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Vegetation composition and soil microbial community structural changes along a wetland hydrological gradient

机译:沿湿地水文梯度的植被组成和土壤微生物群落结构变化

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摘要

Fluctuations in wetland hydrology create an interplay between aerobic and anaerobic conditions, controlling vegetation composition and microbial community structure and activity in wetland soils. In this study, we investigated the vegetation composition and microbial community structural and functional changes along a wetland hydrological gradient. Two different vegetation communities were distinguished along the hydrological gradient; Caricetum gracilis at the wet depression and Arrhenatheretum elatioris at the drier upper site. Microbial community structural changes were studied by a combined in situ (CO2)-C-13 pulse labeling and phospholipid fatty acid (PLFA) based stable isotope probing approach, which identifies the microbial groups actively involved in assimilation of newly photosynthesized, root-derived C in the rhizosphere soils. Gram negative bacterial communities were relatively more abundant in the surface soils of the drier upper site than in the surface soils of the wetter lower site, while the lower site and the deeper soil layers were relatively more inhabited by gram positive bacterial communities. Despite their large abundance, the metabolically active proportion of gram positive bacterial and actinomycetes communities was much smaller at both sites, compared to that of the gram negative bacterial and fungal communities. This suggests much slower assimilation of root-derived C by gram positive and actinomycetes communities than by gram negative bacteria and fungi at both sites. Ground water depth showed a significant effect on the relative abundance of several microbial communities. Relative abundance of gram negative bacteria significantly decreased with increasing ground water depth while the relative abundance of gram positive bacteria and actinomycetes at the surface layer increased with increasing ground water depth.
机译:湿地水文学的波动在需氧和厌氧条件之间产生相互作用,从而控制了湿地土壤中的植被组成以及微生物群落结构和活性。在这项研究中,我们调查了沿湿地水文梯度的植被组成以及微生物群落的结构和功能变化。沿水文梯度区分了两个不同的植被群落。湿depression陷的Caricetum gracilis和较干燥的上部部位的Arrhenatheretum elatioris。通过结合原位(CO2)-C-13脉冲标记和基于磷脂脂肪酸(PLFA)的稳定同位素探测方法研究了微生物群落的结构变化,该方法确定了积极参与新光合的,根源C的同化的微生物在根际土壤中。革兰氏阴性细菌群落在较干燥的较高位点的表层土壤中相对比在较湿润的较低位点的表层土壤中相对丰富,而较低位点和较深的土壤层则相对较多地被革兰氏阳性细菌群落居住。尽管它们的丰度很高,但与革兰氏阴性细菌和真菌群落相比,革兰氏阳性细菌和放线菌群落的代谢活性比例要小得多。这表明革兰氏阳性和放线菌群落对根源碳的吸收要比革兰氏阴性细菌和真菌在两个位点的吸收慢得多。地下水深度对几个微生物群落的相对丰度有显着影响。革兰氏阴性细菌的相对丰度随着地下水深度的增加而显着降低,而革兰氏阳性细菌和放线菌在表层的相对丰度则随着地下水深度的增加而增加。

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