- Listed on more than one “valuable wetland” list by natural resource agencies or nongovernment organizations.
- Protects biological diverse wetland flora, fauna and/or their habitat
- Supports significant numbers of wetland-dependent fauna, such as water birds or fish
- Rare or unique wetland type within its own biogeographical region. (Meeting this criteria would include, but is not limited to, wetlands with unique hydrology or chemistry that make it rare within its own region)
The 500-acre lakeshore wetland complex is a "Wetland Gem" that includes an immense open-water spring that discharges clean water into Lake Waubesa and additonal springs that support a 30-acre species-rich fen, in addition to sedge meadows and shallow marshes. It is unique and highly valued for biodivesity support, conservation of the adjacent lake, research and education. Since the 1970s, it has served as an icon for understanding wetland formation and hundreds of students have benefited from studies of the wetlands, supervised by Prof. Cal DeWitt. It was chosen by the Wisconsin Wetlands Association as a state "Wetland Gem" and designated as a State Natural Area by the Wisconsin Department of Natural Resources. For more information see -- Bedford, B., Zimmerman, E. H., & Zimmerman, J. H. (1974). The Wetlands of Dane County, Wisconsin. Dane County Regional Planning Commission.
- Maintains ecological connectivity/cohesion
- Aesthetic/cultural heritage value/ provisioning
- Recreation (birdwatching, ecotourism)
- Flood storage/mitigation
- Carbon storage
- Water quality improvement
- > 100 ft
The wetland is part of a township that has ~500 ha of privately owned land with conservation easements. This extremely unusual landscape helps protect the wetlands from development. A remaining threat is nutrient-rich inflow from the adjacent upstream township.
Bigholt Deep Spring, shown in the photo, dilutes nutrients in the southern portion of L. Waubesa and keeps algal blooms offshore. This spring is itself a rare treasure.
- Inland Fresh Meadow
- Inland Shallow Fresh Marsh
- Inland Deep Fresh Marsh
- Inland Open Fresh Water
- Inland Fresh Shrub Swamp
Formed after the Wisconsin glacier retreated 14,000 years ago, leaving behind glacial till in old stream valleys; lake sediments accumulated (10-30 m thick) below the current wetland; peat accumulated (1.5-2.5 m thick).
Wetland soil is fibrous peat overlaying lake sediments.