The common name for the tamarack comes from the Algonquian Native American name that means "wood used for snowshoes." Other Algonquian names that are used in English are mainly animals such as caribou, moose, chipmunk, raccoon, muskrat, opossum, woodchuck, and skunk and plants such as hickory and pecan.
There are several hundred occurrences statewide. Some documented occurrences have good viability and are protected on public land or private conservation land. This community has a limited distribution to the northern half of the state, and includes several very large, high quality examples. The current trend of this community is probably stable for occurences on public land, or declining slightly elsewhere due to moderate threats related to development pressure or alteration to the natural hydrology. This community has declined moderately to substantially from historical numbers likely correlated with peat mining and logging and development of the surrounding landscape.
The numbers and acreage of black spruce-tamarack bogs in New York have probably remained stable in recent decades as a result of wetland protection regulations. There may be a few cases of slight decline due to alteration of hydrology from impoundments (conversion to other palustrine community types).
The numbers and acreage of black spruce-tamarack bogs in New York have probably declined moderately to substantially from historical numbers likely correlated with initial peat mining and logging of the surrounding landscape (increasing nutrient run-off into bogs).
Black spruce-tamarack bogs are threatened by development and its associated run-off (e.g., agricultural, roads, railroads), recreational overuse (e.g., hiking trails causing peat compaction), and habitat alteration in the adjacent landscape (e.g., mining, excessive logging, pollution, nutrient loading). Alteration to the natural hydrology is also a threat to this community (e.g., impoundments, blocked culverts, beaver). Several examples of black spruce-tamarack bog are threatened by invasive species, such as reedgrass (Phragmites australis).
Because black spruce-tamarack bogs are naturally acidic and low in nutients, they are particularly susceptible to alteration by elevated nutrient inputs. Bogs may require larger buffers than other wetland types because of their high susceptibility to changes in nutrient concentrations. Direct impacts are typically most serious within 300 feet (90 m) of wetland areas (Sperduto et al. 2000).
Where practical, establish and maintain a natural wetland buffer to reduce storm-water, pollution, and nutrient run-off, while simultaneously capturing sediments before they reach the wetland. Buffer width should take into account the erodibility of the surrounding soils, slope steepness, and current land use. Wetlands protected under Article 24 are known as New York State "regulated" wetlands. The regulated area includes the wetlands themselves, as well as a protective buffer or "adjacent area" extending 100 feet landward of the wetland boundary (NYS DEC 1995). If possible, minimize the number and size of impervious surfaces in the surrounding landscape. Avoid habitat alteration within the wetland and surrounding landscape. For example, roads and trails should be routed around wetlands, and ideally not pass through the buffer area. If the wetland must be crossed, then bridges and boardwalks are preferred over filling. Restore past impacts, such as removing obsolete impoundments and ditches in order to restore the natural hydrology. Prevent the spread of invasive exotic species into the wetland through appropriate direct management, and by minimizing potential dispersal corridors, such as roads.
When considering road construction and other development activities minimize actions that will change what water carries and how water travels to this community, both on the surface and underground. Water traveling over-the-ground as run-off usually carries an abundance of silt, clay, and other particulates during (and often after) a construction project. While still suspended in the water, these particulates make it difficult for aquatic animals to find food; after settling to the bottom of the wetland, these particulates bury small plants and animals and alter the natural functions of the community in many other ways. Thus, road construction and development activities near this community type should strive to minimize particulate-laden run-off into this community. Water traveling on the ground or seeping through the ground also carries dissolved minerals and chemicals. Road salt, for example, is becoming an increasing problem both to natural communities and as a contaminant in household wells. Fertilizers, detergents, and other chemicals that increase the nutrient levels in wetlands cause algae blooms and eventually an oxygen-depleted environment where few animals can live. Herbicides and pesticides often travel far from where they are applied and have lasting effects on the quality of the natural community. So, road construction and other development activities should strive to consider: 1. how water moves through the ground, 2. the types of dissolved substances these development activities may release, and 3. how to minimize the potential for these dissolved substances to reach this natural community.
Survey for occurrences statewide to advance documentation and classification of peatlands. A statewide review of the acidic peatlands is desirable, similar to the studies done in New Hampshire (Sperduto et al. 2000), Massachusetts (Kearsley 1999), and similar to what New York Natural Heritage did for rich fens (Olivero 2001).
Research is needed to fill information gaps about black spruce-tamarack bogs, especially to advance our understanding of their classification, ecological processes (e.g., fire), hydrology, floristic variation, characteristic fauna, and bog development and succession. This research will provide the basic facts necessary to assess how human alterations in the landscape affect peatlands, and supply a framework for evaluating the relative value of peat bogs (Damman and French 1987).
This community is found primarily in the northern half of the state. It is concentrated in the Adirondacks, but is also common in the Great Lakes area. There are very small, scattered examples in the lower Hudson, Tug Hill Plateau, and possibly also the Alleghany area.
The range is probably widespread throughout Canada and along the northeastern fringe of the United States. The range is estimated to span northeast to Newfoundland, northwest possibly to northwestern Canada, west to Minnesota, southwest to Michigan, and southeast to Massachusetts, Pennsylvania and possibly New Jersey.
A conifer forest that occurs on acidic peatlands in cool, poorly drained depressions. The characteristic trees are black spruce (Picea mariana) and tamarack (Larix laricina); in any one stand, either tree may be dominant, or codominant. Canopy cover is quite variable, ranging from open canopy woodlands with as little as 20% cover of evenly spaced canopy trees to closed canopy forests with 80 to 90% cover. In the more open canopy stands there is usually a well-developed shrub layer characterized by several shrubs typical of bogs including sheep laurel (Kalmia angustifolia), Labrador tea (Rhododendron groenlandicum), mountain holly (Nemopathus mucronatus) and highbush blueberry (Vaccinium corymbosum). In closed canopy stands the shrub layer is usually sparse; however the species composition is similar. The dominant groundcover consists of several species of Sphagnum moss with scattered sedges and forbs. Vascular plant diversity is usually low in these forested peatlands; however the bryophyte and epiphytic lichen flora may be relatively diverse. Characteristic herbs are three-seeded sedge (Carex trisperma), cotton grass (Eriophorum spp.), pitcher plant (Sarracenia purpurea), cinnamon fern (Osmunda cinnamomea), and in shady areas where the canopy is dense, gold thread (Coptis trifolia) and creeping snowberry (Gaultheria hispidula). A black spruce-tamarack bog may imperceptibly grade into and form a mosaic with a dwarf shrub bog. As the peat substrate thins and the wetland transitions to terrestrial communities, the black spruce-tamarack bog may grade into spruce flats.
A conifer dominated, peatland swamp forest dominated by black spruce and/or tamarack. Typically the dominant species have >50% combined cover in the canopy, sub-canopy and tall shrub layers.
Known examples of this community have been found at elevations between 318 feet and 2,034 feet.
Open canopy stands with a well-developed bog shrub layer are particularly lovely beginning in late May and continuing through June, when the characteristic shrubs are in full bloom.
This New York natural community encompasses all or part of the concept of the following International Vegetation Classification (IVC) natural community associations. These are often described at finer resolution than New York's natural communities. The IVC is developed and maintained by NatureServe.
This New York natural community falls into the following ecological system(s). Ecological systems are often described at a coarser resolution than New York's natural communities and tend to represent clusters of associations found in similar environments. The ecological systems project is developed and maintained by NatureServe.
Abies balsamea (balsam fir)
Larix laricina (tamarack)
Picea mariana (black spruce)
Picea rubens (red spruce)
Pinus strobus (white pine)
Chamaedaphne calyculata (leatherleaf)
Rhododendron groenlandicum (Labrador-tea)
Vaccinium angustifolium (common lowbush blueberry)
Vaccinium myrtilloides (velvet-leaved blueberry)
Carex trisperma (three-fruited sedge)
Cornus canadensis (bunchberry)
Sarracenia purpurea (purple pitcherplant)
This figure helps visualize the structure and "look" or "feel" of a typical Black Spruce-Tamarack Bog. Each bar represents the amount of "coverage" for all the species growing at that height. Because layers overlap (shrubs may grow under trees, for example), the shaded regions can add up to more than 100%.
Cowardin, L.M., V. Carter, F.C. Golet, and E.T. La Roe. 1979. Classification of wetlands and deepwater habitats of the United States. U.S. Fish and Wildlife Service. Washington, D.C. 131 pp.
Damman, A.W.H. and T.W. French. 1987. The ecology of peat bogs of the glaciated northeastern United States: a community profile. U.S. Fish and Wildlife Service Biological Report 85(7.16). 100 pp.
Edinger, G. J., D. J. Evans, S. Gebauer, T. G. Howard, D. M. Hunt, and A. M. Olivero (editors). 2014. Ecological Communities of New York State. Second Edition. A revised and expanded edition of Carol Reschke’s Ecological Communities of New York State. New York Natural Heritage Program, New York State Department of Environmental Conservation, Albany, NY. http://www.dec.ny.gov/docs/wildlife_pdf/ecocomm2014.pdf
Edinger, Gregory J., D.J. Evans, Shane Gebauer, Timothy G. Howard, David M. Hunt, and Adele M. Olivero (editors). 2002. Ecological Communities of New York State. Second Edition. A revised and expanded edition of Carol Reschke's Ecological Communities of New York State. (Draft for review). New York Natural Heritage Program, New York State Department of Environmental Conservation. Albany, NY. 136 pp.
Kearsley, J. 1999. Non-forested acidic peatlands of Massachusetts: A statewide inventory and vegetation classification. Massachusetts Natural Heritage and Endangered Species Program, Westborough, MA.
Langdon, Stephen F., M. Dovciak, and D.J. Leopold. 2020. Tree Encroachment Varies by Plant Community in a Large Boreal Peatland Complex in the Boreal-Temperate Ecotone of Northeastern USA. Wetlands. https://doi.org/10.1007/s13157-020-01319-z
New York Natural Heritage Program. 2021. New York Natural Heritage Program Databases. Albany, NY.
New York State Department of Environmental Conservation. 1995. Freshwater Wetlands: Delineation Manual. July 1995. New York State Department of Environmental Conservation. Division of Fish, Wildlife, and Marine Resources. Bureau of Habitat. Albany, NY.
Olivero, Adele M. 2001. Classification and Mapping of New York's Calcareous Fen Communities. A summary report prepared for the Nature Conservancy - Central/Western New York Chapter with funding from the Biodiversity Research Institute. New York Natural Heritage Program, New York State Department of Environmental Conservation. Albany, NY. 28 pp. plus nine appendices.
Reschke, Carol. 1990. Ecological communities of New York State. New York Natural Heritage Program, New York State Department of Environmental Conservation. Latham, NY. 96 pp. plus xi.
Sperduto, D.D., W.F. Nichols, and N. Cleavitt. 2000. Bogs and fens of New Hampshire. New Hampshire Natural Heritage Inventory, Concord, New Hampshire.
Information for this guide was last updated on: June 29, 2020
Please cite this page as:
New York Natural Heritage Program. 2021. Online Conservation Guide for Black spruce-tamarack bog. Available from: https://guides.nynhp.org/black-spruce-tamarack-bog/. Accessed January 16, 2021.