Tropical salt pond ecosystem

Salt ponds are a natural feature of both temperate and tropical coastlines. These ponds form a vital buffer zone between terrestrial and marine ecosystems. Contaminants such as sediment, nitrates and phosphates are filtered out by salt ponds before they can reach the ocean. The depth, salinity and overall chemistry of these dynamic salt ponds fluctuate depending on temperature, rainfall, and anthropogenic influences such as nutrient runoff. The flora and fauna of tropical salt ponds differ markedly from those of temperate ponds. Mangrove trees are the dominant vegetation of tropical salt pond ecosystems, which also serve as vital feeding and breeding grounds for shore birds.

Tropical salt ponds form as bays are gradually closed off with berms of rubble from the reef. Mangroves grow atop the berms, which gradually close off the area to create a salt pond. These typically form at the base of watersheds with steep slopes, as sediments transported during storm events begin to fill in and cover up the rubble berm. Mangroves may grow over the berm, also contributing to the isolation of the salt pond. Typically, the ponds communicate with the open sea through ground seepage. Evaporation and precipitation cycles in salt ponds create variable environments with wide ranges of salinity and depth. Due to depth and temperature fluctuation salt pond could be classified as hyposaline 3-20 ppt, mesosaline 20-50 ppt, or hypersaline with ppt greater than 50. Another important aspect of salt ponds is their permanence. Salt ponds can eventually become filled in over time, and transition into an extension of the land. Some are intermittent ponds due to predictable dry and wet seasons while others are episodic (if the region has highly unpredictable weather).

Organisms typically found in and around tropical salt ponds include cyanobacteria, marine invertebrates, birds, algae and mangrove trees. For example, a typical Caribbean salt pond is the permanent or part-time home to the following:

There are 110 species of mangroves found worldwide all with special adaptations that allow for them to inhabit salt ponds. Mangroves are often found near or around salt ponds because of their ability to exist in an ecosystem with high salinity, low dissolved oxygen levels, brackish water, and extreme temperatures. Mangroves’ unique prop roots function as a barrier to the salt water, limiting water loss, and acting as a snorkel for oxygen and nutrients. Mangroves seeds have also evolved to be buoyant and germinate while still attached to the parent increasing the chance of survival in difficult environments. The presence of mangroves augments and helps maintain many of the benefits provided by salt ponds, such as:

Caribbean salt ponds commonly host three types of mangroves:

Salt ponds provide a number of important ecosystem services.

Salt ponds act as natural sediment traps that limit the amount of sedimentation and pollutants that would otherwise end up in the ocean, potentially harming other ecosystems. Salt ponds are home to dense benthic mats of bacteria which also trap nutrients such as nitrogen that otherwise would greatly contribute to detrimental marine eutrophication. Coral reefs are particularly vulnerable to sedimentation, siltation, and eutrophication processes. Salt ponds and their mangrove systems act as a buffer from storm surges associated with hurricanes and greatly dissipate wave energy that could cause erosion, including even large, rare waves such as tsunamis.

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Wikipedia