EGU26-5773, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-5773
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 08 May, 11:40–11:50 (CEST)
 
Room 2.23
Sources, Sinks and Subsidies of Organic Carbon in Saltmarsh Habitats 
Alex Houston1, Mark H Garnett2, and William E N Austin1,3
Alex Houston et al.
  • 1University of St Andrews, University of St Andrews, Geography and Sustainable Development, St Andrews, United Kingdom (ah383@st-andrews.ac.uk)
  • 2NEIF Radiocarbon Laboratory, SUERC, Rankine Avenue, East Kilbride, United Kingdom
  • 3Scottish Association for Marine Science, Oban, Argyll, United Kingdom

Saltmarshes accumulate and store organic carbon through the drawdown of atmospheric CO2 by photosynthesising vegetation (autochthonous carbon), and the deposition of externally derived carbon (allochthonous) during tidal inundation. These organic carbon sources can be different ages and remain stored in the soil for variable lengths of time, from minutes to millennia. International policy frameworks recognise that the management of saltmarshes can provide a climate mitigation service, yet uncertainties remain regarding the inclusion of allochthonous organic carbon in saltmarsh projects.

We employed a novel methodology to compare the radiocarbon (14C) contents of saltmarsh soils and CO2 evolved from aerobic laboratory incubations to show that young (14C-enriched) organic carbon is preferentially respired over old (14C-depleted) organic carbon. The 14C contents of the respired CO2 were compared to the 14C content of carbon pools defined by their thermal reactivity, measured by ramped oxidation. In most cases, the 14C content of the most thermally labile carbon pool was closest to the 14C content of the CO2 evolved from aerobic incubations of the same soils, suggesting the thermal and biological lability of saltmarsh soil carbon in oxic conditions is closely related. These results highlight the role of saltmarshes as stores of both old, thermally recalcitrant organic carbon, as well as younger, thermally labile organic carbon. Management interventions, such as restoration, may help mitigate CO2 emissions by limiting oxygen exposure and preserving these stores of thermally labile carbon.

We also highlight inconsistencies in the treatment of allochthonous carbon across blue carbon (saltmarsh, seagrass and mangrove) accounting methodologies. A review of these frameworks and their scientific basis reveals a lack of standardized, evidence-based approaches for determining the proportion of allochthonous carbon that should be discounted in additionality calculations. This research provides crucial evidence towards addressing these gaps and improving the robustness of blue carbon policy and accounting.

How to cite: Houston, A., Garnett, M. H., and Austin, W. E. N.: Sources, Sinks and Subsidies of Organic Carbon in Saltmarsh Habitats , EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-5773, https://doi.org/10.5194/egusphere-egu26-5773, 2026.