Yang Li, Xuan Qiu, Deng Liu, Hongmei Wang, Xiaoyan Liu, Weiqi Wang, Ting Chen, Haochao Zhangsun, Xinyu Cai, Shengping Jin, Guangquan Yu
{"title":"Unlocking the Secrets of Saline Lakes: How Environmental and Microbial Interactions Shape Protodolomite Formation.","authors":"Yang Li, Xuan Qiu, Deng Liu, Hongmei Wang, Xiaoyan Liu, Weiqi Wang, Ting Chen, Haochao Zhangsun, Xinyu Cai, Shengping Jin, Guangquan Yu","doi":"10.1111/gbi.70035","DOIUrl":null,"url":null,"abstract":"<p><p>Protodolomite formation in saline lakes remains enigmatic, despite favorable conditions for dolomite precipitation. To unravel this mystery, sediment samples were collected from two saline lakes in northeastern Inner Mongolia: Jibuhulangtu Nuur (JBHLT) and Dabusan Nuur (DBS). These samples were subjected to comprehensive analysis, including mineral composition detection, measurement of physicochemical variables, analysis of extracellular polymeric substances (EPS), and 16S rRNA sequencing. Results showed that protodolomite was exclusively observed in JBHLT, even though both lakes were supersaturated with respect to dolomite. Microbial communities in JBHLT were dominated by Gammaproteobacteria and Desulfuromonadia. Polysaccharide in EPS extracted from sediments was significantly enriched in JBHLT and positively correlated with microbial alpha diversity. pH was found to be the main factor significantly impacting microbial community composition, diversity, and functions. In DBS, increased pH led to the dominance of Halanaerobiaeota, while decreased microbial diversity and polysaccharide contents. The interplay of pH, microbial community structure, and sediment EPS content concurrently impacts protodolomite formation. Our findings highlight the interaction between environmental conditions and microbial communities and their consequence in terms of protodolomite mineralization.</p>","PeriodicalId":173,"journal":{"name":"Geobiology","volume":"23 5","pages":"e70035"},"PeriodicalIF":3.4000,"publicationDate":"2025-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geobiology","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1111/gbi.70035","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"BIOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
Protodolomite formation in saline lakes remains enigmatic, despite favorable conditions for dolomite precipitation. To unravel this mystery, sediment samples were collected from two saline lakes in northeastern Inner Mongolia: Jibuhulangtu Nuur (JBHLT) and Dabusan Nuur (DBS). These samples were subjected to comprehensive analysis, including mineral composition detection, measurement of physicochemical variables, analysis of extracellular polymeric substances (EPS), and 16S rRNA sequencing. Results showed that protodolomite was exclusively observed in JBHLT, even though both lakes were supersaturated with respect to dolomite. Microbial communities in JBHLT were dominated by Gammaproteobacteria and Desulfuromonadia. Polysaccharide in EPS extracted from sediments was significantly enriched in JBHLT and positively correlated with microbial alpha diversity. pH was found to be the main factor significantly impacting microbial community composition, diversity, and functions. In DBS, increased pH led to the dominance of Halanaerobiaeota, while decreased microbial diversity and polysaccharide contents. The interplay of pH, microbial community structure, and sediment EPS content concurrently impacts protodolomite formation. Our findings highlight the interaction between environmental conditions and microbial communities and their consequence in terms of protodolomite mineralization.
期刊介绍:
The field of geobiology explores the relationship between life and the Earth''s physical and chemical environment. Geobiology, launched in 2003, aims to provide a natural home for geobiological research, allowing the cross-fertilization of critical ideas, and promoting cooperation and advancement in this emerging field. We also aim to provide you with a forum for the rapid publication of your results in an international journal of high standing. We are particularly interested in papers crossing disciplines and containing both geological and biological elements, emphasizing the co-evolutionary interactions between life and its physical environment over geological time.
Geobiology invites submission of high-quality articles in the following areas:
Origins and evolution of life
Co-evolution of the atmosphere, hydrosphere and biosphere
The sedimentary rock record and geobiology of critical intervals
Paleobiology and evolutionary ecology
Biogeochemistry and global elemental cycles
Microbe-mineral interactions
Biomarkers
Molecular ecology and phylogenetics.