
Environmental Encyclopedia 3
Great Barrier Reef
Great Barrier Reef
The Great Barrier Reef, located in the Coral Sea off the
eastern coast of Queensland in northeastern
Australia
, con-
sists of more than 2,800 reefs that range in size from 1
hectare to over 10,000 hectares in area. As the largest reef
in the world, the Great Barrier Reef is 1,250 mi (2,011 km)
in length, extending from a point near McKay, Queensland
in the
south
to the Torres Strait in the north, which lies
between Australia and New Guinea. The Reef is 45 mi (72
km) across at its widest point, with a total area of more than
300,000 square kilometers. Approximately 20% of the reefs
are submerged reefs or shoals, while about 26% are fringing
reefs around continental islands or along the mainland coast.
The remaining reefs are shelf reef platforms. Water depths
range from 65.6–98 ft (20–30 m) in lagoonal areas to 131–
197 ft (40–60 m) between the reefs on the outer shelf.
Starting in the south near the Tropic of Capricorn, the Great
Barrier Reef is a wide scattering of reefs about 186 mi (300
km) out from the coast; moving north the Reef becomes
more continuous and is within 10–12 mi (16–19 km) of the
coast, with a few individual reefs in the inner
lagoon
(the
area between the reef and the coast). North of Cairns the
reef is almost a continuous barrier between the coast and
the Coral Sea. Drilling has indicated that in places the reef
is over 1,640.5 ft (500 m) thick.
At the end of the last
ice age
, about 20,000 years
ago, the sea level was about 394 ft (120 m) lower than it is
today, and dry land extended from the present day coast to
the location of today’s outer Barrier Reef. As the ice melted,
the sea rose, and by 13,000 years ago the coastal plain had
become a submerged continental shelf. Corals and reefs grow
best where there is water movement, so the reefs tended to
form on submerged hills in the
flooding
coastal plain. By
6000 to 7000 years ago, the sea had reached its present level,
and the reef began to assume its present shape. The Spanish
mariner Luis Vaa
´
ez de Torres was the first European known
to have sailed the northern reef, but the Spanish kept the
route a secret to protect their route between Europe and the
Orient. The Reef was explored and charted by Captain James
Cook, whose ship in 1770 ran aground on the reef that now
is called the Endeavor, after the name of his ship.
The Great Barrier Reef provides homes and shelter
for a wide diversity of life. The Great Barrier Reef is home
to corals, which form the reefs,
dolphins
and
whales
, six
species
of
sea turtles
, more than 1,500 species of fish,
4,000 types of mollusks, 500 species of seaweed, and more
than 200 species of birds. The corals that make up the Reef
consist of individual living coral polyps, which as they divide
in a process called budding, form colonies in fan, antler,
brain, and plate shapes. Each polyp, which is a tiny jelly-
like, sack-like animal with a mouth surrounded by tentacles,
lives inside a shell of aragonite, a type of calcium carbonate
658
that is the hard shell typically recognized as coral. The polyps
are joined together to form a colony. Coral polyps obtain
food by catching
plankton
in their tentacles as well as
deriving nutrients from symbiotic algae, the zooxanthellae,
that live within their tissues. These zooxanthellae produce
nutrients through
photosynthesis
, which are then available
for use by the coral. Association with the algae allow corals
to build skeletons three times faster in the light than in the
dark, and faster than storms and waves can break it down.
Coral bleaching
occurs when stressed corals expel the zoo-
xanthellae and turn white, or bleached. If the zooxanthellae
do not return to the coral, the coral will die.
Every year about one-third of the 350 species of coral
reproduce sexually during a mass spawning event. Spawning
occurs in most of the inner reefs around November and in
the outer reefs in December. The spawning occurs at night,
up to six days after the full moon. Eggs and sperm are
released into the water, where they combine to form a free-
swimming larval stage.
The Great Barrier Reef is completely within the trop-
ics. The
climate
of the Reef is a typical
monsoon
weather
pattern, which consists of strong south-easterly winds domi-
nating during the dry winter months and weaker variable
winds occurring during the summer wet season. Both air
and sea temperatures exhibit seasonal variations. Mean sea
temperatures in inshore areas exhibit a range of temperatures
of 69.8°F (21°C) in July and August to 86°F (30°C) in January
and February. Temperatures on offshore reefs exhibit less
seasonal difference, varying from 73.4°F (23°C) in winter to
82°F (28°C) in summer.
There are two types of islands along the Great Barrier
Reef. The larger islands, such as those of the Whitsunday
group, are the tops of submerged mountains that at one
time were high points of a range running along the coast.
These islands have vegetation similar to the mainland. Some
of these islands that have fertile soils and are affected by
heavy monsoonal rains are covered with rain forests. Other
islands are isolated low-lying coral cays. Cays are formed
when coral grow to levels that are higher than sea level, even
at low tide. Coral can only survive a few hours out of water.
The dead coral on the cays is worn down and broken off
by waves and storm action. Eventually the coral debris is
ground into sand. Through time the sand stabilizes, seabirds
start to nest, and hardy vegetation begins to grow. Decom-
posing plant materials and bird droppings change the sand
into a more developed
soil
, providing an
environment
for
a wider diversity of plant life. Cays are found more frequently
on inner reefs in the Great Barrier Reef, where waves and
currents are less strong than on reefs further away from the
coastline. However, vegetated cays are not sufficiently stable
to withstand severe weather, such as storms and cyclones.
Comprehensive protection of the Great Barrier Reef
was accomplished in 1975 by the formation of the Great