Abstract
Between 24 May and 4 June 1986, the island of Jamaica experienced up to 635 mm of rainfall producing islandwide flooding. Planktonic communities along the south coast were studied before and after the flooding. Flood waters from Kingston Harbour flowed southwest along the Hellshire coast as far as Wreck Reef, but were confined within 4 km of the shore. Water in the bays along the lower Hellshire coast remained clear and unaffected by Harbour water, although planktonic communities there showed marked changes. The Port Royal Cays area and much of the shelf was unaffected (...)
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