We measured soil respiration during two winters in three different ecotypes of the BOREAS northern study area. The production of CO₂was continuous throughout the winter and, when totaled for the winter of 1994–1995, was equivalent to the release of ∼40–55 g C/m²from the soil surface. As soils cooled in the early winter, the CO₂ production rate decreased in a manner that appeared to be exponentially related to shallow soil temperatures. This exponential relationship was not observed when soils began to warm, possibly indicating that there may be additional or different processes responsible for increased CO₂ production during winter warming events. We also measured CO₂ concentrations in soil gas and the Δ¹⁴C of the soil CO₂. These measurements show that the CO₂ produced in winter is not simply the return to the atmosphere of the carbon fixed during the previous growing season. We suggest that the wintertime production of CO₂ originates, at least in part, from the decomposition of old organic carbon stored at depth in the soil.