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Maximum carbon stock was reported from natural forest site (131.8 Mg ha− 1).
The estimated asymptotic maximum carbon stock in the stands increased to 484 (±26) Mg C ha−1 with the inclusion of dead-tree carbon (Table 1) Dead trees in unthinned plots typically represent suppression mortality as tree density decreases through time.
The maximum carbon stock was present in Quercus leucotrichophora forest soils.
In Quercus leucotrichophora forest soils (Table 3), the maximum carbon stock was present in site-I (185.6 t C ha-1) and minimum in site-III (160.8 t C ha-1).
The estimated asymptotic maximum carbon stock in the stands increased to 484 (±26) Mg C ha−1 with the inclusion of dead-tree carbon (Table 1) Dead trees in unthinned plots typically represent suppression mortality as tree density decreases through time.
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Our estimate of peat carbon storage exceeds the 21.6 GtC maximum estimated carbon stock in above- and belowground biomass of all Indonesian forests by 30%[51]], an observation similarly noted by Dommain et al. [9].
In effect, the right side of the distribution indicates maximum potential carbon stocks in the lowlands, which exceeded 200 Mg C ha-1.
(XLSX 18 KB) 13021_2013_95_MOESM2_ESM.xlsx Additional file 2 A comparison of the mean, median, maximum and total carbon stock by country in three datasets: RS1[15], RS2[16] and the FAO Forest Resource Assessment (FRA) 2010.
The higher percent of soil organic carbon in Quercus leucotrichophora forest may be due to dense canopy and higher input of litter which results in maximum storage of carbon stock.
In Quercus leucotrichophora forest soils (Table 3), the maximum and minimum values of carbon stock was 185.6 t C ha-1 (site-I) and 160.8 t C ha-1 (site-III) respectively.
Only slight differences in carbon stock (absolute difference between maximum and minimum value:1604 gC m-2) were found between the three land uses with the highest carbon stocks and that may be either because of differences in plant biodiversity, differences in bulk densities of the soils studied or slight differences in local climatic regimes.
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