Dead Tree Web
To summarize the role of dead trees and the dead wood cycle we have included the
following paper with permission from UBC Press.
Lofroth, Eric. 1998. The dead wood cycle. In: Conservation biology principles for
forested landscapes. Edited by J. Voller and S. Harrison. UBC Press, Vancouver, B.C. pp.
185-214. 243 p.
The Dead Wood Cycle
Eric Lofroth, Ministry of Water, Land and Air Protection, Victoria, British Columbia
Dead wood cycle: This term is rarely used in the literature. It refers to
the process of tree death, tree fall, and decay in the forested ecosystem. The cycle
begins with live healthy trees and ends with their incorporation into the soil organic
horizon and/or aquatic environment.
Coarse woody debris: This term has been defined variously by researchers and
managers. Some (e.g., Harmon et al. 1986) have used it to describe all states of dead wood
in the cycle, from snags to logs and fallen branches. Others (Lofroth 1993; Steventon
1994; Province of British Columbia 1995) define it as downed woody material,
distinguishing it from the 'snag' or standing dead component. The size above which debris
is considered 'coarse' varies among studies and has been identified as greater than 2.5 cm
in diameter (Harmon et al. 1986), greater than 5 cm in diameter (Mattson et al. 1987),
greater than 7.5 cm in diameter (Quesnel 1994; Keenan and Inselberg, in prep.), greater
than 10 cm in diameter (Spies et al. 1988), greater than 15 cm in diameter (Sollins 1982),
and greater than 20 cm in diameter (Harmon et al. 1987).
Here coarse woody debris (CWD) is defined as downed woody material greater than 10 cm
in diameter, and is arbitrarily distinguished from standing dead woody material (wildlife
trees or snags) by the angle of repose (less than 45° from the ground).
Snags: dead standing trees, typically with a specified lower size limit. Cline
et al. (1980) sampled snags greater than 9 cm in diameter at breast height (dbh) and
greater than 4.4 m tall. Raphael and Morrison (1987) set lower boundaries on snags of 13
cm dbh and 1.5 m tall. Lofroth (1993) set a lower limit of 7.5 cm dbh and 2 m tall. The
B.C. Ministry of Forests and B.C. Workers' Compensation Board define a snag as a standing
dead tree greater than 3 m in height (Backhouse and Lousier 1991). Here snags are
considered to be standing dead trees greater than 10 cm dbh and greater than 2 m tall,
with an angle of repose greater than 45° from the ground.
Wildlife tree: 'a tree that provides present or future valuable habitat for the
conservation or enhancement of wildlife' (Guy and Manning 1995). Wildlife trees may be
distinguished by attributes such as structure, age, abundance, location, and surrounding
habitat features. They range from live and healthy trees to decayed stubs, and, as such,
Large organic debris: essentially, coarse woody debris in aquatic ecosystems.
Large organic debris (LOD) is downed woody material, including tree boles, limbs, and
rooting structures. Van Sickle and Gregory (1990) define it as material greater than 10 cm
in diameter and greater than 1.5 m long. Bisson et al. (1987) used a limit of 10 cm in
diameter but did not specify a minimum length. Here LOD is defined as woody material in
aquatic ecosystems greater than 10 cm in diameter.
Fine fuel/slash: the debris left behind following forest harvesting, including
woody material of any size (McRae et al. 1979; Trowbridge et al. 1987).
Dead wood obligate: organism that requires some component of the dead
wood cycle for some or all of its life history. The conservation of populations of such
species can be considered dependent on the presence of dead wood.
Dead wood facultative: organism that may use but does not require some
component of the dead wood cycle for some or all of its life history.
Dead and downed woody debris in western forests is still a common attribute.
However, technology now allows the removal of more and more of this woody debris from the
forest. As well, conversion of forests from old growth to managed stands shortens the
rotation age from centuries to decades, thereby reducing the size and age of the trees
left in the forest. This reduction drastically decreases the amount, size, and quality of
dead and dying trees available for the future (Maser and Trappe 1984).
'Large, fallen trees are unique, critical components of forest systems' (Maser et al.
1979; Maser et al. 1988; Franklin and Hemstrom 1981; Franklin et al. 1981). However, in
the early days of forest harvesting, dead wood was considered a hindrance to reforestation
and stream access and quality (Triska and Cromack 1979). In the past, CWD was routinely
removed in an attempt to limit fuel loading (thereby minimizing wildfires) and make
replanting easier. Also, because of the slow rate at which CWD decayed, its role in
nutrient cycling, and therefore its importance, was not well understood (Triska and
In the Pacific Northwest and British Columbia, removal of LOD in streams began as early
as the mid-1800s and continued well into the mid-1900s. Large streams and rivers were used
for navigation and transportation of logs to the mills, and were therefore kept clear of
debris (Sedell et al. 1988). As logging encroached further up the stream and river
valleys, so did LOD removal. When the streams became too small to transport logs, splash
dams were built, allowing water to build up and sluice logs down to the larger rivers and
streams (Bisson et al. 1987). Some rivers and streams were scoured down to bedrock, and
have not yet recovered from the effects of these practices (Sedell et al. 1988).
In the 1950s and 1960s, fisheries managers were concerned that LOD restricted fish
movement and was the cause of channel scouring during floods, besides creating logjams;
they therefore prescribed its removal. The role of LOD in channel morphology was not yet
understood (Sedell et al. 1988). Although some LOD removal is still prescribed to give
fish access to the upper reaches of a stream, LOD is now considered an important part of a
functioning fish stream.
Standing dead and dying trees (wildlife trees) were also routinely removed during
timber harvest. They were once thought of only as fire and safety hazards that harboured
insects and that were of no marketable value (Bull et al. 1986). Despite their newly
recognized importance, standing dead or dying trees are still a threatened resource in
British Columbia. They are still rapidly declining because of conventional silvicultural
practices, fire prevention, firewood cutting, timber utilization standards, and worker
safety regulations (Steeger and Machmer 1994).
Dead Wood Cycling
Dead wood cycling is the process of the cycling of components of wood (carbon,
minerals, moisture, and so on) in the forest ecosystem through the processes of death,
decomposition, and uptake. The changes to trees, which are the most significant structural
features of forests, during this process affect many other forest components and functions
(Maser et al. 1979; Maser and Trappe 1984; Maser et al. 1988; Hammond 1991). In the
coastal ecosystems they studied, Franklin and Waring (1979) reported that approximately
17% of all ecosystem organic matter was found within logs (CWD) and standing dead trees
The dead wood cycle begins when the stem dies. Stem death may be immediate in some
cases, such as lightning strikes, but this process is usually slow. The trees are usually
the larger ones and remain standing for a relatively long period after they die.
Recruitment of snags from the living tree population may vary with such factors as slope,
aspect, rooting substrate, site moisture and nutrient conditions, tree species, and causes
of mortality. These factors influence the longevity of snags, CWD, and LOD. The dynamics
of each of these components are discussed below.
Dynamics of the Dead Wood Cycle
Thomas et al. (1979) and Backhouse (1993) describe decay classifications of snags
and wildlife trees. Often the important characteristics of snags and wildlife trees are
functions of previous disease or damage, and the result is a tree form or condition that
is valuable to a variety of wildlife species.
In forests that are disturbed by processes other than forest harvesting, most trees
eventually become dead wood; those that die and remain standing become part of the snag
component of the forest. The causes of mortality in live trees are varied and are likely a
combination of factors (Maser 1988). Mortality rates are usually species-specific
(Franklin et al. 1987; Raphael and Morrison 1987) and are extremely variable because of
multiple causal agents and varying site conditions. Mortality rates are reported to be
greater in high-productivity sites than in low-productivity sites (Franklin et al. 1987).
Often the mortality agents affecting trees are very different in different sites.
Researchers have reported regional differences in snag population dynamics. For
example, stocking of dead standing trees in the Sub-Boreal Spruce (SBS) Zone (Meidinger
and Pojar 1991) of interior British Columbia varied both regionally and locally. Mean
stocking of standing dead trees greater than 7.5 cm dbh was 97.7 stems per hectare (n
= 51) in the dry cool (dk) subzone and 218.8 (n = 329) in the moist cold (mc)
subzone (Lofroth, unpublished data). Franklin et al. (1987) also reported regional
differences in snag population dynamics. In mature stands within the SBSmc subzone,
stocking of snags varied by as much as a factor of 25 among different site conditions. Dry
ridgetop sites (Dry Pine) had the highest stocking of dead standing trees and alluvial
sites (Cottonwood Bottomland) had the lowest. Analysis of size distributions revealed that
much of this difference could be explained by mortality of small stems (< 20 cm).
Furthermore, only sites that were mesic and wetter had dead standing stems greater than 40
Although 'standing crop' may be important and useful in describing the structural
characteristics of a site, rates of input and decay are just as important. Mortality rates
are likely highest in younger seral stages (Franklin et al. 1987; Raphael and Morrison
1987; Lofroth, unpublished data), and primary causal agents likely change with succession
(Franklin et al. 1987). Cline et al. (1980) reported that snag production rates and
density (input) fell with increasing stand age, but mean snag size and longevity
increased. Raphael and Morrison (1987) reported that decay rates for pines in their study
area were greater than those for firs. They also reported that, regardless of species,
falling rates declined with increasing tree diameter.
In summary, recruitment of dead standing trees (snags and/or wildlife trees) varies
depending on regional and local ecological conditions. Stem mortality (and therefore snag
density) is often highest in younger seral stages. Snag densities also vary with
ecological condition, but these relationships are influenced to a great extent by
mortality agents. More productive sites generally have larger snags. Snag density
decreases and longevity increases with increasing snag size.
Coarse Woody Debris (CWD)
Coarse woody debris enters the ecosystem either directly through the death and
immediate fall of living trees (e.g., from windthrow), or through tree death and the
eventual fall of standing dead material. As with standing dead trees, there is variability
in the amount, size, species, and decay class of CWD. The amount of CWD in any stand is a
function of mortality agents, site conditions and exposure, and decay mechanisms and rates
(Harmon and Hua 1991). CWD biomass in some coniferous ecosystems may exceed the total
biomass of many deciduous ecosystems (Spies and Cline 1988). Decay classification for CWD
has been described by Maser et al. (1988).
The total volume or biomass of CWD varies with ecological condition (Spies and Cline
1988; Lofroth, unpublished data). Brewer (1993) reported that CWD in plots in some SBS
stands ranged from 37 to 384 m3/ha. Mean volumes for all stand conditions and ages were
44.1 m3/ha in the SBSdk subzone and 159.2 m3/ha in the SBSmc subzone (Lofroth, unpublished
data). The driest sites had the lowest biomass and moist sites the greatest in Douglas-fir
forests of Washington and Oregon (Spies et al. 1988). Within mature stands in the SBSmc
subzone, CWD volumes were lowest in xeric ecosystems (Dry Pine: 36.2 m3/ha and highest in
moist ecosystems (Devil's Club: 268.4 m3/ha (Lofroth, unpublished data). Mean volumes of
CWD in mature stands by natural disturbance type (Province of British Columbia 1995) and
biogeoclimatic zone ranged from a low of 60 m3/ha in the Boreal Black and White Spruce
Zone in ecosystems with frequent stand-initiating events (NDT3) (Province of
British Columbia 1995) to a high of 390 m3/ha in the Coastal Western Hemlock Zone in ecosystems
with rare stand-initiating events (NDT1) (Lofroth, unpublished data). Benson and
Schlieter (1979) reported that CWD volumes were 210 m3/ha in dry-site Douglas-fir stands,
but as much as 560 m3/ha in grand fir stands.
CWD volumes also vary with successional stage. Mean volumes across a range of moisture
and nutrient regimes in the SBSmc subzone were high in early successional stages
(herb/shrub) (174.2 m3/ha), declined to a low of 58.2 m3/ha in young forest successional
stages, and were highest in old-growth stands (261.5 m3/ha (Lofroth, unpublished data).
Spies et al. (1988) reported that amounts of CWD were high in the youngest successional
stages, were lowest in 60-80-year-old forests, and were high in old stands (< 500
years). After 500 years CWD amounts declined to an intermediate level. Spies and Franklin
(1988) reported that CWD input may be low in young stands because of the small size of
dead and dying stems. Volumes in these stands are often high, however, due to residual CWD
from the previous stand. The amount of this residual CWD depends on the disturbance agent
causing the change in succession. In stands where succession has been retarded by natural
catastrophic events (windthrow, fire, etc.), it can be significant. Spies et al. (1988)
suggest that the nature and the timing of disturbance play a key role in CWD dynamics.
Human-caused changes (such as logging) will usually result in conditions different than
those that may have initiated the original stand. In these circumstances, the amount of
CWD, as with standing dead trees, may not be indicative of natural dynamics within
The rates of input and decay also vary with ecological site conditions and stand age,
and between tree species (Sollins 1982; Spies and Franklin 1988). Sollins (1982) reported
that although there was considerable variability in the data, the highest values for CWD
biomass were reported from old-growth stands. Harmon et al. (1987) reported that decay
rates of logs may vary with microclimate, size, substrate, and species of log. Mattson et
al. (1987) reported that decay rates varied by as much as tenfold between tree species.
They also reported that aspect was an important factor in determining decay rates, and
that logs suspended above the ground decayed at slower rates than those on the ground.
Keenan et al. (1993) attribute large accumulations of CWD in western redcedar and western
hemlock stands on Vancouver Island to slow decomposition rates, high rates of input
following windstorms, and the large size and decay resistance of western redcedar. Abbott
and Crossley (1982) reported that in chestnut oak (Quercus prinus) stands,
decomposition was influenced by moisture and temperature and was inversely related to the
diameter of the material.
Large Organic Debris (LOD)
The dynamics of large organic debris (LOD) are influenced by factors that influence
CWD dynamics and those related to hydrological features and processes. Maser and Trappe
(1984) and Sedell et al. (1988) review LOD dynamics in detail. Thomson (1991) produced an
annotated bibliography that reviewed a substantial portion of the literature on this
topic. Much of this review is abridged from these accounts.
LOD enters aquatic ecosystems from a variety of sources, both chronic and episodic.
Chronic input includes debris resulting from litterfall, individual tree mortality, and
treefall; to some extent it is influenced by factors that are also important in CWD
dynamics. Riparian ecosystems are the primary source of chronic input. Input from these
mechanisms are similar in nature to CWD in streamside ecosystems, although some
differences have been noted in abundance and piece size (Van Sickle and Gregory 1990). LOD
also enters streams through episodic events such as floods, mass wasting, debris torrents,
and large-scale mortalities due to events such as insect epidemics. Much of the material
entering stream ecosystems is associated with the riparian zone, but some material
originates in upslope forested ecosystems. McDade et al. (1990) measured source distances
for logs entering small streams in a variety of stream classes and gradients in Oregon and
Washington, and found that over 70% of the logs originated within 20 m of the stream
channel. Chronic inputs of large material tend to be a feature of mature and old-growth
ecosystems. LOD input from younger successional stages tends to be smaller in nature, but
volumes may equal or exceed those originating from older stands. Input of LOD may also be
influenced by the composition of vegetation. In the U.S. Pacific Northwest, red alder is a
common early successional tree in riparian ecosystems and commonly becomes LOD. This is a
consequence of its shallow roots and low resistance to undercutting (Bisson et al. 1987).
LOD 'output' from stream ecosystems is primarily a function of the physical breakdown
of material and the transport of material downstream. Decay and breakdown processes in
stream ecosystems are considerably slower than in terrestrial and marine ecosystems
(Sedell et al. 1988). Biological decay processes are much less important in LOD dynamics
than in CWD dynamics, primarily because of the anaerobic nature of the ecosystem. The
retention time of LOD in stream ecosystems is influenced by the size and orientation of
material, the nature of deposition, the size of the stream, the scale of major flooding
events, the gradient of the stream, and the nature of sediment transfer in the stream
(Maser and Trappe 1984; Bisson et al. 1987; Sedell et al. 1988; O'Connor and Ziemer 1989).
The Roles of Dead Wood in the Ecosystem
Dead wood (snags, CWD, LOD) functions in many ways in forested ecosystems. It provides
habitat for a wealth of invertebrate, vertebrate, and plant species. It affects soil
erosion, slope movement, pool and riffle formation, and nutrient capture and retention.
Nutrient cycling in terrestrial and aquatic ecosystems is influenced by the
characteristics of woody debris.
The following discussion of the relationship between dead wood and forest biota is
strongly biased towards vertebrates. Information on plants and invertebrates is limited
and incomplete. I briefly review the role of woody debris in a variety of ecosystem
processes. The sources of information used to develop Tables 7.1 to 7.7 include Aubry et
al. (1988), Backhouse and Lousier (1991), S. Berch (pers. comm., 1995), Campbell et al.
(1990a, 1990b), S. Cannings (pers. comm., 1995), D.F. Fraser (pers. comm., 1995), Goward
(1993), L. Friis (pers. comm., 1995), E.C. Lea (pers. comm., 1995), Lundquist and Mariani
(1991), Nagorsen and Brigham (1993), J. Ptolemy (pers. comm., 1995), Redhead (1993), Ryan
(1993), Ryan et al. (1993), Scudder (1994), Tripp (1994), and Terres (1991).
Ecological Roles of Snags
The relationship between cavity users (particularly birds) and snags may be one of
the best documented wildlife/habitat relationships in North America (McLelland 1977;
Thomas et al. 1979; Mannan et al. 1980; Davis et al. 1983; Mannan and Meslow 1984; Raphael
and White 1984; Zarnowitz and Manuwal 1985; Lundquist and Mariani 1991; Machmer and
Steeger 1993; and many others). Snags serve as nesting habitat for primary and secondary
cavity-nesters (McLelland 1977; Thomas et al. 1979; and others) and perching habitat for
many bird species. In British Columbia, 26 Red- and Blue-listed vertebrate species or
subspecies depend on or are associated with snags for all or part of their life history
(Tables 7.1 and 7.2). Characteristics that affect the value of individual snags as habitat
include cause of death, diameter, tree form, bark condition, tree species, and height.
The cause of death affects the class and decay characteristics of snags. The ability of
organisms such as fungi and insects to invade wildlife trees greatly affects the value of
the snag for other wildlife. Decay organisms invading dead or dying trees serve to further
weaken or soften the tree, allowing primary cavity-nesters to excavate nests (Thomas et
al. 1979; Terres 1991).
The size of snags strongly influences which species may use them. Cav-ity-nesters in
British Columbia include species as small as nuthatches, chickadees, and small bats to
mammals as large as black bears (Tables 7.1 and 7.2) (Backhouse 1993). Black bears are
known to use large cavities (particularly in western redcedar) as winter dens (Davis
1996). Fishers whelp almost exclusively in cavities in very large cottonwood trees in
central B.C. (Weir 1995). Martens use cavities in trees as resting sites and maternal dens
(Buskirk and Ruggiero 1994). Flying squirrels, red squirrels, and many other mammalian
species utilize cavities in snags and trees for part of their life history. Herpetofauna
will use the space between loose bark and the trunk. Species such as Pileated Woodpeckers
in western North America require trees in the larger diameter classes for the ecological
conditions found there (Thomas et al. 1979; Bull et al. 1992; Bull and Holthausen 1993).
Snags also provide perches for birds of prey and insectivores such as hawking
flycatchers. Tree form and height are often important features of perches.
Bark retention and condition also influence the value of a snag as wildlife habitat.
Species such as nuthatches, a variety of bats (including Red-listed Keen's long-eared
myotis [Myotis keenii] and Northern long-eared myotis [Myotis septentrionalis]),
and the clouded salamander use the space between sloughing bark and the tree bole as
roosting and thermal habitat (Davis and Gregory 1993; Nagorsen and Brigham 1993). Some
plant species, such as licorice fern (Polypodium glycyrrhiza), are epiphytic on
snags. Others may be snag obligates (D.F. Fraser, pers. comm., 1995).
Different trees species differ in their value to wildlife. Harestad and Keisker (1989)
reported a preference for aspen as a primary cavity-nesting tree in southern B.C.
Lundquist and Mariani (1991) report that in the southern Washington Cascade Range, white
pine snags were particularly important for woodpeckers and creepers, while Douglas-fir and
western hemlock were more valuable for chickadees and nuthatches.
Ecological Roles of Coarse Woody Debris
Coarse woody debris plays numerous roles in providing habitat for organisms in
forested ecosystems. Logs become habitat for a variety of invertebrate species shortly
after falling. CWD is used by invertebrates as a source of food, for nesting and brooding
sites, for protection from predators and environmental extremes, as a source of
construction material, and as overwintering and hibernating sites (Samuelsson et al.
1994). Many invertebrates use or require particular species of CWD, and different
communities of invertebrates occupy and use different decay stages of CWD (Harmon et al.
1986; Samuelsson et al. 1994). Insectivorous species such as woodpeckers, small mammals,
and bears forage on insects dwelling in CWD (Maser et al. 1979; Maser and Trappe 1984;
Samuelsson et al. 1994) (Tables 7.3 and 7.4).
Coarse woody debris provides thermal and security cover for a variety of small mammals
in British Columbia. Sound CWD provides secure travel corridors for small mammals (Maser
et al. 1979; Maser and Trappe 1984; Carter 1993), and provides subnivean habitat during
winter. The value of this habitat is positively correlated with piece size (Maser and
Trappe 1984; Hayes and Cross 1987; Carter 1993). Nordyke and Buskirk (1991) found that
southern red-backed vole abundance was positively correlated with the decay stage of logs
in the central Rocky Mountains. Maser and Trappe (1984) and Rhoades (1986) reported
associations of small mammals with CWD because of the food source provided by the fungal
fruiting bodies growing in and on the CWD.
Gyug (1993) reported that fur-bearers (martens and weasels) used clearcuts with logging
debris more than those with no CWD; however, the level of use was much less than that of
the adjacent forest. The value of CWD to mustelids (particularly martens, weasels, and
fishers) is well documented (Baker 1992; Corn and Raphael 1992; Lofroth 1993; Buskirk and
Powell 1994; Buskirk and Ruggiero 1994; and others). Martens select habitats partly on the
basis of thermal microhabitats (Taylor 1993), such as those provided by CWD (Lofroth 1993;
Buskirk and Powell 1994; Buskirk and Ruggiero 1994). Corn and Raphael (1992) reported that
martens selected subnivean access points that had greater volumes of CWD, more layering of
logs, more sound and moderately decayed logs, and fewer highly decayed logs than random
Aubry et al. (1988) found that some species of salamander were most abundant around
CWD. Dupuis (1993) concluded that salamander populations in logged areas were limited by
available moist microhabitats, primarily because of a lack of large logs in intermediate
and advanced stages of decay. Salamanders use logs as reproduction sites, as foraging
sites, and for cover, and also lay their eggs in them (Table 7.5) (Samuelsson et al.
Coarse woody debris functions as seed beds or nurse logs for some trees species and
many species of bryophytes, fungi, and lichens, and some flowering plants (Table 7.6)
(Samuelsson et al. 1994; D.F. Fraser, pers. comm., 1995; E.C. Lea, pers. comm., 1995).
CWD, and the associated epiphytic bryophytes, act as both nutrient and moisture buffers
for the ecosystems (FEMAT 1993). This buffering allows the slow release of water and
nutrients to surrounding plants. In mature and old-growth coastal forests, a large
proportion of western hemlock and Sitka spruce seedlings germinate and grow on CWD
substrates (Harmon and Franklin 1989; G. Davis, pers. comm., 1994). In the Crowsnest
Forest, 40-70% of natural seedlings were rooted in decayed wood in old growth and 24% were
rooted in decayed wood in cutblocks (S. Berch, pers. comm., 1995). CWD may be important to
the establishment of vascular plants around wet sites such as ponds and bogs (D.F. Fraser,
pers. comm., 1995). Red huckleberry (Vaccinium parvifolium) is likely an obligate
CWD user (D.F. Fraser, pers. comm., 1995; E.C. Lea, pers. comm., 1995).
Other species are either associated with CWD or perhaps with the fungi that use CWD as
their parasitic intermediate, such as the gnome plant (Hypopitis congestum),
candystick (Allotropa virgata), and other ericaceous species. Ryan and Fraser
(1993) reported that cryptogam species richness in coastal Douglas-fir forests was
strongly influenced by available substrate. In forested sites, the presence of CWD and
rock substrates resulted in substantial increases in species richness. The review of
Samuelsson et al. (1994) of CWD states that distinct succession of bryophyte and lichen
communities occurs as trees die, fall, and decay. In B.C., known decomposer macrofungi
that are dependent on CWD include 162 species of bracket or shelf fungi/conks, 364 species
of other macrofungi, and some commercially harvested mushrooms, such as oyster mushrooms
(S. Berch, pers. comm., 1995). These communities play roles in the germination and growth
of other epiphytic and quasi-epiphytic communities. Climatic factors influence epiphytic
communities, with lichens dominating drier ecosystems and bryophytes replacing them as
conditions become wetter.
The longevity of individual pieces of CWD is critical to the persistence of many
species with poor dispersal abilities. Dispersal in many species is from one log to the
next, so logs close to each other are required. Samuelsson et al. (1994) note that large
logs play a more important role than small logs in the ecology of bryophytes and lichens.
Large logs last longer, have greater surface area, and have higher, steeper sides that
prevent ground-dwelling species from invading. They may also be important in providing a
relatively litter-free substrate for the establishment of some species of cryptogams (D.F.
Fraser, pers. comm., 1995).
Ecological Roles of Large Organic Debris
The value of woody debris in providing habitat for anadromous and other game fish
in aquatic ecosystems has been well documented (Thomson 1991). Large organic debris (LOD)
increases aquatic habitat diversity by acting as a physical barrier to water, retaining or
detaining sediment and controlling gravel movement (Miller 1987); helping to create and
maintain ponds, back channels, and side pools (Bustard and Narver 1975a; Bisson et al.
1987; Sedell et al. 1988); increasing pool size, frequency, and stability; helping to form
complex habitats such as riffles and plunge pools (Hamilton 1991); and providing a
substrate for biological activity (Sedell et al. 1988). LOD helps regulate local water
flow and depth, and increases water depth variability, providing preferred habitat for
some species (Bustard and Narver 1975b).
LOD provides important cover for fish for hiding and resting (Hamilton 1991). Table 7.7
lists fish species in B.C. that are closely associated with LOD for all or part of their
life history. LOD also acts as a food source and habitat for many types of aquatic
invertebrates (Harmon et al. 1986). Dudley and Anderson (1982) documented 56 taxa of
invertebrates closely associated with wood, and an additional 129 taxa that were dead-wood
facultatives in stream ecosystems in the U.S. Pacific Northwest. Cummins and Klug (1979)
and Maser and Trappe (1984) identified 5 functional groups of aquatic invertebrates
reliant on LOD: borers/tunnellers; wood ingesters and shredders; algae scrapers; those
that attach to wood or hide in its grooves; and piercers and predators. LOD provides
substrate for algae and microbes, which in turn provide food for aquatic invertebrates
(Maser and Trappe 1984). The state of decay of LOD is a critical factor in determining the
biotic community that may take advantage of it as growing substrate, burrowing substrate,
or food source. Aquatic invertebrates are a major food source for aquatic vertebrates. LOD
also provides habitat for mammals, particularly beavers, mink, and otter (Table 7.8), and
long-toed salamanders. LOD is used by some birds (Kingfisher, American Dipper, Wood Duck,
Hooded Merganser), but is likely less critical to them.
Pools formed by LOD act as collection basins for finer organic matter. The size and
position of debris is correlated with the size and amount of pool habitat formed (Sedell
et al. 1988). Trapped organic matter, such as leaves and needles, forms much of the energy
input into stream ecosystems and may be the dominant regulator of ecosystem organic
'output' (Bilby and Likens 1980; Bilby 1981, 1984). Stream rehabilitation after major
floods, debris torrents, or massive landslides is accelerated by large, woody debris along
and within the channel (Sedell et al. 1988). Plant species diversity on river bars is
related to the area, sediment, and woody debris of river bars (Malanson and Butler 1990).
Dead Wood and Ecosystem Processes
Dead wood is a critical component of many ecosystem processes. It supports physical,
chemical, and biological functions in forested ecosystems. These functions include
nutrient cycling, carbon storage, erosion control and slope stabilization, water cycling,
soil formation, and stream movement processes (Harmon et al. 1986; Maser et al. 1988; Caza
1993; Samuelsson et al. 1994).
Coarse woody debris is a significant factor in nutrient cycling processes (Harmon et
al. 1986; Caza 1993). Although the relative concentration of nutrients in wood and bark is
low, much of the nutrient capital and carbon are stored here because of the large biomass
involved (Harmon et al. 1986; Caza 1993). Dead wood facilitates a slow release of
nutrients, ameliorates leaching, and provides a growing substrate for bryophytes. These
buffer water and nutrient release from litterfall and above-ground processes, especially
processes such as nitrogen fixation in above-ground plants such as hepatics (Harmon et al.
1986; FEMAT 1993; Samuelsson et al. 1994). Free-living bacteria in woody residues and soil
wood fix 30-60% of the nitrogen in the forest soil. In addition, 20% of soil nitrogen is
stored in these components (Harvey et al. 1987). Harmon et al. (1986) reported that CWD
accounted for as much as 45% of above-ground stores of organic matter.
Dead wood in terrestrial ecosystems is a primary location for fungal colonization and
often acts as refugia for mycorrhizal fungi during ecosystem disturbance (Triska and
Cromack 1979; Harmon et al. 1986; Caza 1993). Colonization of dead wood by fungi and
microbes may be one of the most important stages in nutrient cycling (Caza 1993); however,
these processes are still relatively poorly understood. Soil wood contains a
disproportionate amount of the coniferous feeder roots or ectomycorrhizae in forests
(Harvey et al. 1987). As one of the dominant sources of organic matter, dead wood is an
important determinant in soil formation and composition (Caza 1993).
Dead wood is also the dominant store of organic matter in stream ecosystems (Harmon et
al. 1986); as such, it is an important source of nutrient and organic matter input. Dead
wood traps leaf and litterfall within aquatic systems, which extends the length of time
this material remains and provides nutrients through decomposition (Triska and Cromack
1979; Harmon et al. 1986).
Dead wood provides physical structure to the ecosystem and fills such roles as sediment
storage (Wilford 1984), protecting the forest floor from mineral soil erosion and
mechanical disturbance during harvesting activities. It ameliorates the effects of cold
air drainage on plants, helps stabilize slopes, and minimizes soil erosion (Maser et al.
1988). Dead wood provides elevated germination platforms with reduced litterfall
accumulation and relatively consistent moisture regimes (Harmon et al. 1986; Maser et al.
1988; Caza 1993; D.F. Fraser, pers. comm., 1995). In stream ecosystems it protects stream
banks from erosion and maintains channel stability (Triska and Cromack 1979; Sedell et al.
1988). Features that influence the ability of LOD to fulfil these functions include size
(length and diameter), whether roots are still attached, orientation, degree of burial,
and proportion of the piece that remains submerged (Sedell et al. 1988).
In both terrestrial and aquatic ecosystems, dead wood functions as a reservoir of
moisture, ameliorating drought conditions and providing a 'perched water table' (Triska
and Cromack 1979).
Management of the Dead Wood Cycle
Almost all aspects of forest management affect the dead wood cycle. Harvesting
initially increases CWD amounts except where utilization is very high. CWD may be
harvested where utilization standards influence the amounts of waste and avoidable waste
retained in second-growth forests. Site preparation (such as broadcast burning,
windrowing, or piling and burning) leave structurally simpler forest floor ecosystems.
These ecosystems lack or have significantly reduced amounts of CWD, and recruitment of new
CWD from the regenerating stand may not occur until after the projected rotation age is
Public perception of CWD as messy logging that wastes wood has influenced CWD
management. This has led to a policy of 'zero waste tolerance.' The importance of LOD in
stream ecosystems and the role of snags are more widely accepted. Management of CWD
requires increased understanding of its importance in the forest management arena, the
environmental community, and the general public.
Management of the dead wood cycle must ensure continued input of material into forested
ecosystems (terrestrial and aquatic) so that the important biological, chemical, and
physical functions are fulfilled. The previous sections point out the need to address a
variety of attributes or characteristics of dead wood to achieve this goal.
The value of snags, CWD, and LOD as a supply of habitat and as components of ecosystem
processes is correlated to a large extent with the amount of material and the piece size.
As with most attributes, however, there is a succession of biota and ecosystem functions
with increasing piece size. Decay characteristics are another important consideration in
managing the dead wood cycle. Distinct biotic communities are associated with different
decay states, and the role of dead wood in ecosystem function changes considerably as
decay progresses (i.e., from sediment storage and aquatic pool formation to nutrient
cycling). Species composition of dead wood is another attribute that must be addressed.
Use by biota, input and decay processes, and nutrient and moisture storage functions
may all be species-dependent. Orientation, distribution, and structural arrangement in the
terrestrial and aquatic landscape influences the value of dead wood in the ecosystem,
particularly in processes such as slope stabilization, sediment control, stream bank
stabilization, fungal recolonization, and habitat value for some species.
Management of the dead wood cycle requires an ecosystem approach because of the dead
wood's ecological variability. Management regimes need to be designed to ensure the
persistence of the full range of natural variation for each of the following
characteristics of dead wood: amount, size, species, decay class, orientation,
distribution, and structural arrangement. Currently little information is available for
effective management. The next section outlines the types of information still needed.
Because wildlife trees and snags are an important source of input to the dead wood
cycle, appropriate management of these components is critical. A system is in place in
British Columbia to guide the management of wildlife trees and snags at the landscape and
stand scales (Province of British Columbia 1995). There is a sanctioned (B.C. Ministry of
Forests and B.C. Workers' Compensation Board) process for assessing and maintaining snags
in silviculture operations with low ground vibration, such as tree planting and juvenile
spacing, and in certain harvesting scenarios (Guy and Manning 1995). Currently there are
no ecosystem management systems or prescriptions in place for the management of CWD and
LOD. Management regimes must be designed to ensure that dead wood input and decay
processes satisfy the criteria for the factors discussed above, and are explicitly
addressed by harvesting and silviculture plans and operations.
Information needs for ecosystem-based management would best be met by a combination
of research and inventory tasks that address the following topics:
Dynamics of wildlife trees and snags: natural mortality rates of trees by
species and size class, and the development of life tables for snags to assess longevity
in the ecosystem.
Dynamics of CWD: rates of input, decay, size and species distribution,
orientation, and distribution in natural and managed stands.
Dynamics of LOD, particularly input characteristics of size, species,
orientation, and relative rates of loss through decay and downstream transport.
Development of models for dead wood cycle dynamics that could be integrated with
tree growth and timber supply models.
The nature of relationships between dead wood and dead wood-obligate species,
particularly taxa that are still poorly understood and undescribed, such as bryophytes,
hepatics, lichens, and invertebrates.
Importance of dead wood in ecosystem processes in different ecological
conditions in B.C.
Pre- and post-assessments of the nature of dead wood during forest-harvesting
operations in a variety of ecological conditions. This information will highlight
attributes and ecological areas that need immediate management attention.
Examination of the effect of a range of silvicultural treatments on the dynamics
and ecosystem value of dead wood.
Relationships between CWD dynamics and Ministry of Forests waste and residue
assessment procedures in order to clarify the potential overlap between these.
Assessment of the extent to which wildlife tree and snag management will ensure
an adequate input of dead wood to the forested ecosystem.
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