Salt pannes and pools


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 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 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:
These factors affect the types of species which can survive within the various types of salt pannes and pools.
Variants of salt pannes and pools:
Low salt marsh
'', a dominant species of halophyte in the intertidal zone, and Egrets feeding in a tidal pool.
Usually devoid of vegetation, that may be present include smooth cordgrass, marine algae such as knotted wrack and rockweeds. The substrate is typically soft, silty mud.
High salt marsh
Briefly flooded, very shallow with a moderate amount of vegetation usually dominated by Arrow grass, with the deeper sections possibly remaining unvegetated.
Shallow depressions with poor drainage, poor water quality due to low nutrient levels and high concentrations of sulfides and similar compounds which inhibit plant growth. Short form smooth cord-grass is the dominant plant species. Typically found on the high salt marsh, but can occasionally be found on the upper margins of low salt marsh.
Salt marsh mosquito panne
Minimal vegetation often found on the upper half of the high salt marsh. It is typically deeper than forb and smooth cord-grass pannes. Usually flooded by the higher of the two spring tides, retains water for 2–3 weeks later until drying out. The female eastern salt marsh mosquito lays eggs on the exposed surface. The eggs lay dormant until the next time the panne floods.
Widgeon grass - marsh minnow deepwater pool
Pools on the high salt marsh that are semi-permanently and permanently flooded. They are able to sustain populations of Sheephead minnow, Mummichogs,, and other species of small fish which may become trapped in the pools and benthic species of vegetation. Occasioanally can be found at the upper edge of the low salt marsh.

Brackish water marsh

Brackish marsh panne variants occur in brackish marshes, one of the native dominant species is spike grass, some brackish marsh pannes are dominated by the narrow-leaved cattail an invasive exotic species.
Shallow depressions flooded for only for a brief time and are characterized by a variable mix of graminoids and forbs. Frequent herbs include three-square rush, stout bulrush, arrow-grass, marsh creeping bent-grass, salt-loving spike-rush. Growing with less frequency are red fescue, New York aster silverweed, saltmeadow cordgrass, and salt marsh rush.
'' in foreground.
Saturated, mud dominated pannes are occasionally found in the transition zone next to forested uplands where they are shaded by overhanging tree branches thus inhibiting evaporation. This is the preferred habitat for the uncommon seaside crowfoot, where prostrate colonies may form small patches over the soil surface. Other graminoids and forbs scattered across the mud, or more often around the panne edge, include Virginia wild rye, chaffy salt sedge seaside goldenrod, marsh creeping bent grass, New York aster and smooth cordgrass.