Yuanshuang Yuan, Xianwang Du, Yicong Yin, Guowei Xia
{"title":"短期氮添加通过调节喀斯特森林磷循环微生物群落提高土壤磷有效性","authors":"Yuanshuang Yuan, Xianwang Du, Yicong Yin, Guowei Xia","doi":"10.1016/j.geoderma.2025.117478","DOIUrl":null,"url":null,"abstract":"<div><div>The widening imbalance between escalating nitrogen (N) deposition and depleting soil phosphorus (P) amplifies the urgency of investigating P cycling processes in terrestrial ecosystems. However, the mechanisms by which P-cycling functional profiles drive soil P mobilization under enhanced N deposition remain to be addressed. After a three-year N-addition experiment at varying rates in a karst forest, we determined the soil P fractions and associated bacterial communities involved in regulating P cycling in rhizosphere and bulk soils. Our results showed that N addition increased plant-available P in both bulk soil (+17 % under low N, +22 % under high N) and rhizosphere soil (+6%, +23 %), while concurrently reducing organic P in bulk soil (−18 %, −24 %) and rhizosphere soil (−8%, –23 %) under corresponding N rates. In addition, N treatment substantially shifted the composition of the P-cycling bacterial community and increased the richness of the community, indicating that N input enhances P availability, potentially through the regulation of the bacterial communities involved in P cycling. Moreover, we found that the functional bacterial genes responsible for P transformation differed between the bulk and rhizosphere soils. Specifically, in the bulk soil, P mineralization genes and P solubilization genes were significantly increased by N treatment. In contrast, in the rhizosphere soil, P mineralization and P regulation genes increased in response to N addition. Together, these results suggest that N addition improves soil P availability by regulating P-cycling functional bacterial communities; however, the specific functional profiles driving P mobilization may differ between bulk and rhizosphere soils. These findings provide novel insight into the regulatory processes of soil P cycling in terrestrial ecosystems under global changes (e.g., N deposition) from a microbial gene perspective.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"461 ","pages":"Article 117478"},"PeriodicalIF":6.6000,"publicationDate":"2025-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Short-term nitrogen addition improves soil phosphorus availability by regulating phosphorus-cycling microbial communities in a karst forest\",\"authors\":\"Yuanshuang Yuan, Xianwang Du, Yicong Yin, Guowei Xia\",\"doi\":\"10.1016/j.geoderma.2025.117478\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The widening imbalance between escalating nitrogen (N) deposition and depleting soil phosphorus (P) amplifies the urgency of investigating P cycling processes in terrestrial ecosystems. However, the mechanisms by which P-cycling functional profiles drive soil P mobilization under enhanced N deposition remain to be addressed. After a three-year N-addition experiment at varying rates in a karst forest, we determined the soil P fractions and associated bacterial communities involved in regulating P cycling in rhizosphere and bulk soils. Our results showed that N addition increased plant-available P in both bulk soil (+17 % under low N, +22 % under high N) and rhizosphere soil (+6%, +23 %), while concurrently reducing organic P in bulk soil (−18 %, −24 %) and rhizosphere soil (−8%, –23 %) under corresponding N rates. In addition, N treatment substantially shifted the composition of the P-cycling bacterial community and increased the richness of the community, indicating that N input enhances P availability, potentially through the regulation of the bacterial communities involved in P cycling. Moreover, we found that the functional bacterial genes responsible for P transformation differed between the bulk and rhizosphere soils. Specifically, in the bulk soil, P mineralization genes and P solubilization genes were significantly increased by N treatment. In contrast, in the rhizosphere soil, P mineralization and P regulation genes increased in response to N addition. Together, these results suggest that N addition improves soil P availability by regulating P-cycling functional bacterial communities; however, the specific functional profiles driving P mobilization may differ between bulk and rhizosphere soils. These findings provide novel insight into the regulatory processes of soil P cycling in terrestrial ecosystems under global changes (e.g., N deposition) from a microbial gene perspective.</div></div>\",\"PeriodicalId\":12511,\"journal\":{\"name\":\"Geoderma\",\"volume\":\"461 \",\"pages\":\"Article 117478\"},\"PeriodicalIF\":6.6000,\"publicationDate\":\"2025-08-13\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geoderma\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0016706125003192\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geoderma","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016706125003192","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
Short-term nitrogen addition improves soil phosphorus availability by regulating phosphorus-cycling microbial communities in a karst forest
The widening imbalance between escalating nitrogen (N) deposition and depleting soil phosphorus (P) amplifies the urgency of investigating P cycling processes in terrestrial ecosystems. However, the mechanisms by which P-cycling functional profiles drive soil P mobilization under enhanced N deposition remain to be addressed. After a three-year N-addition experiment at varying rates in a karst forest, we determined the soil P fractions and associated bacterial communities involved in regulating P cycling in rhizosphere and bulk soils. Our results showed that N addition increased plant-available P in both bulk soil (+17 % under low N, +22 % under high N) and rhizosphere soil (+6%, +23 %), while concurrently reducing organic P in bulk soil (−18 %, −24 %) and rhizosphere soil (−8%, –23 %) under corresponding N rates. In addition, N treatment substantially shifted the composition of the P-cycling bacterial community and increased the richness of the community, indicating that N input enhances P availability, potentially through the regulation of the bacterial communities involved in P cycling. Moreover, we found that the functional bacterial genes responsible for P transformation differed between the bulk and rhizosphere soils. Specifically, in the bulk soil, P mineralization genes and P solubilization genes were significantly increased by N treatment. In contrast, in the rhizosphere soil, P mineralization and P regulation genes increased in response to N addition. Together, these results suggest that N addition improves soil P availability by regulating P-cycling functional bacterial communities; however, the specific functional profiles driving P mobilization may differ between bulk and rhizosphere soils. These findings provide novel insight into the regulatory processes of soil P cycling in terrestrial ecosystems under global changes (e.g., N deposition) from a microbial gene perspective.
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.