No abstract

China's croplands have experienced drastic changes in management practices, such as fertilization, tillage, and residue treatments, since the 1980s. There is an ongoing debate about the impact of these changes on soil organic carbon (SOC) and its implications. Here we report results from an extensive study that provided direct evidence of cropland SOC sequestration in China. Based on the soil sampling locations recorded by the Second National Soil Survey of China in 1980, we collected 4,060 soil samples in 2011 from 58 counties that represent the typical cropping systems across China. Our results showed that across the country, the average SOC stock in the topsoil (0-20 cm) increased from 28.6 Mg C ha in 1980 to 32.9 Mg C ha in 2011, representing a net increase of 140 kg C ha year However, the SOC change differed among the major agricultural regions: SOC increased in all major agronomic regions except in Northeast China. The SOC sequestration was largely attributed to increased organic inputs driven by economics and policy: while higher root biomass resulting from enhanced crop productivity by chemical fertilizers predominated before 2000, higher residue inputs following the large-scale implementation of crop straw/stover return policy took over thereafter. The SOC change was negatively related to N inputs in East China, suggesting that the excessive N inputs, plus the shallowness of plow layers, may constrain the future C sequestration in Chinese croplands. Our results indicate that cropland SOC sequestration can be achieved through effectively manipulating economic and policy incentives to farmers.

ABSTRACTSoils were incubated for 80 days in a continuously labeled14CO2atmosphere to measure the amount of labeled C incorporated into the microbial biomass. Microbial assimilation of14C differed between soils and accounted for 0.12% to 0.59% of soil organic carbon (SOC). Assuming a terrestrial area of 1.4 × 108km2, this represents a potential global sequestration of 0.6 to 4.9 Pg C year−1. Estimated global C sequestration rates suggest a “missing sink” for carbon of between 2 and 3 Pg C year−1. To determine whether14CO2incorporation was mediated by autotrophic microorganisms, the diversity and abundance of CO2-fixing bacteria and algae were investigated using clone library sequencing, terminal restriction fragment length polymorphism (T-RFLP), and quantitative PCR (qPCR) of the ribulose 1,5-bisphosphate carboxylase/oxygenase (RubisCO) gene (cbbL). Phylogenetic analysis showed that the dominantcbbL-containing bacteria wereAzospirillum lipoferum,Rhodopseudomonas palustris,Bradyrhizobium japonicum,Ralstonia eutropha, andcbbL-containing chromophytic algae of the generaXanthophytaandBacillariophyta. Multivariate analyses of T-RFLP profiles revealed significant differences incbbL-containing microbial communities between soils. Differences incbbLgene diversity were shown to be correlated with differences in SOC content. Bacterial and algalcbbLgene abundances were between 106and 108and 103to 105copies g−1soil, respectively. BacterialcbbLabundance was shown to be positively correlated with RubisCO activity (r= 0.853;P< 0.05), and bothcbbLabundance and RubisCO activity were significantly related to the synthesis rates of [14C]SOC (r= 0.967 and 0.946, respectively;P< 0.01). These data offer new insights into the importance of microbial autotrophy in terrestrial C cycling.

No abstract

No abstract

The effect of long-term fertilization on soil-denitrifying communities was determined by measuring the abundance and diversity of the nitrite reductase genes nirK and nirS. Soil samples were collected from plots of a long-term fertilization experiment started in 1990, located in Taoyuan (110°72″ E, 28°52″ N), China. The treatments were no fertilizer (NF), urea (UR), balanced mineral fertilizers (BM), and BM combined with rice straw (BMR). The abundance, diversity, and composition of the soil-denitrifying bacteria were determined by using real-time quantitative PCR, terminal restriction fragment length polymorphism (T-RFLP), and cloning and sequencing of nirK and nirS genes. There was a pronounced difference in the community composition and diversity of nirK-containing denitrifiers responding to the long-term fertilization regimes; however, less variation was observed in communities of nirS-containing denitrifiers, indicating that denitrifiers possessing nirK were more sensitive to the fertilization practices than those with nirS. In contrast, fertilization regimes had similar effects on the copy numbers of nirK and nirS genes. The BMR treatment had the highest copy numbers of nirK and nirS, followed by the two mineral fertilization regimes (UR and BM), and the lowest was in the NF treatment. Of the measured soil parameters, the differences in the community composition of nirK and the abundance of nir denitrifiers were highly correlated with the soil carbon content. Therefore, long-term fertilization resulted in a strong impact on the community structure of nirK populations only, and total organic carbon was the dominant factor in relation to the variations of nir community sizes.

No abstract

No abstract