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Mangroves in Myanmar

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Abstract

The mangrove extent in Myanmar, according to the most recent forest resources assessment in 2020, has been estimated as 1.12 million acres. Among three main tracts of mangroves—Rakhine coastline, Ayeyarwady delta, and Tanintharyi coastline—the mangroves in the Tanintharyi coastline have now turned into the largest areal extent despite the fact that the Ayeyarwady delta had the largest in the past. With a large share of the Bay of Bengal Large Marine Ecosystem, coastal and delta ecosystems including mangroves, coral reefs, seagrass beds, beaches, and dunes largely flourish throughout the Myanmar coastline. In this context, the Tanintharyi coast showed the highest species diversity of mangrove flora while the least species diversity was observed in the Ayeyarwady delta. Provided that a total of ten prominent provisioning, regulating, supporting, and cultural services were considered, fishery nursery and habitat has shown its highest value in the mangrove ecosystem services, followed by coastal protection. In particular for the latter services of coastal protection, local communities and their tremendous properties were saved, and lifelong lessons were learned during the deadliest impacts of Cyclone Nargis 2008. The mangrove ecosystems in Myanmar, however, have been alarmingly threatened due to overexploitation of fuelwood and charcoal production; mangrove conversion to other land uses such as rice fields, shrimp farming, and salt pans; coastal and delta development with human settlement; improper revenue collection on mangrove products in forest management; and climate change and natural disasters. One of the major measures to tackle the existing issues and problems is community-based forest management, called “community forestry (CF)” in mangroves that is a remarkable initiative since 1995 in the aspects of partnership, participation, and decentralization in managing the mangroves in Myanmar. In connection with the findings on the CF study regarding the regeneration of some resilient mangrove species after the impact of Cyclone Nargis, coppice management would be supportive and beneficial to local communities in their own mangrove management. The case study in the chapter demonstrated as well that most of the local stakeholders had fairly sufficient awareness and attitudes to enable active participation in mangrove restoration although there were slight differences between the different stakeholders. In particular, poorer attitudes were observed in some migrant communities compared to the settled communities. In developing a mangrove management strategy, inclusiveness should, therefore, be one of the key take-home messages by prioritizing the subsistence needs of the local people plus economic benefits.

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... Furthermore, the Yangon Region bottleneck area is close to the Dedaye, which is a potentially important dispersal route connecting the eastern section of the Ayeyaewady mangroves and the western section of the Yangon mangroves (Fig. 3b). However, there are considerable losses of mangrove cover in Ayeyarwady and the adjacent Yangon Region due to pressures from human use, and damage from natural disasters in recent decades (De Alban et al., 2020;Aung, 2022). Illegal logging within protected areas, including the Meinmahla Kyun wildlife sanctuary (Wang, 2016), has resulted in sparse mangrove trees, indicating that deforestation extends beyond unprotected regions (Webb et al., 2014). ...
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The resilience perspective is increasingly used as an approach for understanding the dynamics of social–ecological systems. This article presents the origin of the resilience perspective and provides an overview of its development to date. With roots in one branch of ecology and the discovery of multiple basins of attraction in ecosystems in the 1960–1970s, it inspired social and environmental scientists to challenge the dominant stable equilibrium view. The resilience approach emphasizes non-linear dynamics, thresholds, uncertainty and surprise, how periods of gradual change interplay with periods of rapid change and how such dynamics interact across temporal and spatial scales. The history was dominated by empirical observations of ecosystem dynamics interpreted in mathematical models, developing into the adaptive management approach for responding to ecosystem change. Serious attempts to integrate the social dimension is currently taking place in resilience work reflected in the large numbers of sciences involved in explorative studies and new discoveries of linked social–ecological systems. Recent advances include understanding of social processes like, social learning and social memory, mental models and knowledge–system integration, visioning and scenario building, leadership, agents and actor groups, social networks, institutional and organizational inertia and change, adaptive capacity, transformability and systems of adaptive governance that allow for management of essential ecosystem services.
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Storms are considered to have significant impacts on the development of chenier plains, particularly through the devastation of mangrove vegetation, but also in terms of winnowing sand and shell from mudflats and forming chenier ridges. Shoal Bay, in the Beagle Gulf, northern Australia, contains a small chenier plain, which was struck by a severe tropical cyclone, Cyclone Tracy, on Christmas Day 1974 as it devastated the city of Darwin. The morphology, vegetation and stratigraphy of the plain are described. The plain is underlain by lower intertidal sand with shell hash. A radiocarbon age of 6130 years BP, indicates mangrove colonisation of this flat at the time that sea level stabilised around its present level after the postglacial transgression. Subsequently, progradation of mudflats has occurred, especially around 2300 years ago, and shells of this age are found both in growth position from within the mudflats, and incorporated into the shelly chenier ridges. A further phase of build-out, and subsequent erosion is reflected by stumps and in situ bivalves being excavated presently on the foreshore, radiocarbon dating about 900–1100 years BP. Within this context of evolution, Cyclone Tracy can be seen to have had severe consequences upon the patterning of mangroves, with extensive windthrow of Ceriops, and defoliation of Rhizophora at the western end of the plain. Recovery of the mangrove vegetation has been gradual, and is still incomplete. However, the storm had little influence on the pattern of landform development. Indeed, the aerial photographic sequence indicates a trend by which sand shoals are gradually reworked landwards, in places moving through mangrove vegetation. The study suggests that rather than pronounced regional episodes of alternative mudflat buildout and erosion, both processes occur simultaneously at different points along this foreshore.
Article
February 23-25, 2010, Phuket, Thailand Nine species of seagrass were found around Lampi and neighbouring islands of the Myeik Archipelago, Myanmar. Those species were Cymodocea rotundata, Cymodocea serrulata, Enhalus acoroides, Halodule pinifolia, Halodule uninervis, Halophila beccarii, Halophila decipiens, Halophila ovalis and Thalassia hemprichii. Meadows occurred on the east side of islands on flats inshore of coral reefs where they were sheltered from the monsoons. The largest meadows occurred on the eastern sides of Nyaung Wee, Bo Cho and Lampi Islands, and were mixed intertidal meadows with up to six species, not including E. acoroides or H. decipiens. The former was concentrated around the Ko Phawt Island group and the latter occurred in clear water greater than five metres deep on the west side of Nyaung Wee Island. The size of the most significant meadow at Lampi Island was estimated to be 28 hectares. Estimates were made of percent seagrass cover along transects across that meadow. Sampled sites with seagrass averaged 43% cover, including 27% C. rotundata, 11% T. hemprichii, 5% H. ovalis. Dugong feeding trails were found in dense patches of H. ovalis in March 2008 at Lampi, and at both Nyaung Wee and Lampi Islands in November 2008. Those trails are the first concrete evidence of the occurrence of a resident dugong population in the Myeik Archipelago.
Article
The hypothesis that species richness in tropical, tidal (mangrove) forests in the eastern and western portions of the Australian continent is influenced by different suites of environmental parameters is investigated. Maximum and minimum temperatures were positively correlated with species richness in both regions. Increasing temperatures led to increases in species richness. Tidal amplitude is inversely related to species richness in the east and west. Estuary length, the size of the surrounding catchment, rainfall variation and the frequency of tropical cyclones have significant effects on species richness in eastern but not western mangrove forests. Estuaries which are long and have large catchments tend to have more species than those being shorter with smaller catchments. Although similarities do exist, there are important differences between eastern and western mangrove forests in the response of species richness to the environment.
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