有机修正促进了土壤磷相关功能基因和微生物磷循环

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
Wenchao Wu , Yangjian Zhang , Benjamin L. Turner , Yunlong He , Xiaodong Chen , Rongxiao Che , Xiaoyong Cui , Xuejun Liu , Lin Jiang , Juntao Zhu
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引用次数: 0

摘要

土壤微生物的磷动员在决定陆地生态系统的肥力和生产力方面起着至关重要的作用,但施肥策略对这一过程的综合影响尚不清楚。为了填补这一知识空白,我们对85个独立施肥实验的1082个观察结果进行了荟萃分析,以评估磷相关功能基因(phoD, phoC和pqqC)的丰度和多样性以及微生物磷循环对施肥的响应。总体而言,我们发现单独施用有机质(OM)或施用无机肥(OM + IF)可提高土壤微生物P (MBP)、土壤磷酸酶活性和phoD基因丰度。相反,氮肥的添加增加了pqqC基因的丰度,但降低了MBP和phoD基因的丰度。磷肥增加了MBP和phoD基因多样性,而组合添加NP(含或不含钾)增加了酸性磷酸酶活性、MBP、pqqC基因丰度和phoC基因多样性。具体而言,施肥对根际性状的影响随肥料类型的不同而不同:OM提高了根际磷酸酶活性和phoD基因丰度,而P和NP(K)肥降低了它们。此外,随着年气温和降水量的增加,OM对土壤磷酸酶活性和phoD基因丰度的影响增强,而P对phoD Chao1指数的影响减弱。随着实验时间的延长,OM对phoD基因丰度的影响增强,而N添加的影响被抑制。在所有肥料研究中,结构方程模型表明,土壤磷酸酶活性与土壤有机碳(SOC)、土壤pH和phoD或phoC基因丰度密切相关。这项综合分析强调了OM和OM + IF在土壤微生物P循环和相关功能基因方面比合成肥料的优势,为陆地生态系统P的动员和利用效率提供了深刻的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Organic amendments promote soil phosphorus related functional genes and microbial phosphorus cycling
Phosphorus (P) mobilization by soil microorganisms plays a crucial role in determining the fertility and productivity of terrestrial ecosystems, yet the synthesis of impact of fertilization strategies on this process remains poorly understood. To fill this knowledge gap, we conducted a meta-analysis of 1082 observations from 85 independent fertilization experiments to evaluate how the abundance and diversity of P related functional genes (phoD, phoC and pqqC) and microbial P cycling responded to fertilizer addition. Overall, we found that amendment with organic matter (OM) alone or with inorganic fertilizer (OM + IF) enhanced soil microbial P (MBP), soil phosphatase activity, and the phoD gene abundance. Conversely, addition of nitrogen (N) fertilizer increased pqqC gene abundance but decreased MBP and phoD gene abundance. P fertilizer increased MBP and the diversity of the phoD gene, while combined NP addition (with or without potassium, K) increased acid phosphatase activity, MBP, pqqC gene abundance and the diversity of the phoC gene. Specifically, the effects of fertilizer addition on rhizosphere properties varied with fertilizer type: OM increased rhizosphere phosphatase activity and phoD gene abundance, whereas P and NP(K) fertilizers decreased them. Furthermore, as annual temperature and precipitation increased, the influence of OM on soil phosphatase activity and phoD gene abundance increased, while the effect of P addition on the Chao1 index of phoD reduced. As experimental duration lengthens, the effect of OM on phoD gene abundance was strengthened, while the effect of N addition was suppressed. Across all fertilizer studies, structural equation models suggested that soil phosphatase activity was closely correlated with soil organic carbon (SOC), soil pH, and phoD or phoC gene abundance. This comprehensive analysis highlights the benefits of OM and OM + IF over synthetic fertilizer for soil microbial P cycling and associated functional genes, providing profound insights into P mobilization and use efficiency in terrestrial ecosystems.
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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