Dynamics of nitrogen and phosphorus retention during wetland ecosystem succession

We compared the mechanisms of nitrogen (N) and phosphorus (P) removal in four young (<15 years old) constructed estuarine marshes with paired mature natural marshes to determine how nutrient retention changes during wetland ecosystem succession. In constructed wetlands, N retention begins as soon as emergent vegetation becomes established and soil organic matter starts to accumulate, which is usually within the first 1–3 years. Accumulation of organic carbon in the soil sets the stage for denitrification which, after 5–10 years, removes approximately the same amount of N as accumulating organic matter, 5–10 g/m2/yr each, under conditions of low N loadings. Under high N loadings, the amount of N stored in accumulating organic matter doubles while N removal from denitrification may increase by an order of magnitude or more. Both organic N accumulation and denitrification provide for long-term reliable N removal regardless of N loading rates. Phosphorus removal, on the other hand, is greatest during the first 1–3 years of succession when sediment deposition and sorption/precipitation of P are greatest. During this time, constructed marshes may retain from 3 g P/m2/yr under low P loadings to as much as 30 g P/m2/yr under high loadings. However, as sedimentation decreases and sorption sites become saturated, P retention decreases to levels supported by organic P accumulation (1–2 g P/m2/yr) and sorption/precipitation with incoming aqueous and particulate Fe, Al and Ca. Phosphorus cycling in wetlands differs from forest and other terrestrial ecosystems in that conservation of P is greatest during the early years of succession, not during the middle or late stages. Conservation of P by wetlands is largely regulated by geochemical processes (sorption, precipitation) which operate independently of succession. In contrast, the conservation of N is controlled by biological processes (organic matter accumulation, denitrification) that change as succession proceeds.

[1]  W. L. Nelson,et al.  Soil fertility and fertilizers , 1957 .

[2]  E. Odum The strategy of ecosystem development. , 1969, Science.

[3]  Peter M. Vitousek,et al.  Ecosystem Succession and Nutrient Retention: A Hypothesis , 1975 .

[4]  E. D. Seneca,et al.  The Relationship of Mineral Nutrients to Growth of Spartina alterniflora in North Carolina: I. Nutrient Status of Plants and Soils in Natural Stands , 1975 .

[5]  Scott W. Nixon,et al.  Between Coastal Marshes and Coastal Waters — A Review of Twenty Years of Speculation and Research on the Role of Salt Marshes in Estuarine Productivity and Water Chemistry , 1980 .

[6]  R. Delaune,et al.  Rate of Sedimentation and Its Role in Nutrient Cycling in a Louisiana Salt Marsh , 1980 .

[7]  R. Delaune,et al.  Accumulation of plant nutrients and heavy metals through sedimentation processes and accretion in a Louisiana salt marsh , 1981 .

[8]  C. Johnston,et al.  Nutrient Trapping by Sediment Deposition in a Seasonally Flooded Lakeside Wetland , 1984 .

[9]  D. Correll,et al.  Nutrient dynamics in an agricultural watershed: Observations on the role of a riparian forest , 1984 .

[10]  E. D. Seneca,et al.  The influence of duration-of-inundation on development of a man-initiated Spartina alterniflora Loisel. Marsh in north carolina , 1985 .

[11]  C. Richardson,et al.  Mechanisms Controlling Phosphorus Retention Capacity in Freshwater Wetlands , 1985, Science.

[12]  S. Nixon,et al.  Wetlands and Water Quality. A Regional Review of Recent Research in the United States on the Role of Freshwater and Saltwater Wetlands as Sources, Sinks, and Transformers of Nitrogen, Phosphorus, and Various Heavy Metals. , 1986 .

[13]  Curtis J. Richardson,et al.  Processes controlling movement, storage and export of phosphorus in a fen peatland , 1986 .

[14]  E. D. Seneca,et al.  Long-term growth and development of transplants of the salt-marsh grassSpartina alterniflora , 1986 .

[15]  J. W. Gilliam,et al.  Phosphorus redistribution from cultivated fields into riparian areas , 1987 .

[16]  R. L. Knight,et al.  Performance of a natural wetland treatment system for wastewater management , 1987 .

[17]  Mark M. Brinson,et al.  Strategies for assessing the cumulative effects of wetland alteration on water quality , 1988 .

[18]  P. Knutson Role of Coastal Marshes in Energy Dissipation and Shore Protection , 1988 .

[19]  E. D. Seneca,et al.  Nitrogen, phosphorus and organic carbon pools in natural and transplanted marsh soils , 1988 .

[20]  E. D. Seneca,et al.  Exchange of nitrogen, phosphorus, and organic carbon between transplanted marshes and estuarine waters , 1989 .

[21]  Carol A. Johnston,et al.  Sediment and nutrient retention by freshwater wetlands: effects on surface water quality , 1991 .

[22]  P. Ambus,et al.  Comparison of Denitrification in Two Riparian Soils , 1991 .

[23]  E. D. Seneca,et al.  Porewater chemistry of natural and created marsh soils , 1991 .

[24]  J. Cooke Phosphorus Removal Processes in a Wetland after a Decade of Receiving a Sewage Effluent , 1992 .

[25]  William J. Mitsch,et al.  Landscape design and the role of created, restored, and natural riparian wetlands in controlling nonpoint source pollution , 1992 .

[26]  C. Hopkinson A comparison of ecosystem dynamics in freshwater wetlands , 1992 .

[27]  C. Richardson,et al.  Peat Accretion and N, P, and Organic C Accumulation in Nutrient-Enriched and Unenriched Everglades Peatlands. , 1993, Ecological applications : a publication of the Ecological Society of America.

[28]  C. Richardson,et al.  Peat accretion and phosphorus accumulation along a eutrophication gradient in the northern Everglades , 1993 .

[29]  E. D. Seneca,et al.  Vertical Accretion in Microtidal Regularly and Irregularly Flooded Estuarine Marshes , 1993 .

[30]  C. Richardson,et al.  FORMS OF SOIL PHOSPHORUS ALONG A NUTRIENT ENRICHMENT GRADIENT IN THE NORTHERN EVERGLADES , 1995 .

[31]  H. Paerl,et al.  Seasonal patterns of nitrification and denitrification in a natural and a restored salt marsh , 1995 .

[32]  Robert W. Nairn,et al.  Phosphorus Retention in Constructed Freshwater Riparian Marshes , 1995 .

[33]  C. Richardson,et al.  Phosphorus sorption characteristics of everglades soils along a eutrophication gradient , 1995 .

[34]  Debbie Whitall,et al.  WETLANDS , 1995, Restoration & Management Notes.