Assessing the impact of land-use changes on soil respiration (R S ) is of vital significance to understand the interactions between belowground metabolism and regional carbon budgets. In this study, the monthly in situ R S was examined between 09:00 and 12:00 hours over a 3-year period within a representative land-use sequence in the subtropical region of China. The land-use sequence contained natural forest (control treatment), secondary forest, two plantations, citrus orchard and sloping tillage land. Results showed that the R S exhibited a distinct seasonal pattern, and it was dominantly controlled by the soil temperature. After the land-use conversion, the apparent temperature sensitivity of R S (Q 10 ) was increased from 2.10 in natural forest to 2.71 in sloping tillage land except for an abnormal decrease to 1.66 in citrus orchard. Contrarily, the annual R S was reduced by 32% following the conversion of natural forest to secondary forest, 46-48% to plantations, 63% to citrus orchard and 50% to sloping tillage land, with the average reduction of 48%. Such reduction of annual R S could be explained by the decrease of topsoil organic carbon and light-fraction organic carbon storages, live biomass of fine root ( o2 mm) and annual litter input, which indirectly/directly correlated with plant productivity. Our results suggest that substrate availability (e.g., soil organic carbon and nutrients) and soil carbon input (e.g., fine root turnover and litterfall) through plant productivity may drive the R S both in natural and managed ecosystems following strong disturbance events.

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China manages the largest monoculture plantations in the world, with 24% being Chinese fir plantations. Maximizing the ecosystem services of Chinese fir plantations has important implications in global carbon cycle and biodiversity protection. Assisted natural regeneration (ANR) is a practice to convert degraded lands into more productive forests with great ecosystems services. However, the quantitative understanding of ANR ecosystem service benefits is very limited. We conducted a comprehensive field manipulation experiment to evaluate the ANR potentials. We quantified and compared key ecosystem services including surface runoff, sediment yield, dissolved organic carbon export, plant diversity, and aboveground carbon accumulation of ANR of secondary forests dominated by Castanopsis carlesii to that of Chinese fir and C. carlesii plantations. Our results showed that ANR of C. carlesii forest reduced surface runoff and sediment yield up to 50% compared with other young plantations in the first 3 years and substantially increased plant diversity. ANR also reduced the export of dissolved organic carbon by 60–90% in the first 2 years. Aboveground biomass of the young ANR forest was approximately 3–4 times of that of other young plantations, while aboveground biomass of mature ANR forests was approximately 1.4 times of that of mature Chinese fir plantations of the same age. If all Chinese fir plantations in China were replaced by ANR forests, potentially 0.7 Pg more carbon will be stored in aboveground in one rotation (25 years). The results indicate that ANR triggers positive feedbacks among soil and water conservation, biodiversity protection, and biomass accumulation and thereby enhances ecosystem services.

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Partitioning of soil CO 2 flux (FS) into autotrophic and heterotrophic components depends on how the plant carbon is allocated above-vs. belowground and how the belowground carbon is allocated for respiration and production of roots and their microbial associations. Data of litterfall (FA), root respiration (FR), and FS of world old-growth or mature forests (C45 ages) were compiled, and the relationship between carbon allocation above-vs. belowground (indexed as the FA/FS ratio) and FS partitioning (indexed as the FR/FS ratio) was examined. The FA/FS ratio ranged from 0.08 to 0.64 and was positively correlated with mean annual air temperature and mean annual precipitation. The ratio increased from boreal to temperate to tropical forests, and was higher in broadleaved forests than in coniferous forests. Site-specific belowground carbon use efficiency (BCUE, root production per unit carbon used by roots and microbial associations) varied from 0.10 to 0.87, contrasting with the common assumption of a constant BCUE. Sitespecific FR/FS ranged from 0.09 to 0.71 and increased with FS due to a decrease in BCUE. Deciduousness had a significant effect on the FR/FS ratios, with FR/FS ratios greater in deciduous forests than in evergreen forests. Methods of separating root respiration from soil heterotrophic respiration had a significant effect on estimated FR/FS. The estimated FR/FS ratio was negatively related to the FA/FS ratio, indicating that factors favouring carbon allocation belowground over aboveground will increase the autotrophic contribution to total soil respiration. The relatively low explaining power (r 2 = 0.270) of this relationship resulted from deviations from assumptions of constant BCUE and a near steady-state belowground pools.

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Land use/cover change (LUCC) is widely recognized as one of the most important driving forces of global carbon cycles. The influence of converting native forest into plantations, secondary forest, orchard and arable land on stores and quality of soil organic carbon (SOC) was investigated in mid-subtropical mountainous area of southern China. The results showed that LUCC had led to great decreases in SOC stocks and quality. Considerable SOC and light-fraction organic carbon (LFOC) had been stored in the native forest (142.2 t hm −2 and 14.8 t hm −2 respectively). When the native forest was converted to plantations, secondary forest, orchard and arable land, the SOC stocks decreased by 25.6%, 28.7%, 38.0%, 31.8% and 51.2%, respectively. The LFOC stocks decreased by 52.2% to 57.2% when the native forest was converted to woodland plantations and secondary forest, and by 82.1% to 84.2% when converted to economic plantation, orchard and arable land. After the conversion, the ratios of LFOC to SOC (0-60 cm) decreased from 13.3% to about 3.0% to 10.7%. The SOC and LFOC stored at the upper 20 cm were more sensitive to LUCC when compared to the subsurface soil layer. Also, the decline in carbon storage induced by LUCC was greater than the global average level, it could be explained by the vulnerable natural environment and special human management practices. Thus, it is wise to enhance soil carbon sequestration, mitigate elevated atmospheric CO 2 and develop ecological services by protecting vulnerable environment, restoring vegetation coverage, and afforesting in mountainous area in mid-subtropics.