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Seasonal variability in lateral carbon exchange and dissolved organic matter exports from a salt-marsh tidal creek of the Yellow River Delta

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Coastal wetlands play a vital role in the global carbon cycle, yet accurately assessing their carbon sink capacity requires considering lateral carbon exchange. New research quantifies seasonal carbon fluxes within a Yellow River Delta salt-marsh tidal creek, revealing an overall net export of -662.06 g C m−2 yr−1, with significant seasonal shifts. Dominated by terrestrially-derived organic matter, export pulses during low tides are driven by sediment resuspension.
Seasonal variability in lateral carbon exchange and dissolved organic matter exports from a salt-marsh tidal creek of the Yellow River Delta

The burgeoning field of blue carbon research continues to refine our understanding of coastal ecosystems’ role in the global carbon cycle, and a recent study published in Carbon stocks in intertidal Ulva blooms and adjacent sediments in Korean tidal flats highlights the complexity of these systems. This new research, focusing on a salt-marsh tidal creek within the Yellow River Delta, adds crucial detail to that complexity by quantifying the seasonal variability of lateral carbon exchange. While we’ve long recognized coastal wetlands as significant carbon sinks, this study underscores that a complete carbon budget requires a rigorous accounting of carbon fluxes *through* tidal creeks – a previously underestimated component. The findings reveal a net annual export of carbon, a significant detail, and a stark contrast to the often-assumed role of these wetlands as purely storage environments. Understanding these nuances is vital for accurate climate modeling and the development of effective coastal management strategies, particularly given the ongoing ecological shifts documented in areas like the Abandoned Yellow River Delta, where anthropogenic engineering significantly impacts biogeochemical processes, as detailed in Biogeochemical evolution and iron speciation in the abandoned Yellow River Delta: deciphering the impact of anthropogenic engineering and introduced Spartina alterniflora.

The study’s methodology – combining high-frequency observations of carbon fluxes with analyses of dissolved organic matter (DOM) composition – is particularly noteworthy. The use of optical indices, EEM-PARAFAC, and stable carbon isotopes provides a robust characterization of DOM sources, revealing a dominant contribution from marsh-derived material, especially during warmer months. This suggests a strong link between seasonal plant productivity within the salt marsh and the subsequent export of carbon via the tidal creek. Furthermore, the identification of pronounced low-tide carbon pulses driven by sediment resuspension and porewater drainage adds another layer of complexity. These short-lived events, while individually small, collectively contribute significantly to the overall annual carbon budget, emphasizing the importance of high-resolution monitoring for accurate assessments. These findings resonate with the broader discussion around integrating biological factors, like megafauna, into carbon storage strategies, as explored in Integrating megafauna into blue carbon strategies: dugongs could enhance seagrass carbon storage, indicating that a holistic view of ecosystem processes is paramount.

The implications of this research extend beyond the Yellow River Delta. Salt marshes are widespread coastal habitats globally, and lateral carbon exchange through tidal creeks is likely a common phenomenon. The study’s emphasis on seasonal variability and short-lived export events highlights the need for more comprehensive monitoring programs that capture these dynamic processes. Current blue carbon assessment methodologies often focus on long-term carbon storage rates, potentially overlooking the significant role of lateral fluxes. Integrating these findings into coastal wetland carbon budgets and climate models will require a shift towards more sophisticated, spatially and temporally resolved data collection and analysis. Validated, longitudinal data, as the study champions, are essential for refining our predictive capabilities in a rapidly changing climate.

Looking ahead, a critical question arises: how will increasing freshwater inputs, a consequence of altered precipitation patterns and upstream water management, impact these seasonal carbon exchange dynamics? Will increased runoff lead to greater terrestrial DOM inputs, shifting the sources and composition of exported organic matter? Further empirical research examining the interplay between hydrological changes, DOM sources, and lateral carbon fluxes in salt marsh tidal creeks is urgently needed to ensure accurate assessment of coastal carbon cycling and inform effective ocean stewardship strategies.

Coastal wetlands are key components of the global coastal carbon cycle. However, their carbon sink capacity cannot be fully assessed without considering lateral carbon exchange through tidal creeks. Here, we quantified seasonal and within−tide lateral carbon fluxes in a salt−marsh tidal creek in the Yellow River Delta, and characterized the sources and composition of exported dissolved organic matter (DOM) using optical indices, EEM−PARAFAC, and stable carbon isotopes. The annual carbon budget indicated an overall net lateral export of -662.06 g C m−2 yr−1, but both the magnitude and direction of exchange varied markedly among seasons. Net export was strongest in summer and autumn, whereas winter showed net import under some tidal conditions, particularly for DIC, indicating pronounced seasonal shifts in hydrodynamic connectivity and biogeochemical processing. Exported DOM was strongly influenced by terrestrially derived, highly humified material: low fluorescence index (FI), high humification index (HIX), and predominance of humic−like PARAFAC components pointed to a substantial marsh contribution, especially during warm seasons. Stable carbon isotopes further supported a greater contribution of marsh−derived DOC in summer and autumn. High−frequency observations revealed pronounced low−tide carbon pulses, with elevated DIC, dissolved CO2, POC, and (to a lesser extent) DOC during ebb tide and at low water. Their relationships with turbidity and conductivity suggest that sediment resuspension and porewater drainage were important drivers of these short−lived export events. Overall, lateral exchange through tidal creeks is a major component of carbon cycling in this Yellow River Delta salt marsh; seasonal variability, DOM source characteristics, and low−tide pulsed export should therefore be explicitly incorporated into blue carbon assessments and coastal wetland carbon budgets.

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Tagged with

#salt marsh#tidal creek#lateral carbon exchange#dissolved organic matter (DOM)#carbon cycle#Yellow River Delta#seasonal variability#carbon fluxes#stable carbon isotopes#EEM-PARAFAC#optical indices#blue carbon#hydrodynamic connectivity#biogeochemical processing#DIC#POC#DOC#sediment resuspension#porewater drainage#turbidity
Seasonal variability in lateral carbon exchange and dissolved organic matter exports from a salt-marsh tidal creek of the Yellow River Delta | World Data Ocean