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The Ecology of Tidal Freshwater Marshes of the - USGS National ...

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2.4 FACTORS CONT3OLLIVG PLANT DEMOGRAPHY<strong>The</strong> distribution <strong>of</strong> plant speciespopulations in any natural situation reflects<strong>the</strong> response <strong>of</strong> individual speciesto soeci f ic environmental parameters. Inwetl and habitats <strong>the</strong>se parameters areespecially varied, primarily due to <strong>the</strong>i nf 1 uence <strong>of</strong> water on habi tat gradients.Siologically-mediated interactions betweenplant species fur<strong>the</strong>r coqplicate <strong>the</strong> perception<strong>of</strong> physical gradients. Much <strong>of</strong><strong>the</strong> information concerning <strong>the</strong> causes forobserved spatial distributions <strong>of</strong> vascularflora in <strong>the</strong>se marshes is anecdotal, althoughenough exists to warrant a generaldiscussion.Inundation<strong>The</strong>re seems to be a general consensusamong researchers investigating plant demographyin <strong>the</strong> tidal freshwater habitatthat <strong>the</strong> frequency and duration <strong>of</strong> floodingis <strong>the</strong> primary factor governing speciesdistributions (Kiviat 1978a; Ooumleleand Silberhorn 1978; Ferren et al. 1981;McCormick and Somes 1932). Despite <strong>the</strong>fact that <strong>the</strong> vast majority <strong>of</strong> plantsoccurring in <strong>the</strong>se marshes must experienceflooding on a daily basis, speciesvary greatly in <strong>the</strong>ir ability to withstandinundation. For some species, extensiveflooding seems to be a physiological requirement for subsistence, whereas foro<strong>the</strong>rs, it can be a detriment to normalgrowth and development. Scul thorpe (1967)notes that nicmerous terres tri a1 pl ants areable to survive long periods ei<strong>the</strong>rcompletelyor partially submerged. It isconceivable that facultative hydrophyteshave evolved in order to avoid competitionor to exploit open niches in habitats suchas <strong>the</strong>se.stunted progeny in deep-wa ter experimentalplots (Yamisaki and Tange 1981). Manyo<strong>the</strong>r researchers working in sal t marsh,mangrove swamp, and freshwater lake environmentshave concl uded that inundationeffectively contributes to segregation <strong>of</strong>pl ant species ~opul a ti ons a1 ong an el evationalgradient (Filandossian and Mc Intosch1950; Aifains 1963; Scul thorpe 1957; Kerwinand Pedigo 1971; Odum 1971). As yet, thisphenomenon has not been quantitativelydetermined for tidal freshwater marshes.However, evidence from o<strong>the</strong>r wetl and si tuationssuggests that tidal freshwaterplant communi ties segregate a1 ong inundationgradients as well.Substrate<strong>The</strong> soil in tidal freshwater marshescan be described as a waterlogged organicmuck with varying amounts <strong>of</strong> sand, silt,and clay (see Section 1.7). Differencesin soil stability, soil moisture retention,and soil nutrient availabil i t,y areall related to <strong>the</strong> physical characteristics<strong>of</strong> a given substrate and may influencespecies distributions directly. <strong>The</strong>spatial heterogeneity <strong>of</strong> substrate characteristicsis not sufficient to explaindistributions or species performance(1Jhigharn and Simpson 1975; Wetzel andPowers 1978). Wetzel and Powers (1978)concluded that substrate characteristicsaffect plant demography only in local izedzones within <strong>the</strong> marsh, and <strong>the</strong>n, <strong>the</strong>sesubtl e differences are largely obscured bymajor environmental gradients acting toproduce species distributions (e.g., elevationand tidal inundation). In ouropinion, this is an area which needsconsiderably more research.Current FlowIn <strong>the</strong> progression from open water Low-gradi ent river courses <strong>of</strong> <strong>the</strong>channels to <strong>the</strong> tnarsh-upland boundary, <strong>the</strong> Atlantic Coastal Plain tend to flow ra<strong>the</strong>rspecies composition <strong>of</strong> vascular flora sluggishly except during extreme storm orchanges noticedbly, even over almost im- flood events. Aside from channel disperceptablevariation in marsh surface charge, however, <strong>the</strong> daily ebb and floodelevations (Hoover 1983). It is known <strong>of</strong> tidal water onto and <strong>of</strong>f <strong>the</strong> marsh surthatcommon and narrow-leaved cattails face can produce significant currentwill segregate along a gradient <strong>of</strong> water velocities. Much <strong>of</strong> this water becomesdepth in nontidal habitats, <strong>the</strong> latter channel ized into dendri tical ly-shapedspecies found in deeper water (Grace and creeks within <strong>the</strong> marsh. <strong>The</strong>se creeksGetzel 1951). Common reed and wild rice deliver ground water from high marsh toa1 SO respond to varying inundation, each low marsh to channel long after <strong>the</strong> tidespecies producing fewer and somewhat has ebbed (Hoover 1983). Concentrated27

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