EGU26-8649, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-8649
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 06 May, 15:35–15:45 (CEST)
 
Room 2.23
Depth-dependent patterns of microbial carbon and nitrogen metabolism functions in deep East African Rift Valley Lakes
Xiaolong Yao1, Zhonghua Zhao1,2, Ismael Aaron Kimirei3, and Lu Zhang1,2
Xiaolong Yao et al.
  • 1Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, China
  • 2University of Chinese Academy of Sciences, Nanjing, China
  • 3Tanzania Fisheries Research Institute, Dar es Salaam, Tanzania

East African Great Lakes are globally important waters that regulating carbon and nitrogen sources and sinks. Yet, microbial carbon and nitrogen cycling functions as well as their underlying environmental drivers in tropical deep lakes remain largely unexplored. Here, were collected vertical samples from typical large deep lakes in East African Rift Valley to assess environmental gradients and microbial metabolism functions of primary biogenic elements. We examined vertical distributions of nutrients, dissolved organic matter (DOM) properties, and quantified microbial carbon, nitrogen, and phosphorus cycling genes using high-throughput Quantitative Microbial Ecology Chip (QMEC) technique. Preliminary analyses indicate clear depth-dependent patterns in nutrient availability and microbial functional genes. Dissolved organic matter properties are likely important drivers of the depth patterns of these functional genes. The observed relationships between microbial functional genes and environmental variables provide insights into the vertical organization of microbial biogeochemical functions in deep tropical lakes.

How to cite: Yao, X., Zhao, Z., Kimirei, I. A., and Zhang, L.: Depth-dependent patterns of microbial carbon and nitrogen metabolism functions in deep East African Rift Valley Lakes, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-8649, https://doi.org/10.5194/egusphere-egu26-8649, 2026.