This links to a video introducing the Mukwonago River Oak Barrens, a new project of the Glacial Prairie Chapter of The Prairie Enthusiasts. It discusses the setting, ecological significance, early stewardship, and plans for the future. https://youtu.be/iYZmadm-rug
See the recent open access article by Tulowieki, Hanberry, and Abrams linked here. It offers insights, I think, into how we might assess vulnerability of northeastern and upper midwestern oak ecosystems to climate change and into the human relationships needed to sustain them.
“The results revealed a consistently and often significantly greater abundance of fireadapted (mainly oak) taxa near Indigenous settlements (Tables S1–S3). The relative abundances near Indigenous settlements were high for the last five millennia (Figure 3) for oak (median 74–82% from pollen-based reconstructions) and combined pyrophilic (median 86–91%), supporting the notion that Indigenous burning maintained fire-tolerant taxa through climatic changes that would have otherwise benefitted taxa adapted to cooler and/or moister climates [11,85]. These results occurred using different representations of Indigenous settlements, using pollen-based and land survey record-based estimates of relative abundance, analysing at two different resolutions (8 km and 24 km), and analysing various timesteps. Abundances of fire-tolerant vegetation showed greater consistency over time where Indigenous settlements existed and with greater fluctuations elsewhere (Figure 3), suggesting that the sustained presence of Indigenous settlements over millennia stabilised oak-dominated forests. For example, during the regional cooling of the Little Ice Age circa 13th–19th centuries, pyrophilic abundance was still 86–90% in the cells with archaeological sites, versus 66–70% in the cells without. Abundance decreased from previous timesteps in cells without archaeological sites during this time (Figure 3). Indeed, the results show a slight decreasing trend in pyrophilic and oak abundance throughout the region where there were no archaeological sites, perhaps suggesting post-glacial infilling of more mesic species away from Indigenous settlement. The drop in pyrophilic abundance from 1495 to 1745 CE may manifest the effects of an Indigenous depopulation and reductions in cultural burning (Figures 2 and 3).”
White oak and associated old-growth herbaceous sod in a remnant SE WI oak woodland.
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