Power and place: agency, ecology, and history in the American Bottom, Illinois
Antiquity, Dec, 2004 by Sissel Schroeder
Is ecology or agency the principal imperative of the formation of complex societies? Using new survey data, the author shows how both interest in the development of the riverside settlement area of the American Bottom and how the different modern histories of the northern (industrial) and the southern (agricultural) American Bottom, have affected the survival of evidence and how this in turn has favoured a different emphasis in interpretation for each.
Keywords: Mississippian, Cahokia, chiefdoms, settlement patterns, historical ecology
Introduction
The earthen mounds that dot the Eastern Woodlands of North America have fascinated archaeologists and antiquarians since they first began making observations about such features in the late eighteenth century. Early concerns with describing and classifying the mounds have given way to studies that use mounds as a point of departure to flame evolutionary discussions about variation in settlement patterns, hierarchies, and sociopolitical organisation on the one hand and the dynamics of ancient power, influence, leadership, and agency on the other hand.
To bridge the gap between these two archaeological approaches to the past, I present a model of the relationship between settlements, identified from mounds and surface artefact scatters, and the ecological resources available to them in a segment of the Eastern Woodlands of North America called the American Bottom (Figure 1). I then turn to a discussion of the asymmetric nature of archaeological and ecological data between the northern and southern halves of the American Bottom and the impact this imbalance has had on archaeological perceptions of the contemporaneous societies that once existed there. These perceptions range from those based largely on the effects of natural resources and the distribution of sites, to those that emphasise ideology and focus on individual sites. I suggest that both the agency and ecological perspectives are inadequate as applied to the American Bottom, and offer an integrated approach that begins with terrain and ecology, moves on to place as historically created and re-created space, and ends with a consideration of the people and their interactions.
Chiefdoms and the American Bottom
The majority of archaeologists working in the Eastern Woodlands of North America agree that during the millennium before European Contact, from the eleventh to sixteenth centuries, AD, the region was inhabited by diverse cultures that spanned the entire range of variation for middle-range hierarchical societies, from what might be called tribes to chiefdoms (Service 1962), but never made the transition to a state (e.g. Anderson 1994; Blitz 1993; Cobb 2001; Emerson 1997; Hudson 1997; King 2003; Knight & Steponaitis 1998; Milner 1998; Muller 1997; Muller & Stephens 1991; Pauketat 1994; Rountree 1988; Smith 2000; Welch 1991; for contrary views see Conrad 1989; Kehoe 1998:150-171; Gibbon 1991; O'Brien 1991; Sears 1968). One particularly instructive regional example for investigating the dynamic relationships among place, people, history and power is located within the American Bottom, a broad expanse of the central Mississippi River valley. What was arguably the most spectacular of the Mississippian-era (c. AD 1000-1600) Native American societies in eastern North America was located here, centred on the site of Cahokia.
The emergence of chiefdoms in the American Bottom began after AD 600, during the latter half of what is called the Late Woodland period (Figure 2). (The uncalibrated chronology (Bareis & Porter 1984) was used here to facilitate comparison with the southern American Bottom where there is an inadequate quantity of radiocarbon dates to permit calibrating the sequence.) During this time, people in the Mississippi River valley lived in small communities widely scattered across habitable landforms in the floodplain (Bareis & Porter 1984). The principal development of societies that could be called chiefdoms occurred from about AD 900 to 1250, during late Emergent Mississippian times and into the subsequent Mississippian period. Platform mounds may have been built as early as the end of the Emergent Mississippian period (Emerson 1997:57; Griffin 1977; Pauketat et al. 1998:45; Reed et al. 1968:144-145), but most such mounds were constructed during the Mississippian era. Importantly, only a few places in the American Bottom sustained the practice of mound building during Mississippian times and these places were the politically significant communities in the region. The majority of sites, however, lacked mounds. There is little archaeological evidence for sites post-dating AD 1400, indicating that the American Bottom was virtually abandoned and signalling the collapse of chiefdoms in this area by that date.
Settlement patterns and the ecology of the American Bottom
The American Bottom is a stretch of Mississippi River floodplain in Illinois running from near the confluence of the Missouri River south to the mouth of the Kaskaskia River, a distance of about 125km; it was named in the late eighteenth century when it was on the margin of American territory (Ekberg & Foley 1989:52-53; Flint 1970 [1828]:117). It is bordered by steep loess capped bluffs, rising more than 60 metres above the bottomland in some places, and forms a natural physiographic region. For much of the length of this part of the valley, the Mississippi is entrenched at the base of the bluffs on the western side of the river, with nearly all the floodplain land on the eastern side of the river. The floodplain of the southern half of the American Bottom is narrow, between four and eight km, whereas the northern half is considerably broader, about 14km at its widest extent (Milner 1998:35; Milner & Oliver 1999). Accounts by nineteenth century explorers, settlers and land surveyors provide some of the clearest description, s of this landscape prior to Anglo-American settlement. One early nineteenth-century traveller wrote of the American Bottom,
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