Yuan Ma , Qinghang Zhang , Eryang Li , Xiaohui Zhu , Jie Lü
{"title":"古尔班通古特沙漠生物土壤结皮中氮源偏好和群落组合影响微生物功能","authors":"Yuan Ma , Qinghang Zhang , Eryang Li , Xiaohui Zhu , Jie Lü","doi":"10.1016/j.apsoil.2025.106385","DOIUrl":null,"url":null,"abstract":"<div><div>Biological soil crusts (BSCs) play vital roles in stabilizing desert soils, regulating nutrient cycles, and supporting plant establishment, making their spatial and temporal distribution key indicators of desert ecosystem stability. Using metagenomic sequencing, we analyzed microbial communities in bare sand, algal crusts, and moss crusts in the Gurbantunggut Desert, aiming to elucidate the connections between microbial dynamics and key ecological processes during BSC development to uncover how microscale microbial processes shape broader spatial ecosystem patterns. The three soil types exhibited distinct microbial communities and functional capacities, particularly in carbon fixation and nitrogen cycling processes. Microbial network complexity increased from bare sand to algal and moss crusts,with higher clustering in algal crusts and shorter connectivity paths in moss crusts, both indicating intensified microbial interactions and network cohesion. Algal crusts showed reduced prokaryotic carbon sequestration potential, likely driven by ammonium limitation that suppressed carbon cycling gene expression in heterotrophic taxa (e.g., Actinobacteria), while dominant Cyanobacteria sustained baseline photosynthesis to support early crust development. Differences in microbial nitrogen utilization strategies altered nitrogen cycling dynamics and contributed to niche differentiation among crust types. These shifts reflected strong environmental filtering, which shaped both microbial composition and functional potential across the successional gradient. Source tracking analysis indicates that bare ground was the primary microbial source during BSC succession and that microbial inheritance between crust types was selective rather than continuous. Our findings uncover key mechanisms driving microbial community assembly and succession in desert BSCs, offering new insights for ecological monitoring and restoration in arid environments.</div></div>","PeriodicalId":8099,"journal":{"name":"Applied Soil Ecology","volume":"215 ","pages":"Article 106385"},"PeriodicalIF":5.0000,"publicationDate":"2025-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Nitrogen source preference and community assembly shape microbial function in biological soil crusts of the Gurbantunggut Desert\",\"authors\":\"Yuan Ma , Qinghang Zhang , Eryang Li , Xiaohui Zhu , Jie Lü\",\"doi\":\"10.1016/j.apsoil.2025.106385\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Biological soil crusts (BSCs) play vital roles in stabilizing desert soils, regulating nutrient cycles, and supporting plant establishment, making their spatial and temporal distribution key indicators of desert ecosystem stability. Using metagenomic sequencing, we analyzed microbial communities in bare sand, algal crusts, and moss crusts in the Gurbantunggut Desert, aiming to elucidate the connections between microbial dynamics and key ecological processes during BSC development to uncover how microscale microbial processes shape broader spatial ecosystem patterns. The three soil types exhibited distinct microbial communities and functional capacities, particularly in carbon fixation and nitrogen cycling processes. Microbial network complexity increased from bare sand to algal and moss crusts,with higher clustering in algal crusts and shorter connectivity paths in moss crusts, both indicating intensified microbial interactions and network cohesion. Algal crusts showed reduced prokaryotic carbon sequestration potential, likely driven by ammonium limitation that suppressed carbon cycling gene expression in heterotrophic taxa (e.g., Actinobacteria), while dominant Cyanobacteria sustained baseline photosynthesis to support early crust development. Differences in microbial nitrogen utilization strategies altered nitrogen cycling dynamics and contributed to niche differentiation among crust types. These shifts reflected strong environmental filtering, which shaped both microbial composition and functional potential across the successional gradient. Source tracking analysis indicates that bare ground was the primary microbial source during BSC succession and that microbial inheritance between crust types was selective rather than continuous. Our findings uncover key mechanisms driving microbial community assembly and succession in desert BSCs, offering new insights for ecological monitoring and restoration in arid environments.</div></div>\",\"PeriodicalId\":8099,\"journal\":{\"name\":\"Applied Soil Ecology\",\"volume\":\"215 \",\"pages\":\"Article 106385\"},\"PeriodicalIF\":5.0000,\"publicationDate\":\"2025-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Soil Ecology\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0929139325005232\",\"RegionNum\":2,\"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":"Applied Soil Ecology","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0929139325005232","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
Nitrogen source preference and community assembly shape microbial function in biological soil crusts of the Gurbantunggut Desert
Biological soil crusts (BSCs) play vital roles in stabilizing desert soils, regulating nutrient cycles, and supporting plant establishment, making their spatial and temporal distribution key indicators of desert ecosystem stability. Using metagenomic sequencing, we analyzed microbial communities in bare sand, algal crusts, and moss crusts in the Gurbantunggut Desert, aiming to elucidate the connections between microbial dynamics and key ecological processes during BSC development to uncover how microscale microbial processes shape broader spatial ecosystem patterns. The three soil types exhibited distinct microbial communities and functional capacities, particularly in carbon fixation and nitrogen cycling processes. Microbial network complexity increased from bare sand to algal and moss crusts,with higher clustering in algal crusts and shorter connectivity paths in moss crusts, both indicating intensified microbial interactions and network cohesion. Algal crusts showed reduced prokaryotic carbon sequestration potential, likely driven by ammonium limitation that suppressed carbon cycling gene expression in heterotrophic taxa (e.g., Actinobacteria), while dominant Cyanobacteria sustained baseline photosynthesis to support early crust development. Differences in microbial nitrogen utilization strategies altered nitrogen cycling dynamics and contributed to niche differentiation among crust types. These shifts reflected strong environmental filtering, which shaped both microbial composition and functional potential across the successional gradient. Source tracking analysis indicates that bare ground was the primary microbial source during BSC succession and that microbial inheritance between crust types was selective rather than continuous. Our findings uncover key mechanisms driving microbial community assembly and succession in desert BSCs, offering new insights for ecological monitoring and restoration in arid environments.
期刊介绍:
Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.