Spatial variation of organic carbon storage and aggregate sizes in the sediment of the Zhangjiang mangrove ecosystem

Abstract

Sediment organic carbon (SOC) in mangrove ecosystem, known as blue carbon, is a crucial component in estuarine carbon cycles. To get a deep insight into the mechanism of SOC accumulation, the sediment physicochemical properties, SOC density and aggregate sizes were investigated among mangrove (Kandelia obovata), saltmarsh (Spartina alterniflora) and mudflats at different elevations (upland mudflat, midland mudflat, lowland mudflat). The results showed that the higher SOC content was observed both in the 0–60 cm of mangrove and in the 0–40 cm of S. alterniflora compared with mudflats (P < 0.05). The SOC density in the top meter ranged from 99 to 202.7 Mg·ha−1 and had vertical difference at all sites. The highest SOC density were found in mangrove, while no difference was observed between S. alterniflora and mudflats. The mean weight diameter of aggregates was higher in the top 60 cm sediment of mangrove while S. alterniflora had no change indicating the capacity of aggregate formation. RDA analysis showed SOC storage could be more explained by the SOC content than bulk density, all sites in the top 40 cm could be well separated. The MWD had the 8.6 % individual effects on SOC content, reflecting the aggregated protection. The mangrove root system favored aggregates formation and physical protection, which facilitate the SOC accumulation. These findings revealed that mangroves restoration could effectively enhance SOC storage, and the mudflat is also significant SOC pool owning to the large bulk density and area. The invasive S. alterniflora did not enhance the SOC storage compared with mudflats and should be controlled in the future work.