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What controls the availability of organic and inorganic P sources in top- and subsoils? A 33P isotopic labeling study with root exudate addition

文献类型： 外文期刊

作者： Ai, Juanjuan 1 ; Banfield, Callum C. 3 ; Shao, Guodong 3 ; Zamanian, Kazem 5 ; Stuerzebecher, Tobias 4 ; Shi, Lingling 3 ; Fan, Lichao 7 ; Liu, Xia 1 ; Spielvogel, Sandra 8 ; Dippold, Michaela A. 3 ;

作者机构： 1.Maize Res Inst, Shandong Acad Agr Sci, Jinan 250100, Peoples R China

2.Shandong Normal Univ, Coll Life Sci, Jinan 250100, Peoples R China

3.Univ Tubingen, Dept Geosci, Geobiosphere Interact, D-72076 Tubingen, Germany

4.Univ Gottingen, Dept Crop Sci, Biogeochem Agroecosystems, D-37077 Gottingen, Germany

5.Leibniz Univ Hannover, Inst Soil Sci, D-30419 Hannover, Germany

6.Nanjing Univ Informat Sci & Technol, Sch Geog Sci, Nanjing 210044, Peoples R China

7.Northwest A&F Univ, Coll Nat Resources & Environm, Yangling 712100, Peoples R China

8.Univ Kiel, Inst Plant Nutr & Soil Sci, D-24118 Kiel, Germany

关键词： Subsoil; Root exudates; Microbial biomass; 33 P labeling; Microbial community; Enzyme activity

期刊名称：SOIL BIOLOGY & BIOCHEMISTRY （ 影响因子：9.7； 五年影响因子：10.2 ）

ISSN： 0038-0717

年卷期： 2023 年 185 卷

页码：

收录情况： SCI

摘要： Phosphorus (P) is a major limiting nutrient for plant growth implying an often-intensive competition between microorganisms and plants in the rhizosphere. Increasing the P availability in subsoils may help to mitigate potential future P fertilizer shortages and to overcome P limitations due to droughts, which mainly affect topsoils. Root exudates provide easily available carbon and energy sources for microorganisms to mobilize soil nutrients. Nonetheless, details regarding the distinct processes underlying P mobilization from various P sources (free vs. sorbed PO4 3; low molecular vs. complex organic P, e.g. ATP vs. plant litter P) as affected by root exudates are poorly understood, especially in subsoils. This study aimed to identify the controlling factors and microbial processes regulating the availability of organic and inorganic P in top- and subsoils by 33P isotopic labeling. The focus was on the potential key role of root exudates in P mobilization. We found that microbial communities in top- and subsoils used high- and low-available mineral P to a similar extent, but that the subsoil communities were much more efficient in mobilizing and incorporating complex litter-derived organic P. This capability of subsoil communities was even enhanced when root exudates were present. Microbial activity and nutrient-mobilizing mechanisms (e.g., P-related enzymes) clearly increased by root exudate addition, an effect that was generally higher in sub-than in topsoils. We conclude that subsoil communities are well capable of mobilizing and using complex organic P sources, especially if root exudates accelerate overall activity and P cycling. Thus, high root exudation is highly relevant for crops, which depend on subsoil nutrients and litterderived P. Accordingly, detritusphere P, e.g. in subsoil root channels, is likely to be plant-available because of exudate-induced microbial P (re-)cycling processes.

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