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On low lying coral islands, potable water is commonly sourced from shallow, fresh groundwater lenses. Although rainwater is also collected in tanks in the wet periods, dependence on the lense for all water needs becomes critical in dry periods. Protecting the groundwater from pollution is a major concern. In the management of reticulated supplies private land is sometimes converted to a public reserve to restrict access and use in an attempt to ensure that groundwater is protected from surface contaminants. Usually this is achieved by a lease agreement between landholders and the government utility and this arrangement can be politically, socially and economically contentious. However in the village context where private wells are still used by landholders, control of pollution sources is more practically complex, while still raising many sociocultural considerations. This paper describes

Coral atolls are natural laboratories within which to examine ecological processes (Sachet, 1967; Lee, 1984). They are often isolated, in some cases little disturbed, and have a geologically recent history of terrestrial plant colonisation. Reef islands around the rim of most atolls are Holocene in age. They are composed of biogenic skeletal sediments and have developed since reef growth caught up with sea level which stabilized after post-glacial sea-level rise. Plant colonisation of most of these islands must have occurred over a period of no more than 6000 years.