The original article which can be found HERE has a lot of interactive material
Sea
change: the Pacific's Perilous Turn
Ocean
acidification, the lesser-known twin of climate change, threatens to
scramble marine life on a scale almost too big to fathom.
8
October, 2014
NORMANBY
ISLAND, Papua New Guinea — Katharina Fabricius plunged from a dive
boat into the Pacific Ocean of tomorrow.
She
kicked through blue water until she spotted a ceramic tile attached
to the bottom of a reef.
A
year earlier, the ecologist from the Australian Institute of Marine
Science had placed this small square near a fissure in the sea floor
where gas bubbles up from the earth. She hoped the next generation of
baby corals would settle on it and take root.
Fabricius
yanked a knife from her ankle holster, unscrewed the plate and pulled
it close. Even underwater the problem was clear. Tiles from healthy
reefs nearby were covered with budding coral colonies in starbursts
of red, yellow, pink and blue. This plate was coated with a filthy
film of algae and fringed with hairy sprigs of seaweed.
Instead
of a brilliant new coral reef, what sprouted here resembled a slimy
lake bottom.
Isolating
the cause was easy. Only one thing separated this spot from the lush
tropical reefs a few hundred yards away.
Carbon
dioxide.
HEALTHY
REEF: The colorful beginnings of a new reef sprout on a ceramic tile
that was placed near healthy coral in Papua New Guinea. The baby
corals and coralline algae on the tile provide a glimpse of the
next-generation reef.
UNHEALTHY
REEF: Algae and seaweed crowd out reef growth on a tile placed near
Papua New Guinea’s CO2 vents. The more corrosive water mirrors
what’s expected throughout the world’s oceans near the end of
this century.
In
this volcanic region, pure CO2 escapes naturally through cracks in
the ocean floor. The gas bubbles alter the water’s chemistry the
same way rising CO2 from cars and power plants is quickly changing
the marine world.t large — will worsen for decades even if
fossil-fuel emissions are cut.
In
fact, the water chemistry here is exactly what scientists predict
most of the seas will be like in 60 to 80 years.
That
makes this isolated splash of coral reef a chilling vision of our
future oceans.
‘High
rates of extinction’ to come?
Imagine
every person on Earth tossing a hunk of CO2 as heavy as a bowling
ball into the sea. That’s what we do to the oceans every day.
Burning
fossil fuels, such as coal, oil and natural gas, belches carbon
dioxide into the air. But a quarter of that CO2 then gets absorbed by
the seas — eight pounds per person per day, about 20 trillion
pounds a year.
HEALTHY
REEF: Fish swim around branching corals amid a pristine reef near
Dobu Island, Papua New Guinea.
UNHEALTHY
REEF: Fabricius records data from instruments placed alongside corals
in the CO2 vents off Dobu Island.
Scientists
once considered that entirely good news, since it removed CO2 from
the sky. Some even proposed piping more emissions to the sea.
But
all that CO2 is changing the chemistry of the ocean faster than at
any time in human history. Now the phenomenon known as ocean
acidification — the lesser-known twin of climate change — is
helping push the seas toward a great unraveling that threatens to
scramble marine life on a scale almost too big to fathom, and far
faster than first expected.
Here’s
why: When CO2 mixes with water it takes on a corrosive power that
erodes some animals’ shells or skeletons. It lowers the pH, making
oceans more acidic and sour, and robs the water of ingredients
animals use to grow shells in the first place.
Acidification
wasn’t supposed to start doing its damage until much later this
century.
Instead,
changing sea chemistry already has killed billions of oysters along
the Washington coast and at a hatchery that draws water from Hood
Canal. It’s helping destroy mussels on some Northwest shores. It is
a suspect in the softening of clam shells and in the death of baby
scallops. It is dissolving a tiny plankton species eaten by many
ocean creatures, from auklets and puffins to fish and whales — and
that had not been expected for another 25 years.
And
this is just the beginning.
Ocean
acidification also can bedevil fish and the animals that eat them,
including sharks, whales, seabirds and, of course, bigger fish.
Shifting sea chemistry can cripple the reefs where fish live, rewire
fish brains and attack what fish eat.
Those
changes pose risks for our food, too, from the frozen fish sticks
pulled from the grocer’s freezer to the fillets used in McDonald’s
fish sandwiches, to the crab legs displayed at Pike Place Market, all
brought to the world by a Northwest fishing industry that nets half
the nation’s catch.
And
this chemical change is not happening in a vacuum.
Island
reefs of Papua New Guinea offer a window on our future, while fishing
ports in Alaska and along the Washington coast show how the
deterioration of food webs could strike close to home.
Globally,
overfishing remains a scourge. But souring seas and ocean warming are
expected to reduce even more of the plants and animals we depend on
for food and income. The changes will increase ocean pests, such as
jellyfish, and make the system more vulnerable to disasters and
disease. The transformation will be well under way by the time
today’s preschoolers reach middle age.
“I
used to think it was kind of hard to make things in the ocean go
extinct,” said James Barry of the Monterey Bay Aquarium Research
Institute in California. “But this change we’re seeing is
happening so fast it’s almost instantaneous. I think it might be so
important that we see large levels, high rates, of extinction.”
Globally,
we can arrest much of the damage if we bring down CO2 soon. But if we
do not, the bad news won’t stop. And the longer we wait, the more
permanent the change gets.
“There’s
a train wreck coming and we are in a position to slow that down and
make it not so bad,” said Stephen Palumbi, a professor of
evolutionary and marine biology at Stanford University. “But if we
don’t start now the wreck will be enormous.”
You
might think that would lend the problem urgency. So far, it has not.
Combined
nationwide spending on acidification research for eight federal
agencies, including grants to university scientists by the National
Science Foundation, totals about $30 million a year — less than the
annual budget for the coastal Washington city of Hoquiam, population
10,000.
The
federal government has spent more some years just studying sea lions
in Alaska.
So
to understand how acidification could transform marine life, The
Seattle Times crisscrossed the world’s greatest ocean, from the
sun-dappled reefs of the South Pacific to the ice-encrusted surface
of the Bering Sea.
How
much carbon are we putting into the ocean?
We’re
dumping the equivalent of a hopper car of coal — about 100 U.S.
tons — into the ocean every second.
But
the island reefs of Papua New Guinea’s Milne Bay province offer a
window on our future, while fishing ports in Alaska and along the
Washington coast show how damage to fish brains and the deterioration
of food webs may strike close to home.
A
disturbing glimpse of the future
Papua
New Guinea’s Solomon Sea island vents are remarkable because of
where they are: in shallow waters normally fringed by coral reefs as
striking as fields of wildflowers.
These
remnants of earthquakes or eruptions come in all shapes:
mini-geysers, a giant crack that burps basketball-size blobs of gas,
rows of pinprick holes in the sand that exhale curtains of Champagne
bubbles.
Katharina
Fabricius swims through carbon-dioxide bubbles off Papua New Guinea.
The waters here offer a glimpse of how acidification is likely to
transform the seas.
As
Fabricius glided through earlier this year, a bleak portrait emerged.
Instead
of tiered jungles of branching, leafy reefs or a watery Eden of
delicate corals arrayed in fans, she saw mud, stubby spires and squat
boulder corals. Snails and clams were mostly gone, as were most of a
reef’s usual residents: worms, colorful sea squirts and ornate
feather stars.
The
culprit: excess carbon dioxide. When CO2 hits seawater it becomes
carbonic acid — the same weak acid found in club soda — and
releases hydrogen ions, reducing the water’s pH. This chemical
change robs the water of carbonate ions, a critical building block
for many marine organisms. Clams rely on that carbonate, as do
corals, lobsters, shrimp, crabs, barnacles, sand dollars, cucumbers
and sea urchins.
In
Puget Sound, for example, 30 percent of marine life — some 600
species — draws upon carbonate ions to grow.
Reaction
to high CO2 varies by species. Acidification can kill baby abalone
and some crabs, deform squid and weaken brittle stars while making it
tough for corals to grow. It can increase sea grasses, which can be
good, and boost the toxicity of red tides, which is not. It makes
many creatures less resilient to heavy metal pollution.
Roughly
a quarter of organisms studied by researchers actually do better in
high CO2. Another quarter seem unaffected. But entire marine systems
are built around the remaining half of susceptible plants and
animals.
“What
does well in disturbed environments are invasive generalists,” said
Ken Caldeira, a climate expert at Stanford’s Carnegie Institution
for Science, who helped popularize the term ocean acidification. “The
ones that do poorly are the more highly evolved specialists. Yes,
there will be winners and losers, but the winners will mostly be the
weeds.”
Many
species, from sea urchins to abalone, have some capacity to adapt to
high CO2. But it’s not clear if they will have the time.
“It’s
almost like an arms race,” said Gretchen Hofmann, a marine
biologist at the University of California, Santa Barbara. “We can
see that the potential for rapid evolution is there. The question is,
will the changes be so rapid and extreme that it will outstrip what
they’re capable of?”
That
is the underlying problem: The pace of change has caught everyone off
guard.
Already,
the oceans have grown 30 percent more acidic since the dawn of the
industrial revolution — 15 percent just since the 1990s. By the end
of this century, scientists predict, seas may be 150 percent more
acidic than they were in the 18th century.
The
oceans are corroding faster than they did during past periods of
marine extinctions that were linked to souring seas. Even 55 million
years ago, the rate of change was 10 times slower than today. The
current shift has come so quickly that scientists five years ago saw
chemical changes off the West Coast not expected for half a century.
And
the seas are souring even faster in some places.
The
Arctic and Antarctic have shifted more rapidly than other waters
around the world because deep, cold seas absorb more CO2. The U.S.
West Coast has simply seen consequences sooner because strong winds
draw its CO2-rich water to the surface where vulnerable shellfish
live.
Sea
chemistry in the Northwest already is so bad during some windy
periods that it kills young oysters in Washington’s Willapa Bay. In
less than 40 years, half the West Coast’s surface waters are
expected to be that corrosive every day.
That
threatens to reduce the variety of life in the sea.
“That
loss of biodiversity should matter to people just like a lack of
diversity in your stock portfolio should bother people,” said
Jeremy Mathis, an oceanographer with the National Oceanic and
Atmospheric Administration. “It works exactly the same way. If you
go all-in on one stock and that stock crashes, you’re stuck.”
Katharina
Fabricius sees plenty of reason to worry.
In
six trips to Papua New Guinea, she found sea cucumbers and urchins
living near the vents, but the shrimp and crab she expected to see
instead were almost nonexistent. She saw only 60 percent as many hard
corals as she did on healthy reefs nearby. Only 8 percent as many
soft corals survived, and one species dominated. The reefs that
remained were less intricate, offering fewer places for animals to
hide. Dull, rounded boulder corals, which seemed to thrive, still
grew a third slower than normal. Sea grasses flourished but were less
diverse. There was twice as much fleshy algae.
Corals
protect shorelines from erosion and severe weather and provide a
dormitory where staggering varieties of life seek shelter. Those tiny
plants and animals then become food for other creatures. Study after
study shows the same thing — the more reefs collapse and fleshy
algae spreads, the less we see of important tropical fish: wrasses,
tangs, damselfish, parrotfish.
Those
losses come at a price.
One-sixth
of animal protein consumed by humans comes from marine fish — in
some cultures nearly all of it. The vast majority of wild seafood is
fish, and fish account for three-quarters of the money made from
ocean catches.
Yet
reefs are just the first of many ways ocean-chemistry shifts could
hit seafood.
Scientists
once thought fish would dodge the worst direct effects of
acidification. Now it appears that might be wrong — a fact
researchers learned almost by accident.
Losing
Nemo: Fish harmed, with deadly results
In
2007, American biologist Danielle Dixson arrived in Papua New Guinea
hoping to find out how Nemo got home.
Clownfish
live in waggling anemones near coral reefs, often near islands.
Scientists suspected they traced their way through the sea by
following their noses. But how?
Clownfish swim through an anemone near Dobu Island, Papua New Guinea. CO2 can alter how clownfish see, hear and smell, which increases the chance of death.
Solving
this riddle would help uncover one of acidification’s most haunting
problems: its ability to scramble fish behavior.
Dixson,
then a graduate student at Australia’s James Cook University,
wanted to find the olfactory cue that drew clownfish back to the
reef. She tested smells from different water. She tested dirt.
Nothing was quite right, until she looked up.
Since
Papua New Guinea’s island rain forests drape over the sea, Dixson
took five island plants and spread the scent of their leaves in
water. Young clownfish immediately swam toward the smell.
Back
in Australia, she prepared to repeat the experiment in a lab. There
she bumped into Philip Munday.
Munday,
a James Cook University professor, had been trying to see if carbon
dioxide hurts fish. He checked everything: weight, survival,
reproduction. No obvious problems surfaced, which came as no
surprise. Fish are excellent at altering blood chemistry to
accommodate changing seas.
But
he wanted to do more tests. He asked Dixson if she minded raising
some extra clownfish for him.
On
a whim they decided: Why not see if CO2 altered how fish use their
noses?
“We
thought, ‘let’s just combine the two experiments and see how it
goes,’ not expecting that we’d see anything,” Munday said.
Surprises
came right away. Exposed to high CO2, the fish quit distinguishing
between odors and were equally attracted to every scent. Since
clownfish use smell to stay safe, the duo then exposed babies in
high-CO2 water to dottybacks and rock cod — bigger fish that eat
young clownfish.
Normal
clownfish always avoided the danger. The exposed fish lost all fear.
They swam straight at predators.
Over
the next few years, scientists learned CO2 changed many reef fishes’
senses and behaviors: sight, hearing, the propensity to turn left or
right. Baby reef fish exposed to high CO2 and placed back in the wild
died five times more often. Even when baby reef fish and predators
were both exposed to high CO2, young fish were bolder, ventured
farther from home — and died twice as often.
Only
last year did researchers learn why: Elevated CO2 disrupts brain
signaling in a manner common among many fish.
The
clownfish story, in other words, was no longer just about clownfish.
By
then, another American living in Australia, marine scientist Jodie
Rummer, was learning that high CO2 boosted aerobic capacity for some
tropical fish, transforming them into super athletes. Yet even some
of these fish showed behavioral problems. Rummer called it “dumb
jock syndrome.”
“You
might expect that a more athletic fish can be better at chasing food,
or be better at getting away from a predator, or finding a mate,”
she said. “But if their cognitive function — or their brain —
is compromised under these high-CO2 conditions, they might make bad
choices. They might turn the wrong direction and end up right in a
predator’s mouth.”
Most
of this research had been limited to a select few tropical species.
But scientists knew it wouldn’t take much for behavioral problems
to impact consumers.
Acidification
need only harm the wrong fish.
Big
warning for high-stakes fishery
Across
the Pacific Ocean from Papua New Guinea, Tom Enlow climbed a set of
stairs in Dutch Harbor, Alaska, a thousand miles out in the Aleutian
Islands chain. He arrived on the sorting line of a fish-processing
plant owned by Redmond-based UniSea.
Behind
Enlow, giant vacuum hoses spit thousands of oily walleye pollock onto
a conveyor.
Pollock
“is the lifeblood of our local economy, certainly, and the state’s
economy, and one of the largest industries on the Northwest and West
Coast,” said Enlow, the plant’s manager.
The
North Pacific pollock catch is so big it sounds almost absurd. Fleets
of fishermen and factory trawlers haul in 3 billion pounds
annually. No other North American fishery operates on this scale.
Seafood companies reel in $1 billion a year from that catch.
Pollock
gets carved into frozen fish sticks, sold overseas as roe and
imitation crab, or packed in blocks. McDonald’s runs television
commercials trumpeting the Bering Sea fishermen who supply pollock
for Filet-O-Fish sandwiches.
So
pollock was among the first species the U.S. government tested in
high-CO2 water. Results late last year brought no surprise:
Acidification would hurt neither the fish’s body nor its growth.
Adult and young seemed physically unharmed.
But
after tracking clownfish research, government scientists in Oregon
tried new tests.
After
smelling prey, pollock scout around and hunt it down. So NOAA
biologist Thomas Hurst exposed young pollock to high CO2 and
introduced the scent of what they eat. Some of the fish struggled to
recognize their food.
“In
some of the very early work it looks like pollock may show some of
the same kinds of deficits that are seen in coral-reef fishes,”
Hurst said.
It’s
too soon to say how — or even if — that would affect pollock
fishing. Some tropical fish raised in high-CO2 water gave birth to
young that adjusted to their new environment. Pollock might respond
the same way.
But
the fish also might not. And a lot rides on the outcome, particularly
in the Northwest.
Dutch
Harbor might as well be a distant Seattle suburb. Washington
businesses or residents often own or run its trawlers, crab boats and
processors. Employees typically come from the Puget Sound region.
Even the former five-term mayor of Unalaska, Dutch Harbor’s
municipal government, used to fish out of Ballard.
“We
don’t yet know whether it’s going to be a really severe impact or
a modest impact,” Hurst said. But “if the fish is less able to
recognize the scent of its prey and then therefore locate food when
it’s foraging out in the wild, obviously that’s going to have
negative impacts for growth and then survival in the long run.”
And
that’s just one species. Similar tests are under way for rockfish,
cod, several kinds of crab and sharks.
But
brain damage is not even the biggest threat to commercial fish.
This
pteropod, also known as a sea butterfly, comes from Puget Sound. The
tiny shelled creatures are an important food source for many fish and
seabirds. The shells of pteropods already are eroding in Antarctica,
where the water chemistry isn’t as bad as it is in parts of the
Pacific Northwest.
Key
link in food chain dissolving
All
over the ocean, usually too small to see, flutter beautiful, nearly
see-through creatures called pteropods, also known as sea
butterflies. Scientists have known for years that plummeting ocean pH
eventually would begin to burn through their shells.
Few
people would find that significant save for one fact: Many things eat
pteropods.
Birds,
fish and mammals, from pollock to whales, feast on this abundant
ocean snack. Pteropods make up half the diet of baby pink salmon and
get eaten by other fish, such as herring, that then get swallowed by
larger animals.
So
scientists were alarmed late in 2012 when researchers announced that
pteropods in Antarctica were dissolving right now in waters less
corrosive than those often found off Washington and Oregon. What did
that mean for the Northwest?
Pink
salmon swim through Finch Creek, near a salmon hatchery on Hood
Canal. Pteropods make up roughly half the diet of young pink salmon
in Alaska.
The
United States does so little monitoring of marine systems that we
know almost nothing about the health of creatures that form the
bottom of the ocean food chain — things like pteropods, krill or
other important zooplankton called copepods. The most-studied animals
remain those we catch. Little is known about the things they eat.
Computer
modelers such as Isaac Kaplan, at NOAA in Seattle, are scrambling to
figure out how sea-chemistry changes could reverberate through the
ocean.
Initial
results are disturbing.
“Right
now, for acidification in particular,” Kaplan said, “the risks
look pretty substantial.”
Kaplan
tracks the Pacific coast — temperature, pH levels, currents,
salinity. He incorporates studies that detail how CO2 impacts
creatures. Then he extrapolates how all those variables are likely to
affect the fish people catch.
While
the models are rough and uncertainty is high — too many elements
cannot be controlled — the trend is clear.
Kaplan’s
early work predicts significant declines in sharks, skates and rays,
some types of flounder and sole, and Pacific whiting, also known as
hake, the most frequently caught commercial fish off the coast of
Washington, Oregon and California.
“Some
species will go up, some species will go down,” said Phil Levin,
ecosystems leader for NOAA’s Northwest Fisheries Science Center in
Seattle. “On balance, it looks to us like most of the commercially
caught fish species will go down.”
Fearing
‘a mess for this little town’
The
findings confound those who rely on commercial fish.
Capt.
Ben Downs stood atop the wheelhouse of the F/V Pacific Dove, in
Westport, Grays Harbor County, on a recent summer day as he rolled on
a fresh coat of whitewash. Downs spent years piloting one of the
coast’s biggest whiting boats. This day he was prepping for shrimp
fishing.
“The
ocean is always changing,” Downs said. Nearby a ship offloaded
whiting at the city’s largest processor. “This is nothing
different. I’ve battled the ocean all my life.”
Yet
even a skeptic like Downs sees the stakes.
Coastwide,
fishermen bring in tens of million pounds of whiting a year. It’s
the biggest product at Westport’s fish plant, which at times
employs a quarter of the city’s workforce.
“If
the hake went away, it’d be a mess for this little town,” he
said. “Astoria, Oregon, same thing. Newport, Oregon, same thing.”
Dave
Fraser, who runs a whiting fishing cooperative, wasn’t skeptical,
but weary. Fishermen already face tangible crises daily: the dollar’s
value swinging wildly against the yen; quotas falling based on
routine marine shifts.
“Being
able to focus on something 10 or 20 years away … it’s hard,” he
said. “The early warnings are there. We’ve seen the first wave
that hit the oysters. We’re just hoping it doesn’t come our way.”
It
is a problem not limited to fishing fleets.
“If
you go 100 miles from the coast, most people say, ‘Why do I care
about ocean acidification?’ ” Mathis, at NOAA, said.
“Convincing a farmer in Iowa or a teacher in Kansas to care about
ocean acidification is our challenge.”
He
measures progress by the drop in emails from angry Alaskans
challenging his findings.
“Acidification
is very real: There isn’t any doubt it’s happening,” said Clem
Tillion, a former Republican Alaska state Senate president, even
though he still denies human contributions to global warming. “It’s
obvious. And it’s going to be devastating.”
At
stake: food for rural people
On
a warm Papua New Guinea night, a quarter-mile from Fabricius’ CO2
vents, Edwin Morioga and Ridley Guma sat in the dark in a canoe and
prepped their spears.
The
rain-forest jungles of Milne Bay are home to wallabies, flying
rodents, cockatoos and butterflies the size of dinner plates.
Villagers raise taro, yams and other vegetables. Many know increasing
storms and rising seas someday will force them to move their sago
tree huts to higher ground.
But
with a quarter of a million people spread across 600 islands, the
threat to food may be more significant.
Most
of their protein comes from the sea. Fishermen unspool hand lines to
collect sweetlips and sea perch. They gather shrimp and crustaceans.
And at night they dodge tiger sharks and saltwater crocodiles to
spear small fish from beneath bountiful corals.
Globally,
the sea provides the primary source of animal protein for a billion
people. Many, like Morioga and Guma, have few alternatives.
The
pair slipped into the water and floated face down, flashlights
trained on the reef. Neither knew much about Fabricius’
acidification research. But they agreed they did not want CO2 from
the West or an industrializing Asia transforming their reefs into
places resembling the desolate nearby bubble sites.
Away
from the vents, amid the coral, life of all kinds is still plentiful.
In
an instant, Morioga saw a flash. He took a breath and dived, stabbing
beneath a branching coral. After a pause, Morioga surfaced.
On
the end of his spear writhed a tiny rabbitfish, his first catch of
the night from what remains one of the world’s healthiest reefs.
At
least for now.
Changes
come decades faster than expected
Less
than a decade ago, scientists expected acidification wouldn’t harm
marine life until late in the 21st century. In the past five years,
researchers instead have figured out it’s happening now. Here is a
timeline of what we thought we knew — and how that changed.
Early
20th century
Scientists
begin to understand how carbon moves between the atmosphere and the
sea.
1999
A
handful of scientists predict rising CO2 emissions may change sea
chemistry enough to harm corals by late in the 21st century.
2003
Atmospheric
scientist Ken Caldeira predicts sea chemistry will change more
rapidly over the next century than it has in tens of millions of
years.
2006
Seattle
oceanographer Richard Feely, with the National Oceanic and
Atmospheric Administration (NOAA), and others discover North Pacific
sea chemistry has changed dramatically just since they sampled it in
1991.
Top
ocean researchers release first major ocean-acidification report and
brief Congress, highlighting marine changes they fear are possible by
century’s end.
2007
Feely
and colleagues take an ocean research trip between Canada and Mexico
and find enormous stretches of seawater already changing in ways not
expected for 50 to 100 years. Because of ocean currents, weather and
geography, they figure out, West Coast sea chemistry — unlike
oceans at large — will worsen for decades even if fossil-fuel
emissions are cut.
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