Coral reefs decimated by 2050, Great Barrier Reef's
coral 95% dead
Rhett A. Butler, mongabay.com
November 17, 2005

Source >
http://news.mongabay.com/2005/1117-corals.html


Australia's Great Barrier Reef could lose 95 percent
of its living coral by 2050 should ocean temperatures
increase by the 1.5 degrees Celsius projected by
climate scientists. The startling and controversial
prediction, made last year in a report commissioned by
the World Worldwide Fund for Nature (WWF) and the
Queensland government, is just one of the dire
scenarios forecast for reefs in the near future. The
degradation and possible disappearance of these
ecosystems would have profound socioeconomic
ramifications as well as ecological impacts says Ove
Hoegh-Guldberg, head of the University of Queensland's
Centre for Marine Studies.

        
Hoegh-Guldberg, speaking at the Carnegie Institution
Department of Global Ecology at Stanford University,
says the most important threat facing the Great
Barrier Reef and other reefs of the world is higher
sea temperatures that cause thermal stress for corals.

Corals are tiny animals that live in colonies and
derive nourishment and energy from a symbiotic
relationship with zooxanthellae algae known as
dinoflagellates. Coral reefs are formed over the
course of thousands of years as limestone skeletons
constructed by corals accumulate and form a structural
base for living corals. Research indicates that is
takes roughly thousand years for a reef to add a meter
of height. Individual corals are capable of faster
growth -- about one meter every hundred years -- but
wave action and other forms of disturbance moderates
overall reef growth.

        Great Barrier Reef in Australia
The Great Barrier Reef is the world's largest reef,
stretching more than 2,300km along the northeast coast
of Australia. Made up of about 2,900 unconnected coral
reefs and roughly 900 islands, the Great Barrier Reef
is home to over 1,500 species of fish and 400 species
of coral making it one of the most important marine
ecosystems on Earth. Scientists consider it Earth's
largest living organism which makes it the only
individual living thing visible from space.

While the Great Barrier Reef is one of the world's
healthiest reefs, coral reefs are particularly fragile
ecosystems, partly due to their sensitivity to water
temperature. When corals are physiologically stressed
-- as is the case when water temperatures are elevated
-- they may lose much of the their symbiotic algae, an
event known as "bleaching." Corals can recover from
short-term bleaching, but prolonged bleaching can
cause irreversible damage and subsequent death.

The first coral bleaching on record occurred in 1979.
Since then, there have been six events, each of which
has been progressively more frequent and severe. In
the El NiƱo year of 1998, when tropical sea surface
temperatures were the highest yet in recorded history,
coral reefs around the world suffered the most severe
bleaching on record. 48% of reefs in the Western
Indian Ocean suffered bleaching, while 16% of the
world's appeared to have died by the end of 1998. 2002
was even worse: 60 to 95 per cent of individual reefs
of the 110,000 square mile (284,000 square kilometer)
Great Barrier Reef suffered some bleaching, while
reefs in Palau, the Seychelles, and Okinawa suffered
70-95% bleaching. Early surveys suggest the Caribbean
is currently in the midst of a serious event. While
most of these reef ecosystems have recovered to some
degree, warmer water temperatures in the future may
have a more lasting impact.

Great Barrier Reef in Australia         
"An increase in frequency of coral bleaching may be
one of the first tangible environmental effects of
global warming," said Dr. Arnold Dekker of Australia's
Commonwealth Scientific and Industrial Research
Organisation (CSIRO) in a European Space Agency news
release."The concern is that coral reefs might pass a
critical bleaching threshold beyond which they are
unable to regenerate."

Hoegh-Guldberg agrees. "By 2050 bleaching may be an
annual event, that is, if there are still reefs around
to be bleached. If you have bleaching events every
four years and they take 15-20 to recover, you will
start to see bleached reefs not recovering. They will
be dying," he adds.

Acidic Oceans

While rising sea temperatures are likely to have the
biggest impact of coral reefs in the future,
Hoegh-Guldberg notes are there factors that will
affect the health of coral reefs including changes in
sea level, elevated storm frequency and intensity,
altered ocean circulation, variation in precipitation
and land runoff, and increasing ocean acidification.

Ocean acidification is of particular concern to
scientists because it is crucial to the formation of
coral. Coral and other marine organisms use free
carbonate ions in sea water to build calcium carbonate
shells and exoskeletons, but as atmospheric carbon
dioxide levels rise and more carbon dioxide is
absorbed by the world's oceans, sea waters become
increasingly acidic by stripping out carbonate ions.
Lower carbonate ion concentrations make it more
difficult for organisms to form shells, leaving them
vulnerable to predators and environmental conditions.
In the past, changes in ocean acidity have caused mass
extinction events. According to a study published in
the September issue of Geology, dramatically warmer
and more acidic oceans may have contributed to the
worst mass extinction on record, the Permian
extinction. During the extinction event, which
occurred some 250 million years ago, about 95% of
ocean's life forms became extinct. The same fate could
befall modern day marine life. In September 2005, a
team of scientists writing in Nature warned that by
2100, the amount of carbonate available for marine
organisms could drop by 60%. In surface ocean waters,
where acidification starts before spreading to the
deep sea, there may be too little carbonate for
organisms to form shells as soon as 2050.

        
Hoegh-Guldberg believes an atmospheric carbon dioxide
concentration of 500 parts-per-million (ppm) is a key
threshold for coral reefs. "Beyond 500 ppm coral reefs
may no longer exist. Much of the Pacific Ocean will
likely be marginal for coral reefs while net
calcification rates will be approaching zero" says
Hoegh-Guldberg. Currently the concentration of carbon
dioxide in the atmosphere stands around 380 ppm but
the Intergovernmental Panel on Climate Change (IPCC)
projects that if no precautionary action is taken,
carbon dioxide concentrations will rise by 2050 to
between 450 and 550 ppm.

Worldwide impact

The degradation and loss of coral ecosystems in will
likely have a wide-ranging impact on the world
economy. Hoegh-Guldberg points out that more than 500
million people live within 100 kilometers of coral
reefs, many of whom rely on reefs and the services
they provide for daily subsistence. Should reefs
become severely damaged by climate change it could
well create a class of ecological refugees in need
assistance.

Further reefs play an important role in buffering
adjacent shorelines from wave action, erosion, and the
impact of storms. For example Moorea in French
Polynesian, only experiences a 10 cm tidal range due
to its protective barrier reef. Should the reef die
and begin to crumble, the island's low-lying
structures could be at risk.

Impact of a dying Great Barrier Reef in Australia

Australia may be the best example of the potential
ramifications of dying reefs. Though Australia is
among the world's most developed countries, a damaged
Great Barrier Reef would likely have a significant
impact on the country's economy. A recent study found
the reef is worth more to Australia as an intact
ecosystem than an extractive reserve for fishing.

Each year more than 1.8 million tourists visit the
reef, spending an estimated AU$4.3 billion (Australian
dollars) on reef-related industries from diving to
boat rental to posh island resort stays. Revenue from
tourism -- popular activities include snorkeling;
scuba diving; fishing; glass-bottomed boat and
semi-submersible vessel excursions -- dwarfs the
commercial and recreational fishing industries which
generate $360 million (Australian dollars) annually.
Furthermore, tourism is an important source of
employment: in 1998-1999, more than 47,600 people were
employed in the sector compared to around 2,000
involved in commercial fishing in the region.

Tourism has given the Australian government an
incentive to preserve the reef and last summer it
banned all forms of extraction in one-third of the
Great Barrier Reef Marine Park, making it the largest
fully protected area of ocean in the world. The
protected area will also benefit the fishing industry
by serving as a nursery for fish-breeding to restock
the entire reef.

Great Barrier Reef in Australia         
The reef also offers great potential for Australia's
nascent but blossoming biotech industry in the form of
compounds derived from corals and other organisms that
live in the region. Sessile invertebrates -- like
corals -- have a special affinity for providing
medicinally valuable compounds through their
production of toxic chemicals used for defense.
Several promising drugs have been developed from coral
and other invertebrate species.

There is little doubt that the Great Barrier Reef, as
a viable and relatively intact ecosystem, will
continue to play an important role in the thriving
Australian economy. The big question is, how long will
it remain viable and intact?

Disagreement

Some scientists argue that the Great Barrier Reef and
other coral ecosystems may be around longer than has
been suggested by Hoegh-Guldberg's scenario. Critics
say his scenario does not the current level of
uncertainty about either the impact of warmer waters
on the reefs, or likely climate change -- IPCC
projections have been hotly debated.

Since the fossil record for corals is spotty -- the
"resolution" for prehistoric dating is only 400 years
-- so the impact of abrupt changes on coral are
difficult to detect. While corals have certainly
persisted through warmer and more acidic periods in
Earth's geologic history, Hoegh-Guldberg suspects
corals will face a difficult adjustment period in the
face of rapidly rising sea temperatures and falling
carbonate ion concentrations.

"Biological adaptations can't keep pace with the
forecasted level of change," says Hoegh-Guldberg. "In
the past the time scale was likely thousands of years,
not decades."

Hoegh-Guldberg argues that coral reefs will likely
recover in geologic terms, but not in terms of a human
lifetime. The short term impact of dying and degraded
reefs will be significant.

"For a tour operator, two years of bleached coral can
mean the difference in putting food on the table or
finding a new job. The tourism industry will be hit
especially hard by worsening bleaching events."

Over the longer term, reefs will recover. According to
Hoegh-Guldberg model, under the best-case global
warming scenario -- where temperatures stabilize
around 2100 -- the Great Barrier Reef will recover
within a century. Under the pessimistic, it will take
at least 500 years for the reef to regenerate,
populated by coral species adapted to living in warmer
waters. Hoegh-Guldberg says reefs are unlikely to
migrate to cooler, higher latitude waters due to other
conditions -- including light levels and ion
concentrations -- required for their growth.

Despite a bleak future, Hoegh-Guldberg doesn't believe
reef conservation and research efforts should be
abandoned.

"There is still a lot we don't know about coral reefs.
We need to understand these ecosystems to be totally
effective in their preservation. Technologies still in
their infancy may make it possible for us to moderate
some of the effects of climate change on coral reefs."





        
                
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