The carbon density and production were measured using both forest inventory and allometry approaches in the declining valley sprucefir forest in Xiaoxing’an Mountains. Results showed that the total carbon density of the forest was 268.14 t C·hm-2 in 2011, and carbon densities of the vegetation, detritus and soil were 74.25, 16.86 and 177.03 t C·hm-2, respectively. From 2006 to 2011, tree layer carbon density decreased from 80.86 t C·hm-2 to 71.73 t C·hm-2. The average decrease proportions per year of carbon density were 0.5%, 1.2%, 2.7% and 3.7% for Abies nephrolepis, Betula platyphylla, Picea spp., and Larix gmelinii, respectively. However, carbon densities were increased by 2.9%, 3.9% and 7.2% per year for Alnus sibirica, Pinus koraiensis and Acer ukurunduense, respectively. Net primary production (NPP) of the forest was 4.69 t C·hm-2·a-1. The ratio of belowground NPP to aboveground NPP was 0.56. Litterfall accounted for the largest proportion of the NPP of forest with a value of 34.5%. As the two most important carbon output approaches of forest ecosystems, the fluxes of heterotrophic respiration and coarse woody debris decomposition were 293.67 and 119.29 g C·m-2·a-1, respectively. Net ecosystem production (NEP) of the forest was 55.90 g C·m-2·a-1. The results indicated that the valley sprucefir forest in the declining state still had a certain carbon sink capacity.