# Cumulative Impacts of Human Interventions and Climate Change on Mangrove Ecosystems of South and Southeast Asia: An Overview

Authors: Rajarshi DasGupta; Rajib Shaw
Journal: Journal of Ecosystems
 (2013)

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## Abstract

The paper provides an insight into the chronological extinction of the Indo-Malayan mangroves along the South and Southeast Asian coast and categorizes several area-specific anthropogenic and climatic factors that triggered the annihilation of 1.9 million ha of diverse mangroves. On a regional scale, coastal agricultural land development and shrimp farming were identified as major factors accounting for 90% of the reported loss. The paper also focuses on the existing mangrove management framework of nine developing countries of this region and conducts a comparative analysis of the prevailing legislative arrangement for mangrove management. In general, weak enforcements of legal measures and improper monitoring have been identified as major drawbacks in conservation and restoration initiatives. On the other hand, this paper strongly encourages the prospects of community-based mangrove management (CBMM) and provides good examples from the ecoregion through comparative case studies. Finally, it concludes with recommendations that outline a suitable mangrove management strategy involving more community empowerment, legalization and mainstreaming of comanagement initiatives, inclusive benefit sharing, and regional cooperation for transboundary ecosystem management.


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## Body

## 1. Introduction

Mangrove forests, still abundant in South and Southeast Asia, are amongst the world’s most fragile ecosystems and continue to disappear under the increased threat of climate change and human interventions. Researchers from all over the world agree on the fact that the existence of mangroves forests is under great risk due to fragmentation of the habitats. Moreover, ecosystem services offered by the mangroves are likely to be lost completely within the next 100 years [1]. Globally, mangroves are disappearing at an alarming rate of 1 to 2% per year, faster than the adjacent coral reefs or tropical rainforests [1–3]. Deforestation led by increasing demand for land and climate change events such as rise of sea level and reduction in freshwater flow are considered as major players behind the continuous annihilation of mangroves; however, climate change events may impact to only 10–15% reduction of mangrove habitats in distant future, whereas the immediate threat comes from uncontrolled exploitation and deforestation [3]. The consequent impacts of such losses resulted in serious concern amongst conservationists and exposed the coastal communities to a further increased threat of climate change and hydrometeorological disasters.Large stretches of the subtropical and tropical coastlines of South and Southeast Asia are endowed with highly productive mangrove forests. Biogeographically classified as Indo-Malayan mangroves, these mangroves are considered as the oldest and most diverse mangrove habitats in existence. As of 2010, it extends over 6.13 million ha and accounts for nearly 40.4% of global mangroves [4]. Yet, Indo-Malayan mangroves have recorded the highest loss in the last few decades [5]. In general, mangroves of this region are threatened by increasing demand for land, unsustainable production of fish and prawns, mixing of waste water effluents, as well as changing hydroclimatic scenario. Since the entire ecozone is fragmented by political boundaries of several developing nations, the pattern of mangrove exploitation differs significantly under diverse economic priorities. Similarly, restoration and conservation initiatives vary extensively under the different socioeconomic, demographic, and political scenario of the respective country. Following the Indian Ocean Tsunami in 2004, initiatives for mangrove conservation and restoration gained popularity; however, it is highly imperative to identify the key drivers of mangrove delineation and the complex mechanisms of community-environment interactions in order to plan and implement a successful restoration strategy. Against this backdrop, this paper examines contemporary country-specific literatures in order to analyze the major delineating factors and their potential impacts. On the other hand, it identifies the achievements and challenges of mangrove conservation and restoration initiatives among several developing nations of South and Southeast Asia through comparative analysis of existing mangrove management framework. Finally, this paper concludes with an appropriate mangrove management strategy in order to regain the valuable ecological and environmental services of Indo-Malayan mangroves.


## 2. Biogeographical Distribution of Indo-Malayan Mangroves

The Indo-Malayan mangroves occur in stretches in the southern coast of Asia, throughout the Indian subcontinent, in almost all the Southeast Asian countries and on the islands in the Indian Ocean, Bay of Bengal, South China Sea, and the North Pacific Ocean. It extends over at least twelve developing countries of the region. Out of its global share of 40.4%, Indonesian mangrove alone accounts for 22.6%, whereas Malaysia (3.7%), Myanmar (Burma) (3.6%), Bangladesh (3.2%), India (2.7%), and Philippines (1.9%) contribute significantly to this highly fragile ecosystem [6]. Several other South and Southeast Asian countries such as Thailand, Vietnam, Cambodia, Sri Lanka, and Singapore have significant amount of mangroves. On the basis of common ecological and environmental settings, the Indo-Malayan mangroves have been broadly classified into six distinct mangrove ecosystems. However, information on their discrete ecological and environmental settings is still not well documented. A summary of the extent and diversity has been given in Table 1 with a brief discussion in the following paragraphs. The extent of the distribution is also shown in Figure 1.Table 1
Environmental and ecological settings of Indo-Malayan mangroves.
Category
Indus River Delta
Godavari-Krishna mangroves
Sundarban mangroves
Burmese coast mangroves
Indochina mangroves
Sunda Shelf mangrove
(a)
(b)
(c)
(d)
(e)
(f)
Type
Backwater estuarine
Deltaic/estuarine
Deltaic
Deltaic and coastal
Coastal
Coastal
Dominance
Transboundary
Domestic
Transboundary
Transboundary
Transboundary
Transboundary
Major river(s)
Indus
(i) Mahanadi(ii) Godavari(iii) Krishna
(i) Ganges(ii) Brahmaputra(iii) Meghna
Ayeyarwady
(i) Mekong(ii) Red River
Mahakam River
Species richness*
4
34
36
41
40
43
Total forest area (sq·km)**
6000 (approx)
7000 (approx)
25000 (approx)
3822 (approx)
26936  (approx)
40000 (approx)
Mangrove under protected area (sq·km)**
823
920
2700
125
820
6,530
Occurrence
Western of India and eastern coast of Pakistan
Eastern coast of India (Orissa to Tamil Nadu)
(i) Bangladesh(ii) India
(i) Myanmar(ii) Thailand (west coast)(ii) Peninsular Malaysia
(i) Thailand (east coast)(ii) Cambodia(iii) Vietnam(iv) Malaysia(v) Philippines
(i) Eastern Malaysia(ii) Indonesia(iii) Brunei
Status
Critically Degraded and fragmented
Degraded
Degraded
Critically degraded
Critically degraded
Degraded
*Species Richness varies significantly among different locations in each category. The highest reported species richness is mentioned here **Figures provide close approximation.
Source: Assimilated by authors from World Wide Fund for Nature Information Database on World Ecoregions [7, 8].Figure 1
Major mangrove ecosystems in the Indo-Malayan ecozone. (Source: created from google map by the authors.)


### 2.1. Indus River Delta Mangroves

The Indus River Delta mangroves or the Arabian Sea mangroves, to the west of Indo-Malayan ecozone, are the only arid mangroves of the entire ecozone. It spread across the Indus delta along the coast of Pakistan and Gujarat (India). Approximately one third of it belongs to the state of Gujarat, India. The Indus River Delta mangroves represent an ecosystem that is highly adaptable to extreme temperature, high salinity levels, and minimal rainfall. Due to the excessive salinity, species diversity of mangroves is essentially poor with distinct dominance of salt tolerantAvicennia marina [9, 10]. Of late, these mangroves are reported to be adversely affected by massive reduction of freshwater flow in the Indus River.


### 2.2. Godavari-Krishna Mangroves

Godavari-Krishna mangroves spread discontinuously across the eastern coast of India, especially in the states of Orissa, Andhra Pradesh and Tamil Nadu. Sufficient freshwater flow by three major rivers, namely, Mahanadi, Godavari, and Krishna along with a favorable terrain forms the basis of this moderately diverse mangrove ecosystem. The mangrove vegetation is also influenced by tidal fluctuations and varied salinity patterns. The Godavari-Krishna mangrove can be broadly classified into three categories as per their isolated geographical occurrences. In the northern fringes of Godavari-Krishna mangroves, the estuarine areas of the Mahanadi, Brahmani, and Baitarani rivers form the Mahanadi Delta mangroves. It receives plenty of freshwater from Mahanadi and its tributaries resulting in high diversity of 32 true mangrove species [11]. Bhitarkanika, better known for the huge population of migratory birds, is the major mangrove habitat in the Mahanadi delta. In the central fringes, mangrove forest in the delta of the Godavari and Krishna forms the largest mangrove in this region. It covers an area of approximately 400 sq·km. However, this particular stretch is not as diverse as the Mahanadi Delta mangroves. Avicennia marina is the dominant species along with 13 other true mangrove species. In the southern section of the ecoregion, Pichavaram mangroves in the backwaters of the Bay of Bengal remain as one of the healthiest mangrove chunk of the entire Indo-Malayan ecoregion. While Avicennia marinaand Rhizophorasp. are the dominant species, 11 other true mangrove species are also reported from Pichavaram [12, 13].


### 2.3. Sundarban Mangroves

The Sundarban mangrove forest, to the north-east of the Godavari-Krishna mangrove ecozone, is a part of the delta of River Ganges, Brahmaputra, and Meghna and disproportionately shared by India and Bangladesh. Due to the gentle slope of the coast and the low lying nature of the deltaic islands, tidal water penetrates up to an average distance of 110 km. [14]. It forms the basis of the largest tidal halophytic forest in the world which extends over an area of 25000 sq·km. The entire area of Sundarban experiences a subtropical monsoonal climate with an average annual rainfall of 1600–1800 mm [14, 15]. Heavy freshwater flow from the three major rivers and good amount of monsoonal rain essentially justifies the high species diversity of the mangroves. Even though species diversity and distribution differ in India and Bangladesh, it is reported that approximately 30–36 true mangrove species are observed with dominance of Heritiera fomes and Excoecaria agallocha [15]. The mangroves of Sundarban essentially host a number of critically endangered fauna including the royal Bengal tiger (Panthera Tigris).


### 2.4. Burmese (Myanmar) Coast Mangroves

The Myanmar Coast mangroves are the combination of estuarine and coastal mangroves adjoining the eastern coast of the Bay of Bengal. It extends over Myanmar, western coast of Thailand and Peninsular Malaysia. At present, the extent of mangrove area in Myanmar is about 4945 sq·km [6], out of which 46% is located in Irrawaddy (Ayeyarwady) delta, while the rest are confined in Rakhine (17%) and Tanintharyi division (37%) [16]. Twenty-nine true mangrove species are reported from these areas [17]. The western coast of Thailand hosts the majority of Thai mangroves. Presently, mangrove in the provinces of Ranong, Phuket, Krabi, Trang, and Satul along the west coast occupies approximately 1458 sq·km [18]. Similarly, mangroves in Peninsular Malaysia mainly occupy the sheltered west coast close to the Straits of Malacca along the states of Kedah, Perak, Selangor, and Johor. Mangrove reserves of Matang (Perak), South Johor (Johor), and Kelang (Selangor) together constitute 74 percent of the mangrove forest in peninsular Malaysia. All the major near-shore islands, including the Kelang islands in Selangor and Pulau Kukup in Johor, are predominantly colonized by mangroves [19]. The hot and humid climate with high rainfall favors the development of diverse species-rich mangrove habitat. The FAO reported of 41 true mangrove species from the Malaysian coast covering an area of 918 sq·km [20].


### 2.5. Indochina Mangroves

The Indochina mangroves are scattered over the eastern coasts of Thailand, Cambodia, Vietnam, and Philippines. They typically occur in the large river deltas and coastal areas that are inundated at high tide but otherwise remain under the freshwater influence. Indochina mangroves are extremely diverse and account for almost 60% of the mangrove species found in the entire ecozone. Among the large river deltas, Mekong and Red River delta form two major mangrove habitats in the region. The mangroves of Mekong River Delta in the Southwest of Vietnam form the largest stretch of Indochina mangroves. However, much of it was lost during the Vietnam War with a reported reduction of approximately 1000 sq·km [21]. Presently some 25 sq·km of dense mangrove exists in the Mekong delta, while the rest remains degraded. Yet, the mangrove species diversity is moderately high with 29 true mangrove species [22]. The Red River delta in the northern coast of Vietnam is the other major mangrove habitat in the region. It is formed by two rivers, namely, the Thai Binh and the Red River. However, the colder climatic conditions, dense human population in the vicinity, and frequent storm surges limit the growth of mangroves. Hence, it has lower species diversity compared to Mekong Delta mangroves. Yet, some typical species are abundant in this region, such as Rhizophora stylosa,Bruguiera gymnorrhiza, and Kandelia candel which are otherwise less encountered in Mekong delta.In the eastern coast of Thailand, mangroves occur in three different patches surrounding the Gulf of Thailand. The uppermost part is spread over four provinces (Samut Prakan, Samut Sakhon, Samut Songkhram, and a part of Bangkok) covering an area of approximately 273 sq·km. In the south-eastern part, mangroves of five provinces, namely, Trat, Chantaburi, Rayong, Chonburi, and Chachoengsao form another long stretch of 470 sq·km. Along the western side of the Gulf of Thailand, the third mangrove habitat exists over 458 sq·km. Cambodia also had significant amount of mangroves along the Veal Renh and Kompong Som Bays; however, owing to large-scale deforestation, some residual, broken strips of mangroves occur in this area. To the far east of the Indochina ecozone, mangroves in the Philippines are located in the southern fringe of the Filipino archipelago, especially on the Mindanao Island and the western coast of Samar and Palawan province. The province of Palawan hosts the largest mangrove inhabited area covering approximately 562.61 sq·km of dense mangroves and accounts for 22.23% of the Filipino mangroves [23]. However, mangroves are found in almost all the coastal provinces of the country. Mangroves of the Philippines are typically diverse; approximately 40 true mangrove species are encountered in clear stratification.


### 2.6. Sunda Shelf Mangroves

The Sunda Shelf mangroves are found over the island of Borneo, along the fringes of the Riau Archipelago and the east coast of Sumatra. In the Malaysian Borneo, mangrove habitat spreads over the state of Sabah and Sarawak facing the Sulu and Sulawesi Sea. The Sabah mangrove reserve alone accounts for 3174.23 sq·km, while Sarawak has 1320 sq·km of dense mangrove forest [24]. In case of the Indonesian Borneo (Kalimantan), dense and protected mangrove forest spreads over approximately 1500 sq·km along the western Kalimantan; however, mangroves in the southern and eastern Kalimantan area, especially in the delta of Mahakam, are rapidly vanishing under anthropogenic stresses. The Indonesian Borneo accounts for only 32% of the entire Indonesian mangroves, while the rest are confined along the coastal areas of eastern Sumatra islands, Java, Irian Jaya in Papua and in south-eastern Sulawesi. The Irian Jaya covers one of the healthiest and unexplored chunks of mangroves covering 13270 sq·km. The Food and Agricultural Organizations reported about 43 species of true mangroves in Indonesia [20].


## 2.1. Indus River Delta Mangroves

The Indus River Delta mangroves or the Arabian Sea mangroves, to the west of Indo-Malayan ecozone, are the only arid mangroves of the entire ecozone. It spread across the Indus delta along the coast of Pakistan and Gujarat (India). Approximately one third of it belongs to the state of Gujarat, India. The Indus River Delta mangroves represent an ecosystem that is highly adaptable to extreme temperature, high salinity levels, and minimal rainfall. Due to the excessive salinity, species diversity of mangroves is essentially poor with distinct dominance of salt tolerantAvicennia marina [9, 10]. Of late, these mangroves are reported to be adversely affected by massive reduction of freshwater flow in the Indus River.


## 2.2. Godavari-Krishna Mangroves

Godavari-Krishna mangroves spread discontinuously across the eastern coast of India, especially in the states of Orissa, Andhra Pradesh and Tamil Nadu. Sufficient freshwater flow by three major rivers, namely, Mahanadi, Godavari, and Krishna along with a favorable terrain forms the basis of this moderately diverse mangrove ecosystem. The mangrove vegetation is also influenced by tidal fluctuations and varied salinity patterns. The Godavari-Krishna mangrove can be broadly classified into three categories as per their isolated geographical occurrences. In the northern fringes of Godavari-Krishna mangroves, the estuarine areas of the Mahanadi, Brahmani, and Baitarani rivers form the Mahanadi Delta mangroves. It receives plenty of freshwater from Mahanadi and its tributaries resulting in high diversity of 32 true mangrove species [11]. Bhitarkanika, better known for the huge population of migratory birds, is the major mangrove habitat in the Mahanadi delta. In the central fringes, mangrove forest in the delta of the Godavari and Krishna forms the largest mangrove in this region. It covers an area of approximately 400 sq·km. However, this particular stretch is not as diverse as the Mahanadi Delta mangroves. Avicennia marina is the dominant species along with 13 other true mangrove species. In the southern section of the ecoregion, Pichavaram mangroves in the backwaters of the Bay of Bengal remain as one of the healthiest mangrove chunk of the entire Indo-Malayan ecoregion. While Avicennia marinaand Rhizophorasp. are the dominant species, 11 other true mangrove species are also reported from Pichavaram [12, 13].


## 2.3. Sundarban Mangroves

The Sundarban mangrove forest, to the north-east of the Godavari-Krishna mangrove ecozone, is a part of the delta of River Ganges, Brahmaputra, and Meghna and disproportionately shared by India and Bangladesh. Due to the gentle slope of the coast and the low lying nature of the deltaic islands, tidal water penetrates up to an average distance of 110 km. [14]. It forms the basis of the largest tidal halophytic forest in the world which extends over an area of 25000 sq·km. The entire area of Sundarban experiences a subtropical monsoonal climate with an average annual rainfall of 1600–1800 mm [14, 15]. Heavy freshwater flow from the three major rivers and good amount of monsoonal rain essentially justifies the high species diversity of the mangroves. Even though species diversity and distribution differ in India and Bangladesh, it is reported that approximately 30–36 true mangrove species are observed with dominance of Heritiera fomes and Excoecaria agallocha [15]. The mangroves of Sundarban essentially host a number of critically endangered fauna including the royal Bengal tiger (Panthera Tigris).


## 2.4. Burmese (Myanmar) Coast Mangroves

The Myanmar Coast mangroves are the combination of estuarine and coastal mangroves adjoining the eastern coast of the Bay of Bengal. It extends over Myanmar, western coast of Thailand and Peninsular Malaysia. At present, the extent of mangrove area in Myanmar is about 4945 sq·km [6], out of which 46% is located in Irrawaddy (Ayeyarwady) delta, while the rest are confined in Rakhine (17%) and Tanintharyi division (37%) [16]. Twenty-nine true mangrove species are reported from these areas [17]. The western coast of Thailand hosts the majority of Thai mangroves. Presently, mangrove in the provinces of Ranong, Phuket, Krabi, Trang, and Satul along the west coast occupies approximately 1458 sq·km [18]. Similarly, mangroves in Peninsular Malaysia mainly occupy the sheltered west coast close to the Straits of Malacca along the states of Kedah, Perak, Selangor, and Johor. Mangrove reserves of Matang (Perak), South Johor (Johor), and Kelang (Selangor) together constitute 74 percent of the mangrove forest in peninsular Malaysia. All the major near-shore islands, including the Kelang islands in Selangor and Pulau Kukup in Johor, are predominantly colonized by mangroves [19]. The hot and humid climate with high rainfall favors the development of diverse species-rich mangrove habitat. The FAO reported of 41 true mangrove species from the Malaysian coast covering an area of 918 sq·km [20].


## 2.5. Indochina Mangroves

The Indochina mangroves are scattered over the eastern coasts of Thailand, Cambodia, Vietnam, and Philippines. They typically occur in the large river deltas and coastal areas that are inundated at high tide but otherwise remain under the freshwater influence. Indochina mangroves are extremely diverse and account for almost 60% of the mangrove species found in the entire ecozone. Among the large river deltas, Mekong and Red River delta form two major mangrove habitats in the region. The mangroves of Mekong River Delta in the Southwest of Vietnam form the largest stretch of Indochina mangroves. However, much of it was lost during the Vietnam War with a reported reduction of approximately 1000 sq·km [21]. Presently some 25 sq·km of dense mangrove exists in the Mekong delta, while the rest remains degraded. Yet, the mangrove species diversity is moderately high with 29 true mangrove species [22]. The Red River delta in the northern coast of Vietnam is the other major mangrove habitat in the region. It is formed by two rivers, namely, the Thai Binh and the Red River. However, the colder climatic conditions, dense human population in the vicinity, and frequent storm surges limit the growth of mangroves. Hence, it has lower species diversity compared to Mekong Delta mangroves. Yet, some typical species are abundant in this region, such as Rhizophora stylosa,Bruguiera gymnorrhiza, and Kandelia candel which are otherwise less encountered in Mekong delta.In the eastern coast of Thailand, mangroves occur in three different patches surrounding the Gulf of Thailand. The uppermost part is spread over four provinces (Samut Prakan, Samut Sakhon, Samut Songkhram, and a part of Bangkok) covering an area of approximately 273 sq·km. In the south-eastern part, mangroves of five provinces, namely, Trat, Chantaburi, Rayong, Chonburi, and Chachoengsao form another long stretch of 470 sq·km. Along the western side of the Gulf of Thailand, the third mangrove habitat exists over 458 sq·km. Cambodia also had significant amount of mangroves along the Veal Renh and Kompong Som Bays; however, owing to large-scale deforestation, some residual, broken strips of mangroves occur in this area. To the far east of the Indochina ecozone, mangroves in the Philippines are located in the southern fringe of the Filipino archipelago, especially on the Mindanao Island and the western coast of Samar and Palawan province. The province of Palawan hosts the largest mangrove inhabited area covering approximately 562.61 sq·km of dense mangroves and accounts for 22.23% of the Filipino mangroves [23]. However, mangroves are found in almost all the coastal provinces of the country. Mangroves of the Philippines are typically diverse; approximately 40 true mangrove species are encountered in clear stratification.


## 2.6. Sunda Shelf Mangroves

The Sunda Shelf mangroves are found over the island of Borneo, along the fringes of the Riau Archipelago and the east coast of Sumatra. In the Malaysian Borneo, mangrove habitat spreads over the state of Sabah and Sarawak facing the Sulu and Sulawesi Sea. The Sabah mangrove reserve alone accounts for 3174.23 sq·km, while Sarawak has 1320 sq·km of dense mangrove forest [24]. In case of the Indonesian Borneo (Kalimantan), dense and protected mangrove forest spreads over approximately 1500 sq·km along the western Kalimantan; however, mangroves in the southern and eastern Kalimantan area, especially in the delta of Mahakam, are rapidly vanishing under anthropogenic stresses. The Indonesian Borneo accounts for only 32% of the entire Indonesian mangroves, while the rest are confined along the coastal areas of eastern Sumatra islands, Java, Irian Jaya in Papua and in south-eastern Sulawesi. The Irian Jaya covers one of the healthiest and unexplored chunks of mangroves covering 13270 sq·km. The Food and Agricultural Organizations reported about 43 species of true mangroves in Indonesia [20].


## 3. Loss of Indo-Malayan Mangroves and Its Potential Consequences

Information on the chronological country or region specific loss of mangroves is not rigorously documented. In most of the South and Southeast Asian countries, official statistics of mangrove forest is either unavailable or significantly outdated. Meaningful information can only be retrieved through the survey of contemporary scientific literatures. So far, the best initiatives are observed from United Nation’s Food and Agricultural Organization (FAO) which documented the global and country wise changes in mangrove cover till 2005. It states that in South and Southeast Asia, mangrove cover has decreased by 25% from its original extent in 1980, while the Indo-Malayan mangroves suffered a net loss of nearly 1.9 million hectare [20]. More than 90% of this loss has been registered in Indonesia, Myanmar, Pakistan, Vietnam, Malaysia, and India. It used linear regression analysis to understand the country-specific trend of mangrove loss based on the realistic available information. In order to update this database and examine the present trend, a similar methodology has been adopted in this paper. Recent realistic estimation of mangrove cover has been documented from available literature and official reports. Table 2 summarizes the present extent of mangroves in nine countries of South and Southeast Asia. The assessment year is not uniform for all the mentioned countries; however, priorities were given to document the realistic official estimations from the respective countries. Also, it is important to note that these figures provide a close approximation but do not necessarily reflect the exact ground reality.Table 2
Country-specific temporal variation of mangrove cover.
Country/year
Mangrove cover in sq·km
1980
1990
% Change(1980–1990)
2000
% Change(1990–2000)
2005
Present
Assessment year
% Change (2000-latest)
Pakistan
3450
2070
-
40
1580
-
23.67
1570
981.28a
2010
-
37.89
India
5067
4670
-
7.84
4482
-
4.03
4480
4639b
2009
3.50
Bangladesh
4280
4600
7.48
4760
3.48
4760
4810c
2007
1.05
Myanmar
5550
5361
-
3.41
5167
-
3.62
5070
4379.21d
2007
-
15.24
Indonesia
42000
35000
-
16.67
31500
-
10
29000
32440e
2009
2.98
Malaysia
6740
6420
-
4.75
5895
-
8.18
5650
5775f
2007
-
2.03
Vietnam
2691.5
2135
-
20.68
1575
-
26.23
1570
1597.6g
2008
1.43
Philippines
2950
2730
-
7.46
2500
-
8.42
2400
2091h
2007
-
16.36
Thailand
2800
2502
-
10.64
2441
-
2.44
2400
2296i
2007
-
5.94
a[25],b[26], c[27], d[28], e[29], f[24], g[30], h[31], i[32].Analysis of the data presented in Table2 depicts that since the last decade, India, Indonesia, and Vietnam showed an increasing trend in gross mangrove forest area compared to the massive declining trend observed in the previous two decades. This finding can be referred to substantial achievement in mangrove conservation and restoration in the mentioned countries. Among all the countries, mangroves of Bangladesh remain largely unaffected over the years. On the contrary, Pakistan, Thailand, Myanmar, and Philippines continued to suffer the loss of mangroves. With a disappearing rate of more than 2% per year, particularly mangroves in Pakistan and Myanmar remain critically threatened.Potential consequences of the loss of mangroves in this region are multifaceted with distinct ecological, social, and economic dimensions. In many remote coastal areas of this region, mangrove-based livelihood opportunities strongly define the social and economical well-being of the coastal communities. Mangroves are capable of producing a rich natural capital providing enormous economic and environmental services. Over the years, mangroves have sustained more than 70 direct human activities. Of these, on-shore fishing and timber and firewood collection are worth mentioning in the backdrop of South and Southeast Asia, where rural poverty still forms a critical sociopolitical issue. With the advancement of modern petroleum fuels, the dependence on mangrove firewood has reduced significantly; however, on-shore fishing is still widely practiced in different parts of South and Southeast Asia. Degradation of mangroves has adversely impacted traditional fishing activities. Many aquatic species including the commercially important fishes were lost or significantly reduced along with the mangroves. For example, there has been more than 50% reduction in fish catch in the Indus-Delta since 1993 [33]. Similar examples can also be cited from various parts of India, Thailand, Myanmar, and Philippines. Loss of livelihood insisted coastal fishing communities to work as landless labors or to toil in private aquaculture ponds. As a result, crucial alterations of sociological hierarchy are also observed. Women, who were initially engaged in different mangrove-based livelihood activities, such as fish hunting and wood and firewood collection, now engage themselves in alternative livelihoods far away from their places leading to disintegration and improper upbringing of their families [34].On the other hand, the indirect services of mangrove forest in terms of shoreline protection, biofiltration, carbon sequestration, and disaster risk reduction are enormous. Of these, the role of mangroves in mitigating the large-scale hydrometeorological disasters is typically important considering the existing vulnerability of the region. The Indian Ocean Tsunami in 2004 which claimed the lives of more than 230,000 people in fourteen countries particularly marked the importance of coastal mangroves. Following the Tsunami, Kathiresan and Rajendran (2005) reported that the presence of mangrove directly correlated with less number of losses of human lives [35]. Similar conclusive arguments have also been referred by several researchers from different countries in this region, where it was observed that mangroves have shielded the coastal communities from typhoon, cyclones, and a number of other coastal hazards. Extreme events such as Tsunami may be an unfamiliar event in the region; however, degraded and fragmented mangroves increased the disaster loss to several extents. At present, the entire Myanmar coast remains at stake due to its high potential for a giant earthquake and subsequent Tsunami in the Bay of Bengal [36]; also, many South and Southeast Asian countries have already faced the adverse impact of climate change. With sea level rise and increase in ocean water temperature, it is likely that tropical cyclones will become more intense in future along with higher precipitation [37]. Therefore, it is highly imperative to reorganize the perceptions about mangrove and provide them a fair chance to grow and protect the vulnerable coastlines.


## 4.  Factors behind the Degradation of Indo-Malayan Mangroves

Degradation of the Indo-Malayan mangroves has been a result of continuous developmental pressure exerted on the coastal areas of South and Southeast Asia. In the past, several mangrove forests were annihilated and converted to coastal cities. Megacities like Singapore, Jakarta, Bangkok, Manila, Yangon, Kolkata (Calcutta), and Mumbai (Bombay) were built over mangrove forestland. Yet, the loss has been predominantly severe in only the last three decades. At one side, mangrove suffered anthropogenic pressure beyond its ecological threshold; on the other hand, climate change events are also adversely affecting some of the premier mangrove habitats of this region. Climate change components that affect mangroves include changes in sea level, high water events, storms, precipitation, temperature, and oceanic circulation [38]. Cumulative impacts of these factors have a distinct synergy with respect to an accelerated rate of mangrove degradation. However, the delineating factors differ significantly among the diverse mangrove habitats in the Indo-Malayan ecoregion. Table 3 summarizes various factors that are presently adversely affecting different mangrove habitats of Indo-Malayan ecoregion. The following paragraphs describe the impact of various anthropogenic and climatic factors presently persisting on Indo-Malayan mangroves.Table 3
Factors influencing loss of mangroves in Indo-Malayan ecozone.
Type of mangroves
Area/country
Anthropogenic factors
Environmental  factors
Agricultural conversation
Shrimp pond conversation
Clear felling
Wood and  fodder
War and  conflict
Marine pollution
Urbanization
Rise in Sea Level
Increase in salinity
Erosion and sedimentation
High tide and Tsunami
Cyclones
Erosion of shoreline
Indus River Delta
South coast/ Pakistan
S
N
M
M
NS
S
M
NS
S
S
NS
NS
NS
a
Indus River Delta
West coast/India
M
NS
L
L
NS
S
M
NS
M
M
NS
NS
NS
Mahanadi delta
Orissa/India
M
L
L
M
NS
L
M
N
N
M
NS
S
L
b
Godavari-Krishna delta
Andhra Pradesh/India
M
M
L
M
NS
N
L
NS
NS
L
NS
L
L
Pichavaram mangroves
Tamil Nadu/India
L
M
NS
L
NS
L
L
NS
L
NS
L
N
N
c
Sundarban mangroves
West Bengal/India
S
M
L
M
NS
M
M
S
M
M
S
S
S
Sundarban mangroves
Khulna/Bangladesh
S
M
M
S
NS
L
L
M
L
M
M
S
S
d
Irrawaddy delta
Irrawaddy Division/Myanmar
S
M
S
S
L
L
S
L
M
S
L
S
N
Peninsular Malaya mangroves
West (Peninsular)  Malaysia
S
S
M
M
NS
S
N
N
N
M
L
L
M
e
Mekong delta
Southwest coast/Vietnam
S
S
S
S
S
M
M
S
M
M
L
M
S
Red River delta
Northeast coast/Vietnam
S
M
M
M
NS
N
M
L
L
M
L
L
L
Thailand mangroves
East coast/ Thailand
S
S
S
L
L
N
M
L
L
M
S
L
S
Philippines mangrove
West coast/Philippines
M
S
S
L
NS
N
M
L
N
N
L
S
L
f
Indonesian mangroves
Indonesia
S
S
S
M
NS
N
S
M
N
M
S
L
S
a: Indus River Delta mangroves, b: Godavari-Krishna delta mangroves, c: Sundarban mangroves, d:  Myanmar coast mangroves, e: Indochina mangroves, f: Sunda Shelf mangroves.
S: severe impact, M: moderate impact, L: low impact, NS: no significant impact, N: no information.


### 4.1. Anthropogenic Factors

In case of South and Southeast Asia, development of coastal agricultural land and shrimp farming ponds in intertidal areas are considered as the major factors behind mangrove delineation. Of these, conversion of mangrove forest for agriculture is typically prominent in countries like India, Bangladesh, Myanmar, Thailand, and Indonesia. Giri et al. (2008) reported that agricultural activities in the mentioned countries are responsible for nearly 82% of the reported loss during 1975–2005 [39]. Agriculture is also the major livelihood of several coastal communities inhibiting the large deltas of this region. As a result, mangrove forest in Ganga-Brahmaputra-Meghna Delta in India and Bangladesh and Ayeyarwady delta in Myanmar are amongst the worst sufferer due to agricultural land conversion. In the Sundarban mangroves, more than 150000 ha of mangroves were diverted for agricultural land during the past 100 years [40]. Similarly, in the Ayeyarwady delta in Myanmar, rice cultivation accounted for almost 24% (55873 ha) reduction of mangrove forest during 1954 to 1984, and following the next decade, the conversion rate has escalated by threefold [41].Shrimp cultivation is the second largest anthropogenic cause of mangrove deforestation in South and Southeast Asia. The process of shrimp farming is economically lucrative for the coastal communities. Particularly, with huge demands of commercially produced shrimp in the western countries, it ensures high economic return. 75% of the global commercial shrimps are produced in Asia, and Thailand remains the single largest exporter of commercially produced shrimps. In the late eighties, skeptic rise in global price of commercially produced shrimps prompted South and Southeast Asian governments to support this traditional practice which in turn took the shape of an unsustainable polluting industry. The process destroyed nearly 50% of Thai mangroves [42]. In a recent satellite-based observation, it has been estimated that since 1975, approximately 41% (18816 ha) of Thailand mangroves, 63% (20956 ha) of Indonesian mangrove, 22% (7554 ha) of Indian mangrove, and 11% (1070 ha) of the Bangladeshi mangroves were diverted to shrimp ponds [39]. The Mekong delta mangroves also lost approximately 50% of their habitat due to shrimp cultivation.Apart from these two major delineating factors, the South and Southeast Asian mangroves are presently experiencing huge population growth and rapid coastal infrastructure development and urbanization in its vicinity. Even though only 2% of mangrove forests were diverted for establishment of new coastal settlements in this region [39], yet the problem persists with the observed coastward migration. On the other hand, coastal infrastructure development in terms of port and harbors is strongly associated with mangrove degradation. Port Qasim at Karachi (Pakistan) and Port Mundra in Gujarat, India, are largely criticized of degrading the vulnerable Indus delta mangroves. In the eastern coast of India, Paradip port was built over dense patches of Mahanadi delta mangroves [43]. Similar instances are found to occur in Malacca strait (Malaysia), where mangrove habitats were deforested for building up ports (Port Klang and Malacca port), industrial states (Penang), and commercial centers (Malacca and Penang) [44]. One of the important consequences of this development is severe marine pollution unsustainable for the growth of the mangroves. Marine pollution, particularly oil spillage along the coast, has resulted in further loss of mangroves in this region. Mangroves are highly susceptible to oil exposure, and it may kill them within a few weeks to several months [45]. The collision of Panamanian vessels off the Mumbai coast in late 2010 resulted in oil spill of over 800 tonnes in the Arabian seas, with a reported loss 1273 hectares of reclaimed mangroves. Similar instances are also available from the Gulf of Malacca, in Malaysian coast, which serves as an international corridor for cargo vessels. At least 18 reported oil spill incidents were recorded at the Gulf of Malacca; reportedly damaging the coastal mangroves. Lastly, the Indo-Malayan mangroves also experienced the ill effects of armed conflicts. It was reported that at least 1000 sq·km of mangroves were destroyed during the Vietnam War by the widespread use of defoliating herbicide mixtures named as Agent Orange.


### 4.2. Environmental and Natural Factors

Mangroves show exceptional morphological and physiological adaptation skills to counter the environmental and natural stress associated with their intertidal habitat. Yet, tampering of upstream environment and climate change events has contributed significant alteration of the mangrove habitats. Geoclimatically, the Indo-Malayan mangroves now face a more challenging environment for their continual survival. Among the environmental or natural degrading factors of mangroves, rising sea level, increased salinity, and reduction of freshwater flow are considered to be most crucial. Three major South and Southeast Asian rivers, namely, the Indus, Ganges, and the Mekong are listed among the top ten rivers of the world with substantial reduction of flow [46]. As a consequence, deltaic mangroves of these rivers remain at a stake from considerable rise in water and soil salinity. In the past, salinity adversely affected the species diversity of mangroves. It is reported that species diversity in the Indus River Delta mangroves has virtually reduced to only one (Avicennia marina) owing to extreme saline conditions resulting from more than 90% reduction in freshwater flow. Similarly, wide-spread occurrence of the “top dying” disease of mangroves in Sundarbans is now considered to be an impact of salinity rise due to significant reduction in freshwater flow.Among the other environmental factors, coastal dynamics and sea level rise play an important role in degrading the mangroves. Erosion loss and submergence under the rising sea are widespread along the eastern coast of India, eastern and southern coast of Thailand, southern coast of Vietnam, and northern coast of Indonesia. In recent past, several islands of Sundarban mangroves both in India and Bangladesh suffered from severe erosion and inundation due to the rising sea level in the Bay of Bengal. Lohachara Island in the Indian Sundarbans is considered to be the first island to be permanently inundated by the rising sea. An assessment carried out during 2001-2002 showed that out of the remaining 100 islands of Indian Sundarbans, 12 are very much prone to coastal erosion and high-tide events [47]. On the other hand, a recent remote sensing based observation revealed that some 53 sq·km of mangrove forests were affected in the eastern coast of Thailand while 43 sq·km of mangroves were lost in the western coast as a result of erosion. The present rate of coastal erosion in Thailand ranges from 0.04 to 0.13 sq·km/y in the west and east coast, respectively [48]. Mangroves along the western coast of the Peninsular Malaysia are also getting eroded away by the sea. Similar instances can be drawn from Indonesia, where a number of known mangrove patches have been degraded or eroded away. Erosion is severe in the coast of Java islands and other provinces such as Lampung, Northeast Sumatra, Kalimantan, West Sumatra (Padang), Nusa Tenggara, Papua, South Sulawesi, and Bali. On the contrary, Irrawaddy delta mangroves in Myanmar are presently affected by increased sedimentation and coastal accretion. It is interesting that deposition in coastal areas may cause a decrease in the tidal prism in rivers running through the mangrove, resulting in the closing of tidal creeks and the degradation of the forest [49]. Sedimentation rate of the Irrawaddy is the fifth highest in the world. This is largely because of the deforestation that has occurred throughout central Myanmar. The quantity of alluvial deposit is so immense that delta extends further and further into the Bay of Bengal each year resulting in natural thinning of the mangrove forests. Similarly, the Segara Anakan Lagoon of the Central Java of Indonesia lost its complete mangrove habitat due to high sedimentation.In addition, loss of mangrove habitats due to natural disasters is typically prominent in South and Southeast Asia. Over the past, Indo-Malayan mangroves were subjected to several hydrometeorological disasters of great magnitudes. The mangroves have shielded the coastal communities; however, in turn, it absorbed huge losses. Following the Orissa Super Cyclone in 1999, Forest Survey of India assessed that at least 50% and 40% mangrove forests were lost in the two districts of Orissa (Jagatsinghpur and Kendrapara) which had significant share of the Mahanadi mangroves. Similarly, cyclonic storm “Sidr” in 2007 destroyed some 30000 ha of Sundarban mangrove forests. The Myanmar coast also lost sizable mangrove forest following the Cyclone “Nargis” in 2008. Yet, the Indo-Malayan mangroves had the worst possible impact from Indian Ocean Tsunami in 2004. Indonesia, Thailand, Sri Lanka, and India lost considerable amount of mangroves in this event; however, it was reported that the extent of mangrove damage could not be assessed thoroughly due to the large-scale massacre of lives and property [3]. Rough estimations of mangrove loss in Indonesia revealed that almost 25000 ha of mangroves were damaged; however, Indonesian government later revealed that only 300–750 ha of mangroves were lost in the Aceh Province of Sumatra [3, 50]. In India, as per the damage assessment report of Forest Survey of India, the devastation of mangroves was greatly limited to the Nicobar Islands in the Andaman Sea. However, some reports informed that Pichavaram mangroves suffered 5–10% damage due to the Tsunami. In case of Thailand, reported loss of mangroves was about 306 ha [50].


## 4.1. Anthropogenic Factors

In case of South and Southeast Asia, development of coastal agricultural land and shrimp farming ponds in intertidal areas are considered as the major factors behind mangrove delineation. Of these, conversion of mangrove forest for agriculture is typically prominent in countries like India, Bangladesh, Myanmar, Thailand, and Indonesia. Giri et al. (2008) reported that agricultural activities in the mentioned countries are responsible for nearly 82% of the reported loss during 1975–2005 [39]. Agriculture is also the major livelihood of several coastal communities inhibiting the large deltas of this region. As a result, mangrove forest in Ganga-Brahmaputra-Meghna Delta in India and Bangladesh and Ayeyarwady delta in Myanmar are amongst the worst sufferer due to agricultural land conversion. In the Sundarban mangroves, more than 150000 ha of mangroves were diverted for agricultural land during the past 100 years [40]. Similarly, in the Ayeyarwady delta in Myanmar, rice cultivation accounted for almost 24% (55873 ha) reduction of mangrove forest during 1954 to 1984, and following the next decade, the conversion rate has escalated by threefold [41].Shrimp cultivation is the second largest anthropogenic cause of mangrove deforestation in South and Southeast Asia. The process of shrimp farming is economically lucrative for the coastal communities. Particularly, with huge demands of commercially produced shrimp in the western countries, it ensures high economic return. 75% of the global commercial shrimps are produced in Asia, and Thailand remains the single largest exporter of commercially produced shrimps. In the late eighties, skeptic rise in global price of commercially produced shrimps prompted South and Southeast Asian governments to support this traditional practice which in turn took the shape of an unsustainable polluting industry. The process destroyed nearly 50% of Thai mangroves [42]. In a recent satellite-based observation, it has been estimated that since 1975, approximately 41% (18816 ha) of Thailand mangroves, 63% (20956 ha) of Indonesian mangrove, 22% (7554 ha) of Indian mangrove, and 11% (1070 ha) of the Bangladeshi mangroves were diverted to shrimp ponds [39]. The Mekong delta mangroves also lost approximately 50% of their habitat due to shrimp cultivation.Apart from these two major delineating factors, the South and Southeast Asian mangroves are presently experiencing huge population growth and rapid coastal infrastructure development and urbanization in its vicinity. Even though only 2% of mangrove forests were diverted for establishment of new coastal settlements in this region [39], yet the problem persists with the observed coastward migration. On the other hand, coastal infrastructure development in terms of port and harbors is strongly associated with mangrove degradation. Port Qasim at Karachi (Pakistan) and Port Mundra in Gujarat, India, are largely criticized of degrading the vulnerable Indus delta mangroves. In the eastern coast of India, Paradip port was built over dense patches of Mahanadi delta mangroves [43]. Similar instances are found to occur in Malacca strait (Malaysia), where mangrove habitats were deforested for building up ports (Port Klang and Malacca port), industrial states (Penang), and commercial centers (Malacca and Penang) [44]. One of the important consequences of this development is severe marine pollution unsustainable for the growth of the mangroves. Marine pollution, particularly oil spillage along the coast, has resulted in further loss of mangroves in this region. Mangroves are highly susceptible to oil exposure, and it may kill them within a few weeks to several months [45]. The collision of Panamanian vessels off the Mumbai coast in late 2010 resulted in oil spill of over 800 tonnes in the Arabian seas, with a reported loss 1273 hectares of reclaimed mangroves. Similar instances are also available from the Gulf of Malacca, in Malaysian coast, which serves as an international corridor for cargo vessels. At least 18 reported oil spill incidents were recorded at the Gulf of Malacca; reportedly damaging the coastal mangroves. Lastly, the Indo-Malayan mangroves also experienced the ill effects of armed conflicts. It was reported that at least 1000 sq·km of mangroves were destroyed during the Vietnam War by the widespread use of defoliating herbicide mixtures named as Agent Orange.


## 4.2. Environmental and Natural Factors

Mangroves show exceptional morphological and physiological adaptation skills to counter the environmental and natural stress associated with their intertidal habitat. Yet, tampering of upstream environment and climate change events has contributed significant alteration of the mangrove habitats. Geoclimatically, the Indo-Malayan mangroves now face a more challenging environment for their continual survival. Among the environmental or natural degrading factors of mangroves, rising sea level, increased salinity, and reduction of freshwater flow are considered to be most crucial. Three major South and Southeast Asian rivers, namely, the Indus, Ganges, and the Mekong are listed among the top ten rivers of the world with substantial reduction of flow [46]. As a consequence, deltaic mangroves of these rivers remain at a stake from considerable rise in water and soil salinity. In the past, salinity adversely affected the species diversity of mangroves. It is reported that species diversity in the Indus River Delta mangroves has virtually reduced to only one (Avicennia marina) owing to extreme saline conditions resulting from more than 90% reduction in freshwater flow. Similarly, wide-spread occurrence of the “top dying” disease of mangroves in Sundarbans is now considered to be an impact of salinity rise due to significant reduction in freshwater flow.Among the other environmental factors, coastal dynamics and sea level rise play an important role in degrading the mangroves. Erosion loss and submergence under the rising sea are widespread along the eastern coast of India, eastern and southern coast of Thailand, southern coast of Vietnam, and northern coast of Indonesia. In recent past, several islands of Sundarban mangroves both in India and Bangladesh suffered from severe erosion and inundation due to the rising sea level in the Bay of Bengal. Lohachara Island in the Indian Sundarbans is considered to be the first island to be permanently inundated by the rising sea. An assessment carried out during 2001-2002 showed that out of the remaining 100 islands of Indian Sundarbans, 12 are very much prone to coastal erosion and high-tide events [47]. On the other hand, a recent remote sensing based observation revealed that some 53 sq·km of mangrove forests were affected in the eastern coast of Thailand while 43 sq·km of mangroves were lost in the western coast as a result of erosion. The present rate of coastal erosion in Thailand ranges from 0.04 to 0.13 sq·km/y in the west and east coast, respectively [48]. Mangroves along the western coast of the Peninsular Malaysia are also getting eroded away by the sea. Similar instances can be drawn from Indonesia, where a number of known mangrove patches have been degraded or eroded away. Erosion is severe in the coast of Java islands and other provinces such as Lampung, Northeast Sumatra, Kalimantan, West Sumatra (Padang), Nusa Tenggara, Papua, South Sulawesi, and Bali. On the contrary, Irrawaddy delta mangroves in Myanmar are presently affected by increased sedimentation and coastal accretion. It is interesting that deposition in coastal areas may cause a decrease in the tidal prism in rivers running through the mangrove, resulting in the closing of tidal creeks and the degradation of the forest [49]. Sedimentation rate of the Irrawaddy is the fifth highest in the world. This is largely because of the deforestation that has occurred throughout central Myanmar. The quantity of alluvial deposit is so immense that delta extends further and further into the Bay of Bengal each year resulting in natural thinning of the mangrove forests. Similarly, the Segara Anakan Lagoon of the Central Java of Indonesia lost its complete mangrove habitat due to high sedimentation.In addition, loss of mangrove habitats due to natural disasters is typically prominent in South and Southeast Asia. Over the past, Indo-Malayan mangroves were subjected to several hydrometeorological disasters of great magnitudes. The mangroves have shielded the coastal communities; however, in turn, it absorbed huge losses. Following the Orissa Super Cyclone in 1999, Forest Survey of India assessed that at least 50% and 40% mangrove forests were lost in the two districts of Orissa (Jagatsinghpur and Kendrapara) which had significant share of the Mahanadi mangroves. Similarly, cyclonic storm “Sidr” in 2007 destroyed some 30000 ha of Sundarban mangrove forests. The Myanmar coast also lost sizable mangrove forest following the Cyclone “Nargis” in 2008. Yet, the Indo-Malayan mangroves had the worst possible impact from Indian Ocean Tsunami in 2004. Indonesia, Thailand, Sri Lanka, and India lost considerable amount of mangroves in this event; however, it was reported that the extent of mangrove damage could not be assessed thoroughly due to the large-scale massacre of lives and property [3]. Rough estimations of mangrove loss in Indonesia revealed that almost 25000 ha of mangroves were damaged; however, Indonesian government later revealed that only 300–750 ha of mangroves were lost in the Aceh Province of Sumatra [3, 50]. In India, as per the damage assessment report of Forest Survey of India, the devastation of mangroves was greatly limited to the Nicobar Islands in the Andaman Sea. However, some reports informed that Pichavaram mangroves suffered 5–10% damage due to the Tsunami. In case of Thailand, reported loss of mangroves was about 306 ha [50].


## 5. Management of Mangrove Ecosystems in South and Southeast Asia

South and Southeast Asia spans over several postconflict states and some of the world’s poorest countries. Many South and Southeast Asian countries have lowincome despite economic growth in recent decades. Most importantly, coastal areas of these countries are immensely populated, and the mangroves are surrounded by a larger proportion of economically deprived coastal communities. Hence, traditional livelihood dependence on mangroves and an exponential population growth forms a formidable challenge in managing the mangroves. Of late, recent developmental pressure adds woes to it. Yet, since the last decade, some progress has been made in successful conservation and restoration of mangroves. In the South and Southeast Asian region, conservation and restoration of mangroves largely revolve around initiatives and actions made by the federal or provincial governments. Although, previously many governments considered the mangroves as “wasteland” and overlooked their ecological and environmental values in developmental planning, some dense mangrove patches along the South and Southeast Asian coast are presently assigned to a certain level of legislative protection. On the other hand, sustainable forest management (SFM) is also being practiced in some mangrove areas; however, such examples are extremely limited. Diagrammatic representation of key concern and management challenges is presented in Figure2.Figure 2
Schematic diagram of mangrove degradation and its restoration strategies in South and Southeast Asia.


### 5.1. Legislative Protection of Mangroves

Legislative protection of mangroves comes from the idea of in-situ conservation under the “protected area” concept. Although approximately 25% of the global mangroves are presently conserved under varied degree of protection, in case of the Indo-Malayan ecoregion, rough estimation reveals that less than 20% of the mangroves presently possess such status. Yet, evidence of mangrove conservation in the region can be documented since the colonial era, especially under the Forest Conservation Act, 1927 of British India. Under this particular act, approximately 344870 ha of mangrove forests were transferred to Sindh Forest Department for effective conservation which still forms one of the largest protected mangrove areas in Pakistan [51]. Similarly, this act was also instrumental for the protection of Sundarban mangroves both in India and Bangladesh. Nevertheless, legislative protection of mangroves was predominantly ratified after the Ramsar Convention (1971) on “the Wetlands of International Importance.” Two specific measures suggested in the Ramsar Convention were “conservation” and “wise use of wetland resources.” Although initially only 11 Asian countries joined this convention, it strongly initiated the need of mangrove conservation into the national policies of several South and Southeast Asian Countries. Following the convention, Pakistan, India, Philippines, and Indonesia formed National Mangrove Management Committee to promote mangrove conservation. Presently, all the South and Southeast Asian countries with dense to moderate mangroves have joined the convention with the latest addition of Myanmar in 2005. Of late, following the Indian Ocean Tsunami, several countries have mentioned mangrove restoration as a national priority. Also, some of them ratified the “coastal green belt” concept which involved massive mangrove plantation along the coast. For example, about 12000 ha of mangroves were planted by the Vietnamese government only as coastal protection initiatives. On the other hand, Government of Bangladesh initiated massive plantation program of 120,000 ha following the Cyclone “Sidr.” However, despite the legislative protection and massive plantation, poor implementation of laws and by laws largely proved conservation efforts futile in almost all the South and Southeast Asian countries. Coastal communities invaded the mangroves for their continual survival, and as a result, conservation and plantation initiatives could only result in conflicts among the local governments and mangrove-dependent communities. On the other hand, a new set of environmental worries from massive water pollution and unsustainable development of coastal areas escalated mangrove deforestation. Many countries formed a second set of legislation that indirectly controls the mangrove degradation. Yet, the problem persisted with poor level of implementation and inadequate monitoring framework. In this paper, a comparative analysis in terms of existing country-specific legislative arrangements for mangrove is produced in Table 4.Table 4
Country wise comparative analysis of legislative aspects of mangrove conservation.
Country
Main governing department
Legislative aspects of mangrove conservation
In-situ conservation of natural resources
Community participation in mangrove management
Control of shrimp farming
Coastal zoning/integrated coastal zone management
Marine/coastal environmental protection
Legislative provisions of coastal greenbelt development
Pakistan
Provincial Forest Departments
Major Provisions inForest Act,  1927and subsequent  provincial acts
No specific legislative arrangement
No specific legislative arrangement
No specific legislative arrangement
Major Provision inNational Action Plan on Environment
No specific legislative arrangement
India
Ministry of Environment and Forest
Major Provisions inForest Conservation Act,  1980 and Wildlife (Protection) Act,  1972
Major Provisions inJoint Forest Management Initiatives adopted by National Forest Policy, 1988
Major Provisions inCoastal Aquaculture Authority Act,  2005
Major Provisions inCRZ Notification,  1991 (rev.2004) under the Environmental Protection Act of 1986
Major Provisions inEnvironmental Protection Act, 1986,Water Prevention and Control of Pollution Act, 1974
No specific legislative arrangement
Bangladesh
Ministry of Environment and Forest
Major Provisions inForest Act, 1927(Amendments in 1989)
Major Provisions inForest Policy,  1994 allowing community participation
Some Provisions inEnvironmental Regulations,  1997
Major Provisions inCoastal Zone Policy, 2005
Major Provisions inEnvironmental Regulations,  1997
Some provisions inCoastal development strategy
Myanmar
Ministry of Forests
Major Provisions in Forest Act, 1995
Some Provisions inForest Policy, 1995
No specific legislative arrangement
No specificlegislative arrangement
No specificLegislative arrangement
No specific legislative arrangement
Thailand
Royal Forestry Department and Ministry of Natural Resources and Environment
Major Provisions inNational Forest Reserves Act,  1964
Major Provisions in Community Forestry Bill,  2007
No specific legislative arrangement
Some Provisions inLand Development Act, 1983
Some ProvisionsEnhancement and Conservation of National Environment Quality Act, 1992
No specific legislative arrangement
Vietnam
Ministry of Natural Resources and Environment and Ministry of Agricultural and Rural Development
Major Provisions in Forest Protection and Development Law, 2004
Some Provisions in 2003 amendments of Land Law, 1993
Some Provisions in Environment Protection Law, 1994 and Land Law, 1993
Some Provisions inDecree 25
Major  Provisions in Resolution 41/2004 and Environmental Protection Law (Revised 2005)
No specific legislative arrangement
Malaysia
Department of Forestry (Provincial Government)
Major Provisions in National Forestry Act 1984 (revised 1993)
No specific legislative arrangement
No specific legislative arrangement
Major ProvisionsIn 9th Malaysian Plan (2006–2010)
Major ProvisionsEnvironment Quality Act, 1974 and Merchant Shipping (Oil Pollution) Act of 1994
Major ProvisionsIn 9th Malaysian Plan (2006–2010)
Indonesia
Ministry of Forestry
Major Provision in Presidential Decree 32 (1990)/Law no.5 (1990)
Some Provisions in 2004 amendments in Law no. 32/41
No specific legislative arrangement
Major Provisions in Law no. 27 (2008)
Major Provisions in Law no. 32 (2009)
400 m greenbelt as perDecree no. H.1/4/2/18/1975
Philippines
Department of Environment and Natural Resource
Major Provision in  Republic Act 7586 (1992)
Major Provision in  Republic Act 8371 (1997)
Major Provisionsin Republic Act 8550 (1998)
Major Provisions in Coastal Zone Management Plan,  1997
Major Provisions in Presidential Decree no. 979 (1976)
DENR A.O. 76 (1987)—50 m coastal greenbelt development


### 5.2. Sustainable Management of Mangroves and Comanagement Initiatives

Sustainable Forest Management is a key concept that uses the forests in a way, and at a rate, that maintains their biodiversity, productivity, and the regeneration capacity. It essentially allows traditional uses of forest in a regulated way, so that the ecosystem services are not hampered. Although the formal definition of Sustainable Forest Management came after the United Nations Conference on Environment and Development (UNCED) in 1992, Sustainable Mangrove Management can easily be referred to the advocacy of Ramsar Convention about the “wiseuse” of wetlands. In case of Indo-Malayan mangroves, Sustainable Mangrove Management (SMM) is still a less used tool as the countries lack political will and institutional transparency. Yet, the best example of Sustainable Mangrove Management can also be referred from this ecoregion. The Matang mangrove forest, covering some 4000 ha in the peninsular Malaysia, is a classic example of sustainable management of mangroves. The forest is managed over hundred years through the active participation of all stakeholders. Almost 75% of this forest is designated as productive forest and exploited for wood resources, while the rest are conserved for promoting biodiversity. The 30-year rotation cycle of mangrove felling gives the highest net return on capital value. At present, the timber industry from Matang supports almost 2400 people and earns revenue of USD 6 million. The unproductive forest, on the other hand, supports about 10000 people with gross annual revenue of USD 12–30 million through sustainable fishing practices [52].Sustainable Forest Management originates from the key concept of comanagement of forest resources and essentially involves multiple stakeholders. In South and Southeast Asian countries, mangrove-dwelling communities have long been ignored in the centralized mangrove management policies. As a consequence, conservation initiatives could not achieve the desired results. Since late eighties, many countries in the region shifted towards a decentralized management approach involving the local communities as an important stakeholder. Since the last decade, community-based mangrove management (CBMM) has gained popularity in almost all the South and Southeast Asian countries. CBMM is particularly prominent in Indo-Malayan ecoregion, yet the level of its penetration varies significantly. In the Indo-Malayan ecoregion, the present success of mangrove restoration as well as conservation largely depends upon the community participation in mangrove restoration and management. CBMM initiatives are particularly prominent in Thailand, Indonesia, Philippines, Bangladesh, and India. One of the finest examples of CBMM is regarded as the restoration of the Pichavaram mangrove forest in India. Pichavaram is the second largest mangrove forest in India; however, owing to over exploitation of aquatic resources and persisting natural calamities, it was degraded to a great extent. As per the remote sensing evidence of 1986, about 25% of the Pichavaram mangrove was found critically degraded. However, the entire mangrove habitat was restored by the local fishing communities with the intermediation of a leading NGO [13, 53]. Although clear felling is now restricted in Pichavaram, reclaimed mangroves proved essential in restoration of livelihood concerns of large fishing communities.Many countries have modified or presently are modifying the existing mangrove management framework to accommodate CBMM initiative which is by and large turned out to be the most successful mangrove management model in this region. In case of Thailand, it is mentioned by the Royal Government that a greater number of successful CBMM initiatives helped to maintain the desirable nationwide mangrove cover of more than 2000 sq·km. [54] However, CBMM initiatives are still in a nascent stage in several countries of South and Southeast Asia. In countries like Vietnam and Malaysia, CBMM has been adopted; yet, its effectiveness is still not proved beyond doubt. In case of Vietnam, CBMM is initiated under Protection Forest Management Boards (PFMBs) at provincial level, but it neither contains any legal sanctity nor extends the forest rights to the managing communities [55]. Also, it is reported that poor incentive does not essentially interest the community in comanagement initiatives. Yet, CBMM has tremendous potential, especially in countries like Pakistan and Myanmar, where loss of livelihood due to mangrove deterioration adversely affected the coastal communities.


## 5.1. Legislative Protection of Mangroves

Legislative protection of mangroves comes from the idea of in-situ conservation under the “protected area” concept. Although approximately 25% of the global mangroves are presently conserved under varied degree of protection, in case of the Indo-Malayan ecoregion, rough estimation reveals that less than 20% of the mangroves presently possess such status. Yet, evidence of mangrove conservation in the region can be documented since the colonial era, especially under the Forest Conservation Act, 1927 of British India. Under this particular act, approximately 344870 ha of mangrove forests were transferred to Sindh Forest Department for effective conservation which still forms one of the largest protected mangrove areas in Pakistan [51]. Similarly, this act was also instrumental for the protection of Sundarban mangroves both in India and Bangladesh. Nevertheless, legislative protection of mangroves was predominantly ratified after the Ramsar Convention (1971) on “the Wetlands of International Importance.” Two specific measures suggested in the Ramsar Convention were “conservation” and “wise use of wetland resources.” Although initially only 11 Asian countries joined this convention, it strongly initiated the need of mangrove conservation into the national policies of several South and Southeast Asian Countries. Following the convention, Pakistan, India, Philippines, and Indonesia formed National Mangrove Management Committee to promote mangrove conservation. Presently, all the South and Southeast Asian countries with dense to moderate mangroves have joined the convention with the latest addition of Myanmar in 2005. Of late, following the Indian Ocean Tsunami, several countries have mentioned mangrove restoration as a national priority. Also, some of them ratified the “coastal green belt” concept which involved massive mangrove plantation along the coast. For example, about 12000 ha of mangroves were planted by the Vietnamese government only as coastal protection initiatives. On the other hand, Government of Bangladesh initiated massive plantation program of 120,000 ha following the Cyclone “Sidr.” However, despite the legislative protection and massive plantation, poor implementation of laws and by laws largely proved conservation efforts futile in almost all the South and Southeast Asian countries. Coastal communities invaded the mangroves for their continual survival, and as a result, conservation and plantation initiatives could only result in conflicts among the local governments and mangrove-dependent communities. On the other hand, a new set of environmental worries from massive water pollution and unsustainable development of coastal areas escalated mangrove deforestation. Many countries formed a second set of legislation that indirectly controls the mangrove degradation. Yet, the problem persisted with poor level of implementation and inadequate monitoring framework. In this paper, a comparative analysis in terms of existing country-specific legislative arrangements for mangrove is produced in Table 4.Table 4
Country wise comparative analysis of legislative aspects of mangrove conservation.
Country
Main governing department
Legislative aspects of mangrove conservation
In-situ conservation of natural resources
Community participation in mangrove management
Control of shrimp farming
Coastal zoning/integrated coastal zone management
Marine/coastal environmental protection
Legislative provisions of coastal greenbelt development
Pakistan
Provincial Forest Departments
Major Provisions inForest Act,  1927and subsequent  provincial acts
No specific legislative arrangement
No specific legislative arrangement
No specific legislative arrangement
Major Provision inNational Action Plan on Environment
No specific legislative arrangement
India
Ministry of Environment and Forest
Major Provisions inForest Conservation Act,  1980 and Wildlife (Protection) Act,  1972
Major Provisions inJoint Forest Management Initiatives adopted by National Forest Policy, 1988
Major Provisions inCoastal Aquaculture Authority Act,  2005
Major Provisions inCRZ Notification,  1991 (rev.2004) under the Environmental Protection Act of 1986
Major Provisions inEnvironmental Protection Act, 1986,Water Prevention and Control of Pollution Act, 1974
No specific legislative arrangement
Bangladesh
Ministry of Environment and Forest
Major Provisions inForest Act, 1927(Amendments in 1989)
Major Provisions inForest Policy,  1994 allowing community participation
Some Provisions inEnvironmental Regulations,  1997
Major Provisions inCoastal Zone Policy, 2005
Major Provisions inEnvironmental Regulations,  1997
Some provisions inCoastal development strategy
Myanmar
Ministry of Forests
Major Provisions in Forest Act, 1995
Some Provisions inForest Policy, 1995
No specific legislative arrangement
No specificlegislative arrangement
No specificLegislative arrangement
No specific legislative arrangement
Thailand
Royal Forestry Department and Ministry of Natural Resources and Environment
Major Provisions inNational Forest Reserves Act,  1964
Major Provisions in Community Forestry Bill,  2007
No specific legislative arrangement
Some Provisions inLand Development Act, 1983
Some ProvisionsEnhancement and Conservation of National Environment Quality Act, 1992
No specific legislative arrangement
Vietnam
Ministry of Natural Resources and Environment and Ministry of Agricultural and Rural Development
Major Provisions in Forest Protection and Development Law, 2004
Some Provisions in 2003 amendments of Land Law, 1993
Some Provisions in Environment Protection Law, 1994 and Land Law, 1993
Some Provisions inDecree 25
Major  Provisions in Resolution 41/2004 and Environmental Protection Law (Revised 2005)
No specific legislative arrangement
Malaysia
Department of Forestry (Provincial Government)
Major Provisions in National Forestry Act 1984 (revised 1993)
No specific legislative arrangement
No specific legislative arrangement
Major ProvisionsIn 9th Malaysian Plan (2006–2010)
Major ProvisionsEnvironment Quality Act, 1974 and Merchant Shipping (Oil Pollution) Act of 1994
Major ProvisionsIn 9th Malaysian Plan (2006–2010)
Indonesia
Ministry of Forestry
Major Provision in Presidential Decree 32 (1990)/Law no.5 (1990)
Some Provisions in 2004 amendments in Law no. 32/41
No specific legislative arrangement
Major Provisions in Law no. 27 (2008)
Major Provisions in Law no. 32 (2009)
400 m greenbelt as perDecree no. H.1/4/2/18/1975
Philippines
Department of Environment and Natural Resource
Major Provision in  Republic Act 7586 (1992)
Major Provision in  Republic Act 8371 (1997)
Major Provisionsin Republic Act 8550 (1998)
Major Provisions in Coastal Zone Management Plan,  1997
Major Provisions in Presidential Decree no. 979 (1976)
DENR A.O. 76 (1987)—50 m coastal greenbelt development


## 5.2. Sustainable Management of Mangroves and Comanagement Initiatives

Sustainable Forest Management is a key concept that uses the forests in a way, and at a rate, that maintains their biodiversity, productivity, and the regeneration capacity. It essentially allows traditional uses of forest in a regulated way, so that the ecosystem services are not hampered. Although the formal definition of Sustainable Forest Management came after the United Nations Conference on Environment and Development (UNCED) in 1992, Sustainable Mangrove Management can easily be referred to the advocacy of Ramsar Convention about the “wiseuse” of wetlands. In case of Indo-Malayan mangroves, Sustainable Mangrove Management (SMM) is still a less used tool as the countries lack political will and institutional transparency. Yet, the best example of Sustainable Mangrove Management can also be referred from this ecoregion. The Matang mangrove forest, covering some 4000 ha in the peninsular Malaysia, is a classic example of sustainable management of mangroves. The forest is managed over hundred years through the active participation of all stakeholders. Almost 75% of this forest is designated as productive forest and exploited for wood resources, while the rest are conserved for promoting biodiversity. The 30-year rotation cycle of mangrove felling gives the highest net return on capital value. At present, the timber industry from Matang supports almost 2400 people and earns revenue of USD 6 million. The unproductive forest, on the other hand, supports about 10000 people with gross annual revenue of USD 12–30 million through sustainable fishing practices [52].Sustainable Forest Management originates from the key concept of comanagement of forest resources and essentially involves multiple stakeholders. In South and Southeast Asian countries, mangrove-dwelling communities have long been ignored in the centralized mangrove management policies. As a consequence, conservation initiatives could not achieve the desired results. Since late eighties, many countries in the region shifted towards a decentralized management approach involving the local communities as an important stakeholder. Since the last decade, community-based mangrove management (CBMM) has gained popularity in almost all the South and Southeast Asian countries. CBMM is particularly prominent in Indo-Malayan ecoregion, yet the level of its penetration varies significantly. In the Indo-Malayan ecoregion, the present success of mangrove restoration as well as conservation largely depends upon the community participation in mangrove restoration and management. CBMM initiatives are particularly prominent in Thailand, Indonesia, Philippines, Bangladesh, and India. One of the finest examples of CBMM is regarded as the restoration of the Pichavaram mangrove forest in India. Pichavaram is the second largest mangrove forest in India; however, owing to over exploitation of aquatic resources and persisting natural calamities, it was degraded to a great extent. As per the remote sensing evidence of 1986, about 25% of the Pichavaram mangrove was found critically degraded. However, the entire mangrove habitat was restored by the local fishing communities with the intermediation of a leading NGO [13, 53]. Although clear felling is now restricted in Pichavaram, reclaimed mangroves proved essential in restoration of livelihood concerns of large fishing communities.Many countries have modified or presently are modifying the existing mangrove management framework to accommodate CBMM initiative which is by and large turned out to be the most successful mangrove management model in this region. In case of Thailand, it is mentioned by the Royal Government that a greater number of successful CBMM initiatives helped to maintain the desirable nationwide mangrove cover of more than 2000 sq·km. [54] However, CBMM initiatives are still in a nascent stage in several countries of South and Southeast Asia. In countries like Vietnam and Malaysia, CBMM has been adopted; yet, its effectiveness is still not proved beyond doubt. In case of Vietnam, CBMM is initiated under Protection Forest Management Boards (PFMBs) at provincial level, but it neither contains any legal sanctity nor extends the forest rights to the managing communities [55]. Also, it is reported that poor incentive does not essentially interest the community in comanagement initiatives. Yet, CBMM has tremendous potential, especially in countries like Pakistan and Myanmar, where loss of livelihood due to mangrove deterioration adversely affected the coastal communities.


## 6. Recommended Strategies and Way Forward

In this study, it has been observed that irrespective of climate change and persisting natural calamities, anthropogenic interventions are the root causes of the degradation of Indo-Malayan mangroves. Two specific human activities in form of coastal agriculture and shrimp farming have also been highlighted as major depleting factors of the South and Southeast Asian mangroves. It is also observed that the loss of mangroves has been strongly associated with the increasing disaster vulnerability of the coastal communities. Hence, it is highly imperative to form a full proof, sustainable, and comprehensive mangrove management strategy for the revival as well as conservation of Indo-Malayan mangroves. Therefore, a set of recommended strategies has been provided in order to continue the valuable ecosystem and environmental services of the Indo-Malayan mangroves. The recommended strategies are broadly categorized under three sections.Restructuring of Legislative Framework
(i)
South and Southeast Asian countries exhibit tremendous potential of community-based mangrove management (CBMM); however, in many countries, it lacks legal sanctity. Also, it was observed that even though communities are involved, they procure only the secondary role in mangrove management. Hence, it is highly imperative to mainstream CBMM into national mangrove management strategies and empower the local community in decision making process. Better economic incentives are also crucial in terms of economic sustainability of CBMM approaches. At present, CBMM approaches should be legalized, and necessary amendments should be made in all legislative aspects of mangrove management in order to avoid contradictions.
(ii)
The existing legislative arrangements for mangrove conservation are not yet full proof and also contradictory in nature. In one hand, many local governments promote aquaculture in coastal areas; on the contrary, mangrove conservation is also simultaneously prioritized. Therefore, more transparent legislative framework is envisaged. Although countries like India and Bangladesh are typically strong on the policy front, implementation and monitoring mechanism is essentially poor in all the South and Southeast Asian countries. Therefore, protective legislations need to include comprehensive monitoring mechanisms at all levels of governments. All the countries should conduct management audit at central, provincial, and local level.
(iii)
On the other hand, secondary legislative arrangements for mangrove management need to be strengthened. It is observed that despite the huge loss of mangroves due to shrimp farming, most of the countries in this region do not own a suitable legislation for control of shrimp farming in mangrove areas. As a result, virgin mangrove areas are regularly encroached for illegal shrimp farming. Therefore, it is essential for countries like Thailand, Malaysia, and Indonesia to formulate and implement proper legislation for control of shrimp farming in mangrove areas.
(iv)
Coastal zoning and integrated coastal zone management (ICZM) approach is another very important aspect of mangrove management. Although some countries have already formulated legislative framework for coastal zoning; meticulous implementation of the prescribed guidelines is strongly required. Countries like Pakistan, Myanmar, and Vietnam need to strengthen their legislative arrangements for coastal zoning in order to promote sustainable development along the coasts.Governance and Institutional Dimension of Mangrove Management
(i)
In all the South and Southeast Asian countries, multiple government agencies/departments manage different components of the mangrove resources. Although forest departments of federal or provincial governments hold the key responsibility, several other government departments are critically associated with mangrove management, especially, in resource assessment and harvesting, economic valuation, and community development. The civil government is largely responsible for community empowerment. In the past, poor coordination among the various government departments led to mismanagement of mangroves. Therefore, increased coordination among the managing authorities is strongly envisaged. Also, it is recommended to form a central agency that can coordinate the entire management activities through a “bottom up” approach.
(ii)
Institutional capacities of the local government officials need to be improved with proper scientific training. In many restoration initiatives in this region, lack of knowledge in species and site selection resulted in low survival and ineffective restoration. Even if the mangroves were restored, the ecosystem services could not be streamlined. In general, plantation activities should include the broader perspective of ecosystem restoration.Balanced Economic Development and Transboundary Cooperation
(i)
Economic development in coastal areas needs to be done in a sustainable way with proper care of the mangroves. Although provisions of environmental impact assessment for developmental activities are prevalent in almost all the South and Southeast Asian countries, their significance is constantly challenged against the economical and developmental priorities. Special emphasis is therefore required for careful selection of developmental sites. Also, compensatory aforestation should be promoted for developmental activities in mangrove areas.
(ii)
Finally, regional cooperation for transboundary ecosystem management needs to be enhanced. Out of the six mangrove habitats in the Indo-Malayan ecozone, five are shared by two or more nations. Therefore, regional cooperation for joint action plan, joint monitoring program for ecosystem health assessment, and transboundary environmental management form crucial management issues. Presently, some formal initiatives are in place in Sundarban mangroves between India and Bangladesh; however, given the extent of mangrove extent of Indo-Malayan ecoregion, it is highly recommended for a regional platform to share different management experiences, opportunities, and challenges.



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*Source: 379429-2013-04-09.xml*