Shingleton Bog

Status
Established
Year Established
2020

Location

State
Michigan
National Forest Regions
Eastern Region (R9)
Cypripedium reginae, Shingleton Bog RNA. USDA Forest Service Photo by: Sally Sanderson, 6-16-12

MI Natural Community Types:
Based on the Michigan Natural Features Inventory natural community types, Shingleton Bog RNA is composed of the following: 73% Hardwood-conifer Swamp, 15% Dry Northern Forest, 8% Patterned Fen, and 4% Poor Fen.


Potential Research Topics:
Shingleton Bog RNA provides an opportunity to study poor or patterned fens and make comparison with those with more pristine characteristics. The population of rare orchids also presents unique research opportunities. Other topics may include fire succession, invasive species, and climate change impacts on fens and northern wetlands.

Ecological and Physical Description

Size
3,336ac (1,350ha)
Elevation Range
785' (239m) - 838' (255m)
Temperature Range
30°F (-1°C) - 51°F (11°C)
Primary Features

Shingleton bog is an outstanding example of the Shingleton Fen Landtype Association, which is a large wetland complex formed in outwash sand reworked by Lake Algonquin. The RNA includes areas of mixed hardwood forests, patterned fens, and open bogs with associated conifers, northern dry forest, and riparian areas. The north branch of Stutt’s Creek and one of its unnamed tributaries flow through the RNA.

Annual Precipitation

Annual precipitation averages 35inches (88cm);23% received during the growing season. Average seasonal snowfall is 108inches (275cm).

Nearest Weather Station

Munisingis the nearest weather station, (I.D. # 5690, latitude 46 ̊24’N, longitude -86 ̊39+’W). The station is about tenmiles due southeastof the RNA.

Geology and Soils

The bedrock geology of the RNA is of the Ordivician Black River Group and the Trenton Group, while the surface geology is comprised of peat and muck as well as glacial outwash sand and gravel.The majority of the soils within Shingleton Bog fall under the Rubicon Series and the Kalkaska-Tawas-Carbondale Association. This series is described as well-drained, nearly level to very steep soils on outwash plains, lake plains, moraines, and dunes. The fen soils are nearly level and very poorly drained organic soils. These soils formed in sandy material.

Aquatic Features

The north branch of the Stutt’s Creek and one of its unnamed tributaries flow through the RNA. Also, a large portion of the RNA is wetland.

Flora and Fauna

Common Plant Species

Common Animal Species

Last updated February 15, 2023