Portal:Wetlands/Selected article/20
![Salt marsh showing salt pannes and pools during low tide, mean low tide, high tide and very high tide (spring tide).](http://up.wiki.x.io/wikipedia/commons/thumb/5/56/Salt_pannes_and_pools_high_and_low_tide.gif/143px-Salt_pannes_and_pools_high_and_low_tide.gif)
Salt pannes and pools are water retaining depressions located within salt and brackish marshes. Pools tend to retain water during the summer months between high tides, whereas pannes generally do not. Salt pannes generally start when a mat of organic debris (known as wrack) is deposited upon existing vegetation, killing it. This creates a slight depression in the surrounding vegetation which retains water for varying periods of time. Upon successive cycles of inundation and evaporation the panne develops an increased salinity greater than that of the larger body of water. This increased salinity dictates the type of flora and fauna able to grow within the panne. Salt pools are also secondary formations, though the exact mechanism(s) of formation are not well understood; some have predicted they will increase in size and abundance in the future due to rising sea levels.
Salt pannes and pools are unique microhabitats dominated by various species of halophytes, benthic plants and varying estuarine marine life that vary considerably in composition due to a variety of factors including Substrate type: affects the ability of the depression to hold water. (Full article...)