From HMS Beagle at: http://news.bmn.com/hmsbeagle/115/notes/feature1
Mount St. Helens
Disobeying the Rules of Recovery
by Sharon Levy
Posted November 23, 2001 · Issue 115
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Abstract
On the morning of May 18, 1980, Mount St. Helens erupted, belching ash into
the air and sending a blast of hot gas, rock and mud down the side of the
mountain. Shortly after the eruption, scientists arrived to study the
recovery of life on the volcano - and have found surprise after surprise.
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Between the lip of the Mount St. Helens caldera and the blue edge of Spirit
Lake lies an expanse of barren pumice. Twenty-one years ago, this
mountainside in the Cascade Range of southern Washington was cloaked in
old-growth forest, which enfolded the lake. Now the landscape has been blown
wide open, and thousands of tree carcasses float on the water's surface,
bleached by the sun, snow, and wind.
On the morning of May 18, 1980, St. Helens erupted, belching ash into the
air and sending a blast of hot gas, rock, and mud down the side of the
mountain. The blast broke five-hundred-year-old trees as if they were
matchsticks. Six hundred square kilometers of forest were devastated; even
where the trees survived, the ground was coated with a thick layer of ash.
When ecologists arrived to study the recovery of life on the volcano, they
expected to find a moonscape where nothing had survived. But the mountain
didn't meet expectations. "Every time you turned around, from the first hour
of our observations, there was some new stratagem by which nature had
persisted," recalls Jerry Franklin, a forest ecologist at the University of
Washington at Seattle. "We were repeatedly struck in the face by the
realization that hey, this place is alive."
St. Helens was alive in ways that stood scientific dogma on its head. The
textbook version of primary ecological succession held that simple
autotrophs, such as lichens, mosses, and bacteria, should be the first
colonists in a devastated area. These would prepare the ground for the first
vascular plants to move in. Herbivores and then predators would show up only
after the plant community was well established, in a slow, orderly process.
"That's the way it was supposed to work," says Franklin. "There's supposed
to be rules these organisms and successional processes follow. But there
really are none."
Accidents of timing, weather, and topography had powerful effects on
ecosystem recovery. Plants and animals that survived the blast while
sheltered under spring snowbanks were alive and functioning immediately
after the eruption. Wind-blown seeds that happened to lodge in cracks in the
volcanic rock germinated and grew - including some species that had not been
expected to return for years. The chance whims of the wind governed many of
the early events in the recovery.
Long before plants could begin to recolonize the pumice plain above Spirit
Lake, live insects and spiders rained down from the sky. John Edwards, a
zoologist at the University of Washington at Seattle, found that
representatives of 70 different insect families and 43 species of spider
blew in on the wind during the first years after the eruption. The young of
these species disperse by taking to the air and letting the wind determine
their fate. Many land in inhospitable places such as alpine snowfields, or
the blasted landscape of Mount St. Helens. Most of these unlucky animals
die, but they don't go to waste. Within eight weeks of the eruption, Edwards
saw carpenter ants and spiders preying on hapless insects that had fallen
onto the mountain.
Lupines were the dominant plant pioneers on the pumice plain; mosses and
lichens couldn't survive the heat or the drying effects of volcanic ash.
Because they are able to fix atmospheric nitrogen, lupines were expected to
act as nurse plants, creating soil that could sustain other species. This
did happen eventually, but early on, the fallout of insects and spiders
brought far more nutrients to the blast zone.
"At first, fallout was definitely the most important source of nutrients"
says John Bishop, a botanist at Washington State University at Vancouver.
"The same insect rain continues today, but its importance has diminished."
As the ecosystem develops, plants grow up and create habitat for insects
that live and breed on the mountain. The nutrient input from fallout, which
seemed dramatic when the community was starting from zero, is now dwarfed by
the production of living things native to the blast zone.
Bishop, who first came to Mount St. Helens ten years after the eruption,
studies the ecology of the lupine patches. On the pumice plain, the gray of
barren rock is now interrupted by lush carpets of lupine. On a windy summer
day, the same breeze that blows puffs of ash out of the caldera carries the
sweet smell of thousands of purple blossoms.
Bishop has found that the lupines form a stage whereon dramas of competition
and survival play out. Lupines flourished in the blast zone for the first
few years after the eruption, outcompeting most other plants and unfettered
by pressure from herbivores. The first lupine seed germinated on the pumice
plain soon after the eruption, but the insects that feed on lupines didn't
arrive for about six years.
When the herbivores did arrive - principally caterpillars that eat lupine
leaves, roots, or seed pods - their populations exploded. "The caterpillars
were probably escaping their predators for quite a while," says Bishop. "So
the caterpillar population would explode to the point where they'd suppress
the lupines, and the lupine population would start to crash." Lupines were
in decline when they were rescued by the arrival of predatory spiders and
parasitoid flies, which lay their eggs on caterpillars, leaving their young
to hatch out and devour their herbivorous host. Now that caterpillar
populations are controlled by predators, lupines are going strong again.
"When we showed that herbivores were limiting lupine growth, that was a very
novel result," says Bishop. "There's been skepticism that insects may
actually regulate plant populations. In primary successional systems, no one
thought that herbivores could be that important."
Farther down the mountain, below the pumice plain, the 1980 blast flattened
trees or left them standing dead, and the soil was buried under a thick
layer of ash. In this area, called the blow-down zone, some unexpected
survivors have been critical to the recovery.
Charlie Crisafulli, an ecologist with the U.S. Forest Service who has been
working on Mount St. Helens since 1981, has learned a new way of looking at
the animals he studies. "St. Helens was surprise after surprise," he says.
"What the mountain has told us in many ways is that we lack a basic
understanding of many species' natural histories, their tolerance limits,
and their dispersal capabilities."
At first, the most obvious survivor was the pocket gopher, many of which
weathered the cataclysm while safe in their underground burrows. "Gophers
were enormously conspicuous," remembers Crisafulli. "You'd have this uniform
gray ash that had been deposited over the landscape. The gophers were
burrowing down in the old, rich dark forest soil, and they'd kick that up to
the surface. So it was very obvious - in fact, many of the sites where
gophers had survived we located from low-flying aircraft."
Before the mountain exploded, gophers had been confined to small openings in
the forest. Afterwards, much of the blow-down zone was transformed into a
giant meadow. The gopher population boomed, and as more and more gophers
tunneled underground, they helped spread important soil microorganisms.
"We've documented that gophers do transport the spores of mycorrhizal fungi
and lead to the inoculation of plants," says Crisafulli. Many forest plants
rely on a symbiotic relationship with these fungi to help them fix nitrogen.
The gophers have also helped other survivors - the twelve species of
salamanders, frogs, and toads that made it through the eruption. Most of the
amphibians were adapted to life in the cool, damp duff of St. Helens'
old-growth forests. Twenty-one years after the eruption, the ground surface
in summer remains far too hot and dry for these creatures, but hundreds of
miles of gopher tunnels provide them with shelter from the heat.
The larval forms of many of these animals were protected under the frozen
surfaces of lakes and ponds when the volcano blew. "Had the eruption
occurred in August," says Crisafulli, "the consequences would have been
entirely different." Three species of strictly land-living salamander were
wiped out in the blast; the amphibians that still flourish on St. Helens
have both aquatic and terrestrial life stages. Northwestern salamanders, for
example, usually spend the first 15 months of their lives as larvae, living
in and breathing water. Then they metamorphose, lose their gills, and take
to the land, returning to their natal ponds only to breed.
In every population of northwestern salamanders, however, there are a few
individuals that grow up and become sexually mature, but never leave the
water. These eccentric individuals are called neotenes: giant-size larvae
that are capable of breeding. In the aftermath of the St. Helens eruption,
neotenes came to rule the waters of the blast zone. Most salamanders that
metamorphosed were doomed. "They'd disperse away from the ponds looking for
forest, and there was no forest out there, so they'd succumb," explains
Crisafulli.
Today, the northwestern salamanders that populate the ponds and wetlands of
the blast zone are 98 percent percent neotenic. For now, the ability to live
permanently in water is key to their survival. A few of the terrestrial form
of the salamander persist, holing up in the extensive network of gopher
burrows. Over time, as the forest returns, the gopher population will
dwindle and many of the burrows will disappear. But the terrestrial
salamanders will make a comeback when they can once again find shelter in
the cool of the woods.
The trees of St. Helens have taught scientists some profound lessons - even
in death. At first it was feared that thousands of dead old-growth Douglas
firs, which lay scattered everywhere in the blow-down zone, would impede the
forest's recovery. This was one reason why the U.S. Forest Service had some
areas salvage logged after the eruption.
That proved to be another false assumption. The dead wood has nourished new
plant growth and provided habitat for insects, small mammals, and birds,
speeding ecosystem recovery. The insights Jerry Franklin and other forest
ecologists have gained on Mount St. Helens have changed the way forestry is
practiced in the Pacific Northwest. Clear-cut logging was once the standard
practice. Now, on federal lands, 15 percent of the timber in a harvest area
must be left behind - dead or alive.
Today the blow-down zone on St. Helens is bursting with life. Hairy
woodpeckers and northern flickers fly among the snags, feasting on insects.
Pacific silver fir and western hemlock, some of which had spent decades
growing slowly in the shadow of the great Douglas-fir forest, were shielded
by snow on that day in May 1980. In the open sun among the fallen old-growth
trees, they now shoot towards the sky: many that were inches high at the
time of the blast stand 20 feet tall. If the mountain stays quiet for a
couple of hundred years, a new forest, different but as grand as the one the
volcano blasted away, will rise here.
Mount St. Helens yielded many secrets in the first years after the eruption.
Funding and active research waned during the 1990s. But Bishop and
Crisafulli are still finding new twists as the complex renewal of life on
the mountain continues. Much remains to be learned. Nobody has yet tried to
dissect the impact of returning elk on the lupine patches where they love to
snooze, or quantified the differences between parts of the blow-down zone
that were cleared of dead wood and those that were left alone. "There is an
opportunity for new studies here," says Bishop. "I'm hoping we can bring in
a new generation of researchers."
Sharon Levy is a freelance science writer based in northern California. She
is a regular contributor to National Wildlife, New Scientist, and other
science and nature magazines.
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Endlinks
Mount St. Helens from the Ashes - a special report from the May 10, 2000
edition of the Seattle Post-Intelligencer. Includes links to extensive
articles and photographs on the eruption and recovery of Mount St. Helens.
Mount St. Helens National Volcanic Monument - contains tourism, research,
and educational resources. Includes extensive photographs and articles on
the biological responses after the eruption, Life Returns: Animal and Plant
Recovery Around the Volcano.
Cascades Volcano Observatory - provides extensive news, information, maps,
and assessments. From the U.S. Geological Service.
Global Volcanism Program - offers extensive information and worldwide
activity reports on volcanoes. From the Smithsonian Institute.
Volcano World - proclaims itself "the Web's premier source of volcano info."
Includes current eruptions, background information, volcano images by
region, and more. From the University of North Dakota.
Forest Succession - contains a brief discussion of forest succession and the
ecosystem changes that accompany succession.
Related HMS Beagle article:
The Pattern of Evolution - this excerpt from the book by Niles Eldredge
focuses on succession.
© Elsevier Science Limited 2000
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