1201 / 2024-09-20 16:43:38
High variability in organic carbon sources and microbial activities in the hadopelagic waters
Atacama Trench,Particulate organic carbon,dark carbon fixation,microbial community respiration
摘要录用
Xinxin Li / Southern University of Science and Technology
Xin Zhao / Southern University of Science and Technology
Hongyue Dang / Xiamen University
Ronnie Glud / University of Southern Denmark
Hadal sediments are recognized as organic carbon depocenters with intensified microbial activity compared

to adjacent abyssal sites due to focusing of relatively labile organic materials. However, the sources and turnover

of hadopelagic organic carbon and its linkages to microbial activities have not been studied. We present the first

synergic research on particulate organic carbon, dark carbon fixation, and size-fractionated microbial community

respiration proxy over the Atacama Trench. The results demonstrate that all parameters attenuate rapidly

from surface to mesopelagic water ( 1000 m). Progressing deeper, values remain relatively stable throughout

bathypelagic ( 4000 m) and abyssopelagic ( 6000 m) waters. However, in the hadopelagic zone (> 6000 m),

highly variable values indicate dynamic organic carbon sources and microbial activities in the deepest trench.

On average, 71% of the microbial community respiration proxy is attributable to particle-associated communities,

indicating importance of particles for microbial metabolism. No apparent relationship was observed

between the microbial community respiration proxy and microbial 16S rRNA gene abundance below the epipelagic

depth, indicating variable supply and quality of organic carbon likely constrained heterotrophic activities

rather than microbial abundances in the deep ocean. The depth-integrated dark carbon fixation (> 1000 m)

accounts for 11.5%  7.6% of the surface net primary production, of which 2.9%  0.4% is from hadopelagic

depth. Dark carbon fixation is thus an important in situ organic carbon source for hadal life. This study suggests

that high variability in organic carbon sources and microbial activities in the hadopelagic trench cannot be simply

extrapolated from findings in the shallower dark ocean (e.g., 1000–6000 m).
重要日期
  • 会议日期

    01月14日

    2025

    01月17日

    2025

  • 09月27日 2024

    初稿截稿日期

  • 12月14日 2024

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
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