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Chapter 10 - Mangroves, seagrasses and decomposition

Published online by Cambridge University Press:  05 June 2012

Patrick L. Osborne
Affiliation:
University of Missouri, St Louis
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Summary

Mangroves occur between the sea and the land and line approximately 75% of tropical coasts. The term mangrove refers to both the plant community found in this saline, intertidal zone as well as the constituent tree and shrub species that grow there. Even though mangroves include plants from different genera and families, they exhibit similarities in appearance, physiology, reproduction and adaptation to habitat. This provides another example of convergent evolution (see section 8.7). Defining a mangrove as a particular type of plant without reference to its habitat is unsatisfactory since many mangrove adaptations such as stilt roots and pneumatophores are found in plants growing in areas other than the coastal zone. If one accepts the view that mangroves (the habitat) are tidal forests (Schimper 1903), then one can define a mangrove (the plant) as any woody species that grows in these forests. It should be noted that this will include species that grow outside the coastal zone, and indeed, some mangrove plants are not confined to the tidal zone.

Mangroves inhabit a changeable environment. With each high tide the sea inundates the roots and lower portions of mangrove stems. At low tide, the sediment may be completely exposed or, if the mangrove occurs along an estuary, roots may be bathed in fresh water. Tidal range varies from place to place and also with the relative positions of the Earth, moon and sun. The range is at a maximum at new and full moon (spring tides) and at a minimum (neap tides) in between full and new moon; spring tides are highest at the equinox.

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Publisher: Cambridge University Press
Print publication year: 2012

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References

Alongi, D. M. 2009 The energetics of mangrove forests New York Springer Google Scholar
Hogarth, P. J. 2007 The biology of mangroves and seagrasses Oxford Oxford University Press CrossRefGoogle Scholar

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