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首页> 外文期刊>Journal of arid environments >Evolution of organic carbon pools and microbial diversity in hyperarid anthropogenic soils
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Evolution of organic carbon pools and microbial diversity in hyperarid anthropogenic soils

机译:高干旱人为土壤中有机碳库的演化和微生物多样性

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We investigated the organic carbon pools and the microbial diversity and activity in anthropogenic terraced soils in a desert area of Southern Peru to highlight how the introduction of agriculture influences carbon evolution and storage and genetic and functional diversity of soil microbiota over time. Five sites were selected considering soils cultivated since 5, 15, 20, 35 and 65 years, sampled along the profile depth (0-20 and 20-40 cm layer). Soil and microbial parameters comprised by organic carbon pools, microbial respiration, microbial community physiological profile (CLPP) and microbial diversity (PCR-DGGE) were determined. The results showed that the highest C concentrations were reached after a long cultivation time (P65), at both depths. In this site Corg was mainly composed by chemically not extractable C, considered the most stabilized fraction. The remaining extractable C fraction decreased with the depth and was mainly made up of highly mineralizable compounds. Data showed that human transformations has affected organic carbon pools only after several decades of cultivation, whereas the activity and structure of the microbial community changed gradually over time, showing the major differences between the most ancient (65 years) and the most recent (5 years) anthropized soils. (C) 2015 Elsevier Ltd. All rights reserved.
机译:我们调查了秘鲁南部沙漠地区人为阶地土壤中的有机碳库以及微生物多样性和活动,以强调农业的引入如何随着时间的推移影响土壤微生物群的碳进化和存储以及遗传和功能多样性。考虑沿5、15、20、35和65年以来耕种的土壤,沿着剖面深度(0-20和20-40 cm层)取样,选择了五个地点。确定了由有机碳库,微生物呼吸,微生物群落生理概况(CLPP)和微生物多样性(PCR-DGGE)组成的土壤和微生物参数。结果表明,长时间培养(P65)后,两个深度都达到了最高的C浓度。在这个站点中,Corg主要由化学上不可萃取的C组成,被认为是最稳定的部分。剩余的可提取C馏分随深度降低,主要由高度矿化的化合物组成。数据显示,人类的转化仅在培养了几十年后才对有机碳库产生影响,而微生物群落的活性和结构则随时间而逐渐变化,显示出最古老的(65年)和最近的(5年)之间的主要差异。 )人工土壤。 (C)2015 Elsevier Ltd.保留所有权利。

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