Journal
GLOBAL BIOGEOCHEMICAL CYCLES
Volume 35, Issue 4, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2020GB006848
Keywords
Seagrass; Blue Carbon; CO2 Flux; Eddy Covariance; Carbon Cycle; Air‐ sea interaction
Funding
- DAAD, from German Federal Ministry of Education and Research (BMBF) [57429828]
- US National Science Foundation through the Florida Coastal Everglades Long-Term Ecological Research program [DEB-1237517, DEB-1832229]
- Mexican National Council of Science and Technology (CONACYT) [278608]
- Ecology Commission from Sonora (CEDES)
- Japan Society for the Promotion of Science [JP18H04156]
- Swedish Research Council
- Uppsala University
- French Ministry of Higher Education, Research and Innovation
- ANR PROTIDAL project
- CNES-TOSCA SYNIHAL project
- Aquitaine region
- Projekt DEAL
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Coastal vegetated habitats such as seagrass meadows play a crucial role in mitigating anthropogenic carbon emissions by sequestering CO2 as blue carbon. This study highlights the complex interactions between air-water CO2 exchange and organic carbon storage in seagrass meadows, with a focus on global scale patterns and physical drivers influencing CO2 fluxes. The findings underscore the need for a comprehensive approach to carbon assessments in coastal ecosystems, taking into account both biological and physical factors.
Coastal vegetated habitats like seagrass meadows can mitigate anthropogenic carbon emissions by sequestering CO2 as blue carbon (BC). Already, some coastal ecosystems are actively managed to enhance BC storage, with associated BC stocks included in national greenhouse gas inventories. However, the extent to which BC burial fluxes are enhanced or counteracted by other carbon fluxes, especially air-water CO2 flux (FCO2) remains poorly understood. In this study, we synthesized all available direct FCO2 measurements over seagrass meadows made using atmospheric Eddy Covariance, across a globally representative range of ecotypes. Of the four sites with seasonal data coverage, two were net CO2 sources, with average FCO2 equivalent to 44%-115% of the global average BC burial rate. At the remaining sites, net CO2 uptake was 101%-888% of average BC burial. A wavelet coherence analysis demonstrated that FCO2 was most strongly related to physical factors like temperature, wind, and tides. In particular, tidal forcing was a key driver of global-scale patterns in FCO2, likely due to a combination of lateral carbon exchange, bottom-driven turbulence, and pore-water pumping. Lastly, sea-surface drag coefficients were always greater than the prediction for the open ocean, supporting a universal enhancement of gas-transfer in shallow coastal waters. Our study points to the need for a more comprehensive approach to BC assessments, considering not only organic carbon storage, but also air-water CO2 exchange, and its complex biogeochemical and physical drivers.
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