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Shifting cyclone travel speed and its impact on global mangrove ecosystems. [PDF]
Mo Y +4 more
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Compounded effects on wetland greenhouse gas fluxes from climate change and water management along a saline to freshwater gradient. [PDF]
Doughty CL +30 more
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Dataset on ecological health and microbial communities of coastal aquaculture ponds from surrounding region of Sundarban mangroves. [PDF]
Yash +6 more
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Mangrove Phenology From Scale, Data and Species Perspectives. [PDF]
Wang Y +5 more
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Resonance, 2011
Mangroves are one of the world’s dominant coastal ecosystems comprised chiefly of flowering trees and shrubs uniquely adapted to marine and estuarine tidal conditions (Tomlinson, 1986; Duke, 1992; Hogarth, 1999; Saenger, 2002; FAO, 2007). They form distinctly vegetated and often densely structured habitat of verdant closed canopies cloaking coastal ...
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Mangroves are one of the world’s dominant coastal ecosystems comprised chiefly of flowering trees and shrubs uniquely adapted to marine and estuarine tidal conditions (Tomlinson, 1986; Duke, 1992; Hogarth, 1999; Saenger, 2002; FAO, 2007). They form distinctly vegetated and often densely structured habitat of verdant closed canopies cloaking coastal ...
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Biology of mangroves and mangrove Ecosystems
2001Mangroves are woody plants that grow at the interface between land and sea in tropical and sub-tropical latitudes where they exist in conditions of high salinity, extreme tides, strong winds, high temperatures and muddy, anaerobic soils. There may be no other group of plants with such highly developed morphological and physiological adaptations to ...
K. Kathiresan, B.L. Bingham
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1997
Abstract Mangroves are complex and dynamic coastal evergreen formations, generally restricted to subtropical and tropical regions. Their widest latitudinal distribution occurs in the western Pacific, where they extend from the warm temperate parts of southern Japan through the tropics to New Zealand (Chapman 1977).
Tomas Tomascik +3 more
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Abstract Mangroves are complex and dynamic coastal evergreen formations, generally restricted to subtropical and tropical regions. Their widest latitudinal distribution occurs in the western Pacific, where they extend from the warm temperate parts of southern Japan through the tropics to New Zealand (Chapman 1977).
Tomas Tomascik +3 more
openaire +2 more sources

