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Invited Symposia

S4. STA Technology and Everglades Restoration: Organized by Paul J. DuBowy (US Army Corps of Engineers)

The Everglades, Florida’s "River of Grass," extends from Lake Okeechobee southward to Florida Bay. This low-nutrient system is characterized by sawgrass wetlands, tree islands, marl prairie, mangroves and coastal estuaries. Restoration of the Greater Everglades ecosystem, a 50+-year project, involves "getting the water right" in terms of quantity, quality, timing and distribution. Although most interest and effort in restoration of the Greater Everglades ecosystem involves recreation of more-natural hydrology and hydrodynamics, another important aspect is water quality. Unlike most wetland systems, the Everglades is characterized by extremely low phosphorus concentrations (typically below 10 ppb) which have resulted in a distinct native flora. Phosphorus inputs, due to agriculture and urbanization, have lead to phosphorus concentrations in Everglades water and sediment well over an order of magnitude higher than historical levels, leading to extensive stands of invasive cattails (Typha).

The 1991 Settlement Agreement ended the Everglades lawsuit and was entered into by the federal government, the State of Florida and the South Florida Water Management District. The subsequent Consent Decree, as modified in 1995, specified that interim and long-term phosphorus concentration levels for Arthur R. Marshall Loxahatchee National Wildlife Refuge and Everglades National Park must be met. The Agreement calls for the construction of Stormwater Treatment Areas (STAs) to meet the long-term phosphorus limits and for establishment of a regulatory program, with agricultural Best Management Practices as a key component. A five-agency Technical Oversight Committee meets quarterly to review applied research, monitoring and compliance conducted pursuant to the terms of the Settlement Agreement.

S5. Hurricane Hugo: Impacts on Natural Ecosystems and Their Subsequent Recovery: Organized by Mike Duever (South Florida Water Management District)

Extremely severe Hurricane Hugo made landfall near Charleston, South Carolina in September 1989. A number of studies have been conducted on the initial effects of the storm and subsequent recovery from it. Primary study sites included Clemson University’s Baruch Institute along the coast near Georgetown, about 50 miles north of Charleston; National Audubon Society’s Francis Beidler Forest Sanctuary, about 30 miles inland from Charleston; and National Park Service’s Congaree Swamp, about 75 miles inland from Charleston. The latter two sites were located along the track of the storm center, and were affected primarily by high winds. The Georgetown site was somewhat north of the storm center, and affected by the storm surge and high winds. Presentations in this symposium will address the initial and delayed affects of the storm and subsequent recovery of the natural plant communities. Short and long term affects on animal populations will also be presented.

S6. Everglades Ecology and Restoration: Organized by Steve Gilbert (US Fish and Wildlife Service) and Jana Newman (South Florida Water Management District)

This symposium focuses on the multi-billion dollar Comprehensive Everglades Restoration Plan and the associated adaptive management program. Fundamental to effecting beneficial and ecologically meaningful changes to the system, is a better understanding of the current and pre-drainage ecology. The symposium offered a number of papers which explain the key role of conceptual ecological models in this process and discuss investigations which have been performed, or models which have been developed, to aid in understanding the ecology of this complex ecosystem; hence, fostering the restoration and adaptive management effort.

S8. The Human Dimensions of Regional Watershed Assessments: Research, Integration, and Measurements of Success: Organized by Marjorie Holland (The University of Mississippi), Elizabeth Blood (National Science Foundation), and Charles Cooper (USDA Agricultural Research Service)

The human dimension is critical to achieving sustainable freshwater resources. Oftentimes, there is a mismatch between "Public" goals and perceptions and "scientific" capabilities and products. While watersheds encompass rivulets, streams, wetlands, and associated channels of surface river systems, the reality is that watersheds cross political boundaries, that surface waters interface with groundwater systems, and that water users are many times unaware of the long term impacts of freshwater use. This session presented examples where an integrated process has been developed and utilized to incorporate the human dimensions into regional watershed assessments. These examples suggest that only by undergoing process-development, experimenting with innovative policies, and occasionally failing, can adaptable and comprehensive plans be developed for managing and sustaining freshwater resources in perpetuity.

S9. The Ecology of Tidal Freshwater Swamps: Organized by Ken W. Krauss (US Geological Survey), Thomas W. Doyle (US Geological Survey), and William H. Conner (Baruch Institute of Coastal Ecology and Forest Science)

Tidal freshwater swamps comprise a unique forested wetland condition because of their physiographic position of occupying low lying coastal areas where they are subjected to both upland runoff, tidal flooding, and/or aperiodic salt pulses. While these systems have received rather nominal scientific attention, they are among the most sensitive ecosystems from sea-level rise and increased drought or flood frequency. Tidal freshwater wetlands are readily impacted by acute and chronic exposure to even low levels of salinity. The combined stress of flooding and salinity may compound the threat in some systems, such that the margin for survival and compensation to changing climate is much less than for other coastal and upland habitats. In this session, we will bring together a group of investigators whose principal research focus targets hydrological processes, community organization, or stress physiology of freshwater land-margin ecosystems, mostly along the southeastern United States. The session began with a description of hydrological regimes incident to these systems, then discussed aspects of community and describe the physiological processes dictating much of this change. Lastly, specific research programs that target ecological effects of physical and biotic stressors on salt-influenced freshwater forested wetlands were be described. This session was helpful to coastal zone resource managers and ecologists interested in understanding a unique system.

S10. Biogeochemical Transformations in Floodplain Wetlands: Organized by Gregory Noe and Cliff Hupp (US Geological Survey)

Floodplains are potentially important biogeochemical hotspots for reducing nutrient loading from rivers to coastal waterbodies. Large floodplain-river ecosystems are particularly important in the Atlantic Coastal Plain of the southeastern US. This symposium presented recent research on nutrient cycling in river-floodplain ecosystems. The speakers will focus on the biotic, hydrologic, geomorphic, climatic, and geochemical controls on carbon, nitrogen, and phosphorus transformations in floodplains. Research on nutrient biogeochemistry in floodplains can help identify 1) the role of floodplains in altering downstream nutrient loading, and 2) potential management actions that can increase nutrient retention by floodplain wetlands.

S11. Wetlands of the Chesapeake Bay and Tributary Watershed: Organized by James Perry (Virginia Institute of Marine Science)

Draining 166,000 square kilometers of the mid-Atlantic region of the United States, the Chesapeake Bay is one of the largest tidal estuaries in the world. There are approximately 5,000 square kilometers of wetlands in the watershed that serve a number of important functions that are attributed high values by humans, including nutrient recycling, fin and shellfish habitat, and sediment trapping. As well, over three-quarters of the population of the mid-Atlantic region live in the watershed. This population pressure has caused severe impacts to the Chesapeake Bay wetlands to the extent that we have suffered a loss of over ˝ of the original total. The losses were mainly from dredging, filling, urban development, and relative sea level rise. The purpose of this symposium was to explore the past, present, and future of the wetland of the Chesapeake Bay and its tributary watersheds. Presenters discussed the pre-history, human impacts, current research, and future management goals and plans for both the tidal and non-tidal wetlands of the region.

S12. Treatment Wetlands: Applications and Long-Term Management: Organized by Richard Reaves (CH2M Hill)

Speakers discussed the status and future of applications of treatment wetlands. Case studies focusing on the southeastern United States examined the management issues associated with long-term operation of treatment wetlands. Two roundtable discussions were included where speakers participated in open discussions that addressed technology and design issues at the close of the morning session and management issues at the close of the afternoon session.

S13. Coastal Wetland Impoundment Ecology and Management: the Southeast, the Great Lakes, and Beyond: Organized by Daniel Tufford (University of South Carolina), Wiley Kitchens (University of Florida), and Kurt Kowalski (US Geological Survey)

Impounded and formerly impounded wetlands are prominent ecological and economic features in some coastal areas. Political and economic pressure from coastal population growth also presents significant policy and management challenges to the status and condition of these wetlands. Certain aspects of these wetland ecosystems have been studied to the point that the science community can provide substantial input to resource managers. Other aspects, however, are in need of further research, especially to cover the large variability in anthropogenic and natural stressors. Coastal impoundments share the common hydrologic history of being subject to frequent water level fluctuations (tides, seiches) prior to impoundment and the common morphologic feature that they were diked for water level control to achieve specific management objectives. In some settings, the original reason(s) for impounding no longer exist, and many are again open to more natural hydrology because the dikes were intentionally or naturally breached. This symposium focused on the ecology and management of coastal wetland impoundments along the Southeast coast (GA/SC), most of which were originally diked to support rice cultivation in the 18th and 19th centuries. It will also include significant discussion of similar systems in the Great Lakes and along the Pacific coast. The premise is that the resource management and ecosystem integrity challenges relating to coastal impoundments share similar themes regardless of location. This symposium provided a unique opportunity for scientists focused on impounded coastal wetlands to share information and learn about similar issues and research efforts across the nation.

S14. Wetlands of Coastal Watersheds: Organized by Susan-Marie Stedman (National Oceanic and Atmospheric Administration)

The term "coastal wetland" is often mis-construed as encompassing only estuarine wetlands or only tidal wetlands. NOAA has been leading an effort to look at coastal wetlands as all wetlands - estuarine or fresh, tidal or non-tidal - that occur in a coastal watershed. We have defined coastal watersheds based on USGS 8-digit HUCs. Some work by the FWS has concluded that in some coastal watersheds the majority of the wetlands are freshwater non-tidal. Data collected by the USDA's NRI points out that these coastal freshwater non-tidal wetlands are the most heavily affected by development pressure. This symposium featured papers about all types of coastal wetlands, how they interact in coastal watersheds, how they are affected by coastal development, and how they can be responsibly managed. This symposium was of great interest to anyone working in coastal areas, particularly since many of us are moving toward a watershed approach to wetland management.

 

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Last updated: Monday, 20 June 2005


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