by W. Gregory Hood, Ph.D. Skagit System
Cooperative
Sweetgale, Beaver, Salmon, and Large Woody Debris in
the Skagit River Tidal Marshes:
The phrase "estuarine tidal marsh" generally
evokes a pastoral image of tidally flooded meadows of grasses,
sedges, rushes, and occasional wildflowers. However, there is
another type of tidal marsh that is frequently overlooked-estuarine
scrub-shrub wetlands. Shrub-dominated tidal marshes were
historically very common, comprising 33% of the estuarine tidal
wetlands in the Skagit delta, 35% in the Stillaguamish, and 70% in
the Snohomish (Collins 2000). Today less than 6% of this habitat
remains in the Skagit delta (mostly in the South Fork delta; Figure 1), and virtually none remains in
the Stillaguamish and Snohomish deltas. These extensive losses are
probably representative of other historically large regional
estuarine marshes such as the Duwamish (Seattle), Puyallup (Tacoma),
and Fraser (Vancouver, BC) deltas.
Most habitat
loss in the Skagit delta occurred soon after Euro-American
settlement in the 1870s. Tidal scrub-shrub wetlands were easier to
clear than forests and easier to dike and drain than the lower
elevation tidal meadows. In fact, early records show that the former
shrub-lands were more expensive than forested lands because of the
comparative difficulty in developing forest land for agriculture
(Collins 2000).
Because rapid
and extensive loss of estuarine shrub habitat occurred long ago, few
people are aware this habitat ever existed, or whether it was
ecologically significant. Should we be concerned about this habitat
loss? Did this vegetation community play a role in the estuarine
ecology of juvenile salmonids? The Skagit System Cooperative (SSC)
is currently doing research to answer these and related
questions.
Today the most
common estuarine shrub is sweetgale , followed by willows, black twinberry, and wild rose.
Sweetgale is unique among these shrubs, and all other estuarine
plants in the Skagit delta, in being able to convert atmospheric
nitrogen into nitrate, an important plant nutrient. This process is
called nitrogen fixation.
Herbivores are
nitrogen limited compared to carnivores, because plants are a poor
source of nitrogen compared to protein-rich animals. Because
nitrogen-fixing plants have relatively high concentrations of
nitrogen in their tissues, they are a preferred food for herbivores.
This is why horses and cattle prefer clover or alfalfa, which are
both nitrogen-fixing plants. Thus, sweetgale may play an important
role in estuarine foodwebs. It may be a preferred food for insects
that feed on its leaves. When the leaves fall in the autumn, insects
such as midge larvae (chironomids) and crustaceans such as scuds
(amphipods) and pillbugs (isopods) may preferentially feed on the
decomposing leaves. Midge larvae and scuds are common food items for
juvenile salmonids in estuarine marshes, so sweetgale may be an
important part of the salmonid food web in the estuary. A study is
currently underway at the SSC to compare decomposition rates of
three dominant plant species - sweetgale, Lyngby's sedge, and
cattail-in the South Fork tidal marshes, and to compare colonization
rates and abundance of insects and crustaceans that feed on the
decomposing vegetation.
Sweetgale may
also affect salmon by affecting the distribution of beaver in the
estuary. Most people, even some beaver researchers, are unaware that
beaver can be found in estuarine tidal marshes when the salinity is
less than 10 parts per thousand (seawater is typically 30-35 ppt,
while freshwater is less than 0.5 ppt). An ongoing SSC study is
showing that beaver are common in the Skagit River tidal marshes
(where the salinity is typically less than 5 ppt), and preliminary
evidence indicates that beaver are strongly associated with
sweetgale habitat.
In small tidal
channels (less than 7 feet wide), beaver build small dams (less than
2 feet tall) that pond water at low tide, but are completely flooded
at high tide. The apparent function of the dams is to pond
sufficient water in the channels at low tide so that the beaver can
still swim in the channels. Without dams the channels would go dry
at low tide. These beaver ponds are full of small fish at low
tide-juvenile salmon and sticklebacks. Without the ponds the fish would be
forced into larger, wider, and deeper tidal channels that don't go
dry at low tide. There they would be vulnerable to predators such as
great blue herons and large fish. These predators are not found in
the beaver ponds. Great blue herons are kept out by the sweetgale
thickets that border and hang over the channels, sometimes
completely covering the channels.
In contrast,
tidal channels that are located in cattail and sedge habitat never
contain beaver ponds. Some ponds are formed by slumping banks, or
trapped logs, but ponds in these channels are less common and
smaller than those in channels found in sweetgale habitat.
Furthermore, because great blue herons are not obstructed by shrubs,
the herons are commonly found feeding on fish in these channels.
Thus, sweetgale may indirectly benefit juvenile salmon by affecting
the dam building by estuarine beavers and providing low tide refuges
from predation.
Estuarine
vegetation is usually found in distinct bands that parallel the
shoreline. These bands are the result of a gradient of flooding and
salinity stress experienced by plants in the estuary. For example,
eelgrass is found in subtidal and very low intertidal areas. Low
intertidal areas in the South Fork delta are occupied by American
threesquare; higher intertidal areas are dominated by Lyngby's
sedge, then by cattails; and at the highest elevations shrubs
dominate the intertidal zone.
Sweetgale is
found in a half-mile wide band between sedge and cattails at lower
elevations and other shrubs like black twinberry, willow, wild rose,
and spirea at higher elevations. At lower elevations sweetgale
cannot tolerate tidal flooding to the extent that sedges and cattail
can, and at higher elevations other, taller shrubs outcompete
sweetgale for sunlight. Thus sweetgale is squeezed between two
constraints on its estuarine distribution-physical stress at lower
elevations and competition at higher elevations.
Sweetgale's
intertidal distribution would be narrower were it not for the
presence of large logs (large woody debris-LWD) in the tidal marsh.
Logs are common in the South Fork tidal marsh and they allow
sweetgale to expand its distribution into the lower elevation marsh
by providing sweetgale with small elevated "island-logs" upon which
to grow above a critical flooding threshold. SSC research shows that in the low-elevation marsh
sweetgale grows exclusively on logs; the larger the log the greater
the chance that sweetgale is growing on it (Figure 4). As elevation increases the
proportion of sweetgale growing on logs declines steadily, but this
proportion is always much greater than that expected by random
growth on logs and soil, i.e., the proportion of log surface area to
marsh surface area. This pattern indicates that as sediment
accumulates in the marsh over the course of many floods, individual
sweetgale shrubs spread by runners from logs to the elevated
adjacent marsh surface and grow into dense thickets. Eventually, the
original log islands are either buried by sediment or decompose, so
that sweetgale appears to the casual observer to have no association
with logs. Further increases in marsh elevation, allow other woody
species to colonize the marsh and compete with sweetgale.
Other shrubs and
trees in the tidal marsh are also usually found growing on large
logs, and generally these logs are even larger than those on which
sweetgale grows. Where
do these logs come from? It's unlikely that spruce trees growing in
the tidal marsh are significant sources of estuarine wood. Although
spruce is the largest and most abundant tree in the South Fork tidal
marsh, it is sparsely distributed and it does not grow as large or
as quickly as in other habitats. A sample of thirty spruce growing
in the South Fork tidal marsh had a mean diameter at breast height
(DBH) of only 35 cm and a maximum diameter of 61 cm.
In contrast to
the size of living spruce, the average size of a log supporting
sweetgale was 62 cm, and the average size of a "nurse-log"
supporting a spruce tree was 120 cm. Other shrubs and trees in the tidal
marsh also grow on logs that on average are much larger than the
largest live spruce in the tidal marsh. Thus, large logs that are
important in supporting estuarine shrub habitat must come from
outside the estuarine marsh-from coastal or riverine forests. This
implies that management of river margins (riparian zones) has
potentially significant consequences for vegetation composition of
estuarine tidal marshes and for the ecological functions (e.g.,
production of invertebrate prey for juvenile salmon, habitat for
beaver and refuge from predators for juvenile salmon) provided by
that vegetation.
The riparian
zones most likely to contribute large fallen trees to the estuary
would normally have been those of the lower Skagit River. However,
riparian forests in this area are a small fraction of their
historical extent (Collins 2000). Furthermore, dikes and riprap have
hardened the river channel, preventing channel migration and bank
undercutting, thereby reducing treefall from the riparian forests.
Low recruitment of large wood to the estuary may have long-term
consequences for the sustainability of estuarine shrubs and
trees.
Current SSC
research shows that South Fork delta distributary channels and blind
tidal channels can migrate dramatically over time, so that
established marsh vegetation can be eroded away, while new marsh is
created by vegetation colonizing newly deposited sediments. Without
a sufficient supply of large wood to the estuary to facilitate shrub
colonization of new marshland, established shrub habitat will
eventually be lost to channel migration without being
replaced.
In summary, SSC
research suggests that we need to more closely examine the ecology
of an often neglected habitat-tidal shrublands, and we need to be
more cognizant of the ecological connection between riparian zone
management of the lower Skagit River and the long-term
sustainability of estuarine vegetation and its ecological functions.
Due to the extensive loss of this vegetation type and its ecological
functions, consideration should be given to restoring estuarine
scrub-shrub habitat where appropriate.
References Collins, B. D. &
Montgomery, D. R. 2001. Importance of archival and process
studies to characterizing pre-settlement riverine geomorphic
processes and habitat in the Puget Lowland. In: Geomorphic processes
and riverine habitat. Edited by J. M. Dorava, D. R. Montgomery, B.
Palcsak, and F. Fitzpatrick. American Geophysical Union, Washington,
D. C.
Collins, B.
2000. Mid-19th Century Stream Channels and Wetlands Interpreted
from Archival Sources for Three North Puget Sound Estuaries. Report
to the Skagit System Cooperative, LaConner, WA.
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