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A2 GEOGRAPHY
COASTAL ENVIRONMENTS
8.3 CORAL REEFS
WHAT ARE
CORAL REEFS?
Coral reefs are one of the most biologically
diverse ecosystems, rivalled only by the
tropical rainforests in this respect.
Corals are marine animals, and almost a
thousand coral species currently exist.
Human activities are threatening their future.
WHAT ARE THE
CORAL REEFS?
With the majority of the world’s
population living in coastal
regions, many people depend on
living coral reefs for food, and
protection from storm surges and
erosion, as well as the additional
benefits of medical research,
tourism and aesthetic beauty.
WHAT ARE THE CORAL REEFS?
With the majority of the world’s population living in coastal regions,
many people depend on living coral reefs for food, and protection
from storm surges and erosion, as well as the additional benefits of
medical research, tourism and aesthetic beauty.
Coral reefs contribute about 25% of the total fish catch in LIC’s
(LEDCs), providing food for one billion people in Asia alone.
Human activities, such as those associated with global warming,
are threatening coral reefs. Increasing sea temperatures stress
corals and cause damage, including bleaching.
THE DEVELOPMENT OF CORAL
All tropical reefs began
life as polyps – tiny, soft
animals, like sea
anemones – which attach
themselves to a hard
surface in shallow seas
where there is sufficient
light for growth.
As they grow, many of
these polyps exude
calcium carbonate, which
forms their skeleton. As
they grow and die, these
colonies of ‘rock’-forming
corals create reefs.
GROWTH RATES
Tropical reefs can grow at rates of
under 2.5–60 cm/year, forming huge
structures over incredibly long periods
of time, making them the largest and
oldest living systems on Earth.
For example, the 1,250-mile Great
Barrier Reef was formed over five
million years.
POLYPS AND ALGAE
Polyps have growing inside them small
algae, zooxanthellae.
The algae receive shelter and food from
the polyp, while the polyp also gets some
food via photosynthesis.
Algae need sunlight to live, and obviously
photosynthesis (conversion of light
energy from the sun into food) cannot
occur in darkness, hence corals only grow
where the sea is shallow and clear.
REEF FORMATION
Darwin’s
subsidence theory
is illustrating the
evolution of three
reef types (South
Pacific model) i.e.
linking the
formation of the
three types of reef
together.
FRINGING REEFS
Fringing reefs grow
around newly
formed islands.
These islands
subside, or sea
level rises relative
to land.
BARRIER REEFS
If the process is
slow the reef will
grow upwards to
form a larger
barrier reef
separated from the
island by a deeper
lagoon.
ATOLLS
When the island
disappears beneath
the sea an atoll forms.
Corals can continue to
grow on the outside
to keep the reef on
the surface. On the
inside, where the land
used to be, quiet
water with increased
sedimentation
prevails.
A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS
THREATS TO CORAL
THE MAIN THREATS
TO CORAL INCLUDE
• coral bleaching and global
climate change
• diseases of corals and
other reef organisms
• plagues of predators
like the crown of-thorns
starfish (COTS) and other
damaging organisms such
as the sea urchin
• invasive species which
have been introduced onto
new coral reefs.
A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS
OTHER THREATS
These threats are in addition to natural
stresses that have always affected coral
reefs such as storms, freshwater
inundation and seismic and volcanic
events.
Direct human pressures on reefs have,
until recently, been the dominant
factors damaging coral reefs through a
range of stresses, many of the which
can co-occur.
POLLUTION
The delivery of pollution from unsustainable
land-based human activities such as
deforestation, poorly regulated agriculture,
and urban and industrial development
resulting in the release of excess amounts of
sediments and nutrients.
This is exacerbated by the release of
nutrients and other pollutants from
untreated or poorly treated sewage and
industrial and agricultural wastes.
A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS
OIL, GAS, SEWAGE
Pollution from oil, gas, industrial and
urban waste, sewage, and agrochemicals
from farming is poisoning reefs. These
toxins are dumped directly into the
ocean or carried by river systems from
sources upstream.
Some pollutants, such as sewage and
runoff from farming, increase the level
of nitrogen in sea water, causing an
overgrowth of algae, which smothers
reefs by cutting off their sunlight.
OVERFISHING
Over-fishing and overexploitation
of coral reef fisheries and coral rock
and sand resources.
Within the last two decades there has been
an increase in damaging fishing activities
involving the use of home-made bombs,
cyanide and other damaging practices such
as muro-ami that involves dropping
weighted rocks onto corals to drive fish
into set nets.
A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS
ENGINEERING
PRACTICES
Modification and engineering
practices such as building of ports,
airports and groynes on coral
reefs, including the practice of
‘reclamation’, which pours
sediments onto shallow areas,
displacing sea area in exchange
for increased terrestrial area.
CORAL MINING
Coral mining involves live coral
being removed from reefs for use
as bricks or road-fill, while sand
and limestone is made into
cement for new buildings.
Corals are also removed from
their habitats to be sold as
souvenirs to tourists and
exporters.
CORAL DESTRUCTION
FROM CONSTRUCTION
Construction (along coasts and inland),
mining, logging and farming along coastal
rivers can all lead to erosion.
Valuable topsoil and other sediments are
washed by rain into rivers and end up in the
ocean where they smother corals by
depriving them of the light needed to survive.
Additionally, developments are occurring
directly on top of coral reefs.
CORAL
DESTRUCTION
FROM BOATING
AND DIVING
Careless boating, diving,
snorkelling and fishing can
also damage coral reefs.
Substantial damage has
been caused by people
touching the reefs, stirring
up sediment, collecting
coral, or dropping anchor
on the corals.
CORAL DESTRUCTION AND CLIMATE CHANGE
These newer global threats (bleaching, disease and predators) are increasing
rapidly in frequency and severity, coincidentally with direct human disturbances.
Coral disease has caused major disruptions to coral reefs in the Caribbean with a
range of human disturbances potentially implicated, and there are now
increasing reports of similar disturbances from the Indo-Pacific region.
Evidence linking severe coral bleaching and mortality to increasing rates of global
climate change attributed to rising levels of anthropogenic greenhouse emissions
is growing stronger.
A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS
CORAL BLEACHING
Coral lives in a symbiotic relationship with algae called zooxanthellae.
Zooxanthellae live within the coral animal tissue and carry out photosynthesis
providing energy not only for themselves, but for the coral as well.
Zooxanthellae give the coral its colour.
When environmental conditions become stressful, zooxanthellae may leave the
coral, leaving the coral in an energy deficit and without colour, a process that is
referred to as coral bleaching.
If the coral is re-colonised by zooxanthellae in a timely manner, the coral will
likely recover. If not, the coral may die.
Coral bleaching can be caused by increases in temperature of as little as 1–2ºC
above average annual maximum temperatures.
A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS
CORAL BLEACHING: PUERTO RICO/CARIBBEAN
In 1998 there was extensive
and intensive bleaching
affecting the majority of coral
reefs around Puerto Rico and
the US Caribbean.
In the southwest region a
large number of coral colonies
bleached completely (100% of
living surface area) down to
40m deep.
Maximum temperatures
measured during 1998 in
several reef localities ranged
from 30.15°C (20 m deep) to
31.78°C at the surface.
1998 CORAL
BLEACHING EPISODE
The 1998 episode was the largest coral
bleaching and mortality event ever recorded
on coral reefs globally, with major effects in the
Arabian/Persian Gulf, Eastern Africa,
throughout the Indian Ocean, in Southeast
Asia, parts of the western Pacific and the
Caribbean and Atlantic region.
Overall, it was estimated that 16% of the
world’s area of coral reefs was severely
damaged.
BARBADOS CORAL
BLEACHING
In the wider Caribbean region,
there was moderate to severe
coral bleaching in 1998, but
generally there were low levels of
mortality.
At one site on Barbados,
approximately 20% of bleached
corals did not survive, but there
were complicating factors, notably
hurricane damage.
MARINE ORGANISMS
DISEASE
There has been a worldwide
increase in reports of diseases in
marine organisms including fish,
sea urchins, shellfish, sponges,
marine mammals, and corals.
Since the 1990s, coral diseases have
increased in number, affecting over
150 species from the Caribbean and
Indo-Pacific alone.
CORAL DISEASES
The rate of discovery of new diseases
has increased considerably, with more
than 29 coral diseases now described.
Coral diseases can potentially produce
severe population declines, threaten
biodiversity, and shift the structure of
reef communities by challenging the
resilience of these systems.
CORAL STRESS
Stress appears to lower a coral’s
resistance to disease and thus
affects its ability to survive.
Because elevated temperature
is a coral stress, global climate
change may also result in
increasing incidence of coral
disease. It is possible that
proximity to human population
centres may increase the
likelihood of infection.
Stress is often associated with
increased susceptibility to
disease and many studies have
suggested a correlation between
elevated sea temperatures,
sedimentation, and pollution.
MANAGEMENT
TECHNOQUES
Disease outbreaks are
nearly impossible to
manage because the
connectivity of the marine
environment increases the
speed of disease
transmission and renders
standard response such as
quarantine and vaccines
ineffective.
Preventing nutrient runoff
into coastal areas by
managing water quality
could be one important
management technique.
CARIBBEANS
AND THE DISEASE
For some reason, the
Caribbean appears to
have experienced a
far higher incidence
of disease to coral
reef organisms than
reefs of the Indo-
Pacific (at least 82%
of Caribbean coral
species are
susceptible to
disease, compared to
25% of Indo-Pacific
corals).
HYPOTHESES
EMERGING
Several hypotheses have emerged: the
Caribbean is semi-enclosed, hence the
reefs are in relatively close contact due to
the circulation of water; there are higher
concentrations of nutrients and possibly
pollutants because of the large volumes of
waters flowing in from major rivers e.g.
Amazon and Mississippi; and the reefs have
been isolated from the others for millions
of years. The region also has a higher
population of scientists regularly
monitoring the reefs for problems.
COMMERCIAL
SPONGES
In the 1930’s, there was a major
disease outbreak that devastated the
sponge industry.
This seems to have been repeated in
the 1990’s when commercial sponges
to the west of Florida were virtually
eliminated.
But the most dramatic and
devastating diseases have been to
corals and sea urchins.
SEA URCHINS DISEASE
Populations of the sea urchin were virtually obliterated
when a disease killed over 95% of them throughout the
Caribbean during 1983–84.
This emphasised a major difference between coral reefs in
the Caribbean, where urchins are the major grazers on
algae, and elsewhere where the major grazers are fishes.
The disease that killed these urchins probably originated
near the Caribbean entrance to the Panama Canal and
spread to the south-east and north from this point.
MAJOR IMPACT ON THE REEFS
The major impact on the reefs, however,
was a massive explosion in fleshy algae,
causing many corals to be smothered.
This disease outbreak had far-reaching
consequences which were still evident in
2004; 20 years after the death of the
urchins the populations have only
recovered to about 4% of their original
status and the coral cover is still depleted.
PREDATOR PLAGUES
Predator plagues such as COTS are increasingly
reported around areas of human activities, with two
strong hypotheses advanced:
• the plagues may be initiated and certainly
exacerbated by either over-fishing of key starfish
predators, and/or
• increases in nutrient runoff from the land favours
the planktonic stages of the starfish.
COTS OUTBREAKS
The increasing frequency of COTS
outbreaks continues despite
decades of scientific study in the
Pacific and Australasia and the
cause of these plagues remains
unclear.
The negative effects of COTS are
exacerbated by many other
impacts including pollution,
fishing pressures, sedimentation,
river runoff, global climate
change and associated coral
bleaching events.
These synergistic pressures lead
to widespread, largescale losses
of coral cover and biodiversity.
The highest densities of COTS in
recent years have been on coral
reefs in Tanzania and Kenya.
INVASIVE SPECIES
The most likely causes of invasive species
introduction are:
• ballast-water exchange for cargo ships
travelling long distances between ports
releasing gametes, larvae, or juvenile
individuals into new systems; and
• aquaria-related incidents whereby
individuals import specimens from all
over the world and release them into the
wild after a time in captivity.
Since Indo-Pacific live rock is exported
widely, the risk of introducing Pacific
organisms to the tropical Atlantic is high.
STRATEGIC PLANNING
IN ST. LUCIA
A 1998 survey showed that 65% of coral reefs in
the Caribbean are in danger, and the coral reefs
along St. Lucia's west coast are no exception.
Protecting reefs makes sound economic sense as
well as environmental sense.
St. Lucia government including the Department of
Fisheries, the Department of Tourism, local tourist
organisations and the Soufriere Regional
Development Foundation have begun to take
action to prevent the further destruction of this
valuable natural resource.
SOUFRIERE MARINE
MANAGEMENT AREA 1986
In 1986 six areas were declared as marine reserves and another three areas were
created as fishing priority areas. The Soufriere Marine Management Area is a 12 km
stretch of coastline. The SMMA is attempting to manage St Lucia's marine resources in
a sustainable way, although it is not always easy.
SMMA's activities include:
• Scientific research on the natural resources of the region.
• Regular monitoring of coral reefs, water quality and other environmental factors and
resources.
• Provision of public information and sensitisation.
• Provision of facilities for users of the SMMA e.g. moorings.
• Co-ordination of economic activities related to the SMMA and its resources.
GLOBAL ASSESSMENT
OF CORAL REEFS
About one-fifth of the world’s coral reefs are
so damaged they are beyond repair.
While the percentage of reefs recovering
from past damage has risen, 70% of the
world’s reefs are threatened or have already
been destroyed, up from 59% in 2000.
Almost half of the reefs severely damaged by
coral bleaching in 1998 are recovering, but
other reefs are so badly damaged that they
are unrecognisable as coral reefs.
ECONOMIC
AND ECOLOGICAL
CONCERN
The destruction of reefs is
cause for economic, as
well as ecological,
concern, especially for the
communities that depend
on coral reefs for the fish
they provide and the
revenue they draw as
tourist attractions.
2004 STATE OF THE
WORLD’S CORAL
The 2004 State of the World’s
Coral report says the main
causes of reef decline are
climate change which causes
bleaching, poor land
management practices which
damage the reefs with
sediments, nutrients and
other pollutants, over-fishing
and destructive fishing
practices, and coastal
development. Increased
water temperatures have
already been blamed for the
single most destructive event
for corals, the 1998 bleaching.
PERSIAN GULF REEFS
The most damaged reefs are in the
Persian Gulf where 65% have been
destroyed, followed by reefs in South
and Southeast Asia where 45% and 38%,
respectively, are considered destroyed.
There are also recent reports that many
reefs in the wider Caribbean have lost
80% of their corals.
RECOVERING REEFS
The percentage of recovering reefs has
increased compared to the last global
assessment. Most of the recovered reefs
are in the Indian Ocean, part of the Great
Barrier Reef off the coast of Australia and
in Palau. In 2004, Australia increased
protection of the Great Barrier Reef from
4% to 33% and 34% of Ningaloo Reef
Marine Park was made off-limits to
fishing.
PRIMARY CAUSE OF THE CRISIS
The Status of Coral Reefs of the
World: 2004 report documents
how human activities continue to
be the primary cause of the global
coral reef crisis.
The report details many new
initiatives aimed at reversing this
degradation such as by conserving
the biodiversity, the economic
value and beauty of coral reefs.
MAJOR STRESSES
The report recognises that the major stresses
to coral reefs are: natural forces that they have
coped with for millions of years; direct human
pressures, including sediment and nutrient
pollution from the land, overexploitation and
damaging fishing practices, engineering
modification of shorelines; and the global
threats of climate change causing coral
bleaching, rising sea levels and potentially
threatening the ability of corals to form
skeletons in more acid waters.
CONCLUSION
Conclusion At the World Conservation
Union’s (IUCN) meeting in Australia (2005) it
was claimed that up to 20% of the world’s
reefs had been destroyed and that a further
50% could be lost by 2050.
The IUCN called for more marine parks,
which could help protect coral by decreasing
overfishing, mining and other destructive
processes.
Given the diversity within coral reefs, their
protection is as important as that of the
tropical rain forests.

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A2 CAMBRIDGE GEOGRAPHY: COASTAL ENVIRONMENTS - CORAL REEFS

  • 2. WHAT ARE CORAL REEFS? Coral reefs are one of the most biologically diverse ecosystems, rivalled only by the tropical rainforests in this respect. Corals are marine animals, and almost a thousand coral species currently exist. Human activities are threatening their future.
  • 3. WHAT ARE THE CORAL REEFS? With the majority of the world’s population living in coastal regions, many people depend on living coral reefs for food, and protection from storm surges and erosion, as well as the additional benefits of medical research, tourism and aesthetic beauty.
  • 4. WHAT ARE THE CORAL REEFS? With the majority of the world’s population living in coastal regions, many people depend on living coral reefs for food, and protection from storm surges and erosion, as well as the additional benefits of medical research, tourism and aesthetic beauty. Coral reefs contribute about 25% of the total fish catch in LIC’s (LEDCs), providing food for one billion people in Asia alone. Human activities, such as those associated with global warming, are threatening coral reefs. Increasing sea temperatures stress corals and cause damage, including bleaching.
  • 5. THE DEVELOPMENT OF CORAL All tropical reefs began life as polyps – tiny, soft animals, like sea anemones – which attach themselves to a hard surface in shallow seas where there is sufficient light for growth. As they grow, many of these polyps exude calcium carbonate, which forms their skeleton. As they grow and die, these colonies of ‘rock’-forming corals create reefs.
  • 6. GROWTH RATES Tropical reefs can grow at rates of under 2.5–60 cm/year, forming huge structures over incredibly long periods of time, making them the largest and oldest living systems on Earth. For example, the 1,250-mile Great Barrier Reef was formed over five million years.
  • 7. POLYPS AND ALGAE Polyps have growing inside them small algae, zooxanthellae. The algae receive shelter and food from the polyp, while the polyp also gets some food via photosynthesis. Algae need sunlight to live, and obviously photosynthesis (conversion of light energy from the sun into food) cannot occur in darkness, hence corals only grow where the sea is shallow and clear.
  • 8. REEF FORMATION Darwin’s subsidence theory is illustrating the evolution of three reef types (South Pacific model) i.e. linking the formation of the three types of reef together.
  • 9. FRINGING REEFS Fringing reefs grow around newly formed islands. These islands subside, or sea level rises relative to land.
  • 10. BARRIER REEFS If the process is slow the reef will grow upwards to form a larger barrier reef separated from the island by a deeper lagoon.
  • 11. ATOLLS When the island disappears beneath the sea an atoll forms. Corals can continue to grow on the outside to keep the reef on the surface. On the inside, where the land used to be, quiet water with increased sedimentation prevails.
  • 13. THREATS TO CORAL THE MAIN THREATS TO CORAL INCLUDE • coral bleaching and global climate change • diseases of corals and other reef organisms • plagues of predators like the crown of-thorns starfish (COTS) and other damaging organisms such as the sea urchin • invasive species which have been introduced onto new coral reefs.
  • 15. OTHER THREATS These threats are in addition to natural stresses that have always affected coral reefs such as storms, freshwater inundation and seismic and volcanic events. Direct human pressures on reefs have, until recently, been the dominant factors damaging coral reefs through a range of stresses, many of the which can co-occur.
  • 16. POLLUTION The delivery of pollution from unsustainable land-based human activities such as deforestation, poorly regulated agriculture, and urban and industrial development resulting in the release of excess amounts of sediments and nutrients. This is exacerbated by the release of nutrients and other pollutants from untreated or poorly treated sewage and industrial and agricultural wastes.
  • 18. OIL, GAS, SEWAGE Pollution from oil, gas, industrial and urban waste, sewage, and agrochemicals from farming is poisoning reefs. These toxins are dumped directly into the ocean or carried by river systems from sources upstream. Some pollutants, such as sewage and runoff from farming, increase the level of nitrogen in sea water, causing an overgrowth of algae, which smothers reefs by cutting off their sunlight.
  • 19. OVERFISHING Over-fishing and overexploitation of coral reef fisheries and coral rock and sand resources. Within the last two decades there has been an increase in damaging fishing activities involving the use of home-made bombs, cyanide and other damaging practices such as muro-ami that involves dropping weighted rocks onto corals to drive fish into set nets.
  • 21. ENGINEERING PRACTICES Modification and engineering practices such as building of ports, airports and groynes on coral reefs, including the practice of ‘reclamation’, which pours sediments onto shallow areas, displacing sea area in exchange for increased terrestrial area.
  • 22. CORAL MINING Coral mining involves live coral being removed from reefs for use as bricks or road-fill, while sand and limestone is made into cement for new buildings. Corals are also removed from their habitats to be sold as souvenirs to tourists and exporters.
  • 23. CORAL DESTRUCTION FROM CONSTRUCTION Construction (along coasts and inland), mining, logging and farming along coastal rivers can all lead to erosion. Valuable topsoil and other sediments are washed by rain into rivers and end up in the ocean where they smother corals by depriving them of the light needed to survive. Additionally, developments are occurring directly on top of coral reefs.
  • 24. CORAL DESTRUCTION FROM BOATING AND DIVING Careless boating, diving, snorkelling and fishing can also damage coral reefs. Substantial damage has been caused by people touching the reefs, stirring up sediment, collecting coral, or dropping anchor on the corals.
  • 25. CORAL DESTRUCTION AND CLIMATE CHANGE These newer global threats (bleaching, disease and predators) are increasing rapidly in frequency and severity, coincidentally with direct human disturbances. Coral disease has caused major disruptions to coral reefs in the Caribbean with a range of human disturbances potentially implicated, and there are now increasing reports of similar disturbances from the Indo-Pacific region. Evidence linking severe coral bleaching and mortality to increasing rates of global climate change attributed to rising levels of anthropogenic greenhouse emissions is growing stronger.
  • 27. CORAL BLEACHING Coral lives in a symbiotic relationship with algae called zooxanthellae. Zooxanthellae live within the coral animal tissue and carry out photosynthesis providing energy not only for themselves, but for the coral as well. Zooxanthellae give the coral its colour. When environmental conditions become stressful, zooxanthellae may leave the coral, leaving the coral in an energy deficit and without colour, a process that is referred to as coral bleaching. If the coral is re-colonised by zooxanthellae in a timely manner, the coral will likely recover. If not, the coral may die. Coral bleaching can be caused by increases in temperature of as little as 1–2ºC above average annual maximum temperatures.
  • 29. CORAL BLEACHING: PUERTO RICO/CARIBBEAN In 1998 there was extensive and intensive bleaching affecting the majority of coral reefs around Puerto Rico and the US Caribbean. In the southwest region a large number of coral colonies bleached completely (100% of living surface area) down to 40m deep. Maximum temperatures measured during 1998 in several reef localities ranged from 30.15°C (20 m deep) to 31.78°C at the surface.
  • 30. 1998 CORAL BLEACHING EPISODE The 1998 episode was the largest coral bleaching and mortality event ever recorded on coral reefs globally, with major effects in the Arabian/Persian Gulf, Eastern Africa, throughout the Indian Ocean, in Southeast Asia, parts of the western Pacific and the Caribbean and Atlantic region. Overall, it was estimated that 16% of the world’s area of coral reefs was severely damaged.
  • 31. BARBADOS CORAL BLEACHING In the wider Caribbean region, there was moderate to severe coral bleaching in 1998, but generally there were low levels of mortality. At one site on Barbados, approximately 20% of bleached corals did not survive, but there were complicating factors, notably hurricane damage.
  • 32. MARINE ORGANISMS DISEASE There has been a worldwide increase in reports of diseases in marine organisms including fish, sea urchins, shellfish, sponges, marine mammals, and corals. Since the 1990s, coral diseases have increased in number, affecting over 150 species from the Caribbean and Indo-Pacific alone.
  • 33. CORAL DISEASES The rate of discovery of new diseases has increased considerably, with more than 29 coral diseases now described. Coral diseases can potentially produce severe population declines, threaten biodiversity, and shift the structure of reef communities by challenging the resilience of these systems.
  • 34. CORAL STRESS Stress appears to lower a coral’s resistance to disease and thus affects its ability to survive. Because elevated temperature is a coral stress, global climate change may also result in increasing incidence of coral disease. It is possible that proximity to human population centres may increase the likelihood of infection. Stress is often associated with increased susceptibility to disease and many studies have suggested a correlation between elevated sea temperatures, sedimentation, and pollution.
  • 35. MANAGEMENT TECHNOQUES Disease outbreaks are nearly impossible to manage because the connectivity of the marine environment increases the speed of disease transmission and renders standard response such as quarantine and vaccines ineffective. Preventing nutrient runoff into coastal areas by managing water quality could be one important management technique.
  • 36. CARIBBEANS AND THE DISEASE For some reason, the Caribbean appears to have experienced a far higher incidence of disease to coral reef organisms than reefs of the Indo- Pacific (at least 82% of Caribbean coral species are susceptible to disease, compared to 25% of Indo-Pacific corals).
  • 37. HYPOTHESES EMERGING Several hypotheses have emerged: the Caribbean is semi-enclosed, hence the reefs are in relatively close contact due to the circulation of water; there are higher concentrations of nutrients and possibly pollutants because of the large volumes of waters flowing in from major rivers e.g. Amazon and Mississippi; and the reefs have been isolated from the others for millions of years. The region also has a higher population of scientists regularly monitoring the reefs for problems.
  • 38. COMMERCIAL SPONGES In the 1930’s, there was a major disease outbreak that devastated the sponge industry. This seems to have been repeated in the 1990’s when commercial sponges to the west of Florida were virtually eliminated. But the most dramatic and devastating diseases have been to corals and sea urchins.
  • 39. SEA URCHINS DISEASE Populations of the sea urchin were virtually obliterated when a disease killed over 95% of them throughout the Caribbean during 1983–84. This emphasised a major difference between coral reefs in the Caribbean, where urchins are the major grazers on algae, and elsewhere where the major grazers are fishes. The disease that killed these urchins probably originated near the Caribbean entrance to the Panama Canal and spread to the south-east and north from this point.
  • 40. MAJOR IMPACT ON THE REEFS The major impact on the reefs, however, was a massive explosion in fleshy algae, causing many corals to be smothered. This disease outbreak had far-reaching consequences which were still evident in 2004; 20 years after the death of the urchins the populations have only recovered to about 4% of their original status and the coral cover is still depleted.
  • 41. PREDATOR PLAGUES Predator plagues such as COTS are increasingly reported around areas of human activities, with two strong hypotheses advanced: • the plagues may be initiated and certainly exacerbated by either over-fishing of key starfish predators, and/or • increases in nutrient runoff from the land favours the planktonic stages of the starfish.
  • 42. COTS OUTBREAKS The increasing frequency of COTS outbreaks continues despite decades of scientific study in the Pacific and Australasia and the cause of these plagues remains unclear. The negative effects of COTS are exacerbated by many other impacts including pollution, fishing pressures, sedimentation, river runoff, global climate change and associated coral bleaching events. These synergistic pressures lead to widespread, largescale losses of coral cover and biodiversity. The highest densities of COTS in recent years have been on coral reefs in Tanzania and Kenya.
  • 43. INVASIVE SPECIES The most likely causes of invasive species introduction are: • ballast-water exchange for cargo ships travelling long distances between ports releasing gametes, larvae, or juvenile individuals into new systems; and • aquaria-related incidents whereby individuals import specimens from all over the world and release them into the wild after a time in captivity. Since Indo-Pacific live rock is exported widely, the risk of introducing Pacific organisms to the tropical Atlantic is high.
  • 44. STRATEGIC PLANNING IN ST. LUCIA A 1998 survey showed that 65% of coral reefs in the Caribbean are in danger, and the coral reefs along St. Lucia's west coast are no exception. Protecting reefs makes sound economic sense as well as environmental sense. St. Lucia government including the Department of Fisheries, the Department of Tourism, local tourist organisations and the Soufriere Regional Development Foundation have begun to take action to prevent the further destruction of this valuable natural resource.
  • 45. SOUFRIERE MARINE MANAGEMENT AREA 1986 In 1986 six areas were declared as marine reserves and another three areas were created as fishing priority areas. The Soufriere Marine Management Area is a 12 km stretch of coastline. The SMMA is attempting to manage St Lucia's marine resources in a sustainable way, although it is not always easy. SMMA's activities include: • Scientific research on the natural resources of the region. • Regular monitoring of coral reefs, water quality and other environmental factors and resources. • Provision of public information and sensitisation. • Provision of facilities for users of the SMMA e.g. moorings. • Co-ordination of economic activities related to the SMMA and its resources.
  • 46. GLOBAL ASSESSMENT OF CORAL REEFS About one-fifth of the world’s coral reefs are so damaged they are beyond repair. While the percentage of reefs recovering from past damage has risen, 70% of the world’s reefs are threatened or have already been destroyed, up from 59% in 2000. Almost half of the reefs severely damaged by coral bleaching in 1998 are recovering, but other reefs are so badly damaged that they are unrecognisable as coral reefs.
  • 47. ECONOMIC AND ECOLOGICAL CONCERN The destruction of reefs is cause for economic, as well as ecological, concern, especially for the communities that depend on coral reefs for the fish they provide and the revenue they draw as tourist attractions.
  • 48. 2004 STATE OF THE WORLD’S CORAL The 2004 State of the World’s Coral report says the main causes of reef decline are climate change which causes bleaching, poor land management practices which damage the reefs with sediments, nutrients and other pollutants, over-fishing and destructive fishing practices, and coastal development. Increased water temperatures have already been blamed for the single most destructive event for corals, the 1998 bleaching.
  • 49. PERSIAN GULF REEFS The most damaged reefs are in the Persian Gulf where 65% have been destroyed, followed by reefs in South and Southeast Asia where 45% and 38%, respectively, are considered destroyed. There are also recent reports that many reefs in the wider Caribbean have lost 80% of their corals.
  • 50. RECOVERING REEFS The percentage of recovering reefs has increased compared to the last global assessment. Most of the recovered reefs are in the Indian Ocean, part of the Great Barrier Reef off the coast of Australia and in Palau. In 2004, Australia increased protection of the Great Barrier Reef from 4% to 33% and 34% of Ningaloo Reef Marine Park was made off-limits to fishing.
  • 51. PRIMARY CAUSE OF THE CRISIS The Status of Coral Reefs of the World: 2004 report documents how human activities continue to be the primary cause of the global coral reef crisis. The report details many new initiatives aimed at reversing this degradation such as by conserving the biodiversity, the economic value and beauty of coral reefs.
  • 52. MAJOR STRESSES The report recognises that the major stresses to coral reefs are: natural forces that they have coped with for millions of years; direct human pressures, including sediment and nutrient pollution from the land, overexploitation and damaging fishing practices, engineering modification of shorelines; and the global threats of climate change causing coral bleaching, rising sea levels and potentially threatening the ability of corals to form skeletons in more acid waters.
  • 53. CONCLUSION Conclusion At the World Conservation Union’s (IUCN) meeting in Australia (2005) it was claimed that up to 20% of the world’s reefs had been destroyed and that a further 50% could be lost by 2050. The IUCN called for more marine parks, which could help protect coral by decreasing overfishing, mining and other destructive processes. Given the diversity within coral reefs, their protection is as important as that of the tropical rain forests.