Yue Qiu , Wei Ji , Sibei Chen , Guitong Li , Qimei Lin , Xiaorong Zhao , Owen Fenton , Hao Chen
{"title":"Divergent responses of soil bacterial and fungal biomass carbon and phosphorus (P) to a P addition gradient","authors":"Yue Qiu , Wei Ji , Sibei Chen , Guitong Li , Qimei Lin , Xiaorong Zhao , Owen Fenton , Hao Chen","doi":"10.1016/j.pedobi.2026.151112","DOIUrl":null,"url":null,"abstract":"<div><div>Microorganisms mediate element dynamics in soils through biomass turnover, and their activity is largely affected by nutrient inputs. However, as the two major subgroups of soil microbial community, little is known regarding how bacterial and fungal biomass carbon (C) and phosphorus (P) respond to a P addition gradient. Herein, the dynamic changes of bacterial and fungal biomass C and P from the soil in northern China were studied using the selective inhibition technique. A 20-d soil incubation experiment was set up with different P additions: 0, 20 and 60 mg kg<sup>−1</sup> soil. The experiment selected streptomycin (10 mg g<sup>−1</sup> soil) and cycloheximide (20 mg g<sup>−1</sup> soil) as bacterial and fungal inhibitors, respectively. The results showed that P addition did not affect the total microbial biomass C but substantially adjusted the composition contributed by bacteria and fungi. Fungal biomass C contributed highest at the low P addition rate, but its significance tended to decrease as P addition increased, whereas the contribution of bacterial biomass C increased. P addition positively affected both bacterial and fungal biomass P, but at a higher extent for bacteria. In terms of time, bacteria showed a higher potential to release P into soil labile P pools through biomass turnover at an earlier stage after P addition, whereas fungi may have a slow effect as sources of soil labile P. These results indicate divergent responses for bacterial and fungal biomass across different P additions. Such insights should be considered at field scale and should inform C and nutrient managements planning in terms of soil C and P cycling.</div></div>","PeriodicalId":49711,"journal":{"name":"Pedobiologia","volume":"114 ","pages":"Article 151112"},"PeriodicalIF":2.2000,"publicationDate":"2026-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Pedobiologia","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0031405626000016","RegionNum":3,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2026/1/5 0:00:00","PubModel":"Epub","JCR":"Q3","JCRName":"ECOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
Microorganisms mediate element dynamics in soils through biomass turnover, and their activity is largely affected by nutrient inputs. However, as the two major subgroups of soil microbial community, little is known regarding how bacterial and fungal biomass carbon (C) and phosphorus (P) respond to a P addition gradient. Herein, the dynamic changes of bacterial and fungal biomass C and P from the soil in northern China were studied using the selective inhibition technique. A 20-d soil incubation experiment was set up with different P additions: 0, 20 and 60 mg kg−1 soil. The experiment selected streptomycin (10 mg g−1 soil) and cycloheximide (20 mg g−1 soil) as bacterial and fungal inhibitors, respectively. The results showed that P addition did not affect the total microbial biomass C but substantially adjusted the composition contributed by bacteria and fungi. Fungal biomass C contributed highest at the low P addition rate, but its significance tended to decrease as P addition increased, whereas the contribution of bacterial biomass C increased. P addition positively affected both bacterial and fungal biomass P, but at a higher extent for bacteria. In terms of time, bacteria showed a higher potential to release P into soil labile P pools through biomass turnover at an earlier stage after P addition, whereas fungi may have a slow effect as sources of soil labile P. These results indicate divergent responses for bacterial and fungal biomass across different P additions. Such insights should be considered at field scale and should inform C and nutrient managements planning in terms of soil C and P cycling.
期刊介绍:
Pedobiologia publishes peer reviewed articles describing original work in the field of soil ecology, which includes the study of soil organisms and their interactions with factors in their biotic and abiotic environments.
Analysis of biological structures, interactions, functions, and processes in soil is fundamental for understanding the dynamical nature of terrestrial ecosystems, a prerequisite for appropriate soil management. The scope of this journal consists of fundamental and applied aspects of soil ecology; key focal points include interactions among organisms in soil, organismal controls on soil processes, causes and consequences of soil biodiversity, and aboveground-belowground interactions.
We publish:
original research that tests clearly defined hypotheses addressing topics of current interest in soil ecology (including studies demonstrating nonsignificant effects);
descriptions of novel methodological approaches, or evaluations of current approaches, that address a clear need in soil ecology research;
innovative syntheses of the soil ecology literature, including metaanalyses, topical in depth reviews and short opinion/perspective pieces, and descriptions of original conceptual frameworks; and
short notes reporting novel observations of ecological significance.