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Migrations. maritime hammock occurs on old coastal dunes that have been stabilized long enough for the growth of a forest. tree growth often begins in swales between old dune ridges where a higher moisture gradient exists. the isolated strips of tree growth gradually coalesce into a continuous forest. humus buildup contributes to moisture retention, while the dense canopy minimizes temperature fluctuations by reducing soil warming during the day and heat loss at night. soils of maritime hammock are generally well-drained because of the underlying deep sands. the generally mesic conditions and insular locations of well-developed maritime hammock communities inhibit natural fires, which occur no more frequently than once every 26 to 100 years. in mature maritime hammock, fire may alter the original appearance, obscuring former beach ridge vegetation patterns and creating a diversity of plant sub-associations. nutrient recycling is generally accomplished by detrital organisms instead of by fire. maritime hammock is closely associated with and often grades into coastal strand, scrub, hydric hammock, or prairie hammock. because of species overlap, maritime hammock may also be confused with shell mound, coastal berm, xeric hammock, and rockland hammock. maritime hammock is the terminal stage of succession in coastal areas. maritime hammock is prime resort and residential property because of its relatively protected location along the coast. although it originally occurred in virtually continuous bands with coastal strand, maritime hammock is now dissected into short strips by development and is rapidly disappearing. maritime hammock is reasonably resilient so long as the canopy remains intact and the landform stable. removal of large exotic species should be conducted in phases to minimize canopy disruptions. shell mound - synonyms: midden, indian mound, tropical hammock, maritime hammock, coastal hammock ; . shell mound is unusual among the biological communities in that it is largely a result of the activities of indians, instead of natural physical factors. shell mound is generally characterized as an elevated mound of mollusk shells and aboriginal garbage on which a hardwood, closed-canopy forest develops. in some cases, a sparse shrubby community, sometimes with cactus, may develop in lieu of hammock vegetation. typical plants include gumbo-limbo, cabbage palm, mastic, red cedar, hackberry, live oak, forestiera, coral bean, marlberry, saffron plum, sagaretia, coontie, and others. shell mound soils are composed of shells and shell fragments with an organic component derived from forest litter. the soil generally is circumneutral to slightly alkaline ph 7-8 ; and contains 1-20% organic materials. the loose collection of shells allows water to drain extremely rapidly. the calcareous substrate, in combination with their coastal location, often permits tropical or subtropical species of plants to grow much further north on shell mounds than their normal ranges on other substrates. their coastal, usually insular, location generally protects shell mounds from fire, but subjects them to marine influences, including high winds, salt spray, 12 and slot machine software.
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