RESOLVING THE LEDGER
This is one outlet's own report from Phys.org — the article as it was filed. Other outlets are covering the same event; open the full story to compare every source side by side.
See the full story · 1 sources
edited by Gaby Clark , reviewed by Robert Egan
This article has been reviewed according to Science X's editorial process and policies . Editors have highlighted the following attributes while ensuring the content's credibility:
Add as preferred source Salt marshes are coastal wetlands that are alternately inundated and exposed by tides. These marshes, like other coastal ecosystems, are hotspots of carbon cycling.
But salt marshes sit at the complex intersection of land and marine ecosystems, and there is still uncertainty over how they cycle, store and release carbon. One major uncertainty is how much carbon is transported by water rather than stored in marsh soils. Once transported, this carbon may be buried, used by organisms and released into the atmosphere, or exported to the ocean. But this lateral transport between salt marshes and coastal waters has largely been overlooked in research on salt marshes' carbon storage potential.
He and team dove into this understudied process by focusing on tidal creeks, which run high or dry based on the state of the tides. These creeks can move water—and its dissolved components—around the landscape or out to sea, so quantifying their carbon movement is an important part of quantifying salt marshes' carbon budgets. The paper is published in the Journal of Geophysical Research: Biogeosciences .
The researchers installed sensors to collect data on water flow, water chemistry and environmental parameters in a salt marsh creek in coastal Louisiana. They also collected water samples to track dissolved inorganic and organic carbon and total alkalinity.
These observations continued for 3 years, building a rare, continuous water chemistry data set that captures daily, seasonal and annual variability. In contrast, most studies of salt marsh carbon transport use short-term monitoring, an approach that can miss hydrological and biogeochemical changes that occur with tides, seasons and storms.
After taking water flow into account, the team calculated how much carbon was stored or exported. They found that more dissolved organic and inorganic carbon was exported from the marsh than was stored. That net flux was driven primarily by different concentrations of carbon in falling versus rising tides. This pattern held at daily, monthly and seasonal time scales. Lateral transport, then, can act as a dynamic control on a salt marsh's carbon sequestration, boosting or damping it over time.
Total alkalinity also varied with the tides, suggesting that salt marshes can affect the acidity of downstream waters.
The findings suggest that the capacity of tidal streams to transport dissolved carbon out of salt marshes could be larger than that of sediment burial, making lateral carbon transport in tidal creeks a major overlooked component of coastal carbon models and blue carbon assessments.
Quantifying lateral carbon transport in more salt marshes will improve those assessments' accuracy and deepen our understanding of the role salt marshes play in the global carbon budget, the authors say.
Songjie He et al, Multi‐Year Continuous Lateral Fluxes of Dissolved Carbon From a Microtidal Saltmarsh, Journal of Geophysical Research: Biogeosciences (2026). DOI: 10.1029/2026jg009760
MA in English, copy editor since 2021 with experience in higher education and health content. Dedicated to trustworthy science news. Full profile →
Bachelor's in mathematical biology, Master's in creative writing. Well-traveled with unique perspectives on science and language. Full profile →
This story is republished courtesy of Eos, hosted by the American Geophysical Union. Read the original story here .
AIPROPX is an independent multi-source news index — we track, compare, and connect coverage from across the web into one place you won't find anywhere else.