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Salt pannes and pools





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This is an old revision of this page, as edited by 7mike5000 (talk | contribs)at17:45, 16 July 2010 (added/File:Fundulus heteroclitus.jpg|thumb|right|200px|Mummichogs, (''Fundulus heteroclitus''), found in deepwater pools]]). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
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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 and pools are unique microhabitats that vary considerably in composition due to a variety of factors:

  • depth and diameter: affect water temperature and evaporation rate in the depression. A shallow and wide pool will evaporate at a greater rate than a pool of the same volume of water which is deeper and has a smaller surface area. Evaporation rate also affects salinity, the higher the evaporation rate the higher the salinity, with rates as high as a third greater than ocean water.
  • location within the intertidal zone, whether high marshorlow marsh and distance from the mean low tide mark which affects the length and duration of inundation until the depression is subject to evaporation as well as length of time until the rising tide replenishes the water volume.
  • Salt marsh showing salt pannes and pools during high and low tide.

    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:

    Salt marsh panne and pool variants: Low salt marsh

    Usually devoid of vegetation, that may be present include smooth cordgrass (Spartina alterniflora), marine algae such as knotted wrack (Ascophyllum nodosum) and rockweeds (Fucus spp.). 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. Deeper sections may remain unvegetated.

    Shallow anaerobic 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 (6-12" tall)smooth cord-grass (Spartina alterniflora) 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 salt marsh mosquitoe lays eggs on the exposed surface. The eggs lay dormant until the next time the panne floods.

    Mummichogs, (Fundulus heteroclitus), found in deepwater pools

    Widgeon grass (Ruppia maritima) - 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 (Cyprinodon variegatus variegatus), Mummichogs, (Fundulus heteroclitus), 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 (short graminoid variant), some brackish marsh pannes are dominated by the narrow-leaved cattail (Typha angustifolia) 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 (Scirpus pungens), stout bulrush (S. robustus), arrow-grass, marsh creeping bent-grass (Agrostis stolonifera), salt-loving spike-rush (Eleocharis halophila). Growing with less frequency are red fescue (Festuca rubra), New York aster (Symphyotrichum novi-belgii) silverweed, saltmeadow cordgrass (Spartina patens), and salt marsh rush.

    Saturated, mud dominated pannes which are occassionally in 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 (Ranunculus cymbalaria), 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 (Elymus virginicus), chaffy salt sedge (Carex paleacea) seaside goldenrod (Solidago sempervirens), marsh creeping bent grass, New York aster and smooth cordgrass.[1][2]

    References

    1. ^ New Hampshire Division of Forest and Lands [1]
  • ^ ECOLOGICAL SYSTEM: NORTHERN ATLANTIC COASTAL PLAIN TIDAL SALT MARSH[2]

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Salt_pannes_and_pools&oldid=373838508"
     



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    This page was last edited on 16 July 2010, at 17:45 (UTC).

    This version of the page has been revised. Besides normal editing, the reason for revision may have been that this version contains factual inaccuracies, vandalism, or material not compatible with the Creative Commons Attribution-ShareAlike License.



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