Li Jingjing, Yang Chao
College of Grassland Science, Qingdao Agricultural University, Qingdao, China.
College of Grassland Science and Technology, China Agricultural University, Beijing, China.
PeerJ. 2019 Nov 13;7:e8078. doi: 10.7717/peerj.8078. eCollection 2019.
Soil aggregate-size classes and microbial communities within the aggregates are important factors regulating the soil organic carbon (SOC) turnover. However, the response of soil bacterial and fungal communities in aggregates to litter decomposition in different aggregate-size classes is poorly understand.
Soil samples from un-grazed natural grassland were separated into four dry aggregate classes of different sizes (2-4 mm, 1-2 mm, 0.25-1 mm and <0.25 mm). Two types of plant litter (leaf and stem) of were added to each of the four aggregate class samples. The CO release rate, SOC storage and soil microbial communities were measured at the end of the 56-day incubation.
The results showed that the 1-2 mm aggregate had the highest bacterial Shannon and CO release in CK and leaf addition treatments, and the SOC in the <0.25 mm aggregate was higher than that in the others across the treatments. The relative abundance of Ascomycota was higher in the 2-4 mm and <0.25 mm aggregates than in the 1-2 mm and 0.25-1 mm aggregates in the treatment without litter addition, and the relative abundance of Aphelidiomycota was lower in the 2-4 mm and <0.25 mm aggregates than in the 1-2 mm and 0.25-1 mm aggregates. Also, litter addition increased the relative abundance of Proteobacteria and Bacteroidetes, but decreased the relative abundance of Acidobacteria, Gemmatimonadetes, and Actinobacteria. The relative abundance of Ascomycota and Aphelidiomycota increased by more than 10% following leaf litter addition. The bacterial Shannon index had a significantly positive and direct effect on SOC concentration and CO release, while the fungal Shannon index was significantly correlated with SOC concentration. Our results indicate that the soil bacterial diversity contributes positively to both carbon emissions and carbon storage, whereas soil fungal diversity can promote carbon storage and decrease carbon emissions.
土壤团聚体大小类别以及团聚体内的微生物群落是调节土壤有机碳(SOC)周转的重要因素。然而,不同大小团聚体中土壤细菌和真菌群落对凋落物分解的响应尚不清楚。
从未放牧的天然草地采集土壤样本,将其分为四个不同大小的干团聚体类别(2 - 4毫米、1 - 2毫米、0.25 - 1毫米和<0.25毫米)。将两种类型的植物凋落物(叶和茎)添加到四个团聚体类别样本中的每一个中。在56天培养期结束时测量二氧化碳释放速率、SOC储量和土壤微生物群落。
结果表明,在对照和添加叶片处理中,1 - 2毫米团聚体具有最高的细菌香农指数和二氧化碳释放量,并且在所有处理中,<0.25毫米团聚体中的SOC高于其他团聚体。在不添加凋落物的处理中,2 - 4毫米和<0.25毫米团聚体中子囊菌门的相对丰度高于1 - 2毫米和0.25 - 1毫米团聚体,而2 - 4毫米和<0.25毫米团聚体中无柄菌门的相对丰度低于1 - 2毫米和0.25 - 1毫米团聚体。此外,添加凋落物增加了变形菌门和拟杆菌门的相对丰度,但降低了酸杆菌门、芽单胞菌门和放线菌门的相对丰度。添加落叶后,子囊菌门和无柄菌门的相对丰度增加超过10%。细菌香农指数对SOC浓度和二氧化碳释放有显著的正向直接影响,而真菌香农指数与SOC浓度显著相关。我们的结果表明,土壤细菌多样性对碳排放和碳储存均有积极贡献,而土壤真菌多样性可促进碳储存并减少碳排放。