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Even in the quiet of winter, microorganisms are hard at work in peatlands, cycling nutrients such as carbon. As a result, during winter, peatlands tend to release carbon dioxide (CO2) through microbial respiration because the plants that absorb CO2 are dormant. In contrast, plants take in CO2, via photosynthesis, during the growing season (GS). These seasonal dynamics generally balance out, with peatlands acting as net CO2 sinks over the course of the year. In Canada, however, winter temperatures are rising faster than other seasons. Warmer winters result in shorter cold periods and longer GSs. While a longer GS may increase the amount of CO2 peatlands absorb, the warmer conditions could also boost microbial activity, potentially offsetting the extra CO2 absorbed by plants. This shift in seasonal dynamics could tip the balance and weaken the ability of peatlands to act as carbon sinks. Understanding these seasonal changes is crucial for predicting how peatlands will respond to a changing climate and provide insights into their potential role as nature-based solutions.