6. CONCLUSIONS

Previous Page Table of Contents Next Page

6. CONCLUSIONS

Environmental change occurs at two extremes: (1) slow and incremental (e.g. fishing pressure, pollution) and (2) catastrophic (e.g. tsunamis and other natural disasters). It would appear that humans are very good at responding to catastrophic change but are more accepting of incremental change. This would explain how according to Adger et al. (2005) resilience can be eroded gradually and go unrecognized or be thought unimportant. The lessons learned of increased impacts from the tsunami in chronically impacted and degraded ecosystems should be taken as an alert for future management.

The evidence from the sources reviewed shows strongly that although there are localized cases of clear impact caused directly by the tsunami, most of the fished resources and their supporting ecosystems were not severely impacted by the tsunami but had already been in decline. Such pre-existing trends were acknowledged in the two national workshops run as part of this project in Indonesia and Sri Lanka (MMAF 2006; NARA 2006) though for Indonesia, there was a consensus among participants that there may still be some resources not yet fully exploited in Aceh. Overall, the current condition of resources is the result of these same trends and/or interactive effects resulting from reduced environmental resilience. In this study Maldeniya and Jayamanne (2006), Tampubolon et al. (2006) and others undertaken elsewhere (e.g. India, Salagrama 2006) fisherfolk agreed that declines in fish catches after the tsunami were generally a continuation of existing trends. This observation is generally supported by the scientific studies reviewed. It should be noted, however, that the fisherfolk of the Coromandel Coast were quite clear that the tsunami did influence fisheries resources, as their catches had never been as bad as they were in 2005, particularly during peak fishing seasons. In Aceh and Sri Lanka it was found that fisherfolk generally blamed the loss of boats and gear for this decline, though in some cases they seemed to suggest that abundance of some species had declined after the tsunami. An examination of historical catch data in Sri Lanka showed that declines occurred in all coastal fisheries and often extended back decades. Catch data and the fisherfolk in both countries indicate that catch rates continued to decline after the tsunami. In fact the main post-tsunami issues for the fishing communities raised in both countries were related not to declining catches but to "human factors" such as the rising fuel and falling fish prices.

It is also possible that the long-term effects of the tsunami could include some positive changes in resources, though information is generally lacking at this stage. Salagrama (2006) suggested that the
"vigorous churning" of the waters in the Bay of Bengal from the tsunami contributed to an upwelling from the nutrient-rich benthic strata to the upper layers, and enhanced primary productivity which might be reflected further down the food chain as an increase in fish production over the coming years. In this study, there was evidence from the PRAs that prawn numbers increased in a damaged mangrove in Aceh Jaya in Indonesia and increased temporarily in Galle and Hambantota in Sri Lanka. Hilsa numbers were also increased in Hambantota.

The important lessons learned on fisheries, fished resources and their ecosystems are:

Previous Page Top of Page Next Page