as the Peten at the Terminal Classic center of Ucanal and possibly also at Jimbal (Halperin and Garrido Reference Halperin and Garrido2019; Simon Martin, personal communication April 2023). In addition to this “foreign” architecture, there is evidence for physical migration of select elite individuals as marriage partners in the hieroglyphic record at both Ucanal and Jimbal. In texts from the latter site, the mother of the ninth-century ruler is named 8 Alligator, which is written with a Mexicanized, square day sign and suggestive of a Gulf lowland origin (Carter Reference Carter2014:202). She is also the wife of Olom Jaatz’, who is the ochik'in kaloomte’—or “western overlord”—in the eastern Maya Lowlands during the ninth century, according to inscriptions on monuments from Jimbal (Stelae 1 and 2), Ceibal (Stelae 10 and 11), and Uaxactun (Stelae 7 and 13). Olom Jaatz’ is also referenced on numerous mold-made Ahk'utu’ ceramics (see Helmke and Reents-Budet Reference Helmke and Reents-Budet2008:Figures 1 and 3). It is significant that the hieroglyphic dates for all references to Olom Jaatz’ span the ninth-century Terminal Classic, between a.d. 830 and 889 (Carter Reference Carter2014:203; Helmke and Reents-Budet Reference Helmke and Reents-Budet2008; Simon Martin, personal communication 2019). At Ucanal, Simon Martin (Reference Martin2020:295–296) has observed that the name of the ruler Papmalil derives from a Chontal naming practice. It is noteworthy that this ruler and Olom Jaatz’ had achieved superior status in the Peten by the first decades of the ninth century, which suggests that intermarriage with the Chontal-Itza nobility from the north had occurred in the southern Maya Lowlands right at the transition from the Classic to the Terminal Classic (see Harrison-Buck and Pugh Reference Harrison-Buck and Pugh2020 for further discussion).

Although no carved glyphic monuments have been found in the Sibun and eastern Belize Valleys, Terminal Classic circular architecture and mold-made Ahk'utu’ ceramics are present (see Figure 12). These traits and other rarer northern imports (Figure 13) signal that these sites were actively participating in this long-distance, circum-peninsular interaction sphere with the Chontal–Itza, which Kowalski (Reference Kowalski, Diehl and Berlo1989) has dated to the Terminal Classic (a.d. 790–909) based on the extant epigraphic data. Cacao, honey, jade, and bird feathers—commodities highly sought after by the Chontal–Itza merchants, according to ethnohistoric documents—were also prized as gifts in the petitioning of marriages (Harrison-Buck Reference Harrison-Buck, Matthews and Guderjan2017, Reference Harrison-Buck2021). These products were readily available in the subtropical environments of Belize and may have been what stimulated regional interaction and the population movements that may have involved intermarriage among groups in this part of the eastern Maya Lowlands during the ninth century.

Figure 12.

Ahk'utu’ Molded-carved ceramics from the Sibun Valley, Belize. Illustrations by the author.

Figure 13.

Imported Yucatec-style ceramics from the Sibun Valley, Belize. Illustrations by the author; photograph by D. Buck.

Joseph Ball (Reference Ball1974:87–88) describes an “intrusive tradition” at Becan in southern Quintana Roo, Mexico, during the Terminal Classic period that resembles the patterns described in the eastern Belize and Sibun Valleys. Becan has a circular structure and also evidence of ceramics that are “clearly of northern derivation, blended with the indigenous to produce a new, ‘hybrid’ ceramic expression” (Ball Reference Ball1974:87). At Becan, Ball reports that nonlocal forms were accompanied by imported types, such as Thin Slate, Balancan, and Altar group Fine Orange. In the eastern Belize and Sibun Valleys, we see the introduction of locally produced ceramics with northern attributes, but only a select few northern imports (Figure 13; Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013; Harrison-Buck et al. Reference Harrison-Buck, Burg, Murata, Robinson, Kaeding and Gantos2016:144; see also Fry Reference Fry and Aimers2013:88–89). Scholars have long argued that Ceibal's Bayal phase and Altar's Boca-Jimba phases experienced a similar coeval disjunction in the ceramic assemblages with “new, northern-derived forms, but without the large quantities of “slate ware” that characterize Becan's Xcocom phase and other assemblages from the Northern Lowlands (Ball Reference Ball1974:88). According to Ball (Reference Ball1974:88), the “northern forms were transferred via central-southern types,” blending local and foreign stylistic and modal attributes.

In more recent ceramic studies in northern Belize, at the site of Chau Hiix, Fry (Reference Fry and Aimers2013) has made a similar observation, noting that imported slate wares appear alongside local variants. These imitations “successfully integrate local shape classes and modes with the pastes and slip characteristics of northern slate wares” (Fry Reference Fry and Aimers2013:89). Fry (Reference Fry and Aimers2013:89) concludes that local potters in northern Belize may have emulated these “foreign” styles after acquiring “production secrets or recipes” of paste and slip characteristics of slate wares from Yucatan. Alternatively, he suggests the possibility that some northern craftspeople were physically present in north-central Belize, resulting in the hybrid mix (see also Harrison-Buck et al. Reference Harrison-Buck, Moriarty, McAnany and Card2013).

I suggest that trading diasporas may help to explain the select imports and hybrid mixing of local and foreign traits in the Sibun and eastern Belize Valleys during this time. If trading diasporas did occur in this area, small groups of northerners may have entered parts of north-central Belize, intermarried with locals, and established settlements along the waterways, perhaps becoming permanent or semipermanent residents. In the case of trading diasporas, individuals tend to “[maintain] a distinct social identity for an extended period of time” (Stein Reference Stein, Lyons and Papadopoulos2002: 28; see Abner Cohen's [Reference Cohen and Meillassoux1971] “trading diaspora” model). Through a pattern of circular migration, perhaps involving regular long-distance trading activities, the “foreigners” in places such as north-central Belize may have retained strong ties with their northern homeland and perhaps ultimately returned. That these were two-way engagements explains the hybrid mix of local and “foreign” Yucatec influence in ceramics and architecture during the Terminal Classic. Both Fry (Reference Fry and Aimers2013) and Ball (Reference Ball1974) conclude that these ongoing movements of people and goods impacted local (subregional or microregional) spheres of interaction not only in north-central Belize but across a broad area of the Maya Lowlands during this time.

Concluding thoughts: Interpreting new spheres of interaction in Terminal Classic times

In this study, I have defined the Ik'hubil Ceramic Complex in the Sibun Valley of Belize using type-variety analysis. Comparative analysis suggests that the Ik'hubil Complex is not a member of the neighboring Spanish Lookout Sphere but may represent its own discrete ceramic sphere in an area of north-central Belize (see Figure 1). Attempts to define discrete ceramic complexes and spheres offer useful analytical and comparative tools for the archaeologist to determine the degree of chronological overlap and the extent of interaction among groups. In this case, sites in the mid-to-lower Sibun Valley (e.g., Oshon, Obispo, and Pechtun Ha) suggest full membership in the Ik'hubil Ceramic Sphere, indicating that they shared a sphere of interaction that involved some degree of social integration.

Ceramicists have long struggled with how to interpret ceramic spheres. The type-variety system is analytically useful, but as a standalone approach, it is somewhat limited from a theoretical perspective. It runs the risk of creating fixed culture histories and bounded spheres of interaction that were, in reality, probably much more complex, fluid, and fuzzy than this idealized model allows. The “interaction sphere” model, first introduced by Joseph Caldwell (Reference Caldwell1959, Reference Caldwell1964), was introduced to replace the notion of a fixed “culture area” (Freidel Reference Freidel1979). This paradigm considers both local and regional networks of interaction as integrative mechanisms that further promote innovation (Matthews Reference Matthews1998:5). The strength of the interaction sphere model is its emphasis on reciprocal relationships between groups and its ongoing formation. Rather than a fixed entity, spheres of interaction are mutually constituted and constantly forming at multiple scales. The interaction sphere approach emphasizes the trade of goods and exchange of information as the key to solidifying a relationship of mutual need and controlling the integration of local and regional exchange networks (Freidel Reference Freidel1979:50). Despite its strengths, the interaction sphere model still suffers from the implicit assumption that “pristine” states ever existed in the first place. Although the notion of a defined sphere of interaction is useful from an analytical perspective, the boundedness of this model—like the type-variety approach—in many ways gives the false impression that these categories were consciously maintained and are somehow fixed and unchanging through time, which we know is simply not the case (Bill Reference Bill and Aimers2013:30).

A relational perspective may be useful for further conceptualizing both local and regional interaction spheres involving material culture such as ceramics. From a relational perspective, the social and economic are never distinct spheres of interaction, and influence is never unidirectional (Harris and Cipolla Reference Harris and Cipolla2017; Harrison-Buck Reference Harrison-Buck2021). Rather than static entities, interaction sphere networks are perhaps best understood as an ongoing “meshwork” of entangled relationships that “become comprehensively entangled with one another” (Ingold Reference Ingold2006:13). In this way, interaction spheres—whether they involve trading partners (“formal friendships” [Brightman et al. Reference Brightman, Fausto, Grotti, Brightman, Fausto and Grotti2016:12]) or marriage partners—invariably conjoin aspects of material possession and acts of nurturing in such a way that ownership or “belonging-to” something or someone always co-occurs through multiple relationships rather than as a single act of individualized possession (Brightman et al. Reference Brightman, Fausto, Grotti, Brightman, Fausto and Grotti2016:19).

Through such ongoing relationships involving two-way exchange, often shared or hybrid material forms occur (Card Reference Card2013). For the archaeologist, determining whether such forms represent trade, local emulation, or the coexistence of multiple groups with distinctive identities poses an interpretive challenge (see Cecil Reference Cecil2004). Scholars seeking to explain shared or hybrid material forms must consider models of interaction beyond a simple one-way diffusion and engage in the possibility of migration and the formation and/or maintenance of group identities. In archaeology, migration as an explanatory process has a long-standing bias as an external model (Braswell Reference Braswell and Braswell2003:15–18). Bernard Knapp (Reference Knapp2008:51) observes, “Continuing skepticism about using migration to explain cultural change…is clearly part of the processual legacy that rejects diffusionism and migration as hallmarks of cultural history” (see also Rowlands Reference Rowlands and Harris1994). As Susan Alt (Reference Alt, Butler and Welch2006:290) notes, previous models dealing with culture change often suffered from an all-or-nothing approach, proposing either local evolutionary development or wholesale population replacement as a result of colonization. More recent migration models in archaeology are concerned with explicit methods, and they view migration as a process that frequently involves multiple variables and produces latent and long-term effects (Braswell Reference Braswell and Braswell2003:18; Knapp Reference Knapp2008:51). Christopher Beekman (Reference Beekman and Beekman2019:3) suggests that greater attention should be given specifically to the processes of incorporation, not just the migration itself.

Building on these ideas, I argue that intermarriage played a key role in such incorporation processes in the Maya area during the ninth-century Terminal Classic period. Intermarriage is surprisingly underrepresented in current archaeological discussions of Mesoamerican migration. Yet across Mesoamerica, both indigenous and ethnohistoric accounts indicate that intermarriage is what made integration possible among various ethnic groups from Classic to Postclassic times, even in the midst of hostilities (e.g., Byland and Pohl Reference Byland and Pohl1994; Diel Reference Diel, Lee and Brokaw2014; Megged Reference Megged2023; Pohl Reference Pohl, Smith and Berdan2003; Spores Reference Spores1984; Townsend Reference Townsend, Lee and Brokaw2014). I conclude that the hybrid mix of local and “foreign” Yucatec influence in ceramics and architecture that appear in north-central Belize during the Terminal Classic is perhaps best understood as the result of multiple relationships that were mutually constituted through ongoing two-way movements, which included migration and trading diasporas that relied on intermarriage as an important means of social integration. This would explain why the changes taking place include an influx of not only Yucatec architecture and trade goods but also new foodways and other domestic practices that signal the movement of groups and the formation of new social identities in north-central Belize. These two-way exchanges formed economic and interpersonal relations simultaneously and generated new spheres of interaction in the eastern Maya Lowlands during Terminal Classic times.

Thinking about ceramic spheres as one part of a complex meshwork of nurturing social and economic relations helps to better understand the shared and hybridized forms of material culture and the fuzziness of sphere boundaries. These material signatures reflect the ongoing movement of people, goods, and ideas. From a relational perspective, shared “commodities”—such as ceramics and similar architectural styles—are not strictly material property, but they embody “nurturing relations” (sensu Brightman et al. Reference Brightman, Fausto and Grotti2016), where social and economic spheres of interaction are ongoing formations that are mutually constituted among groups.