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Warming experiments turn Minnesota peat bogs from carbon sinks into emitters in three years

Researchers heating a Minnesota peatland found that even modest temperature rises caused the ecosystem to switch from storing to releasing carbon within three years.

In a large-scale field study, Oak Ridge National Laboratory researchers warmed peatland enclosures in Minnesota's Marcell Experimental Forest by up to 9 °C, some with added carbon dioxide. Within three years, all heated plots reversed from carbon sinks to sources, releasing carbon dioxide and methane at rates up to twenty times faster than past accumulation. The transition occurred even at the lowest temperature increase of roughly 4 °F, showing a strong linear link between heat and carbon loss.

Declining sphagnum moss, a key carbon-storing species, contributed significantly to the net emissions. The findings, published in AGU Advances, suggest that rising temperatures could rapidly turn peatlands into major greenhouse-gas sources worldwide.

Why it matters

Peatlands store a third of global soil carbon; their rapid shift to emissions could accelerate climate warming.

In this story

peatland warmingcarbon emissionssphagnum mossclimate feedbackgreenhouse gasesSPRuce experimentsoil carbon storage
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