4.3 Article

Carbon Dynamics Vary Among Tidal Marsh Plant Species in a Sea-level Rise Experiment

Journal

WETLANDS
Volume 43, Issue 7, Pages -

Publisher

SPRINGER
DOI: 10.1007/s13157-023-01717-z

Keywords

Bacterial community composition; Carbon flux; Marsh organ; Phragmites; Sea level rise; Spartina; Tidal marsh

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Tidal wetlands, which act as important blue carbon reservoirs, may be affected by sea-level rise (SLR), resulting in changes in carbon cycling and soil microbial communities. In this study, SLR scenarios and vegetation treatments were tested to determine their effects on CO2 fluxes, soil carbon mineralization rates, potential denitrification rates, and microbial community composition. The results showed that increasing inundation frequency due to SLR decreased the carbon sink strength and increased carbon emissions. However, SLR did not impact soil chemistry, microbial processes, or bacterial community structure. Vegetation treatments had a significant effect on carbon flux measurements, with S. alterniflora and S. patens showing higher CO2 uptake and ecosystem respiration compared to P. australis. The findings suggest that plant species play a central role in the carbon dynamics of vegetated tidal marshes undergoing rapid SLR.
Tidal wetlands are important blue carbon reservoirs, but it is unclear how sea-level rise (SLR) may affect carbon cycling and soil microbial communities either by increased inundation frequency or via shifting plant species dominance. We used an in-situ marsh organ experiment to test how SLR-scenarios (0, + 7.5, + 15 cm) and vegetation treatments (Spartina alterniflora, Spartina patens, Phragmites australis, unvegetated controls) altered CO2 fluxes (net ecosystem exchange, ecosystem respiration), soil carbon mineralization rates, potential denitrification rates, and microbial community composition. Increasing inundation frequency with SLR treatments decreased the carbon sink strength and promoted carbon emissions with + 15-cm SLR. However, SLR treatments did not alter soil chemistry, microbial process rates, or bacterial community structure. In contrast, our vegetation treatments affected all carbon flux measurements; S. alterniflora and S. patens had greater CO2 uptake and ecosystem respiration compared to P. australis. Soils associated with Spartina spp. had higher carbon mineralization rates than P. australis or unvegetated controls. Soil bacterial assemblages differed among vegetation treatments but shifted more dramatically over the three-month experiment. As marshes flood more frequently with projected SLR, marsh vegetation composition is predicted to shift towards more flood-tolerant S. alterniflora, which may lead to increased CO2 uptake, though tidal marsh carbon sink strength will likely be offset by increased abundance of unvegetated tidal flats and open water. Our findings suggest that plant species play a central role in ecosystem carbon dynamics in vegetated tidal marshes undergoing rapid SLR.

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