An Environment Transitional Zone Buffers Peatlands Carbon Loss
Abstract An environment transitional zone (ETzone) is usually deemed as a hotspot in biogeochemical cycle, but little is known about its response to climate change. A typical ETzone develops at the subsurface of peatland after experiencing long-term water table fluctuation, characterized by alternative aerobic and anaerobic conditions. By an extensive incubation, we found that the CO2 emission at this ETzone was 28.31 ± 3.55 μg g-1 d-1, 41.6% and 34.4% lower than the upper (aerobic) and lower (anaerobic) layers, respectively. Moreover, with a lowest Q10 of 1.37, its CO2 emission was also the least warming-responsive, which could reduce 33.7% CO2 loss in warming scenario. This result clearly revealed that the ETzone worked as a buffer to retard carbon loss, rather than a hotspot. Surprisingly, this buffer capacity of ETzone was easily collapse if being primed by fresh carbon. Therefore, maintaining a relatively stable ETzone is critical for protecting peatland carbon stock, and the priority is to block priming effect through maintaining an intact vegetation composition.