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A guide for planners and managers - IUCN

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276 MARINE AND COASTAL<br />

PROTECTED AREAS<br />

Silt deposition accelerates the succession from productive lagoon to coastal plain.<br />

The turbid waters inhibit primary productivity, which adversely affects the production<br />

of commercial fishes <strong>and</strong> shrimps. Lower production of commercial species means<br />

lowered fishery yield. Lower fishery yield means lowered per capita income from<br />

fisheries with consequent effects throughout the community of Tacarigua de la<br />

Laguna village. Madre Casanas was built to avoid a flood problem, but it has created<br />

a new problem in the economic base of the fishing community.<br />

Rainwater runoff <strong>and</strong> streams carry a great deal of silt to the river from such<br />

sources as the earthworks at the base of the dam on the Rio Guapo, small farms, <strong>and</strong><br />

houses close to the river bank.<br />

Obstruction of Freshwater Drainage<br />

Adequate freshwater input is vital to the functioning of the brackish lagoon. Too little<br />

freshwater will cause a drop in lagoon water level, an increase in temperature <strong>and</strong><br />

salinity, <strong>and</strong> a decrease in dissolved oxygen with potential massive mortality of fishes.<br />

Too much water may cause local flooding <strong>and</strong>, if sustained, drown mangrove<br />

vegetation.<br />

Completion of the dam on the Rio Guapo will enable regulation of the flow of<br />

freshwater to the Laguna de Tacarigua. This has both advantages <strong>and</strong> disadvantages.<br />

Chief among the advantages is the ability to avoid the recurrence of massive fish<br />

mortalities during unusually dry periods by maintaining a flow of freshwater into the<br />

lagoon. Chief among the disadvantages is the ability to abruptly alter conditions in<br />

the shallow western part of the lagoon by sudden large differences in the volume of<br />

water released from the dam. For example, sudden increase in the volume of released<br />

water may cause a localised precipitous drop in salinity in the lagoon, stressing or<br />

even killing organisms in the affected area.<br />

An east-west highway runs south of the lagoon, separating it from the southern<br />

water catchment. There are frequent bridges <strong>and</strong> culverts along this road, but it<br />

blocks drainage in some places.<br />

The Controversial Inlet<br />

The water level of the lagoon is variable <strong>and</strong> depends on the interaction of many factors.<br />

High water level in the lagoon maintains a strong flow of water to the sea <strong>and</strong> keeps<br />

the mouth open, so fishes <strong>and</strong> shrimps are free to enter or leave the lagoon. The juveniles<br />

of fishes spawning at sea enter the lagoon to feed <strong>and</strong> shelter in the mangrove<br />

nurseries.<br />

In the past the mouth opened naturally once the lagoonal water level had risen<br />

sufficiently to break through the bar. However, people have settled in low-lying areas<br />

that flood be<strong>for</strong>e the water level rises high enough to open the mouth naturally.

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