was observed in Deer Park Township on 2026-10-18, recorded multiple times in October.1 This native conifer is listed as threatened in Illinois and declining across its eastern range due to white pine blister rust and other pathogens, making its presence in local woodlands significant for tracking remnant populations.1
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Early September adds a second load on top of the first. Leaves are beginning to drop into the channels. In a stream that is flowing, that litter gets torn apart and carried downstream by caddisflies, stoneflies and mayfly larvae, the shredders that do most of the work in a forested headwater. In a stream that has stopped moving, breakdown falls mostly to bacteria and fungi. The leaves rot in place and pull oxygen out of the same pools the heat is already squeezing. The bedrock underneath most of this lowland is old metavolcanic and metasedimentary rock with almost no limestone, so the streams have little chemical capacity to buffer anything that concentrates as the water shrinks.
The trees are the other place to look. True fall color comes on gradually, at about the same time each year for a given species, and moves through the whole canopy. Drought damage looks different. It shows up weeks early, patchy, one branch or one side of the tree first, with scorched brown leaf margins and leaves dropping before they finish turning. On
and
that is browning from the leaf tips inward. On
it is rust-colored branch tips where needles have died. A maple that goes brown and drops in early September has not had an early autumn. It has sealed off leaves it can no longer afford to keep, and the nutrients in those leaves are lost rather than drawn back into the wood.
What breaks the pattern is rain, enough of it to reconnect the pools and put the riffles back to work before the water cools on its own schedule. Until then the streams of this lowland are running a deficit that started in August and is compounding into September.
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