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. 2019 Dec 4;9(1):18275.
doi: 10.1038/s41598-019-54893-6.

Preservation and recovery of mangrove ecosystem carbon stocks in abandoned shrimp ponds

Affiliations

Preservation and recovery of mangrove ecosystem carbon stocks in abandoned shrimp ponds

Angie Elwin et al. Sci Rep. .

Abstract

Mangrove forests capture and store exceptionally large amounts of carbon and are increasingly recognised as an important ecosystem for carbon sequestration. Yet land-use change in the tropics threatens this ecosystem and its critical 'blue carbon' (carbon stored in marine and coastal habitats) stores. The expansion of shrimp aquaculture is among the major causes of mangrove loss globally. Here, we assess the impact of mangrove to shrimp pond conversion on ecosystem carbon stocks, and carbon losses and gains over time after ponds are abandoned. Our assessment is based on an intensive field inventory of carbon stocks at a coastal setting in Thailand. We show that although up to 70% of ecosystem carbon is lost when mangroves are converted to shrimp ponds, some abandoned ponds contain deep mangrove soils (>2.5 m) and large carbon reservoirs exceeding 865 t carbon per hectare. We also found a positive recovery trajectory for carbon stocks in the upper soil layer (0-15 cm) of a chronosequence of abandoned ponds, associated with natural mangrove regeneration. Our data suggest that mangrove carbon pools can rebuild in abandoned ponds over time in areas exposed to tidal flushing.

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Conflict of interest statement

The authors declare no competing interests.

Figures

Figure 1
Figure 1
Total Ecosystem C stock of mangroves and abandoned shrimp ponds. (a) The mean value for all mangrove forest sites compared to the mean of all pond sites. (b) Ecosystem C stocks separated into aboveground and belowground C for the mangrove sites and sites of each pond category. Mangroves contained on average 1,029.5 t C ha−1 and ponds contained on average 541.65 t C ha−1. Mean total ecosystem C stocks of the pond sites was significantly lower than the mangrove sites (p = 0.0015).
Figure 2
Figure 2
Soil C stock (t C ha−1) within each depth interval down to 1 m. Data shows means for the mangrove sites and the four pond categories.
Figure 3
Figure 3
Changes in the soil properties (mean ± 1 standard error (SE)) of the mangroves and the four pond categories with depth. (a) Soil C density. (b) Soil bulk density. (c) Soil C concentration (%).
Figure 4
Figure 4
Soil C stock (t C ha−1) in the 15-cm soil layer. Data shows means for the mangrove sites and the four pond categories.
Figure 5
Figure 5
Density of (a) saplings, and (b) seedlings recorded at three of the pond categories (abandoned 10 years, 15 years, 22 years).
Figure 6
Figure 6
Map of the study area, Koh Klang (Krabi Province). Displayed are the location of the mangrove sites (black triangles) and abandoned shrimp pond sites (pink circles).

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