Historical Retrospect of Aquatic Microbial Communities Based on Water–Carbonate Equilibrium and pH Values in Dianchi Lake Using the Random Forest AlgorithmClick to copy article linkArticle link copied!
- Yucheng XieYucheng XieKey Laboratory of Groundwater Resources and Environment Ministry of Education, Jilin University, Changchun 130021, PR ChinaCollege of New Energy and Environment, Jilin University, Changchun 130021, PR ChinaMore by Yucheng Xie
- Danni Li
- Feng HeFeng HeWater Environment Research Division, Kunming Dianchi & Plateau Lakes Institute, Kunming 650000, PR ChinaMore by Feng He
- Jinsong DuJinsong DuWater Environment Research Division, Kunming Dianchi & Plateau Lakes Institute, Kunming 650000, PR ChinaMore by Jinsong Du
- Guanghe Li
- Dayi Zhang*Dayi Zhang*E-mail: [email protected]. Tel: +86(0)10-62773232. Fax: +86(0)10-62795687.Key Laboratory of Groundwater Resources and Environment Ministry of Education, Jilin University, Changchun 130021, PR ChinaCollege of New Energy and Environment, Jilin University, Changchun 130021, PR ChinaKey Laboratory of Regional Environment and Eco-restoration, Ministry of Education, Shenyang University, Shenyang 110044, PR ChinaMore by Dayi Zhang
Abstract
Aquatic microbial communities are crucial for the dynamics of algal blooms. Due to the limited development history and high cost of high-throughput sequencing, microbial information is commonly unavailable in past aquatic quality surveys. This study comprehensively analyzed 19 years of historical data from alkalitrophic Dianchi Lake to explore the interrelationships among pH, carbonate equilibrium (CO32– and HCO3–), and physicochemical/microbial variables, and developed predictive models of carbonate equilibrium and pH using the Random Forest (RF) algorithm. Microbial taxa, particularly Proteobacteria, Cyanobacteria, and Bacteroidetes, were more predictive of pH and carbonate equilibrium than physicochemical variables. The Mean Absolute Percentage Error (MAPE) was 1.5%, 26.9%, and 30.1% for pH, CO32–, and HCO3–, respectively. Different microorganisms played predominant roles across varying pH ranges, with photoautotrophs (e.g., Cyanobacteria) determining carbonate equilibrium at pH < 9.0 and heterotrophs (e.g., Proteobacteria and Bacteroidetes) at pH > 9.0. Furthermore, a backtracking algorithm was used to reconstruct the historical microbial community structure based on pH values, with the backtracked cyanobacterial abundance matching well with historical chlorophyll-a data from 2000 to 2018. Our results highlight the strong correlations between microbial community structure, aquatic pH, and carbonate equilibrium and provide a powerful backtracking algorithm to obtain historical microbial information for lake management.
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