The geographic extent and role of Native American land use in modifying past forests in eastern North America remains a contested issue (Whitney 1996; Bowman et al. 2011; Abrams and Nowacki 2020). Native Americans have utilized various strategies to boost the productivity of the land, such as via in-place promotion of perennial plant species, creation of habitats for game, and transplantation of favored plant species (Doolittle 2002; Abrams and Nowacki 2008; Smith 2011). Most importantly, Native Americans ignited low-intensity surface fires in forests, woodlands, and grasslands for the many benefits it provided with respect to food procurement and travel (Williams 2000), unlike current forest management that maximizes for maximizing number of trees and forest products. Understanding cultural burning by Native Americans has major implications for modern forest management and policy decisions. It relates to broader debates over whether to preserve lands in an unmanaged state or conserve lands via sustainable human use (Foreman 2014), and whether to manage lands to promote carbon sequestration (e.g. Oswald et al., 2020) or mimic cultural burning to restore fire-dependent ecological communities (e.g. Ryan et al., 2013). Researchers have implicated suppression of cultural burning in the decline of drought- and fire-tolerant trees (e.g. oak, Quercus spp.) and increase in drought- and fire-intolerant trees (e.g. maple, Acer spp.) throughout eastern North America (Abrams 1998; Nowacki and Abrams 2008), but other causes have also been considered (McEwan et al. 2011; Hanberry et al. 2020). For Native American communities, past cultural fire regimes can inform present-day management on their territories to counteract post-colonial alterations to ecosystems, support traditional plants, reestablish sovereignty over their land, and foster community wellbeing (Adlam et al. 2022).
Providing physical evidence of past cultural burning, tree-ring fire-scar records (FSRs) have allowed researchers to establish fire chronologies, estimate fire return intervals, and determine the seasonality of fire during Native American occupation (Abrams et al. 2022; Margolis et al. 2022). As summarized by Margolis et al. (2022), fire scars result from non-lethal injuries to tree trunks that kill the cambial cells that are covered by subsequent growth; fire scars typically occur in low- to moderate-severity fires, or along the outskirts of high-severity fires. Findings from fire-scar chronologies suggest cultural burning in eastern North America with fire return intervals as low as roughly 3 to 6 years, as ascertained in a meta-analysis (Abrams et al. 2022). If estimated from an unbiased sample, these intervals may be viewed as maximum estimates in locations where frequent low-severity fires occur, since such fires may injure few to no trees, and since fire scars are rare from consecutive annual burns due to lower fuel loads in the second year (McEwan et al. 2007). However, elsewhere studies have suggested that fire return intervals are artificially short due to bias in sampling procedures that favors fire-scarred trees (Baker and Ehle 2001) and fire-prone vegetation types (Matlack 2013). In the eastern US, the presence of fire scars where lightning ignitions are rare year-round, as well as scars during the dormant season when lightning is uncommon, suggest anthropogenic ignition sources. FSRs complement other historical and physical records in studying Native American use of fire such as fossil pollen (e.g. Munoz & Gajewski, 2010), fossil charcoal (e.g. Oswald et al., 2020), firsthand historical accounts (e.g. Scherjon et al., 2015; Tulowiecki et al., 2020), and early land survey records (e.g. Fulton II & Yansa, 2019).
Recently efforts have compiled FSRs into the North American Fire-Scar Network (NAFSN; Margolis et al., 2022). Margolis et al. (2022) explored the spatial representativeness of records in the NAFSN with respect to environmental conditions such as forest type, elevation, slope, aspect, elevation, and climate variables. In a more limited analysis, the same paper informally compared the locations of FSRs to Native American geography, such as the location of former Indigenous territories and date of land-use transitions from Indigenous to white tenure. However, their analysis lacked analysis at a finer spatial resolution, e.g. a comparison of the locations of FSR sites with contemporaneous Native American settlement locations, to reveal whether FSRs collectively and adequately represent locations near and far from settlement.
Understanding the geography of cultural burning requires description of Native American settlement (e.g. villages, camps, travel corridors) relative to FSRs, both at continental scales (captured by an entire fire-scar network) and at local scales (captured in individual fire-scar studies). Geographic contextualization relative to Native American settlement would serve to develop better understanding of where burning occurred: such as whether burning occurred close to population centers and travel routes, and whether burning was typified by selective patch burning or broadcast burning over large geographic extents. For example, one model of burning proposes that burning occurred most frequently near Native American villages and within barrens driven by geology or other microsite characteristics (Matlack 2013); other studies have proposed the “yard and corridor” model whereby burning occurred away from villages in patches that were connected by travel corridors similarly maintained by fire (Lewis and Ferguson 1988; Larson et al. 2021). Better geographic contextualization of FSR-based results relative to Native American settlement would also help quantify the geographic extent of cultural burning.
In this paper, we first assess whether FSRs in the NAFSN are located close to Native American settlement and across a range of Native American territories, prior to their dispossession by Euro-Americans. We then assess whether studies using or developing FSRs provide adequate geographic contextualization of their study sites with respect to Native American geography. Finally, we assess what relationships exist between Native American settlement and fire frequency as gleaned from available FSR-based studies. As a case study we focus on circa late 18th and early 19th century Native American settlement since cultural burning during this time is reasonably expected to be captured in FSRs, and since research has mapped features of Native American settlement such as village locations during this time. The study region is eastern North America defined as temperate forest and northern mixed woods of the eastern United States and southeastern Canada (Omernik 1987; United States Environmental Protection Agency 2022). We are not aware of any review of FSRs and related studies making such an investigation.
We hypothesize that FSRs do not collectively capture cultural burning near settlement, and that individual studies utilizing FSRs do not adequately contextualize their study sites against Native American settlement features. A past synthesis paper has called for improved data on past human fire regimes to accommodate cross-cultural analysis globally and to enhance understanding of different cultures’ use of fire (Bowman et al. 2011). In that light, should this study’s hypotheses be accepted, it would motivate targeted development of FSRs in former Native American territories underrepresented by the fire-scar record, and improved description of Native American geography in future studies using such records.