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Changes in the soil microbial community structure with latitude in eastern China, based on phospholipid fatty acid analysis

机译:基于磷脂脂肪酸分析的中国东部土壤微生物群落结构随纬度的变化

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摘要

Phospholipid fatty acid (PLFA) profiles were measured in soils from 14 sites in eastern China representing typical geographic zones of varying latitude from north (47.4pN) to south (21.4pN). Amounts of soil microbial biomass, measured as total amounts of PLFAs, showed no regular trend with latitude, but were positively correlated with soil organic carbon content, the concentration of humic acid and amorphous iron oxide. Soil microbial community structure showed some biogeographical distribution trends and was separated into three groups in a cluster analysis and principal coordinate analysis of log transformed PLFA concentrations (mol%). Soils in the first group came from northern China with medium mean annual temperature (1.2-15.7pC) and rainfall (550-1021mm). Soils in the second group originated from southern China with a relatively higher mean annual temperature (15.7-21.2pC) and rainfall (1021-1690mm). Soils clustered in the third group originated from the most southerly region. The northern soils contained relatively more bacteria and Gram-negative PLFAs, while the southern soils had more fungi and pressure indexed PLFAs. These differences in soil microbial community structure were largely explained by soil pH, while other site and soil characteristics were less important.
机译:在中国东部14个站点的土壤中测量了磷脂脂肪酸(PLFA)的分布,这些站点代表了从北(47.4pN)到南(21.4pN)不同纬度的典型地理区域。以PLFAs总量衡量的土壤微生物生物量的量,随纬度呈无规律变化,但与土壤有机碳含量,腐殖酸和无定形氧化铁浓度呈正相关。土壤微生物群落结构表现出一定的生物地理分布趋势,并通过聚类分析和对数转化PLFA浓度(mol%)的主坐标分析分为三类。第一组土壤来自中国北方,年平均气温(1.2-15.7pC)和降雨(550-1021mm)中等。第二组土壤起源于中国南部,年平均温度(15.7-21.2pC)和降雨(1021-1690mm)相对较高。在第三组中聚集的土壤起源于最南端的地区。北部土壤含有相对较多的细菌和革兰氏阴性PLFA,而南部土壤则具有更多的真菌和压力指数PLFA。土壤微生物群落结构的这些差异主要由土壤pH值解释,而其他部位和土壤特性则不那么重要。

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