With 213,000 ha of remaining mangroves in 2016 [1] , Madagascar has about 4260 ha of mangrove on its Eastern coast. Very little studied so far, this Eastern ecosystem remains unrecognized [2] despite the ecological, social and economic functions it provides [3] . However, the two recent articles of Rakotomavo et al. [4] [5] confirm not only how important the Malagasy Mangroves of eastern Madagascar are, but also the new knowledge on some Mangrove sites in the area. Described as small mangroves [6] for the most part, the mangroves of the Eastern Malagasy coast are generally located in bays where the wave strength is more attenuated [7] ; that is to say, the low tide which is comprised between 0.5 to 1 m according to [8] , as well as the difficulty of the hydro-dynamic sedimentation process described by [4] [5] , do not favor the installation of mangroves along the East coast of the island.

Comprising a rich, varied and complex ecosystem [9] , mangroves constitute an important ecological niche for the food and financial resources of the riparian population. As small as they are, they must be considered in the same way as other development factors. This article gives an inventory and a first description of this ecosystem of the East Malagasy coastline. Its purpose is to provide essential data on its spatial distribution, its ecological potential and the pressures it undergoes. It started from a hypothesis on the absence of pressure on this ecosystem, as well as on the floristic poverty of the latter.

Five main mangrove sites on the Eastern coast of Madagascar were chosen from South to North because of their accessibility and spatial position: Foulpointe, Sainte Marie, Manompana, Mananara Nord and Rigny (Figure 1). All these sites belong to the warm and humid climate area of eastern Madagascar. However, the value of their climatic parameters vary in terms of average annual temperatures and rainfall, respectively: 25˚C and 1330 mm in Rigny Bay, 26˚C and 2476 mm in Mananara Nord, 24˚C and 3060 mm in Manompana, 25.5˚C and 3369 mm in Sainte Marie, 22˚C and 2986 mm in Foulpointe. With 110 to 280 mm of monthly rainfall, the five study sites have no dry season [2] [5] [10] .

From June 2017 to September 2017, floristic and forest inventory work was carried out at these sites to know their floristic biodiversity, their forest potential in terms of aboveground biomass and regeneration capacity. Transects of 50 - 100 m, perpendicular to the coast line and/or water courses, including 10 m × 10 m plots [11] , were surveyed to assess abundance and the tree density of different development stages, as well as their dimensions in terms of diameter at breast height and heights (total and that of the bole). The regeneration potential of trees was assessed from the ratio between regenerated individuals and seed individuals. This potential is very low for a regeneration rate T < 100%; it is average for a value between 100% and 300%. The potential is respectively good to very good for 300% < T < 1000% and T > 1000% ( [12] [13] ).

35 - 55 trees per site were randomly selected, slashed to the ground and weighed on site using a precision scale at 0.001. Samples of boles, aerial roots, leaves, flowers, seeds and branches were taken and brought back to the laboratory

for drying in an oven at 105˚C for 48 hours. This operation allowed calculating the dry weight of tree samples taken from fields. Knowledge of the dry weight of the aboveground biomass B was used to calculate the carbon stock C content in their above-ground portion, according to the formula C = B/2 [14] .

The diachronic satellite image analysis Landsat 8 OLI and Google Earth 2016, combined with interviews of residents living on the mangrove lots, allowed to understand the magnitude of the anthropogenic pressures experienced by each site. From June 2017 to September 2017, 33 people living near mangrove sites were surveyed in Foulpointe, 158 in Sainte Marie, 33 in Manompana and 78 in Rigny. In other words, 10% to 17% of the residents and/or direct users of the mangrove lots studied were surveyed. It should be noted that the interviews had been focused on the qualitative and quantitative anthropogenic use of Mangrove resources.

Compared with the mangroves of the West Malagasy coast where the tidal range can reach 4.75 m [15] , those of the East are subject to a low tidal range of less than 1 m [8] . Also, the weak hydrodynamic sedimentation process, as well as the strong exposure to coastal waves due to its straight shape and its position perpendicular to the wave forces, are not favorable factors for the installation of mangroves; hence the scattered and localized nature of the latter. The mangrove sites in the East are more concentrated in the few areas with muddy accumulation and little exposed to the sea currents. [16] describes them as small mangroves because of their small surface area; a qualification re used by several authors such as [1] . It should also be noted that other small mangrove sites, other than the five surveyed in this study, are reported by [17] , in Diego Suarez bay, at Nosy Komba, at Loky Manambato and at Mangerina, respectively in Diana and Sava Regions (North of Madagascar). According to [18] , the protected area of Loky Manambato (Sava Region) has, at its three sites of Ampasimbania, Antafianivony and Loky, a few lots of dense mangrove from 200 to 1220 individuals・ha⁻¹, with a basal area of 2.1 to 32.8 m²・ha⁻¹ and a biovolume of 0.7 to 34.5 m³・ha⁻¹.

All the mangroves of the East and West of Madagascar belong to the Indo-Pacific region [19] and have the same floristic diversity. 8 species out of the 9 characteristics of the Eastern African coastscited by [20] and [21] can be found in the East of Madagascar; only the Avicennia officinalis species is absent. It

*: human dwelling, conservation, tourism, etc.

The presence of Heritiera littoralis Ait (Sterculiaceae) and Lumnitzera racemosa Willd (Combretaceae) on the Eastern coast of Madagascar shows that the following ecological conditions of installation of those two species also exist in the East: a site located in back mangrove where water is less salty and banks of fresh water subject to tides. It means it would be possible to find micro-habitats similar to those recorded in the West of the big island, in the East of Madagascar.

The abundance of natural regenerations in a mangrove ecosystem is common, if one refers to the study conducted by [11] in the Mangoky Delta, in southwestern Madagascar where mangrove seedlings account for 89% of all trees, as well as to works carried out by [23] in Vietnam, [24] and [25] in the Tsiribihina Delta―SW Madagascar, and [26] in Besalampy―NW Madagascar, all of which confirm the spatial advance of mangroves as per the fattening mechanism described by [27] and [28] . The mangroves of Eastern Madagascar are no exception, given the importance of seed trees on the one hand (>1000 individual s・ha⁻¹, Table 4), and the abundance of seedlings on the other hand (more than 3 times the number of seed trees, Table 5). The regenerations are particularly abundant in bays and lagoons less exposed to wave as Rigny, Analapenja (Manompana), Forbans Ikoa, Ambodiforaha and Ampanihy (Sainte Marie).

Referring respectively to the trees of the Mangoky Delta (southwestern Madagascar), Tsiribihina and Sahamalaza (West Madagascar) where the total height of the trees is between 3.66 and 7.14 m [11] and 2 to 12 m [29] , those of the East are lower (2.47 to 6.88 m). 50.40% and 1% of the delta trees measure respectively 2 - 4 m, 4 - 6 m and more than 12 m [11] compared to 63.25 and 0.6% for all 5 sites studied in the East. Consisting mainly of isolated Sonneratia alba trees at seafront, of Rhizophora mucronata individuals in quiet places undisturbed by waves and human actions, or Avicennia marina trees more than 50 years in back mangrove, big trees over 12 m with a diameter greater than 20 cm are rare on the Eastern coast. If average diameters range from 2.88 and 14.83 cm in the East, they are respectively lesser than 5 cm and between 5 and 15 cm for 40% and nearly the third the Mangoky Delta trees [11] . Compared to that of the delta (9.69 to 43.86 m²・ha⁻¹ depending on the facies), the average basal area of the East is lower, ranging from 6.35 to 24.33 m²・ha⁻¹. With values ranging from 2.1 to 32.8 m²・ha⁻¹ [18] , that of the protected areas as Loky Manambato, do however have higher maximum mean basal area.

In terms of aboveground biomass, those of Sainte Marie, Manompana, Mananara Nord and Rigny are comparable with the figures obtained by [11] in the Mangoky Delta where 20 to 180 t・ha⁻¹ of leaves, branches, boles, flowers and fruits were harvested. However, the effectiveness of the allometric relations between the diameter at breast height of trees x and the aboveground biomass y, with y = 0.248x²³⁷³ (R² = 0.959) for Rhizophora mucronata, and y = 0.134x²³⁹⁹ (R² = 0.915) for Avicennia marina [11] , still needs verifications for the case of the Malagasy East.

The amount of carbon sequestered at the level of the aboveground part of the mangroves of East Madagascar is not negligible if one refers to ecosystem services that derive from it. Indeed, with a hypothetical price of 9 USD the ton¹, an annual carbon income of around 191,700 to 766,800 USD could be generated, just at the aboveground part of this ecosystem. It should be noted that according to [30] , 35% of the carbon is in the aboveground part of a mangrove, while 65% are stored in soils and roots. In other words, the carbon contained in the climax of the eastern mangrove could also be sold on the carbon market. With such a financial opportunity, we can fund the preservation activities that should be done at the level of each mangrove lot, support the stakeholders in charge of the management of the various lots, by granting them control and monitoring tools essential to their activities, and strengthening their socio-organizational and technical capacities.

In addition to the possible spatial advances related to the fattening mechanism and the abundance of regeneration [11] [23] - [28] , the small annual spatial losses recorded at the main mangrove sites on the east coast of Madagascar are also linked to the availability of woody plants such as fuel and construction timber on the dry land. The woodlands of Eucalyptus sp. and Acacia sp., just as the formations with Melaleuca quinquenervia are not only more accessible, but their energy quality are more appreciated by the local residents. Such is the case of Rigny where its mangrove lots are spared from cutting thanks to the existence of continental formations in the area [10] . For the case of the Tsiribihina (west coast of Madagascar), the greater the distance between the village and the Mangrove sites, the less villagers stock up on mangrove wood [29] . The same is true for the case of Sainte Marie where residents prefer to go for the Eucalyptus and Melaleuca trees, rather than harvesting mangrove trees for energy and/or construction purposes [2] . The spatial decline rates of the Sainte Marie, Manompana, Foulpointe, Tampolo and Rigny mangroves thus remain below the annual national rates of 1.34% [31] and 1.06% [1] . They are also still low, if we refer to the annual spatial loss of 1.75% advanced by [32] over the past two decades.

The mangroves of Madagascar eastern coast have a certain number of ecological potentials, especially at homogenous mangrove sites such as Irodo, Ambodivahibe, Rigny and Sainte Marie, where the horizontal and vertical structures of the trees are comparable to those of the Malagasy West. They are dynamic ecosystems subject to generally weak but more significant pressures in urbanized areas such as Sainte Marie and Foulpointe. Their natural regeneration capacity is an asset for their recovery, as is their capacity for carbon sequestration, a promising aspect in terms of mangrove economic valuation.

The authors declare no conflicts of interest regarding the publication of this paper.

Rakotomavo, A. (2018) The Mangroves of the East of Madagascar: Ecological Potentials and Pressures. Open Journal of Ecology, 8, 447-458. https://doi.org/10.4236/oje.2018.88027