Key Research Findings
Natural disturbances such as eruptions, floods, fires, and earthquakes
are heterogeneous events, meaning that the disturbance creates a complex mosaic
of disturbed areas and effects are not evenly distributed. The May 18, 1980,
eruption of Mount St. Helens involved several distinct large disturbances—a
huge debris avalanche, an explosive blast out the mountain’s north side,
mudflows, hurricane-force winds of hot gases, and ejected volcanic rock and
ash (tephra). These events interacted with a diverse landscape to create a
complex mosaic of disturbance zones covering several hundred square miles.
The severity of disturbance ranged from areas where all life perished to zones
with nearly complete survival.
Chance events, such as the timing of a disturbance, greatly determine
the extent of environmental change. For Mount St. Helens, the season and
time of day strongly influenced survival and recovery. The 1980 eruption occurred
on a spring morning; plant buds had not yet opened, patches of snow and ice
protected some organisms, and nocturnal animals had returned to their underground
burrows. If it had happened on a summer night, more plants and animals would
have perished.
Life history characteristics of species are an important factor in
survival rates. In the case of Mount St. Helens, some Pacific
salmon and steelhead trout were at sea when the eruption occurred. When they returned to mountain
streams to spawn in the years after the eruption, stream conditions had improved.
Many migrant songbirds had not yet returned to their summer nesting grounds
at Mount St. Helens when the eruption occurred, so these birds escaped the
immediate effects.
The Mount St. Helens eruption had many specific mechanisms that also
occur in other types of disturbances: the heat was comparable to wildfires,
wind blast comparable to hurricanes, mudflows comparable to rain-caused mudflows,
wave surge in Spirit Lake comparable to tsunamis, and so forth. Thus the findings
on ecological responses at Mount St. Helens have broad relevance to ecological
responses to other types of disturbances.
Living and dead organisms left after the eruption, termed “biological
legacies,” accelerated recovery at Mount St. Helens. Surviving plants,
fungi, and animals served many ecological functions—plants provided forage
and shelter, animals were prey and predators, and so forth. Dead organisms
provided significant amounts of nutrients. Biological legacies made it much
easier for species to colonize the landscape and in areas with many survivors,
complex biological communities developed rapidly. Mount St. Helens showed that
even in a radically disturbed environment, organisms can survive and become
source populations for colonizing the disturbed area. This finding challenged
the theory that colonization comes primarily from outside the disturbed area.
The biological response to the spectacular 1980 eruption was rapid,
with the most important factors being the biological legacies, the diverse
source populations surrounding the blast area, the presence of unconsolidated
volcanic deposits in which animals could burrow and plants could take root,
and a moist climate with plenty of rain and snow encouraging plant growth.
At
Mount St. Helens, erosion cut through the new volcanic deposits and exposed
soil where plants could sprout. Thus in this disturbance, erosion was
a positive
process for plants, improving habitat.
Lakes, streams, and forests responded
at different rates after the 1980 eruption. A key factor for response rate
was the extent to which ecosystems became
nutrient-enriched
or impoverished. Lakes were greatly enriched with nutrients, and life
in lakes multiplied rapidly. Within 6 years after the 1980 eruption, most
lakes had
returned to conditions typical of undisturbed Cascade Range lakes.
In sharp
contrast, terrestrial ecosystems, covered with nutrient-poor volcanic
ash and rock, had greatly diminished biological productivity after the 1980
eruption.
Although terrestrial ecosystems increased their biological productivity
by
2004, their productivity was still far below that of a mature forest.
Disturbance
eliminates or reduces the amount of many habitats, but it can also create
new habitats. At Mount St. Helens, about 90 square miles of
forest habitat
were lost because of the 1980 eruption, but the amount of lake
and pond habitat increased fivefold. These new habitats were quickly colonized
by a great
diversity
of aquatic life, such as amphibians, insects, plankton, and plants.
Many of these new ponds are among the most productive ecosystems,
terrestrial
or aquatic,
at Mount St. Helens.
In the Mount St. Helens National Volcanic Monument, where natural processes
have been allowed to take place since 1980, the biological communities
that have developed are highly varied with respect to species diversity, composition,
and structure. Chance and contingencies have strongly influenced the
rates
and patterns at which these communities developed. These naturally
recovering herb and shrub communities are very different ecologically from the
highly
managed stands of young conifers growing on land outside the national
monument but within the blast area. The naturally recovering communities may
play an
important role in the regional biodiversity of the Pacific Northwest.
Human
actions taken to protect life, property, or commerce influenced the patterns
and rates of ecological response at Mount St. Helens. The most significant
actions ecologically were engineering projects to reduce hydrologic
and sediment
hazards, fish stocking in lakes and streams, salvage logging of
blowdown trees, and creation of even-aged, single-species, conifer plantations
(the
last two
actions occurred outside the national monument).
Twenty-five
years after the 1980 eruption, the landscape at Mount St. Helens is a patchwork
of biological hot spots and cold spots embedded
within a larger
landscape of intermediate biological diversity. Biological
cold spots include areas that are episodically or chronically disturbed
by erosion, landslides,
or animal burrowing. Biological hot spots are areas of high
biodiversity that developed around pockets of survivors or around places such
as
seeps and springs
where moisture was available and plants grew. Although these
hot spots, or “oasis” habitats
compose less than one percent of the total landscape they contribute
much of the total biodiversity. Many animals have colonized
these isolated habitat
patches. This finding calls into question the necessity of
dispersal corridors for connecting source populations with newly created
habitat patches.
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