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  • 1
    Electronic Resource
    Electronic Resource
    Decomposition and nutrient dynamics of litter from four species of freshwater emergent macrophytes (1986)
    Springer
    Hydrobiologia 131 (1986), S. 215-223 
    Details
    ISSN: 1573-5117
    Keywords: decomposition ; model ; nitrogen ; phosphorus ; marsh ; Typha latifolia ; Carex lacustris ; Calamagrostis canadensis ; Zizania aquatica
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Nitrogen and phosphorus concentrations and mass remaining were followed for 30 months in decomposing litter of the perennial macrophytes Typha latifolia L., Carex lacustris Willd., Calamagrostis canadensis (Michx.) Nutt., and the annual Zizania aquatica L. in a fresh water tidal marsh in Massachusetts. Step-wise decreases in the mass remaining that corresponded to seasonal temperature changes were observed for all species. A model that assumes that initial litter inputs to the marsh surface consist of refractory and labile fractions and that the decay rate of the labile fraction is an exponential function of inverse temperature produced an acceptable description of the observed litter decomposition. The model suggests that a refractory fraction of 11% of initial litter weight of the annual Zizania and from 18 to 23% in the perennial species persists while labile organics are largely degraded within 1 yr. Zizania litter, which had the highest initial concentrations of both N and P, contained the lowest amounts of N and P after 30 months of decomposition. In the three perennial species studied, which are the dominant macrophytes in this marsh, there was a net accumulation of N and P in litter during the first 5 months of decomposition that was about 36% and 100%, respectively, of the annual N and P losses by vegetation in litterfall. This phase of nutrient accumulation was followed by nutrient release, particularly of N, after plant roots had invaded the litter. This sequence of nutrient accumulation, root invasion, and nutrient release represents a mechanism for nutrient conservation and/or accumulation in this ecosystem.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00008857
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  • 2
    Electronic Resource
    Electronic Resource
    Distribution and speciation of phosphorus along a salinity gradient in intertidal marsh sediments (1999)
    Springer
    Biogeochemistry 45 (1999), S. 197-221 
    Details
    ISSN: 1573-515X
    Keywords: intertidal marshes ; phosphorus ; sediments
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract We examined forms of solid phosphorus fractions in intertidal marsh sediments along a salinity (0–22‰) gradient in a river-dominated estuary and in a marine-dominated salt marsh with insignificant freshwater input. Freshwater marsh sediments had the highest ratio of organic N:P of between 28:1 and 47:1 mol:mol, compared to 21:1 to 31:1 mol:mol in the saltmarshes, which is consistent with a trend toward P-limitation of primary production in freshwater and N-limitation in salt marshes. However, total P concentration, 24.7 ± 11.1 µmol P g dw-1 (±1 SD) averaged over the upper meter of sediment, was greatest in the freshwater marsh where bioavailablity of P is apparently limited. In the freshwater marsh the greatest fraction of total P (24–51%) was associated with humic acids, while the importance of humic-P decreased with increasing salinity to 1–23% in the salt marshes. Inorganic P contributed considerably less to total sediment P in the freshwater marsh (15–40%) than in the salt marshes (33–85%). In reduced sediments at all sites, phosphate bound to aluminum oxides and clays was an important inorganic P pool irrespective of salinity. Inorganic P associated with ferric iron [Fe(III)] phases was most abundant in surface sediments of freshwater and brackish marshes, while Ca-bound P dominated inorganic P pools in the salt marshes. Thus, our results showed that particle-bound P in marsh sediments exhibited changes in chemical association along the salinity gradient of an estuarine system, which is a likely consequence of changes in ionic strength and the availability of iron and calcium.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1006136621465
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  • 3
    Electronic Resource
    Electronic Resource
    Distribution and speciation of phosphorus along a salinity gradient in intertidal marsh sediments (1999)
    Springer
    Biogeochemistry 45 (1999), S. 197-221 
    Details
    ISSN: 1573-515X
    Keywords: intertidal marshes ; phosphorus ; sediments
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract We examined forms of solid phosphorus fractions in intertidal marsh sediments along a salinity (0–22%.) gradient in a river-dominated estuary and in a marine-dominated salt marsh with insignificant freshwater input. Freshwater marsh sediments had the highest ratio of organic N:P of between 28:1 and 47:1 mol:mol, compared to 21∶1 to 31∶1 mol∶mol in the saltmarshes, which is consistent with a trend toward P-limitation of primary production in freshwater and N-limitation in salt marshes. However, total P concentration, 24.7±11.1μmol P g dw−1 (±1 SD) averaged over the upper meter of sediment, was greatest in the freshwater marsh where bioavailablity of P is apparently limited. In the freshwater marsh the greatest fraction of total P (24–51%.) was associated with humic acids, while the importance of humic-P decreased with increasing salinity to 1–23%. in the salt marshes. Inorganic P contributed considerably less to total sediment P in the freshwater marsh (15–40%.) than in the salt marshes (33–85%.). In reduced sediments at all sites, phosphate bound to aluminum oxides and clays was an important inorganic P pool irrespective of salinity. Inorganic P associated with ferric iron [Fe(III)] phases was most abundant in surface sediments of freshwater and brackish marshes, while Ca-bound P dominated inorganic P pools in the salt marshes. Thus, our results showed that particle-bound P in marsh sediments exhibited changes in chemical association along the salinity gradient of an estuarine system, which is a likely consequence of changes in ionic strength and the availability of iron and calcium.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01106781
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    Paper (German National Licenses)
    Fulltext
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