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<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Ecol. Evol.</journal-id>
<journal-title>Frontiers in Ecology and Evolution</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Ecol. Evol.</abbrev-journal-title>
<issn pub-type="epub">2296-701X</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.3389/fevo.2023.1216567</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Ecology and Evolution</subject>
<subj-group>
<subject>Original Research</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Producers and drivers of odor compounds in a large drinking-water source</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname>Qiu</surname>
<given-names>Pengfei</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Zhang</surname>
<given-names>Yuheng</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Mi</surname>
<given-names>Wujuan</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2230984"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Song</surname>
<given-names>Gaofei</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Bi</surname>
<given-names>Yonghong</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="author-notes" rid="fn001">
<sup>*</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/400624"/>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>State Key Laboratory of Freshwater Ecology and Biotechnology, Institute of Hydrobiology, Chinese Academy of Sciences</institution>, <addr-line>Wuhan</addr-line>, <country>China</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>College of Advanced Agricultural Sciences, University of Chinese Academy of Sciences</institution>, <addr-line>Beijing</addr-line>, <country>China</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>Edited by: M. Belal Hossain, Noakhali Science and Technology University, Bangladesh</p>
</fn>
<fn fn-type="edited-by">
<p>Reviewed by: Cuong Tu Ho, Vietnam Academy of Science and Technology, Vietnam; Youji Wang, Shanghai Ocean University, China</p>
</fn>
<fn fn-type="corresp" id="fn001">
<p>*Correspondence: Yonghong Bi, <email xlink:href="mailto:biyh@ihb.ac.cn">biyh@ihb.ac.cn</email>
</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>20</day>
<month>07</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="collection">
<year>2023</year>
</pub-date>
<volume>11</volume>
<elocation-id>1216567</elocation-id>
<history>
<date date-type="received">
<day>04</day>
<month>05</month>
<year>2023</year>
</date>
<date date-type="accepted">
<day>21</day>
<month>06</month>
<year>2023</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2023 Qiu, Zhang, Mi, Song and Bi</copyright-statement>
<copyright-year>2023</copyright-year>
<copyright-holder>Qiu, Zhang, Mi, Song and Bi</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p>
</license>
</permissions>
<abstract>
<sec>
<title>Introduction</title>
<p>Taste and odor (T&amp;O) problems have been affecting drinking water safety. As a eutrophicated drinking water reservoir in Tianjin city, the Yuqiao Reservoir was threatened by 2-MIB and geosmin in recent years.</p>
</sec>
<sec>
<title>Methods</title>
<p>In this study, quantile regression analysis and metagenome were used to quickly and accurately screen the producers and drivers of 2-MIB and geosmin in this reservoir.</p>
</sec>
<sec>
<title>Results</title>
<p>The mean concentrations of 2-MIB and geosmin in the four-year were 103.58 &#xb1; 128.13 ng/L and 14.29 &#xb1; 27.95 ng/L, respectively. 2-MIB concentrations were higher in summer and autumn, with a bimodal variation throughout the year. Geosmin concentrations showed a decreasing trend from year to year from 2018 to 2021. Metagenome revealed that <italic>Pseudanabaena</italic> sp. dqh15, <italic>Microcoleus pseudautumnalis</italic> Ak1609, <italic>Pseudanabaena limnetica</italic>, and <italic>Planktothricoides raciborskii</italic> were the 2-MIB-producers, while <italic>Streptosporangium caverna</italic> and <italic>Dolichospermum circinale</italic> were the geosmin-producers. Multivariate quantile regression analysis indicated Pseudanabaena sp. and CODMn were the best predictors of 2-MIB concentrations, temperature and CODMn were the most useful parameters for describing geosmin concentration change. 2-MIB concentrations increased with the increase of <italic>Pseudanabaena</italic> sp. cell density and COD<sub>Mn</sub>. Geosmin concentrations were higher at harsh temperatures and increased with higher COD<sub>Mn</sub>. COD<sub>Mn</sub> was significantly and positively correlated with the biosynthesis of secondary metabolites synthesis and terpenoid backone biosynthesis pathway. Both quantile regression and metagenome results showed that COD<sub>Mn</sub> was an important driver of odor compounds.</p>
</sec>
<sec>
<title>Discussion</title>
<p>Metagenome achieved higher resolution of taxonomic annotation than amplicons to identify odor-producers, which helps us to understand the main taxa of odor-producing microorganisms in Chinese water bodies and the genetic basis of odor compounds in microorganisms. Understanding the sources and drivers of odor compounds was useful for improving taste and odor problem management. This is the first time that the main odor-producing microorganisms in water bodies have been resolved by microbial metagenomic functional gene prediction.</p>
</sec>
</abstract>
<kwd-group>
<kwd>odor producers</kwd>
<kwd>drivers</kwd>
<kwd>metagenomic sequencing</kwd>
<kwd>quantile regression</kwd>
<kwd>cyanobaceria</kwd>
</kwd-group>
<counts>
<fig-count count="7"/>
<table-count count="3"/>
<equation-count count="0"/>
<ref-count count="83"/>
<page-count count="15"/>
<word-count count="6424"/>
</counts>
<custom-meta-wrap>
<custom-meta>
<meta-name>section-in-acceptance</meta-name>
<meta-value>Biogeography and Macroecology</meta-value>
</custom-meta>
</custom-meta-wrap>
</article-meta>
</front>
<body>
<sec id="s1" sec-type="intro">
<label>1</label>
<title>Introduction</title>
<p>Since the 1950s, China has built 87,000 reservoirs and dams to address water shortage and water security, making them an increasingly important source of drinking water (<xref ref-type="bibr" rid="B41">Liu and Yang, 2012</xref>; <xref ref-type="bibr" rid="B70">Wang Y. et&#xa0;al., 2021</xref>). However, the frequent occurrence of taste and odor (T&amp;O) events in reservoirs recently has posed a huge challenge to tap water treatment plants, while threatening the safety of drinking water resources (<xref ref-type="bibr" rid="B78">Xu et&#xa0;al., 2022</xref>). Odor compounds are often misunderstood as an aesthetic issue, but they are also a major indicator of public acceptance of drinking water (<xref ref-type="bibr" rid="B76">Wu et&#xa0;al., 2021b</xref>). Due to their low odor thresholds (both &lt; 10 ng/L), 2-methylisocampheol (2-MIB) and trans-1,10-dimethyl-trans-9-decalol (geosmin) are the most common and typical contaminants that affect water quality in reservoirs (<xref ref-type="bibr" rid="B11">Devi et&#xa0;al., 2021</xref>). In China, 2-MIB and geosmin are listed as the main control compounds to ensure the safety of drinking water sources (<xref ref-type="bibr" rid="B55">Rong et&#xa0;al., 2018</xref>). Given the chemical stability and small molecular weight of 2-MIB and geosmin, it is difficult to remove them through conventional water treatment processes (coagulation, flocculation, filtration, aeration, and disinfection/oxidation by chlorine), and chemical methods of removing odor substances can produce hazardous oxidation by-products (<xref ref-type="bibr" rid="B57">Sagehashi et&#xa0;al., 2005</xref>; <xref ref-type="bibr" rid="B78">Xu et&#xa0;al., 2022</xref>). Once encountering T&amp;O episodes in drinking water, it is difficult for water treatment to take applicable control measures, resulting in enormous financial damages. It is necessary to identify and monitor the producers of odor substances in advance to ensure the safety of drinking water and reduce economic losses.</p>
<p>As to the producer of 2-MIB and geosmin, there are mainly producers such as cyanobacteria, fungi, myxobacteria and actinomycetes have been reported (<xref ref-type="bibr" rid="B28">Juttner and Watson, 2007</xref>), and cyanobacteria was proven as the main source of 2-MIB and geosmin in the aquatic environment (<xref ref-type="bibr" rid="B34">Lee E.S. et&#xa0;al., 2020</xref>). Among more than 100 articles published since 1990 on cyanobacteria associated geosmin/2-MIB in drinking water systems, mainly distributed in North America, Australia, Europe, China, Japan, South Korea, Philippines and South Africa (<xref ref-type="bibr" rid="B62">Su et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B11">Devi et&#xa0;al., 2021</xref>). Cyanobacterial species that have been associated with 2-MIB- or geosmin-related off-flavors include <italic>Anabaena, Aphanizomenon, Lyngbya, Oscillatoria, Phormidium, Planktothrix</italic>, and <italic>Pseudanabaena</italic> (<xref ref-type="bibr" rid="B52">Peterson et&#xa0;al., 1995</xref>; <xref ref-type="bibr" rid="B63">Sugiura et&#xa0;al., 1997</xref>; <xref ref-type="bibr" rid="B83">Zimba et&#xa0;al., 1999</xref>; <xref ref-type="bibr" rid="B62">Su et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B82">Zhang et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B5">Cai et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B55">Rong et&#xa0;al., 2018</xref>). A total of 132 cyanobacterial strains from 21 genera and 72 cyanobacterial strains from 13 genera produced geosmin and 2-MIB, respectively. The fungi, myxobacteria and actinomycetes that produce geosmin and 2-MIB have been less studied than cyanobacteria (<xref ref-type="bibr" rid="B11">Devi et&#xa0;al., 2021</xref>). The higher incidence of geosmin events in the United States, Canada and Australia, and the higher incidence of 2-MIB events in China and Korea suggest that differences in geographical distribution influence the occurrence and frequency of T&amp;O events (<xref ref-type="bibr" rid="B11">Devi et&#xa0;al., 2021</xref>). The Yuqiao Reservoir has experienced eutrophication during the last decade, accompanied by the frequent occurrence of bloom events (<xref ref-type="bibr" rid="B24">Huo et&#xa0;al., 2018</xref>). The Yuqiao reservoir has been reported to have earthy-musty taste and odor (T&amp;O) issues with a relatively high amount of 2-MIB. Due to the diversity of these microorganisms, it is still necessary to identify the main producer of 2-MIB and geosmin in the specific waterbody.</p>
<p>On the other hand, not all these microorganisms can be cultured in the laboratory, so it becomes critical to use culture-independent molecular tools to track the odor-producers (<xref ref-type="bibr" rid="B10">Cristina Casero et&#xa0;al., 2019</xref>). The biosynthesis pathways of 2-MIB and geosmin were elucidated in actinobacteria and cyanobacteria, providing a molecular basis for traceability analysis of odor compounds (<xref ref-type="bibr" rid="B20">Hamano et&#xa0;al., 2002</xref>; <xref ref-type="bibr" rid="B6">Cane and Watt, 2003</xref>; <xref ref-type="bibr" rid="B43">Ludwig et&#xa0;al., 2007</xref>; <xref ref-type="bibr" rid="B32">Komatsu et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B73">Wang et&#xa0;al., 2011</xref>). In the synthesis of 2-MIB, the generic precursor of monoterpenoids, GPP (geranyl pyrophosphate), is methylated to methyl-GPP, and then 2-MIB synthase cyclizes methyl-GPP to 2-MIB (<xref ref-type="bibr" rid="B49">Oldfield and Lin, 2012</xref>; <xref ref-type="bibr" rid="B4">Brock et&#xa0;al., 2013</xref>). Geosmin is generated from farnesyl diphosphate (FPP) synthesized by the bifunctional single sesquiterpene cyclase (geosmin synthase) in the presence of Mg<sup>2+</sup> (<xref ref-type="bibr" rid="B25">Jiang et&#xa0;al., 2006</xref>; <xref ref-type="bibr" rid="B26">Jiang et&#xa0;al., 2007</xref>). The geosmin synthase gene and the 2-MIB synthase gene are indicators to investigate the producer of geosmin and 2-MIB, which provided a useful tool to screen the producer of geosmin and 2-MIB. Moreover, high-throughput sequencing is a lower-cost and more efficient sequence determination technology compared to traditional Sanger sequencing, and has played an increasingly important role in the life sciences since its introduction in 2005 (<xref ref-type="bibr" rid="B44">Margulies et&#xa0;al., 2006</xref>). Applying high-throughput sequencing to odor compounds biosynthetic genes provides a time-saving, high-resolution tool for the diversity of odor-producing microorganisms in freshwater bodies worldwide. High-throughput sequencing, including amplicon sequencing and metagenomic sequencing, could rapidly detect unculturable low-abundance microorganisms in the environment (<xref ref-type="bibr" rid="B40">Liu et&#xa0;al., 2021</xref>). Amplicon sequencing is widely used in the study of microbial diversity, especially for toxic or odor-producing cyanobacteria (<xref ref-type="bibr" rid="B10">Cristina Casero et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B54">Qiu et&#xa0;al., 2021</xref>). However, the identification of species by amplicon sequencing can only reach a genus-level resolution, and the selection of primers and the determination of the number of PCR cycles during sequencing have a large impact on the sequencing results. Currently, the developed geosmin/2-MIB primers have focused on cyanobacteria, thus quantifying the species composition of geosmin/2-MIB-producing cyanobacteria (<xref ref-type="bibr" rid="B11">Devi et&#xa0;al., 2021</xref>). These primers could rapidly identify a lot of geosmin/2-MIB-producing cyanobacteria, such as <italic>Anabaena</italic> sp. <italic>Planktothrix</italic> sp., <italic>Phormidium</italic> sp., <italic>Oscillatoria</italic> sp., <italic>Pseudoanabaena</italic> sp (<xref ref-type="bibr" rid="B17">Giglio et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B18">Giglio et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B66">Tsao et&#xa0;al., 2014</xref>). This neglected the contribution of actinomycetes and bacteria to geosmin/2-MIB in the environment. In previous studies, the correlation between the qPCR of geosmin/2-MIB synthase gene and geosmin/2-MIB content was not correlated, low correlated, and highly correlated (<xref ref-type="bibr" rid="B61">Su et&#xa0;al., 2013</xref>; <xref ref-type="bibr" rid="B66">Tsao et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B8">Chiu et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B71">Wang et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B23">Huang et&#xa0;al., 2018</xref>). When the correlation between gene copy numbers and geosmin/2-MIB concentration is low, it indicates that cyanobacteria contribute only a small fraction of geosmin/2-MIB in water. The presence of odor-producing actinomycetes and bacteria in the water is one of the important factors affecting the correlation value. Metagenomic sequencing is performed by randomly interrupting microbial genomes and assembling small fragments into longer sequences (<xref ref-type="bibr" rid="B40">Liu et&#xa0;al., 2021</xref>). Metagenomic sequencing has no primer biases. Metagenomic sequencing can provide not only a more accurate species composition (species or strain level) compared to amplicon sequencing, but also functional gene information (<xref ref-type="bibr" rid="B59">Smits et&#xa0;al., 2017</xref>). Nevertheless, the application of metagenomic sequencing technology in odor-producer identification and monitoring is still rare, and more research work is needed.</p>
<p>Besides the above, the synthesis and release of odor compounds were influenced by environmental factors. Temperature and light intensity were the major factors that affect the production of 2-MIB and geosmin (<xref ref-type="bibr" rid="B58">Shen et&#xa0;al., 2022</xref>). Unfavorable conditions, such as strong light, low and high temperatures, could increase the potential for geosmin/2-MIB synthesis in cyanobacterial cells (<xref ref-type="bibr" rid="B83">Zimba et&#xa0;al., 1999</xref>; <xref ref-type="bibr" rid="B73">Wang et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B82">Zhang et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B5">Cai et&#xa0;al., 2017</xref>). Moreover, nitrogen and phosphorus could affect the production of geosmin and 2-MIB. TN : TP &lt; 29 : 1 favored the generation and accumulation of 2-MIB concentration in the Yangcheng Lake (<xref ref-type="bibr" rid="B75">Wu et&#xa0;al., 2021a</xref>). Ammonium was essential to promote the production of 2-MIB and geosmin compounds (<xref ref-type="bibr" rid="B51">Perkins et&#xa0;al., 2019</xref>). The microbial communities in waters were diverse, and the production of odor compounds might change under the interaction between different microbial species. <italic>Microcystis aeruginosa</italic> could obviously promote 2-MIB production of <italic>Pseudanabaena</italic> sp. (<xref ref-type="bibr" rid="B81">Zhang et&#xa0;al., 2020</xref>). Identifying key influencing environmental factors could reduce the risk of T&amp;O outbreaks (<xref ref-type="bibr" rid="B73">Wang et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B5">Cai et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B48">Oh et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B1">Alghanmi et&#xa0;al., 2018</xref>) and be useful for adaptive environmental management. Further work is still needed to identify the environmental drivers for geosmin and 2-MIB.</p>
<p>In this study, a long-term field investigation was conducted from 2018 to 2021 in the Yuqiao Reservoir, Tianjin. Macrogenomic approaches were used to investigate the main producers of 2-MIB and geosmin and their related functional genes, while quantile regression was used to find the drivers of 2-MIB and geosmin. The results would be helpful to get insight into the problems of T&amp;O and support drinking water resource management.</p>
</sec>
<sec id="s2" sec-type="materials|methods">
<label>2</label>
<title>Materials and methods</title>
<sec id="s2_1">
<label>2.1</label>
<title>Study area and sampling</title>
<p>The Yuqiao Reservoir (40&#xb0; 02&#x2019; N, 117&#xb0; 25&#x2019; E) is an important source of drinking water for Tianjin and a large storage reservoir for the Luanhe River-Tianjin water diversion project, adjacent to Hebei Province and Beijing. The Yuqiao Reservoir is mainly formed by the confluence of three major tributaries, namely the Shahe River, the Luanhe River, and the Lihe River, with a total storage capacity of 15.59 &#xd7; 10<sup>8</sup> m<sup>3</sup> and a utilizable storage capacity of 3.85 &#xd7; 10<sup>8</sup> m<sup>3</sup> and an average water depth of 4.5 m. Samples (0.5 m below the surface) from 1# to 3# were collected in 2018. From 2019, four additional sites (4# to 7#) have been added. The Yuqiao Reservoir and the sampling stations are shown in <xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>.</p>
<fig id="f1" position="float">
<label>Figure&#xa0;1</label>
<caption>
<p>The sampling sites in the Yuqiao Reservoir.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g001.tif"/>
</fig>
</sec>
<sec id="s2_2">
<label>2.2</label>
<title>Environmental parameters and phytoplankton composition</title>
<p>During sampling, oxidation-reduction potential (ORP), water temperature (Temp), dissolved oxygen (DO), and pH were measured <italic>in situ</italic> with a multi-parameter probe (YSI-6600, USA). Transparency (SD) was measured with a Secchi disk (diameter: 20 cm, black and white). Water samples were collected at 0.5 m below the surface water monthly for biological, physical, and chemical analysis from 2018 to 2021. 1000 ml of Subsample was preserved with 1% Lugol&#x2019;s iodine solution (<xref ref-type="bibr" rid="B21">Hawkins et&#xa0;al., 2005</xref>). After 48 hours of sedimentation, the residues were condensed to 50 ml for quantitative phytoplankton analysis (<xref ref-type="bibr" rid="B22">Hu and Wei, 2006</xref>). Phytoplankton species were identified and counted by taking 100 ml of the concentrate and placing it in a phytoplankton counting frame under a 400 &#xd7; magnification optical microscope according to the method in <xref ref-type="bibr" rid="B22">Hu and Wei (2006)</xref>.</p>
<p>Subsamples for nutrient analysis were kept in ice boxes until transferred to the laboratory&#x2019;s 4 &#xb0;C refrigerator. Concentrations of nitrate nitrogen (NO<sub>3</sub>-N), total nitrogen (TN), total phosphorus (TP), ammonium (NH<sub>4</sub>-N) and phosphate (PO<sub>4</sub>-P) were measured according to the general laboratory methods (<xref ref-type="bibr" rid="B9">Clescerl, 1998</xref>). The permanganate index (COD<sub>Mn</sub>) was determined by the acidic potassium permanganate method by taking 100 ml of unfiltered subsamples. Chlorophyll <italic>a</italic> was determined by UV spectrophotometer after 90% acetone extraction (<xref ref-type="bibr" rid="B77">Xu et&#xa0;al., 2010</xref>).</p>
</sec>
<sec id="s2_3">
<label>2.3</label>
<title>Geosmin/2-MIB analysis and DNA preparation</title>
<p>Geosmin and 2-MIB concentrations were extracted and absorbed from the water samples by headspace solid-phase microextraction (HSPME) using 65 mm PDMS/DVB fiber (57310-U, Supelco, USA). Then, the extracted fiber was used for gas chromatography-mass spectrometry (GC-MS) analysis (HP 6890 GC-5973 MSD; Agilent Technologies, USA) to quantify geosmin and 2-MIB concentrations (<xref ref-type="bibr" rid="B74">Watson et&#xa0;al., 2000</xref>; <xref ref-type="bibr" rid="B38">Li et&#xa0;al., 2007</xref>). Water samples from four typical sites were selected for metagenomic sequencing, namely the outlet (1#), the inlet (3#), the center (2#) and the high human activity area (4#) of the reservoir. Water samples from these sites were extracted for DNA. Microbial biomass in the water samples was collected onto 0.22-&#x3bc;m membrane filters (Millipore) and stored in a refrigerator at &#x2212;80 &#xb0;C. Total genomic DNA was extracted from the membrane filters by the cetyltrimethylammonium bromide (CTAB) method as described by <xref ref-type="bibr" rid="B77">Xu et&#xa0;al. (2010)</xref>. The quality and concentration of DNA were determined by measuring the 260 nm and 280 nm absorbance using a spectrophotometer.</p>
</sec>
<sec id="s2_4">
<label>2.4</label>
<title>Metagenomic sequencing and data mining</title>
<p>The 2 &#xb5;g DNA samples were mechanically interrupted by ultrasound, and then 300 bp DNA fragments were selected for library construction using NEBNext<sup>&#xae;</sup> UltraTM DNA Library Prep Kit for Illumina (NEB, USA) following the manufacturer&#x2019;s instructions. High-throughput sequencing of microbial metagenomic sample libraries was performed using Illumina HiSeq2500. Fastp (v 0.23.1) software was used to filter the raw sequencing data according to its default parameters to obtain high-quality sequencing data (<xref ref-type="bibr" rid="B7">Chen et&#xa0;al., 2018</xref>). The filtered high-quality data was used to perform metagenomic assembly using MEGAHIT software in default mode and filtered for contig sequences shorter than 300 bp (<xref ref-type="bibr" rid="B37">Li et&#xa0;al., 2015</xref>). The metagenomic assembly results were evaluated using QUAST software (<xref ref-type="bibr" rid="B19">Gurevich et&#xa0;al., 2013</xref>). The MetaGeneMark software (v 2.10) was used for gene prediction (<xref ref-type="bibr" rid="B14">Fu et&#xa0;al., 2012</xref>). Redundancy removal was performed using the MMseqs2 software with a 95% similarity threshold and a 90% coverage threshold (<xref ref-type="bibr" rid="B46">Mirdita et&#xa0;al., 2019</xref>). Non-redundant contigs were compared with the KEGG (Kyoto Encyclopedia of Genes and Genomes) database using BLAST. A contig was identified as the sequence of the functional gene if the BLAST hit (BLASTn, e-value cut-off: 10<sup>&#x2212;5</sup>) had a sequence identity of &gt; 90% (<xref ref-type="bibr" rid="B33">Kristiansson et&#xa0;al., 2011</xref>). Non-redundant contigs were compared to the Nr (Non-Redundant protein) database and annotated as characteristic sequences of the species based on their best BLASTn hits (nucleotide sequence identity &gt; 90%) with a threshold e-value of 10<sup>&#x2212;5</sup>. To calculate the relative abundance of KEGG functional genes and species abundance in metagenomic samples, the raw reads were mapped back to non-redundant contigs using bbmap (v 37.81) and then homogenized using the R package vegan (v 2.5-7) to eliminate the effect of total readings when comparing abundance between samples (<xref ref-type="bibr" rid="B68">Wang C. et&#xa0;al., 2021</xref>). Based on the gene functional composition matrix and species composition matrix obtained from Beta diversity analysis, samples were hierarchically clustered by the Unweighted pair-group method with arithmetic mean (UPGMA) through R language tools to determine the similarity of gene functional composition and species composition among samples (<xref ref-type="bibr" rid="B16">Giangreco et&#xa0;al., 2010</xref>). The closer the samples were, the shorter the branch lengths were, indicating that the functional composition or species composition was more similar between samples. Spearman correlations between environmental factors and functional genes and species, respectively, were analyzed using the R package psych (v 2.2.5), and correlation heat maps were drawn using the R package pheatmap (v 1.0.12). The nucleotide sequences were deposited in SRA database under accession numbers PRJNA895910.</p>
</sec>
<sec id="s2_5">
<label>2.5</label>
<title>Quantile regression</title>
<p>Before performing quantile regression analysis, all independent variables need to be unit normalized (X = X &#x2212; Xmin/Xmax &#x2212; Xmin) due to the wide range of values of the original data. A variance inflation factor (VIF) greater than 10 is generally considered to represent a serious covariance problem in the model (<xref ref-type="bibr" rid="B13">Fornaroli et&#xa0;al., 2016</xref>). To reduce multicollinearity, independent variable screening is required, and VIF (VIF &lt; 10) is used to stepwise select variables. Quantile regression was used to study the linear relationship among 2-MIB and geosmin concentrations and environmental variables at 5 quantiles (0.05th, 0.1th, 0.25th, 0.50th, 0.75th, 0.90th, and 0.95th). Quantile regression models can estimate the upper or lower boundaries of 2-MIB and geosmin concentrations to measure limiting factors. The relationships between univariate environmental variables and 2-MIB or geosmin concentrations were fitted as linear, exponential, logarithmic, and quadratic curves. The statistical analyses used the quantreg package in R Project software (<xref ref-type="bibr" rid="B39">Lipsitz et&#xa0;al., 2016</xref>). Due to the small sample size (n = 122), we converted Akaike Information Criterion (AIC) to the corrected Akaike Information Criterion (AICc) for every studied quantile. AICc differences (&#x394;i = AICci &#x2212; minimum AICc) were used to choose the best-fitting model and to calculate a set of Akaike weights (<italic>w</italic>i) (<xref ref-type="bibr" rid="B27">Johnson and Omland, 2004</xref>). We determined the best model for the quantile under study by averaging the <italic>w</italic>i of each model from all five quantile model selection analyses. In general, variables from univariate models greater than 10% <italic>w</italic>i were selected for subsequent analyses (<xref ref-type="bibr" rid="B2">Allen and Vaughn, 2010</xref>). We then used the variables and shapes from the best-fit univariate model to fit the multivariate quantile regression model.</p>
</sec>
</sec>
<sec id="s3" sec-type="results">
<label>3</label>
<title>Results</title>
<sec id="s3_1">
<label>3.1</label>
<title>Phytoplankton community and odor compounds</title>
<p>A total of 103 genera of cyanophyta (20 genera), bacilariophyta (21 genera), chlorophyta (46 genera), cryptophyta (2 genera), chrysophyta (4 genera), pyrrophyta (4 genera), euglenophyta (4 genera), and xanthophyta (2 genera) were identified from 2018 to 2021 (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2A</bold>
</xref>). Cyanophyta (94.62%), bacilariophyta (2.84%) and chlorophyta (1.74%) were the main taxa, whereas the other algal abundances together accounted for only 0.80%. The dominant genera wer<italic>e Pseudanabaena, Cylinderspermopsis, Aphanizonmenon, Microcystis, Panktothrix, Leptolyngbya, Raphidiopsis, Synedra, Merimopedia</italic>, and <italic>Limnothrix</italic>, which represented 43.77, 16.48, 9.67, 6.24,5.49, 4.90, 1.90, 1.63 and 1.50% of the phytoplankton community.</p>
<fig id="f2" position="float">
<label>Figure&#xa0;2</label>
<caption>
<p>
<bold>(A)</bold> The variations of the phytoplankton community in the Yuqiao Reservoir. <bold>(B)</bold> Concentrations of 2-MIB from the Yuqiao Reservoir during 2018&#x2013;2021. <bold>(C)</bold> Concentrations of geosmin from the Yuqiao Reservoir during 2018&#x2013;2021.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g002.tif"/>
</fig>
<p>The variation characteristics of 2-MIB and geosmin concentrations were shown in <xref ref-type="fig" rid="f2">
<bold>Figures&#xa0;2B, C</bold>
</xref>. The concentrations of 2-MIB ranged from 0 to 938.30 ng/L, with an annual average of 103.58 &#xb1; 128.13 ng/L. The annual variation of 2-MIB concentrations showed a bimodal pattern. It is noteworthy that 2-MIB concentrations were below the odor threshold in March and April during the survey period. Geosmin concentrations ranged from 0 to 193 ng/L with an average of 14.29 &#xb1; 27.95 ng/L. From 2018 to 2021, the concentration of geosmin decreases year by year. Geosmin concentrations reached the maximum in August 2018 and November 2019. Geosmin concentration for 2020 to 2021 was very low with an average of 3.35 &#xb1; 3.77 ng/L.</p>
<p>Functional genes of terpenoid backone biosynthesis and biosynthesis of secondary metabolites pathway directly related to 2-MIB and geosmin synthesis at each point have high expression levels in June and July 2021 (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3A</bold>
</xref>). The expression levels of functional genes in these two pathways were lower in November 2021.</p>
<fig id="f3" position="float">
<label>Figure&#xa0;3</label>
<caption>
<p>
<bold>(A)</bold> Correlation heatmap for the relationship between environmental samples and functional genes. <bold>(B)</bold> Correlation heatmap for the relationship between environmental factors and functional genes. * <italic>p</italic> &lt; 0.05; ** <italic>p</italic> &lt; 0.01.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g003.tif"/>
</fig>
</sec>
<sec id="s3_2">
<label>3.2</label>
<title>Spatio-temporal distribution of odor-producers</title>
<p>Powerful macrogenomic analysis of 2-MIB and geosmin biosynthesis genes was used to explore to identify potential odor-producers and their dynamics in the Yuqiao Reservoir. Based on the four distance matrices obtained from Beta diversity analysis, the samples were hierarchically clustered using UPGMA through R language tools to determine the similarity of species composition among samples (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4A</bold>
</xref>). The results showed that the species composition of samples from the same month clustered together, and the species composition of samples from the same month was more similar. As shown in <xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4A</bold>
</xref>, <italic>Pseudanabaena</italic> and <italic>Acidimicrobium</italic> were the predominant bacterial genera. The relative abundance of <italic>Pseudanabaena</italic> sp. gradually increased with the increase of months, and the maximum relative abundance of <italic>Pseudanabaena</italic> sp. was 17.93% in November. The relative abundance of <italic>Acidimicrobium</italic> sp. ranged from 1.62% to 4.65%, with the maximum value in July and the minimum value in November.</p>
<fig id="f4" position="float">
<label>Figure&#xa0;4</label>
<caption>
<p>
<bold>(A)</bold> Cluster analysis and microorganism distribution of environmental samples. <bold>(B)</bold> The variation of 2-MIB-producer by metagenomic sequencing. <bold>(C)</bold> The variation of geosmin-producer by metagenomic sequencing. <bold>(D)</bold> Variation trend of odor compounds concentrations and the 2-MIB-producer cell density. <bold>(E)</bold> Variation trend of odor compounds concentrations and the geosmin-producer cell density.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g004.tif"/>
</fig>
<p>Geosmin-producers were <italic>Streptosporangium caverna</italic> and <italic>Dolichospermum circinale</italic> based on the analysis of geosmin synthase genes (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4B</bold>
</xref>). <italic>Streptomyces</italic> was found only at 2# in June. No geosmin-producer was found in 1# in July, 2# in July, 3# in October, and 4# in November. The percentages of <italic>Dolichospermum circinale</italic> were 0%, 75%, 59%, 67%, and 83% from June to November excluding September. The content of geosmin in the reservoir was detected by gas chromatography-mass spectrometry (GC-MS), and geosmin in June was below the detection limit. Geosmin concentrations in the remaining four months were in the following order: October (7.41 &#xb1; 0.85 ng/L) &gt; August (3.96 &#xb1; 1.26 ng/L) &gt; July (2.47 &#xb1; 1.22 ng/L) &gt; November (1.72 &#xb1; 0.39 ng/L).</p>
<p>According to the 2-MIB synthesis pathway analysis, 2-MIB-producers were <italic>Pseudanabaena</italic> sp. dqh15, <italic>Microcoleus pseudautumnalis</italic> Ak1609, <italic>Pseudanabaena limnetica</italic>, and <italic>Planktothricoides raciborskii</italic> (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4C</bold>
</xref>). The relative abundance of <italic>Microcoleus pseudautumnalis</italic> Ak1609 and <italic>Planktothricoides raciborskii</italic> tended to increase from June to July and decrease from August to November. <italic>Pseudanabaena</italic> sp. is the main producer of 2-MIB, with <italic>Pseudanabaena</italic> sp. dqh15 highly dominating. 2-MIB concentrations in the five months followed the order: July (208.59 &#xb1; 87.61 ng/L) &gt; June (77.01 &#xb1; 36.61 ng/L) &gt; October (72.43 &#xb1; 16.42 ng/L) &gt; August (34.86 &#xb1; 10.22 ng/L) &gt; November (33.50 &#xb1; 5.10 ng/L). Temperature (R<sup>2</sup> = 0.60), transparency (R<sup>2</sup> = 0.61), total phosphorus (R<sup>2</sup> = 0.43), total nitrogen (R<sup>2</sup> = 0.38), ammonia nitrogen (R<sup>2</sup> = 0.52), dissolved oxygen (R<sup>2</sup> = 0.40), oxidation-reduction potential (R<sup>2</sup> = 0.33) and permanganate index (R<sup>2</sup> = 0.35) were the significantly key environmental factors affecting odor-producing phytoplankton communities (<italic>p &lt;</italic> 0.05) (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>). Comparison between the odor-producer cell density and odor compounds concentrations was shown in <xref ref-type="fig" rid="f4">
<bold>Figures&#xa0;4D, E</bold>
</xref>. The variation trends of 2-MIB-producers cell density by microscope and 2-MIB concentration were roughly the same, but the variation trends of geosmin-producers cell density by microscope and geosmin concentration are different.</p>
<fig id="f5" position="float">
<label>Figure&#xa0;5</label>
<caption>
<p>Diagram of RDA analysis between odor-producing phytoplankton communities and environmental factors.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g005.tif"/>
</fig>
</sec>
<sec id="s3_3">
<label>3.3</label>
<title>Drivers of odor compounds</title>
<p>The statistical description of the total 23 environmental variables in the model was shown in <xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>. To reduce multicollinearity among the variables, 21 environmental variables (VIF &lt; 10) were retained, and 2 variables (total algal cell density and cyanobacterial cell density) were removed. These 21 environmental variables were analyzed with 2-MIB or geosmin concentrations separately, and then ranked by Akaike weights.</p>
<table-wrap id="T1" position="float">
<label>Table&#xa0;1</label>
<caption>
<p>Environmental variables investigated in the study.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left">Variable</th>
<th valign="top" align="left">Mean</th>
<th valign="top" align="center">Std. Dev.</th>
<th valign="top" align="left">Min</th>
<th valign="top" align="left">Max</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">Temperature (&#xb0;C)</td>
<td valign="top" align="left">16.19</td>
<td valign="top" align="left">9.52</td>
<td valign="top" align="left">1.00</td>
<td valign="top" align="left">30.40</td>
</tr>
<tr>
<td valign="top" align="left">pH</td>
<td valign="top" align="left">8.58</td>
<td valign="top" align="left">0.38</td>
<td valign="top" align="left">7.90</td>
<td valign="top" align="left">9.93</td>
</tr>
<tr>
<td valign="top" align="left">Ammonia nitrogen (mg/L)</td>
<td valign="top" align="left">0.24</td>
<td valign="top" align="left">0.16</td>
<td valign="top" align="left">0.05</td>
<td valign="top" align="left">1.22</td>
</tr>
<tr>
<td valign="top" align="left">Total nitrogen (mg/L)</td>
<td valign="top" align="left">2.40</td>
<td valign="top" align="left">1.40</td>
<td valign="top" align="left">0.31</td>
<td valign="top" align="left">6.53</td>
</tr>
<tr>
<td valign="top" align="left">Total phosphorus (mg/L)</td>
<td valign="top" align="left">0.06</td>
<td valign="top" align="left">0.05</td>
<td valign="top" align="left">0.01</td>
<td valign="top" align="left">0.25</td>
</tr>
<tr>
<td valign="top" align="left">Total nitrogen/total phosphorus</td>
<td valign="top" align="left">63.25</td>
<td valign="top" align="left">65.30</td>
<td valign="top" align="left">4.48</td>
<td valign="top" align="left">288.00</td>
</tr>
<tr>
<td valign="top" align="left">Permanganate index (mg/L)</td>
<td valign="top" align="left">3.48</td>
<td valign="top" align="left">1.38</td>
<td valign="top" align="left">0.10</td>
<td valign="top" align="left">6.30</td>
</tr>
<tr>
<td valign="top" align="left">Dissolved oxygen (mg/L)</td>
<td valign="top" align="left">10.29</td>
<td valign="top" align="left">2.80</td>
<td valign="top" align="left">2.70</td>
<td valign="top" align="left">16.42</td>
</tr>
<tr>
<td valign="top" align="left">Chlorophyll <italic>a</italic> (mg/L)</td>
<td valign="top" align="left">0.04</td>
<td valign="top" align="left">0.03</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">0.17</td>
</tr>
<tr>
<td valign="top" align="left">total algae cell density (cells/L)</td>
<td valign="top" align="left">1.27E+08</td>
<td valign="top" align="left">1.63E+08</td>
<td valign="top" align="left">1.94E+06</td>
<td valign="top" align="left">8.47E+08</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Microcystis</italic> cell density (cells/L)</td>
<td valign="top" align="left">6.33E+06</td>
<td valign="top" align="left">1.29E+07</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">8.69E+07</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density (cells/L)</td>
<td valign="top" align="left">5.82E+05</td>
<td valign="top" align="left">1.76E+06</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">8.00E+06</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Aphanizomenon</italic> cell density (cells/L)</td>
<td valign="top" align="left">4.73E+06</td>
<td valign="top" align="left">1.17E+07</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">1.10E+08</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Planktothrix</italic> cell density (cells/L)</td>
<td valign="top" align="left">5.53E+06</td>
<td valign="top" align="left">1.52E+07</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">8.59E+07</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Anabaena</italic> cell density (cells/L)</td>
<td valign="top" align="left">1.14E+06</td>
<td valign="top" align="left">2.73E+06</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">1.73E+07</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Cylindrospermopsis</italic> cell density (cells/L)</td>
<td valign="top" align="left">1.24E+07</td>
<td valign="top" align="left">3.12E+07</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">2.12E+08</td>
</tr>
<tr>
<td valign="top" align="left">
<italic>Pseudanabaena</italic> cell density (cells/L)</td>
<td valign="top" align="left">6.85E+07</td>
<td valign="top" align="left">1.04E+08</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">5.68E+08</td>
</tr>
<tr>
<td valign="top" align="left">Cyanophyta cell density (cells/L)</td>
<td valign="top" align="left">1.16E+08</td>
<td valign="top" align="left">1.63E+08</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">8.32E+08</td>
</tr>
<tr>
<td valign="top" align="left">Chlorophyta cell density (cells/L)</td>
<td valign="top" align="left">4.96E+06</td>
<td valign="top" align="left">4.83E+06</td>
<td valign="top" align="left">3.10E+05</td>
<td valign="top" align="left">2.41E+07</td>
</tr>
<tr>
<td valign="top" align="left">Bacillariophyta cell density (cells/L)</td>
<td valign="top" align="left">5.07E+06</td>
<td valign="top" align="left">4.36E+06</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">2.44E+07</td>
</tr>
<tr>
<td valign="top" align="left">Cryptophyta cell density (cells/L)</td>
<td valign="top" align="left">2.00E+05</td>
<td valign="top" align="left">4.40E+05</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">2.77E+06</td>
</tr>
<tr>
<td valign="top" align="left">Chrysophyta cell density (cells/L)</td>
<td valign="top" align="left">2.24E+05</td>
<td valign="top" align="left">7.30E+05</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">5.46E+06</td>
</tr>
<tr>
<td valign="top" align="left">Euglenophyta cell density (cells/L)</td>
<td valign="top" align="left">5.00E+04</td>
<td valign="top" align="left">1.25E+05</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">6.45E+05</td>
</tr>
<tr>
<td valign="top" align="left">2-MIB (ng/L)</td>
<td valign="top" align="left">98.81</td>
<td valign="top" align="left">112.79</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">938.30</td>
</tr>
<tr>
<td valign="top" align="left">Geosmin (ng/L)</td>
<td valign="top" align="left">8.51</td>
<td valign="top" align="left">13.31</td>
<td valign="top" align="left">0.00</td>
<td valign="top" align="left">97.00</td>
</tr>
</tbody>
</table>
</table-wrap>
<p>To better describe 2-MIB and geosmin concentrations, we selected the models with average Akaike weights greater than 10% of the highest one for multiple quantile regression analysis (<xref ref-type="table" rid="T2">
<bold>Table&#xa0;2</bold>
</xref>). For 2-MIB concentration, the selected univariate model had a quadratic relationship with permanganate index (<italic>w</italic>i = 0.30), followed by a linear relationship with chlorophyll <italic>a</italic> (<italic>w</italic>i = 0.23), a logarithmic relationship with <italic>Aphanizomenon</italic> cell density (<italic>w</italic>i = 0.18), a quadratic relationship with <italic>Oscillatoria</italic> cell density (<italic>w</italic>i = 0.14), a logarithmic relationship with <italic>Pseudanabaena</italic> cell density (<italic>w</italic>i = 0.06) and a logarithmic relationship with temperature (<italic>w</italic>i = 0.05), respectively. For geosmin concentrations, the selected univariate model was a quadratic relationship with <italic>Oscillatoria</italic> cell density (<italic>w</italic>i = 0.44), permanganate index (<italic>w</italic>i = 0.34), and temperature (<italic>w</italic>i = 0.11), and a logarithmic relationship with <italic>Cylindrospermopsis</italic> cell density (<italic>w</italic>i = 0.10).</p>
<table-wrap id="T2" position="float">
<label>Table&#xa0;2</label>
<caption>
<p>The selection of univariate quantile regression models for 2-MIB and geosmin concentrations.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="middle" align="left" rowspan="2">Rank</th>
<th valign="middle" align="left" colspan="3">2-MIB</th>
<th valign="top" align="left" colspan="3">Geosmin</th>
</tr>
<tr>
<th valign="middle" align="left">Model</th>
<th valign="middle" align="left">Shape</th>
<th valign="middle" align="left">Average <italic>w</italic>i
</th>
<th valign="middle" align="left">Model</th>
<th valign="middle" align="left">Shape</th>
<th valign="middle" align="left">Average <italic>w</italic>i
</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="middle" align="left">1</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.30</td>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.44</td>
</tr>
<tr>
<td valign="middle" align="left">2</td>
<td valign="top" align="left">Chlorophyll <italic>a</italic>
</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">0.23</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.34</td>
</tr>
<tr>
<td valign="middle" align="left">3</td>
<td valign="top" align="left">
<italic>Aphanizomenon</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">0.18</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.11</td>
</tr>
<tr>
<td valign="middle" align="left">4</td>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.14</td>
<td valign="top" align="left">
<italic>Cylindrospermopsis</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">0.10</td>
</tr>
<tr>
<td valign="middle" align="left">5</td>
<td valign="top" align="left">
<italic>Pseudanabaena</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">0.06</td>
<td valign="top" align="left">Cryptophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">3.35E-03</td>
</tr>
<tr>
<td valign="middle" align="left">6</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.05</td>
<td valign="top" align="left">Bacillariophyta cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">1.15E-03</td>
</tr>
<tr>
<td valign="middle" align="left">7</td>
<td valign="top" align="left">Dissolved oxygen</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">0.02</td>
<td valign="top" align="left">Chlorophyll <italic>a</italic>
</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">9.18E-04</td>
</tr>
<tr>
<td valign="middle" align="left">8</td>
<td valign="top" align="left">
<italic>Microcystis</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">0.01</td>
<td valign="top" align="left">Null model</td>
<td valign="top" align="left"/>
<td valign="top" align="left">2.60E-04</td>
</tr>
<tr>
<td valign="middle" align="left">9</td>
<td valign="top" align="left">pH</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">1.87E-03</td>
<td valign="top" align="left">Euglenophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">1.66E-04</td>
</tr>
<tr>
<td valign="middle" align="left">10</td>
<td valign="top" align="left">Total phosphorus</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">2.62E-04</td>
<td valign="top" align="left">
<italic>Planktothrix</italic> cell density</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">11</td>
<td valign="top" align="left">Ammonia nitrogen</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">5.79E-05</td>
<td valign="top" align="left">Ammonia nitrogen</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">12</td>
<td valign="top" align="left">Chlorophyta cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">4.59E-05</td>
<td valign="top" align="left">
<italic>Aphanizomenon</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">13</td>
<td valign="top" align="left">
<italic>Anabaena</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">1.73E-05</td>
<td valign="top" align="left">
<italic>Microcystis</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">14</td>
<td valign="top" align="left">
<italic>Cylindrospermopsis</italic> cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">1.30E-05</td>
<td valign="top" align="left">Chlorophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">15</td>
<td valign="top" align="left">Total nitrogen</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">5.30E-06</td>
<td valign="top" align="left">
<italic>Anabaena</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">16</td>
<td valign="top" align="left">Total nitrogen/total phosphorus</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.44E-06</td>
<td valign="top" align="left">Chrysophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">9.23E-05</td>
</tr>
<tr>
<td valign="middle" align="left">17</td>
<td valign="top" align="left">Bacillariophyta cell density</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">2.01E-06</td>
<td valign="top" align="left">
<italic>Pseudanabaena cell density</italic>
</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.55E-05</td>
</tr>
<tr>
<td valign="middle" align="left">18</td>
<td valign="top" align="left">Cryptophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">1.41E-06</td>
<td valign="top" align="left">Total nitrogen</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.41E-05</td>
</tr>
<tr>
<td valign="middle" align="left">19</td>
<td valign="top" align="left">Chrysophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">5.13E-07</td>
<td valign="top" align="left">Total nitrogen/total phosphorus</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.22E-05</td>
</tr>
<tr>
<td valign="middle" align="left">20</td>
<td valign="top" align="left">Euglenophyta cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">3.47E-07</td>
<td valign="top" align="left">Dissolved oxygen</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.22E-05</td>
</tr>
<tr>
<td valign="middle" align="left">21</td>
<td valign="top" align="left">
<italic>Planktothrix</italic> cell density</td>
<td valign="top" align="left">Log</td>
<td valign="top" align="left">2.18E-07</td>
<td valign="top" align="left">pH</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.22E-05</td>
</tr>
<tr>
<td valign="middle" align="left">22</td>
<td valign="top" align="left">Null model</td>
<td valign="middle" align="left"/>
<td valign="top" align="left">6.77E-08</td>
<td valign="top" align="left">Total phosphorus</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">3.22E-05</td>
</tr>
</tbody>
</table>
</table-wrap>
<p>The model considering permanganate index and <italic>Pseudanabaena</italic> cell density as the independent variables was selected as the best (averaged <italic>w</italic>i = 0.57) for describing 2-MIB concentrations (<xref ref-type="table" rid="T3">
<bold>Table&#xa0;3</bold>
</xref>). The best-fit model that considered both permanganate index and temperature explained geosmin concentrations better (average <italic>w</italic>i = 0.35). For 2-MIB and geosmin concentrations, the 5th quantile is a constant model (y = 0), so the lower boundary is not considered. Only the upper boundary represented by the 95h quantile is used to describe how 2-MIB and geosmin concentrations vary through the two environmental factors. 2-MIB concentrations were generally higher in high permanganate index and increased with increasing <italic>Pseudanabaena</italic> cell density (<xref ref-type="fig" rid="f6">
<bold>Figure&#xa0;6A</bold>
</xref>). Geosmin concentrations had higher concentrations at lower or higher temperatures and increased with increasing COD<sub>Mn</sub> (<xref ref-type="fig" rid="f6">
<bold>Figure&#xa0;6B</bold>
</xref>). The final model equations of quantile regression are in <xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Tables&#xa0;1&#x2013;3</bold>
</xref>.</p>
<table-wrap-group id="T3" position="float">
<label>Table&#xa0;3</label>
<caption>
<p>The selection of multivariate quantile regression models for 2-MIB and geosmin concentrations.</p>
</caption>
<table-wrap>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left" rowspan="3">Rank</th>
<th valign="top" colspan="5" align="left">2-MIB</th>
</tr>
<tr>
<th valign="top" align="center" rowspan="2">Average <italic>w</italic>i</th>
<th valign="top" colspan="2" align="left">1st Variable</th>
<th valign="top" colspan="2" align="left">2nd Variable</th>
</tr>
<tr>
<th valign="top" align="left">Variable</th>
<th valign="top" align="left">Shape</th>
<th valign="top" align="left">Variable</th>
<th valign="top" align="left">Shape</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">1</td>
<td valign="top" align="left">0.57</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">
<italic>Pseudanabaena</italic> cell density</td>
<td valign="top" align="left">Log</td>
</tr>
<tr>
<td valign="top" align="left">2</td>
<td valign="top" align="left">0.22</td>
<td valign="top" align="left">Chlorophyll <italic>a</italic>
</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">Qua</td>
</tr>
<tr>
<td valign="top" align="left">3</td>
<td valign="top" align="left">0.14</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density</td>
<td valign="top" align="left">Qua</td>
</tr>
<tr>
<td valign="top" align="left">4</td>
<td valign="top" align="left">0.04</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">
<italic>Aphanizomenon</italic> cell density</td>
<td valign="top" align="left">Log</td>
</tr>
<tr>
<td valign="top" align="left">5</td>
<td valign="top" align="left">0.01</td>
<td valign="top" align="left">Chlorophyll <italic>a</italic>
</td>
<td valign="top" align="left">Lin</td>
<td valign="top" align="left">
<italic>Pseudanabaena</italic> cell density</td>
<td valign="top" align="left">Log</td>
</tr>
</tbody>
</table>
</table-wrap>
<table-wrap>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left" rowspan="3">Rank</th>
<th valign="top" colspan="5" align="left">Geosmin</th>
</tr>
<tr>
<th valign="top" align="left" rowspan="2">Average <italic>w</italic>i</th>
<th valign="top" colspan="2" align="left">1st Variable</th>
<th valign="top" colspan="2" align="left">2nd Variable</th>
</tr>
<tr>
<th valign="top" align="left">Variable</th>
<th valign="top" align="left">Shape</th>
<th valign="top" align="left">Variable</th>
<th valign="top" align="left">Shape</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" align="left">1</td>
<td valign="top" align="left">0.35</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">Temperature</td>
<td valign="top" align="left">Qua</td>
</tr>
<tr>
<td valign="top" align="left">2</td>
<td valign="top" align="left">0.28</td>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left"/>
<td valign="top" align="left"/>
</tr>
<tr>
<td valign="top" align="left">3</td>
<td valign="top" align="left">0.10</td>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">
<italic>Cylindrospermopsis</italic> cell density</td>
<td valign="top" align="left">Log</td>
</tr>
<tr>
<td valign="top" align="left">4</td>
<td valign="top" align="left">0.09</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left">
<italic>Oscillatoria</italic> cell density</td>
<td valign="top" align="left">Qua</td>
</tr>
<tr>
<td valign="top" align="left">5</td>
<td valign="top" align="left">0.09</td>
<td valign="top" align="left">Permanganate index</td>
<td valign="top" align="left">Qua</td>
<td valign="top" align="left"/>
<td valign="top" align="left"/>
</tr>
</tbody>
</table>
</table-wrap>
</table-wrap-group>
<fig id="f6" position="float">
<label>Figure&#xa0;6</label>
<caption>
<p>Multivariate quantile regression models for <bold>(A)</bold> 2-MIB concentrations and <bold>(B)</bold> geosmin concentrations. Surfaces represent the 95th quantile regression model.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g006.tif"/>
</fig>
<p>According to the correlation heatmap in <xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3B</bold>
</xref>, oxidation-reduction potential (<italic>p</italic> &lt; 0.05), permanganate index (<italic>p &lt;</italic> 0.01), pH (<italic>p &lt;</italic> 0.01), chlorophyll <italic>a</italic> (<italic>p &lt;</italic> 0.01), temperature (<italic>p &lt;</italic> 0.01), and total phosphorus (<italic>p &lt;</italic> 0.01) were positively correlated with Biosynthesis of secondary metabolites synthesis pathways, whereas dissolved oxygen (<italic>p &lt;</italic> 0.01), transparency (<italic>p &lt;</italic> 0.01), and phosphate (p &lt; 0.05) were negatively correlated with the pathway. Terpenoid backone biosynthesis was positively correlated with oxidation-reduction potential, permanganate index (<italic>p</italic> &lt; 0.01), pH (<italic>p &lt;</italic> 0.01), chlorophyll <italic>a</italic> (<italic>p &lt;</italic> 0.01), temperature (<italic>p &lt;</italic> 0.01), and total phosphorus (<italic>p &lt;</italic> 0.01), and negatively correlated with dissolved oxygen (<italic>p &lt;</italic> 0.05), transparency (<italic>p &lt;</italic> 0.01), and phosphate (<italic>p &lt;</italic> 0.05).</p>
</sec>
</sec>
<sec id="s4" sec-type="discussion">
<label>4</label>
<title>Discussion</title>
<p>The Yuqiao Reservoir has experienced eutrophication during the last decade, accompanied by the frequent occurrence of bloom events (<xref ref-type="bibr" rid="B24">Huo et&#xa0;al., 2018</xref>). The coexistence of multiple odors and multiple odor-producers has threatened the Yuqiao Reservoir since 2018. Many studies have shown that phytoplankton was important sources of odor compounds with little consideration given to bacteria and actinomycetes, probably because phytoplankton is easier to observe, isolate and culture compared to actinomycetes and bacteria (<xref ref-type="bibr" rid="B76">Wu et&#xa0;al., 2021b</xref>). Amplicon sequencing is commonly used to study microbial diversity in the environment, and the main genes marked are 16srDNA, 18S rDNA and internal transcribed spacer (ITS) (<xref ref-type="bibr" rid="B40">Liu et&#xa0;al., 2021</xref>). Amplicon sequencing to analyze microbial functional gene diversity is flawed due to the immaturity of comparative databases and primers. Metagenomic sequencing provides more information, not only extending taxonomic resolution to the species or strain level but also providing potential functional information (<xref ref-type="bibr" rid="B79">Xu et&#xa0;al., 2018</xref>). However, metagenomic sequencing requires more funding, high sample quality requirements and increased difficulty in data analysis. <italic>Streptosporangium</italic> sp. is a member of the family Actinomycetaceae (<xref ref-type="bibr" rid="B29">Kemmerling et&#xa0;al., 1993</xref>). 2-MIB and geosmin were first identified from the actinomycete and its molecular formula and exact chemical structure were determined successively in the following years (<xref ref-type="bibr" rid="B15">Gerber and Lecheval, 1965</xref>; <xref ref-type="bibr" rid="B45">Medsker et&#xa0;al., 1968</xref>). <italic>Dolichospermum</italic> sp., <italic>Pseudoanabaena</italic> sp., <italic>Microcoleu</italic> sp., and <italic>Planktothricoides</italic> sp. have been frequently reported to be odor-producers all over the world (<xref ref-type="bibr" rid="B47">Niiyama et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B82">Zhang et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B1">Alghanmi et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B23">Huang et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B31">Kim et&#xa0;al., 2020</xref>). <italic>Planktothricoides raciborskii</italic> and <italic>Dolichospermum circinale</italic> were not detected by microscopic observation from June to September 2021. Since <italic>Planktothricoides raciborskii</italic> and <italic>Microcoleus pseudautumnalis</italic> Ak1609 are benthic cyanobacteria, water samples were collected only 0.5 m below the water surface for fixation (<xref ref-type="bibr" rid="B60">Stielow and Ballantine, 2003</xref>; <xref ref-type="bibr" rid="B62">Su et&#xa0;al., 2015</xref>). Odor-producing and non-odor-producing strains often coexist in the field (<xref ref-type="bibr" rid="B5">Cai et&#xa0;al., 2017</xref>). Changes in the rise and fall of odor-producing and non-odor-producing strains are considered to be the most important factors regulating the concentration of odors in freshwater (<xref ref-type="bibr" rid="B11">Devi et&#xa0;al., 2021</xref>). The abundance of <italic>Pseudanabaena</italic> sp., <italic>Microcoleus</italic> sp., and <italic>Planktothricoides</italic> sp. in the microbial community in July was 1.27%, 0.04%, and 0.87%, respectively, while the abundance of <italic>Pseudanabaena</italic> sp., <italic>Microcoleus</italic> sp. and <italic>Planktothricoides</italic> sp. in the 2-MIB producers in the same month was 29.28%, 45.49%, and 25.22%, respectively. It can be speculated that the proportion of 2-MIB-producing taxa was higher in <italic>Microcoleus</italic> sp. and <italic>Planktothricoides</italic> sp. than in <italic>Pseudanabaena</italic> sp. The relationship between odor compounds and microorganisms in water bodies is a widespread concern at home and abroad. The risk of 2-MIB exceeding 15 ng/L in water was as high as 90% when the <italic>Planktothrix</italic> sp. density was more than 4.0 &#xd7; 10<sup>5</sup> cells/L (<xref ref-type="bibr" rid="B62">Su et&#xa0;al., 2015</xref>). <italic>Phormidium</italic> sp. was the 2-MIB-producing microorganism, accounting for 80&#x2013;95% of the algal cell density, with an estimated 2-MIB production of 0.022 pg/cell (<xref ref-type="bibr" rid="B65">Sun et&#xa0;al., 2013</xref>). A strong positive correlation was detected between 2-MIB concentrations and <italic>Pseudanabaena</italic> sp. cell numbers (<xref ref-type="bibr" rid="B36">Lee et&#xa0;al., 2022</xref>). Geosmin concentrations was positively correlated with cyanobacteria (R<sup>2</sup> = 0.84, <italic>p &lt;</italic> 0.0001) and not significantly correlated with actinomycetes (R<sup>2</sup> = 0.01, p = 0.709) (<xref ref-type="bibr" rid="B35">Lee J. E. et&#xa0;al., 2020</xref>). Significant correlation between odor-producers cell densities and 2-MIB/geosmin concentrations was acquired according to the Pearson correlation test (<italic>p &lt;</italic> 0.01) (<xref ref-type="fig" rid="f7">
<bold>Figure&#xa0;7</bold>
</xref>). The concentration of geosmin/2-MIB in the reservoir may be controlled not only by the density of odor-producer cells but also by environmental factors (<xref ref-type="bibr" rid="B82">Zhang et&#xa0;al., 2016</xref>).</p>
<fig id="f7" position="float">
<label>Figure&#xa0;7</label>
<caption>
<p>Correlation relationship between odor-producers cell densities and odor compounds concentrations. <bold>(A)</bold> 2-MIB <bold>(B)</bold> Geosmin.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fevo-11-1216567-g007.tif"/>
</fig>
<p>Different odor-producing microorganisms vary greatly in their ability to produce odor, and external physicochemical and biological factors may affect growth and odor production (<xref ref-type="bibr" rid="B73">Wang et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B72">Wang et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B81">Zhang et&#xa0;al., 2020</xref>). COD<sub>Mn</sub> was the driver for both 2-MIB and geosmin, and both odors increased with increasing COD<sub>Mn</sub>. Geosmin and 2-MIB are terpenoids produced and secreted by microorganisms (<xref ref-type="bibr" rid="B42">Lovell et&#xa0;al., 1986</xref>). In the correlation analysis between functional genes and environmental factors, a significantly positive correlation between COD<sub>Mn</sub> and the biosynthetic pathway of secondary metabolites/terpenoid backbone biosynthesis pathway could be found (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3B</bold>
</xref>). In previous studies, several empirical models have been developed based on the strong correlation between chlorophyll <italic>a</italic> or COD and odor compounds (<xref ref-type="bibr" rid="B3">Bowmer et&#xa0;al., 1992</xref>; <xref ref-type="bibr" rid="B56">Rosen et&#xa0;al., 1992</xref>; <xref ref-type="bibr" rid="B50">Panova and Dimkov, 2008</xref>; <xref ref-type="bibr" rid="B30">Kim et&#xa0;al., 2015</xref>). COD had a significant effect on the T&amp;O prediction model and was positively correlated with &#x3b1;-&#x3b2;-ionone concentrations (<xref ref-type="bibr" rid="B53">Qi et&#xa0;al., 2012</xref>). The odor occurrence of 2-MIB and geosmin was effectively predicted and validated using multiple linear regression and artificial neural network techniques with chlorophyll <italic>a</italic> and COD as explanatory variables (<xref ref-type="bibr" rid="B64">Sugiura et&#xa0;al., 2004</xref>). COD is an important indicator to determine the pollution of organic matter in water. The decay of aquatic plants in the Yuqiao Reservoir led to an increase in COD<sub>Mn</sub>, higher COD<sub>Mn</sub> plays a stress factor to phytoplankton and significantly stimulated the synthetize of T&amp;O, and made the increase of odor compounds concentration (<xref ref-type="supplementary-material" rid="SM1">
<bold>Supplementary Figure&#xa0;1</bold>
</xref>). The three temperature treatments could be arranged in descending order as 10 &#xb0;C, 35 &#xb0;C, and 25 &#xb0;C based on geosmin produced by <italic>Dolichospermum ucrainica</italic> (<xref ref-type="bibr" rid="B69">Wang and Li, 2015</xref>). The production of geosmin was increased with incubation temperature (20&#x2013;30 &#xb0;C) by <italic>Streptomyces roseoflavus</italic> (<xref ref-type="bibr" rid="B67">Tung et&#xa0;al., 2005</xref>). <italic>Streptomyces tendae</italic> cultures incubated at 30 and 45 &#xb0;C for 48 h produced more geosmin than those incubated at 10 and 20 &#xb0;C (<xref ref-type="bibr" rid="B12">Dionigi and Ingram, 1994</xref>). Many studies found that when external conditions were not adapted to the growth of Cyanobacteria and its growth rate was low, more 2-MIB and geosmin were produced by individual algal cells (<xref ref-type="bibr" rid="B83">Zimba et&#xa0;al., 1999</xref>; <xref ref-type="bibr" rid="B72">Wang et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B82">Zhang et&#xa0;al., 2016</xref>). The direct precursors of geosmin and 2-MIB synthesis, GPP and FPP, are intermediate products of the chlorophyll <italic>a</italic> synthesis pathway. Some experimental evidence suggests that the biosynthesis of geosmin and 2-MIB in cyanobacteria is associated with chlorophyll <italic>a</italic> synthesis (<xref ref-type="bibr" rid="B17">Giglio et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B80">Zhang et&#xa0;al., 2009</xref>; <xref ref-type="bibr" rid="B18">Giglio et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B73">Wang et&#xa0;al., 2011</xref>). Since geosmin and 2-MIB have common precursors with chlorophyll <italic>a</italic> synthesis in cyanobacterial cells, the synthesis of earthy-musty odorants and photosynthetic pigments is largely a competition for substrates, i.e., GPP and FPP tend to be converted to 2-MIB and geosmin during the phase of reduced photosynthetic activity and pigment synthesis (<xref ref-type="bibr" rid="B17">Giglio et&#xa0;al., 2008</xref>; <xref ref-type="bibr" rid="B80">Zhang et&#xa0;al., 2009</xref>; <xref ref-type="bibr" rid="B18">Giglio et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B73">Wang et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B69">Wang and Li, 2015</xref>). At lower or higher temperatures, the production of geosmin by <italic>Dolichospermum</italic> sp. and <italic>Streptomyces</italic> sp. is elevated. To our knowledge, our study is one of the first applications of quantile regression in long-term studies of odorant substances in reservoirs, a method that can help managers focus on specific factors, focus future monitoring efforts, and critically provide information.</p>
</sec>
<sec id="s5" sec-type="conclusions">
<label>5</label>
<title>Conclusion</title>
<p>A four-year survey revealed the distribution of 2-MIB/geosmin and the distribution of odor-producers in the Yuqiao Reservoir, and the following conclusions were drawn. Metagenome unmasked that <italic>Pseudanabaena</italic> sp. dqh15, <italic>Microcoleus pseudautumnalis</italic> Ak1609, <italic>Pseudanabaena limnetica</italic>, and <italic>Planktothricoides raciborskii</italic> were the 2-MIB-producers, while <italic>Streptosporangium caverna</italic> and <italic>Dolichospermum circinale</italic> were the geosmin-producers. Metagenome is a rapid, high-precision and high-throughput method for detecting odor-producers. Quantile regression analysis indicated <italic>Pseudanabaena</italic> sp. and COD<sub>Mn</sub> were the best predictors of 2-MIB concentrations, temperature and COD<sub>Mn</sub> were the most useful parameters for describing geosmin concentration change. Combining quantile regression and metagenome results showed that COD<sub>Mn</sub> was an important driver of odor compounds. Quantile regression has the advantages of not assuming the existence of moment functions, not being affected by anomalous observations, and not making any distributional assumptions. When accurate and complete data are obtained, quantile regression can quickly find the drivers of odor compounds in the reservoir.</p>
</sec>
<sec id="s6" sec-type="data-availability">
<title>Data availability statement</title>
<p>The datasets presented in this study can be found in online repositories. The names of the repository/repositories and accession number(s) can be found below: <ext-link ext-link-type="uri" xlink:href="https://www.ncbi.nlm.nih.gov/">https://www.ncbi.nlm.nih.gov/</ext-link>, PRJNA895910.</p>
</sec>
<sec id="s7" sec-type="author-contributions">
<title>Author contributions</title>
<p>PQ: Conceptualization, methodology, software, visualization, formal analysis, writing &#x2013; original draft, data curation. YZ: Investigation. WM: Project administration. GS: Software, validation. YB: Writing &#x2013; review &amp; editing, supervision. All authors contributed to the article and approved the submitted version.</p>
</sec>
</body>
<back>
<sec id="s8" sec-type="funding-information">
<title>Funding</title>
<p>This research was Jointly funded by National key R&amp;D plan (No: 2021YFC3200900) and National Natural Science Foundation of China (No: 31971477).</p>
</sec>
<ack>
<title>Acknowledgments</title>
<p>The calculating resource was supported by the Wuhan Branch, Supercomputing Center, Chinese Academy of Sciences. We thank all members in the Analysis and Testing Center at IHB for technical supports.</p>
</ack>
<sec id="s9" sec-type="COI-statement">
<title>Conflict of interest</title>
<p>The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
</sec>
<sec id="s10" sec-type="disclaimer">
<title>Publisher&#x2019;s note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
<sec id="s11" sec-type="supplementary-material">
<title>Supplementary material</title>
<p>The Supplementary Material for this article can be found online at: <ext-link ext-link-type="uri" xlink:href="https://www.frontiersin.org/articles/10.3389/fevo.2023.1216567/full#supplementary-material">https://www.frontiersin.org/articles/10.3389/fevo.2023.1216567/full#supplementary-material</ext-link>
</p>
<supplementary-material xlink:href="DataSheet_1.pdf" id="SM1" mimetype="application/pdf"/>
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