Seagrass blue carbon spatial patterns at the meadow-scale

• Published in: PloS one 2017-04, Vol.12 (4), p.e0176630-e0176630
• Main Authors: Oreska, Matthew P J, McGlathery, Karen J, Porter, John H
• Format: Article
• Language: English
• Subjects: Age; Autoregressive models; Autoregressive processes; Bathymetry; Carbon; Carbon - metabolism; Carbon dioxide; Coasts; Computer and Information Sciences; Conservation of Natural Resources; Data processing; Earth Sciences; Ecology and Environmental Sciences; Ecosystem; Engineering and Technology; Environmental science; Fluid mechanics; Geologic Sediments - chemistry; Grain size distribution; Grasses; Internet; Marine ecology; Models, Biological; Organic carbon; Particle size; Physical Sciences; Proximity; Restoration; Sediments; Social Sciences; Soil density; Soil erosion; Spatial distribution; Stratigraphy; Tidal currents; Wave power; Zostera marina; Zosteraceae - metabolism; Zosteraceae - physiology
• ISSN: 1932-6203; 1932-6203
• DOI: 10.1371/journal.pone.0176630

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 (Corg) concentrations may vary with distance from the meadow edge, resulting in spatial gradients that affect the accuracy of stock estimates. We mapped sediment Corg concentrations throughout a large (6 km2) restored seagrass meadow to determine whether Corg distribution patterns exist at different spatial scales. The meadow originated from ≤1-acre plots seeded between 2001 and 2004, so we expected Corg 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 Corg concentrations. We found that edge proximity, not age, significantly predicted the meadow-scale Corg distribution. We also evaluated relationships between Corg 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 Corg distribution. Strong correlations between Corg, 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 Corg 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 Corg, approximately 1200 t more Corg 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.