Purpose
Winter snow cover is a key control over soil biogeochemical cycles in cold biomes but has decreased with climate warming, particularly in high-latitude and high-altitude areas. Previous studies have found a decline in carbon (C) release from decomposing litter without snow cover, yet partitioning of what C fractions in response to snow removal remains not fully understood.
Methods
Here we incubated fir and birch litter in microcosms over two years of decomposition in an alpine forest to assess the release of various C fractions with and without snow cover using 13C nuclear magnetic resonance (NMR).
Results
We found that 51% and 61% of total C were lost from fir and birch litter, respectively, after two years of decomposition, and 59% and 60% of these C were decomposed during winter time. More C was lost from both fir and birch litter under snow cover, and the decomposition rate of birch litter C was decreased by 50% after snow removal. However, only O-alkyl C (particularly carbohydrate C) release was reduced with snow removal, and the release of other C fractions (i.e., alkyl C, aromatic C and carbonyl C) did not change significantly after removing snow cover. Reduction in O-alkyl C release from fir and birch litter was in accordance with the declines in soil dissolved organic C, invertase activity and microbial respiration rate under removed snow plots.
Conclusion
We conclude that a reduction in winter snow cover regulates early decomposition of plant litter by controlling the rapid release of more labile C fractions in seasonally snow-covered ecosystems.