1997
DOI: 10.1007/bf03161415
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Habitat structure and plant community composition in a northern Everglades wetland landscape

Abstract: The structure of a priori-defined aquatic habitats was compared within the Arthur R. Marshall Loxahatchee National Wildlife Refuge, which comprises the northern remnant of the Everglades ecosystem. Total plant biomass, canopy height, water depth, and the relative abundance (percent cover) of plant species in adjacent sloughs (including alligator holes), wet prairies, and sawgrass stands were compared over a 30-month period. These habitats formed a mosaic of aquatic habitats of differing structure and plant com… Show more

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Cited by 43 publications
(27 citation statements)
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References 17 publications
(23 reference statements)
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“…Using the resulting, albeit preliminary, depth-to-age relationship, we found that peaks in C. jamaicense seed profile corresponded to historic minimum water levels (e.g., at 1989-1990, and 2000-2001), while low points in the seed profile corresponded to historic maxima in water levels (e.g., 1995). This negative correlation between C. jamaicense seed abundance and higher water levels is consistent with the autecology of C. jamaicense: that high water levels decrease C. jamaicense biomass production (Newman et al, 1996;Childers et al, 2006) and that C. jamaicense biomass is less abundant in the deeper (long hydroperiod) areas of peat marshes (Gunderson, 1994;Snyder et al, 1994;Jordan et al, 1997). We emphasize that the soil dates presented here are tentative, and our inferred accretion rates ($5 mm year )1 ) appear relatively high compared to most peat-accumulating marshes in the Everglades (2.8-4.0 mm year )1 , Craft & Richardson, 1993;1.4-6.7 mm year )1 , Craft & Richardson, 1998; 1.2-1.8 mm year )1 , Cohen et al, 1999) although they are not unprecedented for South Florida peatlands (5-9 mm year )1 , Donders et al, 2004).…”
Section: Discussionsupporting
confidence: 75%
“…Using the resulting, albeit preliminary, depth-to-age relationship, we found that peaks in C. jamaicense seed profile corresponded to historic minimum water levels (e.g., at 1989-1990, and 2000-2001), while low points in the seed profile corresponded to historic maxima in water levels (e.g., 1995). This negative correlation between C. jamaicense seed abundance and higher water levels is consistent with the autecology of C. jamaicense: that high water levels decrease C. jamaicense biomass production (Newman et al, 1996;Childers et al, 2006) and that C. jamaicense biomass is less abundant in the deeper (long hydroperiod) areas of peat marshes (Gunderson, 1994;Snyder et al, 1994;Jordan et al, 1997). We emphasize that the soil dates presented here are tentative, and our inferred accretion rates ($5 mm year )1 ) appear relatively high compared to most peat-accumulating marshes in the Everglades (2.8-4.0 mm year )1 , Craft & Richardson, 1993;1.4-6.7 mm year )1 , Craft & Richardson, 1998; 1.2-1.8 mm year )1 , Cohen et al, 1999) although they are not unprecedented for South Florida peatlands (5-9 mm year )1 , Donders et al, 2004).…”
Section: Discussionsupporting
confidence: 75%
“…Approximately 65% of the Everglades is SAW, dominated by C. jamaicense Crantz (Davis 1943;Loveless 1959), with shorter hydroperiods and more frequent fires than other Everglades wetlands (Wood and Tanner 1990;Herndon et al 1991;Gunderson 1994;Jordan et al 1997). WP, the second most common wetland type, is dominated by two spikerush species, Eleocharis cellulosa and E. elongata (henceforth collectively referred to as Eleocharis spp.)…”
Section: Study Sitementioning
confidence: 98%
“…The ridge-slough landscape of the central Everglades is a lotic peatland in which distinct vegetation assemblages are organized by microtopographic variation and associated differences in hydroperiod [37], [38]. Higher elevation ridges experience annual hydroperiods of 300–340 days [39]–[41], and are occupied by largely monotypic stands of sawgrass ( Cladium jamaicense ); sloughs contain a mixture of floating and submerged plants and calcareous periphyton mats that thrive under continuous inundation.…”
Section: Introductionmentioning
confidence: 99%
“…Prior to modern hydrologic changes, elevation differences between ridges and sloughs are estimated to have ranged from 30 to 60 cm [41], [44]. Intermediate depths between ridges and sloughs were relatively rare historically [41] and in conserved landscapes [40], but support a more diverse assemblage of emergent species, in a community commonly referred to as wet prairie [37]–[39]. The abundance of the wet prairie community varies considerably across the landscape [39], [40] and increases during dry periods when slough hydroperiods and inundation depths decline [38], [45].…”
Section: Introductionmentioning
confidence: 99%