[SustainableTompkins] New Scientist article: Imagine Earth without people
GayNicholson at aol.com
GayNicholson at aol.com
Tue Oct 17 14:04:47 PDT 2006
Disquieting thought experiment on how quickly the Earth would heal itself of
us....
http://www.newscientist.com/channel/life/mg19225731.100
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Imagine Earth without people
* 12 October 2006
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* Bob Holmes
Humans are undoubtedly the most dominant species the Earth has ever
known. In just a few thousand years we have swallowed up more than a
third of the planet's land for our cities, farmland and pastures. By
some estimates, we now commandeer 40 per cent of all its productivity.
And we're leaving quite a mess behind: ploughed-up prairies, razed
forests, drained aquifers, nuclear waste, chemical pollution, invasive
species, mass extinctions and now the looming spectre of climate change.
If they could, the other species we share Earth with would surely vote
us off the planet.
Now just suppose they got their wish. Imagine that all the people on
Earth - all 6.5 billion of us and counting - could be spirited away
tomorrow, transported to a re-education camp in a far-off galaxy. (Let's
not invoke the mother of all plagues to wipe us out, if only to avoid
complications from all the corpses). Left once more to its own devices,
Nature would begin to reclaim the planet, as fields and pastures
reverted to prairies and forest, the air and water cleansed themselves
of pollutants, and roads and cities crumbled back to dust.
"The sad truth is, once the humans get out of the picture, the outlook
starts to get a lot better," says John Orrock, a conservation biologist
at the National Center for Ecological Analysis and Synthesis in Santa
Barbara, California. But would the footprint of humanity ever fade away
completely, or have we so altered the Earth that even a million years
from now a visitor would know that an industrial society once ruled the
planet?
If tomorrow dawns without humans, even from orbit the change will be
evident almost immediately, as the blaze of artificial light that
brightens the night begins to wink out. Indeed, there are few better
ways to grasp just how utterly we dominate the surface of the Earth than
to look at the distribution of artificial illumination (see Graphic). By
some estimates, 85 per cent of the night sky above the European Union is
light-polluted; in the US it is 62 per cent and in Japan 98.5 per cent.
In some countries, including Germany, Austria, Belgium and the
Netherlands, there is no longer any night sky untainted by light pollution.
"Pretty quickly - 24, maybe 48 hours - you'd start to see blackouts
because of the lack of fuel added to power stations," says Gordon
Masterton, president of the UK's Institution of Civil Engineers in
London. Renewable sources such as wind turbines and solar will keep a
few automatic lights burning, but lack of maintenance of the
distribution grid will scuttle these in weeks or months. The loss of
electricity will also quickly silence water pumps, sewage treatment
plants and all the other machinery of modern society.
The same lack of maintenance will spell an early demise for buildings,
roads, bridges and other structures. Though modern buildings are
typically engineered to last 60 years, bridges 120 years and dams 250,
these lifespans assume someone will keep them clean, fix minor leaks and
correct problems with foundations. Without people to do these seemingly
minor chores, things go downhill quickly.
The best illustration of this is the city of Pripyat near Chernobyl in
Ukraine, which was abandoned after the nuclear disaster 20 years ago and
remains deserted. "From a distance, you would still believe that Pripyat
is a living city, but the buildings are slowly decaying," says Ronald
Chesser, an environmental biologist at Texas Tech University in Lubbock
who has worked extensively in the exclusion zone around Chernobyl. "The
most pervasive thing you see are plants whose root systems get into the
concrete and behind the bricks and into doorframes and so forth, and are
rapidly breaking up the structure. You wouldn't think, as you walk
around your house every day, that we have a big impact on keeping that
from happening, but clearly we do. It's really sobering to see how the
plant community invades every nook and cranny of a city."
With no one to make repairs, every storm, flood and frosty night gnaws
away at abandoned buildings, and within a few decades roofs will begin
to fall in and buildings collapse. This has already begun to happen in
Pripyat. Wood-framed houses and other smaller structures, which are
built to laxer standards, will be the first to go. Next down may be the
glassy, soaring structures that tend to win acclaim these days. "The
elegant suspension bridges, the lightweight forms, these are the kinds
of structures that would be more vulnerable," says Masterton. "There's
less reserve of strength built into the design, unlike solid masonry
buildings and those using arches and vaults."
But even though buildings will crumble, their ruins - especially those
made of stone or concrete - are likely to last thousands of years. "We
still have records of civilisations that are 3000 years old," notes
Masterton. "For many thousands of years there would still be some signs
of the civilisations that we created. It's going to take a long time for
a concrete road to disappear. It might be severely crumbling in many
places, but it'll take a long time to become invisible."
The lack of maintenance will have especially dramatic effects at the 430
or so nuclear power plants now operating worldwide. Nuclear waste
already consigned to long-term storage in air-cooled metal and concrete
casks should be fine, since the containers are designed to survive
thousands of years of neglect, by which time their radioactivity -
mostly in the form of caesium-137 and strontium-90 - will have dropped a
thousandfold, says Rodney Ewing, a geologist at the University of
Michigan who specialises in radioactive waste management. Active
reactors will not fare so well. As cooling water evaporates or leaks
away, reactor cores are likely to catch fire or melt down, releasing
large amounts of radiation. The effects of such releases, however, may
be less dire than most people suppose.
The area around Chernobyl has revealed just how fast nature can bounce
back. "I really expected to see a nuclear desert there," says Chesser.
"I was quite surprised. When you enter into the exclusion zone, it's a
very thriving ecosystem."
The first few years after people evacuated the zone, rats and house mice
flourished, and packs of feral dogs roamed the area despite efforts to
exterminate them. But the heyday of these vermin proved to be
short-lived, and already the native fauna has begun to take over. Wild
boar are 10 to 15 times as common within the Chernobyl exclusion zone as
outside it, and big predators are making a spectacular comeback. "I've
never seen a wolf in the Ukraine outside the exclusion zone. I've seen
many of them inside," says Chesser.
The same should be true for most other ecosystems once people disappear,
though recovery rates will vary. Warmer, moister regions, where
ecosystem processes tend to run more quickly in any case, will bounce
back more quickly than cooler, more arid ones. Not surprisingly, areas
still rich in native species will recover faster than more severely
altered systems. In the boreal forests of northern Alberta, Canada, for
example, human impact mostly consists of access roads, pipelines,
andother narrow strips cut through the forest. In the absence of human
activity, the forest will close over 80 per cent of these within 50
years, and all but 5 per cent within 200, according to simulations by
Brad Stelfox, an independent land-use ecologist based in Bragg Creek,
Alberta.
In contrast, places where native forests have been replaced by
plantations of a single tree species may take several generations of
trees - several centuries - to work their way back to a natural state.
The vast expanses of rice, wheat and maize that cover the world's grain
belts may also take quite some time to revert to mostly native species.
At the extreme, some ecosystems may never return to the way they were
before humans interfered, because they have become locked into a new
"stable state" that resists returning to the original. In Hawaii, for
example, introduced grasses now generate frequent wildfires that would
prevent native forests from re-establishing themselves even if given
free rein, says David Wilcove, a conservation biologist at Princeton
University.
Feral descendants of domestic animals and plants, too, are likely to
become permanent additions in many ecosystems, just as wild horses and
feral pigs already have in some places. Highly domesticated species such
as cattle, dogs and wheat, the products of centuries of artificial
selection and inbreeding, will probably evolve back towards hardier,
less specialised forms through random breeding. "If man disappears
tomorrow, do you expect to see herds of poodles roaming the plains?"
asks Chesser. Almost certainly not - but hardy mongrels will probably do
just fine. Even cattle and other livestock, bred for meat or milk rather
than hardiness, are likely to persist, though in much fewer numbers than
today.
What about genetically modified crops? In August, Jay Reichman and
colleagues at the US Environmental Protection Agency's labs in
Corvallis, Oregon, reported that a GM version of a perennial called
creeping bentgrass had established itself in the wild after escaping
from an experimental plot in Oregon. Like most GM crops, however, the
bentgrass is engineered to be resistant to a pesticide, which comes at a
metabolic cost to the organism, so in the absence of spraying it will be
at a disadvantage and will probably die out too.
Nor will our absence mean a reprieve for every species teetering on the
brink of extinction. Biologists estimate that habitat loss is pivotal in
about 85 per cent of cases where US species become endangered, so most
such species will benefit once habitats begin to rebound. However,
species in the direst straits may have already passed some critical
threshold below which they lack the genetic diversity or the ecological
critical mass they need to recover. These "dead species walking" -
cheetahs and California condors, for example - are likely to slip away
regardless.
Other causes of species becoming endangered may be harder to reverse
than habitat loss. For example, about half of all endangered species are
in trouble at least partly because of predation or competition from
invasive introduced species. Some of these introduced species - house
sparrows, for example, which are native to Eurasia but now dominate many
cities in North America - will dwindle away once the gardens and bird
feeders of suburban civilisation vanish. Others though, such as rabbits
in Australia and cheat grass in the American west, do not need human
help and will likely be around for the long haul and continue to edge
out imperilled native species.
Ironically, a few endangered species - those charismatic enough to have
attracted serious help from conservationists - will actually fare worse
with people no longer around to protect them. Kirtland's warbler - one
of the rarest birds in North America, once down to just a few hundred
birds - suffers not only because of habitat loss near its Great Lakes
breeding grounds but also thanks to brown-headed cowbirds, which lay
their eggs in the warblers' nests and trick them into raising cowbird
chicks instead of their own. Thanks to an aggressive programme to trap
cowbirds, warbler numbers have rebounded, but once people disappear, the
warblers could be in trouble, says Wilcove.
On the whole, though, a humanless Earth will likely be a safer place for
threatened biodiversity. "I would expect the number of species that
benefit to significantly exceed the number that suffer, at least
globally," Wilcove says.
On the rebound
In the oceans, too, fish populations will gradually recover from drastic
overfishing. The last time fishing more or less stopped - during the
second world war, when few fishing vessels ventured far from port - cod
populations in the North Sea skyrocketed. Today, however, populations of
cod and other economically important fish have slumped much further than
they did in the 1930s, and recovery may take significantly longer than
five or so years.
The problem is that there are now so few cod and other large predatory
fish that they can no longer keep populations of smaller fish such as
gurnards in check. Instead, the smaller fish turn the tables and
outcompete or eat tiny juvenile cod, thus keeping their erstwhile
predators in check. The problem will only get worse in the first few
years after fishing ceases, as populations of smaller, faster-breeding
fish flourish like weeds in an abandoned field. Eventually, though, in
the absence of fishing, enough large predators will reach maturity to
restore the normal balance. Such a transition might take anywhere from a
few years to a few decades, says Daniel Pauly, a fisheries biologist at
the University of British Columbia in Vancouver.
With trawlers no longer churning up nutrients from the ocean floor,
near-shore ecosystems will return to a relatively nutrient-poor state.
This will be most apparent as a drop in the frequency of harmful algal
blooms such as the red tides that often plague coastal areas today.
Meanwhile, the tall, graceful corals and other bottom-dwelling organisms
on deep-water reefs will gradually begin to regrow, restoring complex
three-dimensional structure to ocean-floor habitats that are now largely
flattened, featureless wastelands.
Long before any of this, however - in fact, the instant humans vanish
from the Earth - pollutants will cease spewing from automobile tailpipes
and the smokestacks and waste outlets of our factories. What happens
next will depend on the chemistry of each particular pollutant. A few,
such as oxides of nitrogen and sulphur and ozone (the ground-level
pollutant, not the protective layer high in the stratosphere), will wash
out of the atmosphere in a matter of a few weeks. Others, such as
chlorofluorocarbons, dioxins and the pesticide DDT, take longer to break
down. Some will last a few decades.
The excess nitrates and phosphates that can turn lakes and rivers into
algae-choked soups will also clear away within a few decades, at least
for surface waters. A little excess nitrate may persist for much longer
within groundwater, where it is less subject to microbial conversion
into atmospheric nitrogen. "Groundwater is the long-term memory in the
system," says Kenneth Potter, a hydrologist at the University of
Wisconsin at Madison.
Carbon dioxide, the biggest worry in today's world because of its
leading role in global warming, will have a more complex fate. Most of
the CO_2 emitted from burning fossil fuels is eventually absorbed into
the ocean. This happens relatively quickly for surface waters - just a
few decades - but the ocean depths will take about a thousand years to
soak up their full share. Even when that equilibrium has been reached,
though, about 15 per cent of the CO_2 from burning fossil fuels will
remain in the atmosphere, leaving its concentration at about 300 parts
per million compared with pre-industrial levels of 280 ppm. "There will
be CO_2 left in the atmosphere, continuing to influence the climate,
more than 1000 years after humans stop emitting it," says Susan Solomon,
an atmospheric chemist with the US National Oceanic and Atmospheric
Administration (NOAA) in Boulder, Colorado. Eventually calcium ions
released from sea-bottom sediments will allow the sea to mop up the
remaining excess over the next 20, 000 years or so.
Even if CO_2 emissions stop tomorrow, though, global warming will
continue for another century, boosting average temperatures by a further
few tenths of a degree. Atmospheric scientists call this "committed
warming", and it happens because the oceans take so long to warm up
compared with the atmosphere. In essence, the oceans are acting as a
giant air conditioner, keeping the atmosphere cooler than it would
otherwise be for the present level of CO_2 . Most policy-makers fail to
take this committed warming into account, says Gerald Meehl, a climate
modeller at the National Center for Atmospheric Research, also in
Boulder. "They think if it gets bad enough we'll just put the brakes on,
but we can't just stop and expect everything to be OK, because we're
already committed to this warming."
That extra warming we have already ordered lends some uncertainty to the
fate of another important greenhouse gas, methane, which produces about
20 per cent of our current global warming. Methane's chemical lifetime
in the atmosphere is only about 10 years, so its concentration could
rapidly return to pre-industrial levels if emissions cease. The wild
card, though, is that there are massive reserves of methane in the form
of methane hydrates on the sea floor and frozen into permafrost. Further
temperature rises may destabilise these reserves and dump much of the
methane into the atmosphere. "We may stop emitting methane ourselves,
but we may already have triggered climate change to the point where
methane may be released through other processes that we have no control
over," says Pieter Tans, an atmospheric scientist at NOAA in Boulder.
No one knows how close the Earth is to that threshold. "We don't notice
it yet in our global measurement network, but there is local evidence
that there is some destabilisation going on of permafrost soils, and
methane is being released," says Tans. Solomon, on the other hand, sees
little evidence that a sharp global threshold is near.
All things considered, it will only take a few tens of thousands of
years at most before almost every trace of our present dominance has
vanished completely. Alien visitors coming to Earth 100,000 years hence
will find no obvious signs that an advanced civilisation ever lived here.
Yet if the aliens had good enough scientific tools they could still find
a few hints of our presence. For a start, the fossil record would show a
mass extinction centred on the present day, including the sudden
disappearance of large mammals across North America at the end of the
last ice age. A little digging might also turn up intriguing signs of a
long-lost intelligent civilisation, such as dense concentrations of
skeletons of a large bipedal ape, clearly deliberately buried, some with
gold teeth or grave goods such as jewellery.
And if the visitors chanced across one of today's landfills, they might
still find fragments of glass and plastic - and maybe even paper - to
bear witness to our presence. "I would virtually guarantee that there
would be some," says William Rathje, an archaeologist at Stanford
University in California who has excavated many landfills. "The
preservation of things is really pretty amazing. We think of artefacts
as being so impermanent, but in certain cases things are going to last a
long time."
Ocean sediment cores will show a brief period during which massive
amounts of heavy metals such as mercury were deposited, a relic of our
fleeting industrial society. The same sediment band will also show a
concentration of radioactive isotopes left by reactor meltdowns after
our disappearance. The atmosphere will bear traces of a few gases that
don't occur in nature, especially perfluorocarbons such as CF_4 , which
have a half-life of tens of thousands of years. Finally a brief,
century-long pulse of radio waves will forever radiate out across the
galaxy and beyond, proof - for anything that cares and is able to listen
- that we once had something to say and a way to say it.
But these will be flimsy souvenirs, almost pathetic reminders of a
civilisation that once thought itself the pinnacle of achievement.
Within a few million years, erosion and possibly another ice age or two
will have obliterated most of even these faint traces. If another
intelligent species ever evolves on the Earth - and that is by no means
certain, given how long life flourished before we came along - it may
well have no inkling that we were ever here save for a few peculiar
fossils and ossified relics. The humbling - and perversely comforting -
reality is that the Earth will forget us remarkably quickly.
>From issue 2573 of New Scientist magazine, 12 October 2006, page 36-41
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