Oct 2026· Water Research· Vol 309 Pt A, pp.
127137
· 0 citations· 48 references
Medicine
Abstract
Hydrological regulation can enhance carbon accumulation in coastal wetlands, yet whether this carbon is merely retained or transformed into chemically recalcitrant forms remains unclear. Here, we investigated sediment geochemistry, DOM molecular composition, and microbial communities across adjacent subtropical coastal habitats in Hong Kong, including semi-enclosed, hydrologically regulated ponds embedded within mangrove wetlands (GW), mangroves, tidal flats, and seagrass habitats. Compared with adjacent open habitats, GW sediments contained substantially higher organic carbon stocks and isotopic signatures indicative of enhanced retention of terrestrial and mangrove-derived organic matter. FT-ICR MS revealed a pronounced enrichment of high-molecular-weight, highly unsaturated, aromatic, and oxidized molecules, indicating the accumulation of chemically recalcitrant DOM. This molecular shift coincided with a distinct microbial community. Redundancy analysis revealed strong associations among microbial community structure, DOM molecular characteristics, and sedimentary δ15N, while variation partitioning showed that DOM molecular variation was jointly associated with organic matter source, sediment environment, and microbial community composition. Differential abundance analysis further identified 108 genera significantly enriched in GW sediments. Within GW, exploratory structural equation modeling suggested a potential pathway linking substrate conditions and the GW-enriched microbial assemblage with δ15N and recalcitrant DOM, while Random Forest analysis identified candidate genera strongly associated with specific DOM molecular characteristics. Together, these patterns suggest that hydrological regulation enhances organic matter retention while creating conditions conducive to chemically recalcitrant DOM accumulation, with potential implications for carbon persistence in coastal wetlands.
Bacteria-dissolved organic matter (DOM) interactions profoundly influence organic carbon fate along the land-ocean aquatic continuum. Halogenated DOM (H-DOM) is recognized as a widespread component of the DOM pool in natural waters, but its interactions with bacterial communities and ecological functions remain poorly...
Zhen-Li Guo, Hua-Long Hong, Guang-Long Zhang et al.· Water Research· 0 citations
Estuarine wetlands are important 'blue carbon' sinks, yet their carbon storage exhibits pronounced spatial heterogeneity. The mechanisms by which vegetation distribution and tidal flooding affect sediment organic carbon (SOC) content and stabilization remain unclear. Here, we analyzed the SOC fractions, microbial commu...
Huan-Peng Li, Hong-Jie Zhang, Run-Han Yang et al.· Environmental Research· 1 citation
Accelerated sea level rise, combined with human-induced changes to hydrology and sediment transport, threatens the long-term persistence of coastal wetlands. Sediment addition is increasingly used to enhance wetland resilience to sea level rise, and incorporating biochar, a carbon-rich material produced through pyrolys...
Brittany P. Wilburn, R. Ikeh, Marina Potapova et al.· Journal of Environmental Man...· 0 citations
Estuarine intertidal sediments occur in freshwater-seawater mixing zones where hydrological processes simultaneously alter salinity and redox conditions, potentially regulating dissolved organic matter (DOM) transformation and microbial processes. However, how DOM and its interactions with microbial communities respond...
Dissolved organic matter (DOM) plays a key role in lake carbon cycling, yet the geographic patterns and environmental associations of sediment DOM chemodiversity remain poorly understood. Here, we analyzed sediment DOM from 92 lakes across China spanning a broad latitudinal gradient of 23–50°N using Fourier‐transform i...
Fan-Fan Meng, Jin Zeng, Ang Hu et al.· Global Biogeochemical Cycles· 0 citations
ABSTRACT Coastal wetlands, including mangrove-cordgrass mosaics, are among Earth’s most effective carbon stores sequestering >1 Pg C/year. Rapid sea level rise, warming, and storm intensification are now reshaping these habitats. Vegetation type influences root exudates, sediment redox profiles, and organic matter qual...
G. Aitolo, I. Rambo, R. Weisend et al.· mSystems· 0 citations
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