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Seagrass blue carbon spatial patterns at the meadow-scale

Most information on seagrass carbon burial derives from point measurements, which are sometimes scaled by meadow area to estimate carbon stocks; however, sediment organic carbon (C(org)) concentrations may vary with distance from the meadow edge, resulting in spatial gradients that affect the accura...

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Detalles Bibliográficos
Autores principales: Oreska, Matthew P. J., McGlathery, Karen J., Porter, John H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5407773/
https://www.ncbi.nlm.nih.gov/pubmed/28448617
http://dx.doi.org/10.1371/journal.pone.0176630
Descripción
Sumario:Most information on seagrass carbon burial derives from point measurements, which are sometimes scaled by meadow area to estimate carbon stocks; however, sediment organic carbon (C(org)) concentrations may vary with distance from the meadow edge, resulting in spatial gradients that affect the accuracy of stock estimates. We mapped sediment C(org) concentrations throughout a large (6 km(2)) restored seagrass meadow to determine whether C(org) distribution patterns exist at different spatial scales. The meadow originated from ≤1-acre plots seeded between 2001 and 2004, so we expected C(org) to vary spatially according to the known meadow age at sample sites and with proximity to the meadow edge. Applying spatial autoregressive models allowed us to control for spatial autocorrelation and quantify the relative effects of edge proximity and age on C(org) concentrations. We found that edge proximity, not age, significantly predicted the meadow-scale C(org) distribution. We also evaluated relationships between C(org) and a variety of specific explanatory variables, including site relative exposure, shoot density, sediment grain size, and bathymetry. Factors known to affect carbon burial at the plot-scale, such as meadow age and shoot density, were not significant controls on the meadow-scale C(org) distribution. Strong correlations between C(org), grain size, and edge proximity suggest that current attenuation increases fine-sediment deposition and, therefore, carbon burial with distance into the meadow. By mapping the sediment C(org) pool, we provide the first accurate quantification of an enhanced carbon stock attributable to seagrass restoration. The top 12 cm of the bed contain 3660 t C(org), approximately 1200 t more C(org) than an equal area of bare sediment. Most of that net increase is concentrated in a meadow area with low tidal current velocities. Managers should account for the effects of meadow configuration and current velocity when estimating seagrass blue carbon stocks. Our results suggest that a large, contiguous meadow should store more blue carbon than an equal area of small meadow patches.