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中国河口潮汐湿地中的微生物坏死物质碳:影响因素与环境意义

Microbial necromass carbon in estuarine tidal wetlands of China: Influencing factors and environmental implication.

作者信息

Wei Jine, Zhang Fenfen, Ma Dongliang, Zhang Jing, Zheng Yanling, Dong Hongpo, Liang Xia, Yin Guoyu, Han Ping, Liu Min, Hou Lijun

机构信息

State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China.

State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China.

出版信息

Sci Total Environ. 2023 Jun 10;876:162566. doi: 10.1016/j.scitotenv.2023.162566. Epub 2023 Mar 6.

Abstract

Microbial necromass is an important component of the stable soil organic carbon (SOC) pool. However, little is known about the spatial and seasonal patterns of soil microbial necromass and their influencing environmental factors in estuarine tidal wetlands. In the present study, amino sugars (ASs) as biomarkers of microbial necromass were investigated along the estuarine tidal wetlands of China. Microbial necromass carbon (C) contents were in the range of 1.2-6.7 mg g (3.6 ± 2.2 mg g, n = 41) and 0.5-4.4 mg g (2.3 ± 1.5 mg g, n = 41), which accounted for 17.3-66.5 % (44.8 % ± 16.8 %) and 8.9-45.0 % (31.0 % ± 13.7 %) of the SOC pool in the dry (March to April) and wet (August to September) seasons, respectively. At all sampling sites, fungal necromass C predominated over bacterial necromass C as a component of microbial necromass C. Compared to bacterial necromass C, fungal necromass C showed a stronger connection with ferrous oxides (Fe) and total Fe concentrations. Both fungal and bacterial necromass C contents revealed large spatial heterogeneity and declined in the estuarine tidal wetlands with the increase in latitude. Statistical analyses showed that the increases in salinity and pH in the estuarine tidal wetlands suppressed the accumulation of soil microbial necromass C.

摘要

微生物残体是土壤稳定有机碳(SOC)库的重要组成部分。然而,对于河口潮汐湿地土壤微生物残体的空间和季节模式及其影响环境因素,我们知之甚少。在本研究中,沿着中国河口潮汐湿地对作为微生物残体生物标志物的氨基糖(ASs)进行了调查。微生物残体碳(C)含量在1.2 - 6.7 mg g(3.6 ± 2.2 mg g,n = 41)和0.5 - 4.4 mg g(2.3 ± 1.5 mg g,n = 41)范围内,分别占旱季(3月至4月)和雨季(8月至9月)SOC库的17.3 - 66.5%(44.8% ± 16.8%)和8.9 - 45.0%(31.0% ± 13.7%)。在所有采样点,作为微生物残体碳的一个组成部分,真菌残体碳在数量上超过细菌残体碳。与细菌残体碳相比,真菌残体碳与氧化亚铁(Fe)和总铁浓度的联系更强。真菌和细菌残体碳含量均表现出较大的空间异质性,且在河口潮汐湿地中随纬度增加而下降。统计分析表明,河口潮汐湿地盐度和pH值的升高抑制了土壤微生物残体碳的积累。

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