Abstract
Patterns of biomass and carbon (C) storage distribution across Chinese pine (Pinus tabulaeformis) natural secondary forests are poorly documented. The objectives of this study were to examine the biomass and C pools of the major ecosystem components in a replicated age sequence of P. tabulaeformis secondary forest stands in Northern China. Within each stand, biomass of above- and belowground tree, understory (shrub and herb), and forest floor were determined from plot-level investigation and destructive sampling. Allometric equations using the diameter at breast height (DBH) were developed to quantify plant biomass. C stocks in the tree and understory biomass, forest floor, and mineral soil (0–100 cm) were estimated by analyzing the C concentration of each component. The results showed that the tree biomass of P. tabulaeformis stands was ranged from 123.8 Mg·ha–1 for the young stand to 344.8 Mg·ha–1 for the mature stand. The understory biomass ranged from 1.8 Mg·ha–1 in the middle-aged stand to 3.5 Mg·ha–1 in the young stand. Forest floor biomass increased steady with stand age, ranging from 14.9 to 23.0 Mg·ha–1. The highest mean C concentration across the chronosequence was found in tree branch while the lowest mean C concentration was found in forest floor. The observed C stock of the aboveground tree, shrub, forest floor, and mineral soil increased with increasing stand age, whereas the herb C stock showed a decreasing trend with a sigmoid pattern. The C stock of forest ecosystem in young, middle-aged, immature, and mature stands were 178.1, 236.3, 297.7, and 359.8 Mg C ha–1, respectively, greater than those under similar aged P. tabulaeformis forests in China. These results are likely to be integrated into further forest management plans and generalized in other contexts to evaluate C stocks at the regional scale.
Highlights
Biomass and carbon (C) storage in forest ecosystems play dominant roles in global C cycle [1,2,3,4], and serve as the most significant C sinks to reduce global warming [5]
Biomass of ecosystem components Based upon the power regression equations of tree components (Table 2), the biomass were estimated for all P. tabulaeformis forests (Table 3)
We found that the total C stock of forest floor increased with stand age
Summary
Biomass and carbon (C) storage in forest ecosystems play dominant roles in global C cycle [1,2,3,4], and serve as the most significant C sinks to reduce global warming [5]. This is largely due to their huge potential for sequestering carbon in vegetation and soil [6,7,8,9], and interact with atmospheric processes through the absorption and respiration of CO2 [2,10,11]. There is a need for accurate information concerning the biomass and C storage in forest ecosystems to improve our understanding in processes and mechanisms of the global C cycle
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