Print Report
G360 Picea mariana / Ledum groenlandicum / Eriophorum brachyantherum Boreal Bog & Acidic Fen Group
Type Concept Sentence: This group extends across the western boreal regions of North America, extending south into the Pacific Maritime and Rocky Mountain divisions on wet organic soils (bogs) with tree- or shrub-dominated or dwarf-shrub/herbaceous vegetation.
Common (Translated Scientific) Name: Black Spruce / Bog Labrador-tea / Northland Cottonsedge Boreal Bog & Acidic Fen Group
Colloquial Name: Western North American Boreal Bog & Acidic Fen
Hierarchy Level: Group
Type Concept: This group extends across the western boreal regions of North America, extending south into subboreal regions of the Pacific Maritime and Rocky Mountain divisions. It occurs in wet depressions and old lake basins. Occurrences form where the rate of peat accumulation exceeds its decomposition, resulting in ombrotrophic and acidic peatlands in which the bog surface is raised above the water table. Patch size is small to large. These are primarily depressional wetlands, and secondary bog pools may also be present. This group may be tree- or shrub-dominated or dwarf-shrub/herbaceous. Trees may be stunted and dwarfed. Trees are dense or scattered, with common species including Picea mariana, Picea glauca, and Larix laricina. Dominant shrubs include Betula nana, Ledum palustre ssp. decumbens, Ledum groenlandicum, Andromeda polifolia, Kalmia polifolia, Chamaedaphne calyculata, Empetrum nigrum, Rubus chamaemorus, Vaccinium oxycoccos, Vaccinium vitis-idaea, and Vaccinium uliginosum. The herbaceous layer is typically graminoid-dominated. Species include Carex chordorrhiza, Carex lasiocarpa, Carex limosa, Carex livida, Carex membranacea, Carex microglochin, Carex pauciflora, Carex pluriflora, Carex rariflora (more eastern), Carex rotundata (more eastern), Carex stylosa, Eriophorum brachyantherum, and Eriophorum angustifolium.
Diagnostic Characteristics: This group represents tree, shrub or dwarf-shrub/herbaceous vegetation that occupies acidic peatlands in western North America. Strong diagnostic species that separate eastern from western acidic peatlands are not currently known. Stronger diagnostic species that are found across both eastern and western more northern boreal acidic peatlands, but are uncommon to absent further south, may include Carex membranacea, Carex microglochin, Carex rotundata, and Eriophorum brachyantherum. Two Carices, Carex rariflora and Carex rotundata, may be absent from the western peatland.
Rationale for Nominal Species or Physiognomic Features: No Data Available
Classification Comments: North American Arctic Bog & Fen was moved under this group, based on the opinion that arctic bogs (which are uncommon) are not that different from boreal bogs. Strong diagnostic species that separate eastern from western acidic peatlands are not currently known. Clarification of the limits of this type with respect to Vancouverian (North Pacific) and Rocky Mountain acidic fens is also needed. Joe Rocchio (pers. comm. 2015) suggests that for a fen to be boreal, it needs boreal indicator species to be dominant/characteristic. Those fens in Washington (and presumably Oregon) may have boreal relict rare plants in them, but the overall floristics are more akin to the Rocky Mountain group for acidic fens.
Similar NVC Types: No Data Available
note: No Data Available
Physiognomy and Structure: This group is defined by a mixed physiognomy which may be characterized by needle-leaved evergreen trees, broad-leaved deciduous shrubs or hydrophytic graminoids, particularly sedges. Trees, when present, are often dwarfed.
Floristics: This group may be tree- or shrub-dominated or dwarf-shrub/herbaceous. Trees may be stunted and dwarfed. Trees are dense or scattered, with common species including Picea mariana, Picea glauca, and Larix laricina. Dominant shrubs include Betula nana, Ledum palustre ssp. decumbens, Ledum groenlandicum, Andromeda polifolia, Kalmia polifolia, Chamaedaphne calyculata, Empetrum nigrum, Rubus chamaemorus, Vaccinium oxycoccos, Vaccinium vitis-idaea, and Vaccinium uliginosum. The herbaceous layer is typically graminoid-dominated. Species include Carex chordorrhiza, Carex lasiocarpa, Carex limosa, Carex livida, Carex membranacea, Carex microglochin, Carex pauciflora, Carex pluriflora, Carex rariflora (more eastern), Carex rotundata (more eastern), Carex stylosa, Eriophorum brachyantherum, and Eriophorum angustifolium.
Dynamics: In boreal wetlands the general successional trend is from marsh to fen to treed bog; however, succession is not necessarily directional, and environmental conditions, such as nutrient content and abundance of groundwater, may prevent fens from developing into bogs (Zoltai et al. 1988). Succession begins in shallow ponds or low-lying wetlands formed by processes such as glacial recession and floodplain dynamics (oxbows) or thermokarst. An organic root mat typically develops and is either anchored to the mineral soil or floating on water such as a pond''s edge. Over time, peat-forming mosses and sedges may fill in the basin. As the peat layer develops, low and/or dwarf-shrubs become established. Dwarf-trees may establish on the well-developed peat and also around the margin of the peatland.
Many peatlands on the Kenai Lowland formed in kettles after remnant glacial ice melted. In this region there is a trend toward peatlands drying and ponds shrinking and filling in.
Permafrost degradation leading to collapse scars and thaw ponds is common in boreal Alaska, and studies from the Tanana Flats show areas of widespread degradation. Thaw ponds form when ice-rich permafrost degrades and collapses forming a basin. Aquatic plants rapidly colonize the pond. Over time, marsh plants and sphagnum moss invade creating peatland conditions. This trend is leading to widespread ecosystem conversion in the Tanana Flats (Jorgenson et al. 2001b). If a collapse scar is isolated, succession follows a bog development model, whereas in an open hydrologic setting, succession follows a fen development model. Pond systems may become connected as adjacent permafrost thaws.
Many peatlands on the Kenai Lowland formed in kettles after remnant glacial ice melted. In this region there is a trend toward peatlands drying and ponds shrinking and filling in.
Permafrost degradation leading to collapse scars and thaw ponds is common in boreal Alaska, and studies from the Tanana Flats show areas of widespread degradation. Thaw ponds form when ice-rich permafrost degrades and collapses forming a basin. Aquatic plants rapidly colonize the pond. Over time, marsh plants and sphagnum moss invade creating peatland conditions. This trend is leading to widespread ecosystem conversion in the Tanana Flats (Jorgenson et al. 2001b). If a collapse scar is isolated, succession follows a bog development model, whereas in an open hydrologic setting, succession follows a fen development model. Pond systems may become connected as adjacent permafrost thaws.
Environmental Description: This group extends across the western boreal regions of North America, extending south into sub-boreal regions of the Pacific Maritime and Rocky Mountain divisions. Sites are generally flat to gently sloping terrain, on slopes up to 8°. Occurrences form where the rate of peat accumulation exceeds its decomposition, resulting in ombrotrophic and acidic peatlands in which the bog surface is raised above the water table. Patch size is small to large. These are primarily depressional wetlands, and secondary bog pools may also be present. Soils are poorly-drained and acidic, often with a well-developed peat layer. Permafrost is generally present and may form permafrost plateaus supporting the system in boreal Alaska but is generally absent in the boreal transition region.
Geographic Range: This group extends across the western boreal regions of North America, extending south into sub-boreal regions of the Pacific Maritime and Rocky Mountain divisions.
Nations: CA,US
States/Provinces: AB, AK, BC, ID, MB, MT, NT, NU, SK, YT
Plot Analysis Summary:
http://vegbank.org/natureserve/ELEMENT_GLOBAL.2.860841
Confidence Level: Moderate
Confidence Level Comments: No Data Available
Grank: GNR
Greasons: No Data Available
Type | Name | Database Code | Classification Code |
---|---|---|---|
Class | 2 Shrub & Herb Vegetation Class | C02 | 2 |
Subclass | 2.C Shrub & Herb Wetland Subclass | S44 | 2.C |
Formation | 2.C.2 Temperate to Polar Bog & Fen Formation | F016 | 2.C.2 |
Division | 2.C.2.Na North American Bog & Fen Division | D029 | 2.C.2.Na |
Macrogroup | 2.C.2.Na.1 Leatherleaf - Small Cranberry - Few-seed Sedge Bog & Acidic Fen Macrogroup | M876 | 2.C.2.Na.1 |
Group | 2.C.2.Na.1.d Black Spruce / Bog Labrador-tea / Northland Cottonsedge Boreal Bog & Acidic Fen Group | G360 | 2.C.2.Na.1.d |
Alliance | A3448 Small Cranberry - Bog-rosemary / Peatmoss species Shrub Bog Alliance | A3448 | 2.C.2.Na.1.d |
Alliance | A4298 Black Spruce / Peatmoss species Western Boreal Scrub Bog Alliance | A4298 | 2.C.2.Na.1.d |
Alliance | A4299 Creeping Sedge - Water Sedge - Mud Sedge Poor Fen Alliance | A4299 | 2.C.2.Na.1.d |
Alliance | A4300 Dwarf Birch Poor Fen Alliance | A4300 | 2.C.2.Na.1.d |
Concept Lineage: No Data Available
Predecessors: No Data Available
Obsolete Names: No Data Available
Obsolete Parents: No Data Available
Synonomy: > I.A.3.d - Black spruce (Viereck et al. 1992)
> II.C.2.d - Shrub birch-ericaceous shrub bog (Viereck et al. 1992)
> II.C.2.d - Shrub birch-ericaceous shrub bog (Viereck et al. 1992)
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