TY - JOUR
T1 - Potential N processing by southern Everglades freshwater marshes
T2 - Are Everglades marshes passive conduits for nitrogen?
AU - Wozniak, Jeffrey R.
AU - Anderson, William T.
AU - Childers, Daniel
AU - Gaiser, Evelyn E.
AU - Madden, Christopher J.
AU - Rudnick, David T.
N1 - Funding Information:
We would like to thank numerous people for their admirable assistance both in the field and in the laboratory. These include: J. Richards, D. Rondeau, K. Lamb, T. Grahl, G. Losada, S. Ridgway, S. Ewe, C. Saunders, G Juszli, G. Noe, A. Renshaw for GIS assistance, C. Powell, R. Olvarretia, M. Dacosta, D. Iwaniec, P. Gibson & EcoTank, and the Texas Research Institute for Environmental Studies at Sam Houston State University. Funding for this research was provided by the South Florida Water Management District under several contracts to DLC, and the National Science Foundation through the Florida Coastal Everglades Long-Term Ecological Research program under Cooperative Agreements #DBI-0620409 and #DEB-9910514 . This is contribution #529 in the Southeast Environmental Research Center series.
PY - 2012/1/1
Y1 - 2012/1/1
N2 - The degree of hydrological connectivity in wetlands plays a vital role in determining the flux of energy, material, and nutrients across these wet landscapes. During the last century, compartmentalization of hydrologic flows in the Florida Everglades by canals and levees has had a profound impact on the natural timing and supply of freshwater and nutrients across the southern Everglades. Nitrogen (N) is an understudied nutrient in the phosphorus-limited Everglades; it plays an important role in many Everglades processes. To gain a better understanding of the overall N-dynamics in southern Everglades' marshes and the role that canals play in the distribution of N across this landscape, we analyzed δ 15N natural abundance data for the primary ecosystem components (the macrophyte Cladium jamaicense, marl soils, peat soils, and periphyton). Three sample transects were established in the three main basins of the southern Everglades: Shark River Slough, Taylor Slough, and the C-111 basin. Each transect included sample sites near canal inflows, in interior marshes, and at the estuarine ecotone. Natural abundance δ 15N signatures provided insights into processes that may be enriching the 15N content of ecosystem components across the marsh landscape. We also conducted a combined analysis of δ 15N data, tissue N concentrations, and water column N data to provide a broad overview of N cycling in the freshwater marshes of the southern Everglades. The primary trend that emerged from each basin was a significant 15N enrichment of all ecosystem components at near-canal sites, relative to more downstream sample sites. These data suggest that the phosphorus-limited marshes of the southern Everglades are not inactive conduits for N. Rather, these marshes appear to be actively cycling and processing N as it flows from the canal-marsh interface through downstream freshwater marshes. This finding has important implications to downstream coastal estuaries, including Florida Bay, and to nearshore coastal ocean ecosystems, such as coral reefs, where N is the limiting nutrient.
AB - The degree of hydrological connectivity in wetlands plays a vital role in determining the flux of energy, material, and nutrients across these wet landscapes. During the last century, compartmentalization of hydrologic flows in the Florida Everglades by canals and levees has had a profound impact on the natural timing and supply of freshwater and nutrients across the southern Everglades. Nitrogen (N) is an understudied nutrient in the phosphorus-limited Everglades; it plays an important role in many Everglades processes. To gain a better understanding of the overall N-dynamics in southern Everglades' marshes and the role that canals play in the distribution of N across this landscape, we analyzed δ 15N natural abundance data for the primary ecosystem components (the macrophyte Cladium jamaicense, marl soils, peat soils, and periphyton). Three sample transects were established in the three main basins of the southern Everglades: Shark River Slough, Taylor Slough, and the C-111 basin. Each transect included sample sites near canal inflows, in interior marshes, and at the estuarine ecotone. Natural abundance δ 15N signatures provided insights into processes that may be enriching the 15N content of ecosystem components across the marsh landscape. We also conducted a combined analysis of δ 15N data, tissue N concentrations, and water column N data to provide a broad overview of N cycling in the freshwater marshes of the southern Everglades. The primary trend that emerged from each basin was a significant 15N enrichment of all ecosystem components at near-canal sites, relative to more downstream sample sites. These data suggest that the phosphorus-limited marshes of the southern Everglades are not inactive conduits for N. Rather, these marshes appear to be actively cycling and processing N as it flows from the canal-marsh interface through downstream freshwater marshes. This finding has important implications to downstream coastal estuaries, including Florida Bay, and to nearshore coastal ocean ecosystems, such as coral reefs, where N is the limiting nutrient.
KW - Freshwater flow
KW - Hydrological restoration
KW - Marl soils
KW - N
KW - Nitrogen cycle
KW - Oligotrophic
KW - Peat soils
KW - Periphyton
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U2 - 10.1016/j.ecss.2011.08.024
DO - 10.1016/j.ecss.2011.08.024
M3 - Article
AN - SCOPUS:84655169196
SN - 0272-7714
VL - 96
SP - 60
EP - 68
JO - Estuarine, Coastal and Shelf Science
JF - Estuarine, Coastal and Shelf Science
IS - 1
ER -