Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin, 300072, China.
Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin, 300072, China; Tianjin Bohai Rim Coastal Earth Critical Zone National Observation and Research Station, Tianjin, 300072, China.
Water Res. 2024 Sep 15;262:122100. doi: 10.1016/j.watres.2024.122100. Epub 2024 Jul 22.
The production of refractory dissolved organic matter (RDOM) is complex and closely related to microbial consortia in aquatic ecosystems; however, it is still unclear how microorganisms regulate the production of RDOM and its molecular composition in inland waters. Therefore, we conducted a large-scale survey of inland waters and analyzed the optical and mass spectrometric characteristics of DOM, the microbial community and functional genes, as well as related environmental parameters, to understand the abovementioned issues. Here, the RDOM production was found mainly regulated by microbial (e.g., phylogeny and community assembly) rather than other environmental factors in inland waters. Biostatistical analyses and carbon isotopic evidence indicated that the successive microbial processing from labile DOM to RDOM (i.e., carboxyl-rich alicyclic molecules, CRAMs) was widely present in inland waters, involving the microbially mediated carbon skeleton turnover and heteroatom conversion. There was a significant empirical relationship between CRAMs and the ratio of Proteobacteria to Actinobacteria, highlighting the intraspecific interaction of bacteria more important than other microbial groups (i.e., archaea, eukaryotes, and fungi) for the RDOM production. This study demonstrated a fundamental role of microbial regulation in RDOM production within the inland waters, thereby facilitating future estimation of carbon sequestration potential in inland aquatic ecosystems.
难处理溶解性有机质(RDOM)的产生十分复杂,与水生生态系统中的微生物群落密切相关;然而,微生物如何调节内陆水中 RDOM 的产生及其分子组成仍不清楚。因此,我们对内陆水进行了大规模调查,并分析了 DOM 的光学和质谱特征、微生物群落和功能基因以及相关环境参数,以了解上述问题。在这里,发现内陆水中 RDOM 的产生主要受微生物(如系统发育和群落组装)而不是其他环境因素的调节。生物统计分析和碳同位素证据表明,从易处理的 DOM 到 RDOM(即富含羧基的脂环族分子,CRAMs)的连续微生物处理在内陆水中广泛存在,涉及微生物介导的碳骨架周转和杂原子转化。CRAMs 与变形菌门与放线菌门的比值之间存在显著的经验关系,这突出表明细菌的种内相互作用比其他微生物群(即古菌、真核生物和真菌)对 RDOM 的产生更为重要。本研究证明了微生物调节在内陆水中 RDOM 产生中的基础性作用,从而有助于未来对内陆水生态系统碳固存潜力的估计。