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Updated: Feb 10, 2026

Coral Reef Arks: An In Situ Mesocosm and Toolkit for Assembling Reef Communities
Published on: January 6, 2023
Artificial reefs promote coastal carbon stabilization potential through hydrological condition and microbial pathways
Lu Wang1, Zhenlin Liang1, Dechen Lu2
1Marine College, Shandong University, Weihai, Shandong, 264209, China; Key Laboratory of Modern Marine Ranching Technology of Weihai, Weihai 264209, Shandong, China.
Artificial reefs (ARs) enhance coastal carbon storage by altering water flow and microbial activity. Complex ARs promote finer sediments and increase organic carbon, aiding long-term carbon stabilization.
Area of Science:
- Marine Ecology
- Geochemistry
- Microbial Ecology
Background:
- Artificial reefs (ARs) influence hydrodynamics and benthic microbial processes.
- The connection between ARs, hydrodynamics, microbial functions, and coastal carbon stabilization is not fully understood.
Purpose of the Study:
- To investigate how artificial reefs impact coastal carbon stabilization.
- To link hydrodynamic changes and microbial functions to sediment organic carbon content.
Main Methods:
- Hydrodynamic modeling, sediment geochemistry, fluorescence spectroscopy, and metagenomics were employed.
- Experiments were conducted across different AR habitats in the northern Yellow Sea.
- A 42-day dark incubation assessed microbial reworking of dissolved organic matter.
Main Results:
- Complex ARs increased upwelling and turbulence, leading to finer sediments and higher total organic carbon (TOC).
- Hydrodynamics, microbial genes, and environmental factors explained variations in TOC and humic-like fluorescence.
- Microbial activity enriched humic-like dissolved organic matter (DOM) and increased genes for aromatic compound transformation and nitrogen redox pathways.
Conclusions:
- ARs modulate hydrodynamics, which, coupled with nitrogen-redox microbial functions, enhances carbon stabilization.
- Findings support a framework where ARs promote carbon storage through altered water flow and microbial processes.
- Humic-like DOM enrichment and benthic carbon storage are key indicators of AR-driven carbon stabilization.
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