301. Keystone taxa drive the synchronous production of methane and refractory dissolved organic matter in inland waters.
- Author
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Shi, Xinjie, Li, Wanzhu, Wang, Baoli, Liu, Na, Liang, Xia, Yang, Meiling, and Liu, Cong-Qiang
- Abstract
• The synchronous production of CH 4 and RDOM could be widespread in inland waters. • Keystone taxa regulate the intensity of microbial cooperation. • Microbial cooperation links the synchronous production of CH 4 and RDOM. The production of both methane (CH 4) and refractory dissolved organic matter (RDOM) depends on microbial consortia in inland waters, and it is unclear yet the link of these two processes and the underlying microbial regulation mechanisms. Therefore, a large-scale survey was conducted in China's inland waters, with the measurement of CH 4 concentrations, DOM chemical composition, microbial community composition, and relative environmental parameters mainly by chromatographic, optical, mass spectrometric, and high-throughput sequencing analyses, to clarify the abovementioned questions. Here, we found a synchronous production of CH 4 and RDOM linked by microbial consortia in inland waters. The increasing microbial cooperation driven by the keystone taxa (mainly Fluviicola and Polynucleobacter) could promote the transformation of labile DOM into RDOM and meanwhile benefit methanogenic microbial communities to produce CH 4. As such, CH 4 and RDOM showed consistent spatial differences, which were mainly influenced by total nitrogen and dissolved oxygen concentrations. This finding deepened the understanding of microbial-driven carbon transformation and will help to more accurately evaluate the carbon source-sink relationship in inland waters. [Display omitted] [ABSTRACT FROM AUTHOR]
- Published
- 2025
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