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Chemical Technology • May 2016

T

he Great Barrier Reef comprises thousands of

reefs, over 600 types of hard and soft coral, and

an almost endless variety of fish and sea-life. It

is also worth over US$6 billion to Australia in tourism.

The cause of the corals’ dying is coral bleaching. Here’s

how it happens. Corals are tiny marine invertebrates

living in vast compact colonies of polyps. A particular

coral group forms a coherent structure and creates a

recognisable pattern. The polyps are a few millimetres in

width and maybe a centimetre or two in length with a hard

exoskeleton secreted at its base. Over generations, these

secretions build up on themselves and become vast reefs.

The corals themselves depend for their survival on

a symbiotic relationship with photosynthetic unicellular

flagellates which live within their tissues. These are called

zooxanthellae. Corals require sunlight so that the zooxan-

thellae can photosynthesise, and water temperature that

is not too warm or too cold.

There are corals that don’t rely on this symbiotic rela-

tionship, and they can grow at much greater depths and

in the absence of sunlight. Recently, a vast and previously

unknown reef was discovered beneath the very murky wa-

ters where the Amazon river stretches out into the ocean.

The colour you see in a healthy reef is mostly as a result

of the zooxanthellae living in the tissues of coral polyps.

When the water temperature changes too much, or the

amount of light is diminished, the zooxanthellae die. This

leads to dramatic colour loss across the affected reef.

Coral bleaching indicates that the coral itself is not dead

yet, but it is starving. If the zooxanthellae do not return, then

the reef is doomed. The Great Barrier Reef has experienced

bleaching events, of increasing severity, every few years co-

inciding with the El Niño current, which raises temperatures.

However, this current has become more frequent, and of a

higher temperature, as a result of global warming.

In March of this year, Professor Terry Hughes of James

Cook University, flew over 600 km of reef. More than 60 %

of it was bleached. These bleaching events, while devastat-

ing, also lead to major structural changes across the reef.

A reef that fails to recover will be colonised by other types

of algae and sea weeds. This impacts on the fish which used

to depend on the reef and consequently leads to major

species loss. This phenomenon is known as a ‘phase-shift’

to a reef dominated by macroalgae (as compared to the

microalgae of the zooxanthellae).

This does not always happen, however, and scientists

have been attempting to figure out why. For starters, there

is a very wide range of species differentiation between cor-

als with some surviving post-bleaching events significantly

better than others. They use the space created to colonise

dying reefs and come to dominate. There are also herbivores

which eat the macroalgae and hold back growth until the

reef can recover.

The question about how to encourage coral survival is

more than just about tourists on their summer vacations.

Over 500 million people in 100 countries depend on coral

reefs for their food and livelihoods.

One organisation working on coral restoration and reme-

diation is the Coral Reef Targeted Research and Capacity

Building for Management (CRTR) Program based at the

University of Queensland. They rear nearly 10 000 nursery-

grown colonies for reef transplants every year. The problem

with the nursery-led approach of CRTR is that transplanted

corals have a higher mortality rate and grow more slowly

than do the reefs where they are cemented. Scientists’

concern is that they still know very little about the life-cycle

and biology of specific species.

In American Samoa, lagoons full of coral survive 35 °C

Rehabilitation

in a time of

coral bleaching

by Gavin Chait

Divers consider the Great Barrier

Reef, off the far northern coast of

Queensland, Australia, to be one of the

greatest destinations for viewing coral

anywhere in the world. At 2 300 km

long, the system is the largest living

thing on earth, and it is dying.