Keystone taxa drive the synchronous production of methane and refractory dissolved organic matter in inland waters

Xinjie Shi; Wanzhu Li; Baoli Wang; Meiling Yang; Cong-Qiang Liu

doi:https://doi.org/10.5194/egusphere-egu25-4681

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EGU25-4681, updated on 14 Mar 2025

https://doi.org/10.5194/egusphere-egu25-4681

EGU General Assembly 2025

© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.

Keystone taxa drive the synchronous production of methane and refractory dissolved organic matter in inland waters

Xinjie Shi¹, Wanzhu Li¹, Baoli Wang

^1,2, Meiling Yang¹, and Cong-Qiang Liu^1,2

Xinjie Shi et al.

¹Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China
²Tianjin Bohai Rim Coastal Earth Critical Zone National Observation and Research Station, Tianjin 300072, China

How to cite: Shi, X., Li, W., Wang, B., Yang, M., and Liu, C.-Q.: Keystone taxa drive the synchronous production of methane and refractory dissolved organic matter in inland waters, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-4681, https://doi.org/10.5194/egusphere-egu25-4681, 2025.

This abstract has been withdrawn on 25 Jul 2025.