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Mangroves maintain coastal water quality by abiotic and biotic retention, removal, and cycling of nutrients, pollutants, and particulate matter from land-based sources, filtering these materials from water before they reach seaward coral reef and seagrass habitats. [9] Mangrove root systems slow water flow, facilitating the deposition of sediment.
The nature of these deposits depends on the environment and the types of mangroves involved. Termites process fallen leaf litter, root systems and wood from mangroves into peat to build their nests. [35] Termites stabilise the chemistry of this peat and represent approximately 2% of above ground carbon storage in mangroves. [35]
Mangroves are hardy shrubs and trees that thrive in salt water and have specialised adaptations so they can survive the volatile energies of intertidal zones along marine coasts. A mangrove is a shrub or tree that grows mainly in coastal saline or brackish water. Mangroves grow in an equatorial climate, typically along coastlines and tidal ...
Previously, attempts to restore mangrove environments were made by replanting mangrove seedlings grown elsewhere, but this proved to be ineffective. Lewis took to moving dirt and relying on tide systems, which proved more effective . There are currently multiple mangrove restoration organizations across the world to help protect biodiversity. [10]
The sea wall was reshaped to accommodate terraced planters, while the fish farm’s ponds and dikes were turned into a mangrove habitat. Inland, porous green space helps slow the flow of water and ...
In most of these regions mangroves provide many services including; shelter, climate regulation through carbon sequestration, [7] decrease coastal erosion, create a link between terrestrial and marine ecosystems, and maintain water quality along the coast. Mangroves have recently become susceptible to deforestation due to human activities and ...
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Mangroves extend along the Pacific coast south to 5°32' at the estuary of the Piura River in the north of Peru. South of that the cold Humboldt Current causes high soil salinity and very arid conditions, with hardly any fresh water streams. This is an inhospitable environment for mangroves, particularly during El Niño years. [12]