Natural Resources
Conservation Service
Ecological site F088XY003MN
Open Peatland
Last updated: 8/12/2024
Accessed: 11/21/2024
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 088X–Northern Minnesota Glacial Lake Basins
MLRA 88 consists of the lake beds of glacial Lakes Agassiz, Upham, and Aitkin. These vast glacial lake beds were formed by meltwaters associated with the last glaciation of the Wisconsin age. The large, flat, wet landscapes are filled with lacustrine lake sediments, wave-washed glacial till, and vast expanses of organic soils. This area is entirely in Minnesota and makes up about 11,590 square miles (30,019 square kilometers).
The western boundary of MLRA 88 with MLRA 56B is gradual. MLRA 56B is a portion of the Red River Valley that was formed by glacial Lake Agassiz and is dominantly prairie. The southern boundary of MLRA 88 with MLRA 57 consists of distinct moraines that formed from the glacial drift sediments of Late Wisconsin age. The eastern and southeastern boundaries are with portions of MLRAs 90A and 93A. These MLRAs are in a distinct glaciated region of sediments of the Rainy and Superior Lobes, and much of MLRA 93A is bedrock controlled (USDA-Ag Handbook 296, 2022).
Classification relationships
MN DNR Native Plant Community (MN DNR, 2003); the reference community of this Provisional Ecological Site is most similar to:
OPn81 Northern Shrub Shore Fen
OPn91 Prairie Rich Fen
OPn92 Northern Rich Feb (Basin)
Ecological site concept
Open Peatland sites typically occur on level to gently sloping surfaces on all landforms through the area. Soils have greater than 16” of organic material and soil pH values are greater than 4.5.
Associated sites
F088XY002MN |
Marsh Marsh occurs on level or slightly concave landscape positions in closed depressions, shallow wetland basins, drainage ways, and adjacent to open water. They are very poorly drained soils and are frequently inundated with water for long durations. Soil surface textures are typically muck or mucky-modified surface layers over variable parent materials. |
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F088XY004MN |
Acid Peatland Acid Peatland occurs in shallow wetland basins, closed depressions, and along drainage ways. Soils and water content have lower pH than the open peatland sites, lending to different vegetation. Soils are occasionally ponded with standing water in spring but tend to recede by late summer. Soil surface layers are typically muck 8 to 16” thick over variable parent materials. |
F088XY005MN |
Forestland Peatland Forestland Peatland occurs on level to gently sloping surfaces. Soils have greater than 16” of organic material and soil pH values are greater than 4.5. This site has a water table typically below the peat surface that drops during the summer to allow for the establishment of significant tree cover. |
Similar sites
F088XY004MN |
Acid Peatland Acid Peatland occurs in shallow wetland basins, closed depressions, and along drainage ways. Soils and water content have lower pH than the open peatland sites, lending to different vegetation. Soils are occasionally ponded with standing water in spring but tend to recede by late summer. Soil surface layers are typically muck 8 to 16” thick over variable parent materials. |
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F088XY005MN |
Forestland Peatland Forestland Peatland occurs on level to gently sloping surfaces. Soils have greater than 16” of organic material and soil pH values are greater than 4.5. This site has a water table typically below the peat surface that drops during the summer to allow for the establishment of significant tree cover. |
Table 1. Dominant plant species
Tree |
(1) Larix laricina |
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Shrub |
(1) Salix pedicellaris |
Herbaceous |
(1) Carex lasiocarpa |
Click on box and path labels to scroll to the respective text.
Ecosystem states
T1B | - | Impoundment of water on-site, maintenance of water on-site, and/or establishment of invasive species |
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T1C | - | Tile drainage, tilling, seeding, herbicide |
T2A | - | Tile drainage, tilling, seeding, herbicide. |
State 1 submodel, plant communities
1.1A | - | Lack of fire and/or periodic drought |
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1.1C | - | Seasonal water oscillations becomes high compared to the more stable groundwater |
1.1B | - | Beaver dam off-site restricts water flow or contributes to ponding on-site |
1.2A | - | Fire, higher than average precipitation. and/or decreased frequency of inundation by surface runoff. |
1.2C | - | Seasonal water oscillations becomes high compared to the more stable groundwater. |
1.2B | - | Beaver dam off-site restricts water flow or contributes to ponding on-site |
1.3A | - | Accumulating of peat and water levels stabilize (but still remain fairly high) with stable groundwater influence. |
1.3B | - | Lack of fire and/or periodic drought. |
1.4C | - | Increased beaver dam off-site restricts water flow and contributes to ponding on-site or fire. |
1.3A | - | Removal of beaver or beaver dam. |