首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Response of soil microbial respiration of tidal wetlands in the Yangtze River Estuary to different artificial disturbances
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Response of soil microbial respiration of tidal wetlands in the Yangtze River Estuary to different artificial disturbances

机译:长江口潮汐湿地土壤微生物呼吸对不同人工干扰的响应

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摘要

To clarify the effects of artifical disturbances on the soil microbial respiration (SMR) of existed tidal wetlands, the SMR of three typical areas in Chongming Dongtan and Jiuduansha of the Yangtze River Estuary, China, were evaluated. The causes of the differences in the SMR were also evaluated by analyzing the microbial activity factors and community structure, as well as the physical-chemical characteristics of the different wetland soils. The results showed that the SMR of the existed wetlands in the area of siltation promotion was significantly higher (P < 0.01) than that of the natural area. Different agricultural practices on the inner land also affected the SMR of the tidal wetlands. Overall, the results indicated that the difference in soil microbial characteristics between the artificially disturbed and natural tidal wetlands may be the primary cause of their different SMR. Path analysis indicated that the correlation between soil bacterial diversity and SMR were especially strong. Phylogenetic analysis showed that the bacterial microbial community structure in wetland soil that had been subject to artificial disturbance was changed due to the alteration of the soil physicochemical characteristics, and Pseudomonas sp., Bacillus sp., Uncultured Lactococcus sp. and Streptococcus sp., which have high heterotrophic metabolism or stress tolerance capability, became the dominant bacterial flora in the artificially disturbed wetland soil, ultimately strengthening the SMR. This may be the essential cause of the higher SMR in wetland soils that have been subjected to artificial disturbance, resulting in a low organic carbon accumulation capability.
机译:为了阐明人为干扰对现有潮汐湿地土壤微生物呼吸(SMR)的影响,对长江口崇明东滩和九段沙三个典型地区的SMR进行了评估。通过分析微生物活性因子和群落结构以及不同湿地土壤的理化特性,评估了SMR差异的原因。结果表明,淤积促进区中现有湿地的SMR比自然区高(P <0.01)。内陆地区不同的农业实践也影响了潮湿地的SMR。总体而言,结果表明,人为干扰和自然潮汐湿地之间土壤微生物特征的差异可能是造成其SMR不同的主要原因。通径分析表明,土壤细菌多样性与SMR之间的相关性特别强。系统发育分析表明,受到人工干扰的湿地土壤中的细菌微生物群落结构由于土壤理化性质的改变而发生了变化,假单胞菌(Pseudomonas sp。),芽孢杆菌(Bacillus sp。),未培养的乳球菌(Lactococcus sp。)具有高异养代谢或抗逆能力的链球菌和链球菌已成为人为干扰的湿地土壤中的优势细菌菌群,最终增强了SMR。这可能是受到人工干扰的湿地土壤中较高SMR的根本原因,导致有机碳累积能力低。

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