Northern peatlands store approximately one third of global soil carbon, namely around 500 gigatons.
Northern peatlands store approximately one third of global soil carbon, namely around 500 gigatons. Because the peatland carbon cycling is largely controlled by partly anaerobic soil conditions, the carbon stored in these soils is extremely vulnerable to climate warming that is expected to reduce soil moisture and therefore increase soil aeration. Understanding the interactions between warming and soil moisture is particularly important in peatland types found in boreal and arctic areas expected to experience high rates of climate warming. This region happens to be the core area for northern peatlands and therefore increased mineralization could have high potential to further accelerate climate change.
A new study led by researchers from the University of Eastern Finland and Natural Resources Institute Finland suggests that peatland CO2 exchange is more strongly influenced by drying than warming as such, and that soil moisture may be critical to determining whether fen ecosystems are able to adapt to a changing climate. The study was recently published in Global Change Biology – a leading journal in environmental science.
Read more at University of Eastern Finland
Image: Small scale water level drawdown had a stronger impact on sedge fen CO2 exchange than warming induced by open top chambers. (Credit: Timo Penttilä)
