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Shoreline protection and other ecosystem services
from mangroves and coral reefs

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International Coral Reet Action Network The World Conservation Union

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in 2010 with funding from
UNEP-WCMC, Cambridge

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Shoreline protection and other ecosystem services
from mangroves and coral reefs

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The World Conservation Union

ICRAN

In the front line

UNEP World Conservation Monitoring Centre
219 Huntingdon Road,

Cambridge CB3 ODL,

United Kingdom

Tel: +44 (0) 1223 277314

Fax: +44 (0) 1223 277136

Email: info@unep-wemc.org

Website: www.unep-wcmc.org

THE UNITED NATIONS ENVIRONMENT PROGRAMME WoRLD
CONSERVATION MoniToRING CENTRE [UNEP-WCMC) is the
biodiversity assessment and policy implementation arm of
the United Nations Environment Programme [UNEP], the
world’s foremost intergovernmental environmental
organization. The Centre has been in operation for over 25
years, combining scientific research with practical policy
advice.

UNEP-WCMC provides objective, scientifically rigorous
products and services to help decision makers recognize
the value of biodiversity and apply this knowledge to all
that they do. Its core business is managing data about
ecosystems and biodiversity, interpreting and analysing
that data to provide assessments and policy analysis, and
making the results available to national and international
decision makers and businesses.

Lead Author: Sue Wells
Contributing authors: Corinna Ravilious and
Emily Corcoran

Front cover photos: Y Yusuf; UNEP/Topham;

E Clua/CRISP, 2005; S Wells; UNEP-WCMC World
Atlas of Coral Reefs.

Back cover photo: S Wells

Citation: UNEP-WCMC (2005) /n the front line: shoreline
protection and other ecosystem services from
mangroves and coral reefs. UNEP-WCMC. 33 pp

©UNEP-WCMC/UNEP 2006

A Banson production
Printed in the UK by Cambridge Printers

ACKNOWLEDGEMENTS

We gratefully acknowledge the many partners and
institutions who contributed to this publication, in
particular the following individuals who provided
information and comments on early drafts: John Agard,
Tundi Agardy, Jackie Alder, Daniel Alongi, Andrew Baird,
Nicola Barnard, Juan Bezaury, Simon Blyth, Barbara
Brown, Marion Cheatle, Isabelle Cote, Salif Diop, Alasdair
Edwards, Norberto Fernandez, Harinda Fernando, Phil
Fox, Alison Glass, Stefan Hain, Mark Huxham, Val Kapos,
Carmen Lacambra, lan May, Nick Nuttal, Pascal Peduzzi,
Pasi Rinne, Toby Roxburgh, Charles Sheppard, Jerker
Tamelander, Kristian Teleki, Ruben Torres, Collette
Wabnitz, Alan White, Victoria Wood and Kaveh Zahedi.

The contents of this report do not necessarily reflect the views or policies of the United Nations Environment Programme, the UNEP World Conservation
Monitoring Centre, the International Coral Reef Action Network or |IUCN-The World Conservation Union. The designations employed and the presentations
do not imply the expressions of any opinion whatsoever on the part of these organizations concerning the legal status of any country, territory, city or area

or its authority, or concerning the delimitation of its frontiers or boundaries

In the front line

Contents

4

5

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In the front line

Introduction

The Indian Ocean tsunami of 26 December 2004 and its
tragic and devastating consequences were a wake-up call
for the global community, dramatically drawing attention to
the vulnerability of tropical coastal ecosystems and the
dangers of undermining the services they provide to
humankind. This was further emphasized by the
catastrophic hurricane season in the Gulf of Mexico in
2005 when Hurricanes Katrina, Rita and Wilma caused
much publicized and extensive damage to coastal areas.
The numerous other tropical storms that affected coastal
communities and ecosystems in other parts of the world
in the same year received much less attention, but were
also notable.

The lessons learnt in terms of loss of life, damage
sustained, and approaches to reconstruction and mitigation
are critically relevant to future management of the coast in
a context of increasing severe weather events such as

hurricanes and typhoons, and other potential consequences
of global warming. More than ever, it is essential to consider
the full value of ‘ecosystem services’ [the benefits that
people obtain from ecosystems] when making decisions
about coastal development.

The aim of this publication is to help decision
makers and policy makers around the world understand the
importance of coastal habitats to humans, using coral reefs
and mangroves as an example. It looks at the role of these
ecosystems in protecting the coast, and takes into account
new studies of this complex topic triggered by the tsunami
and tropical storms. The publication also addresses the
huge range of other benefits provided by these ecosystems
and the role that they can play in coastal development and
in restoring and maintaining the livelihoods of those who
have suffered from extreme events, whether natural or
induced by human activity.

Key messages

GLOBAL STATUS OF CORAL REEFS AND MANGROVES
Coral reefs and mangroves are two of the world’s rarest
ecosystems, covering an area that is an order of magnitude
less than that of tropical and subtropical forests. Both
ecosystems are under serious threat.

4 Some 30 per cent of reefs are already seriously
damaged and 60 per cent could be lost by 2030.
Threats include overfishing, use of destructive
fishing methods, coral mining, pollution, sedi-
mentation, anchor damage and tourism, as well
as coral bleaching, disease and tropical storms.
This combination of impacts is causing a shift, on
many reefs, from a coral-dominated ecosystem to
one dominated by algae.

(4) An estimated 35 per cent of the world’s original
Mangrove cover has already gone, with some
countries having lost up to 80 per cent. Mangroves
have been degraded by conversion to aquaculture,
timber extraction, use of wood for fuel and
charcoal production, diseases and storms.

ECOSYSTEM BENEFITS
Coral reefs and mangroves provide benefits under the four
categories of ecosystem services defined by the 2005
Millenium Ecosystem Assessment:
O Regulating - e.g. protection of shores from storm
surges and waves; prevention of erosion.
O Provisioning - e.g. fisheries, building materials.
4 Cultural - e.g. tourism, spiritual appreciation.
() Supporting - e.g. cycling of nutrients, fish nursery
habitats.

They are among the most valuable ecosystems in terms of
their benefits to humankind:

(4 Economic valuation of ecosystems needs to be
treated with caution but annual values per km’
have been calculated at US$100 000-600 000 for
reefs and US$200 000-900 000 for mangroves.

J The small total area of coral reefs and mangroves
belies their importance in terms of fisheries,
other extractive uses, shoreline protection and, in
the case of reefs, tourism and recreation.

(1 Both ecosystems contribute significantly to
national economies, particularly those of small
island developing states (SIDS), 90 per cent of
which have coral reefs and over 75 per cent of
which have mangroves.

In the front line

Ecosystems that can no longer provide their full ecological
services have a social and economic cost’ that can be felt
locally and many miles away. Degradation of coral reefs and
mangroves may, and in some cases already does, cause:

(4 Reduced fish catches and tourism revenue in
coastal communities, and potentially even loss
of food security and malnutrition due to lack
of protein.

(J Loss of export earnings and decline of the
tourism industry.

Q Increased coastal erosion and destruction from
storms and catastrophic natural events, which
affects coastal residents, tourism operations and
many other economic sectors.

SHORELINE PROTECTION

Reefs and mangroves naturally form barriers and thus
inevitably provide some shore protection, a fact long
recognized by coastal communities, fishers and vessels
which use the sheltered waterways behind these
ecosystems. Both reefs and mangroves can themselves be
damaged by strong winds and waves, and so their buffering
capacity is a balance between their resilience and their
vulnerability. The current consensus is that:

(4 Reefs and mangroves play an important role in
shore protection under normal sea conditions
and during hurricanes and tropical storms. At
least 70-90 per cent of the energy of wind-
generated waves is absorbed, depending on how
healthy these ecosystems are and their physical
and ecological characteristics.

QJ In a tsunami, the buffering capacity of reefs and
Mangroves is more variable and often reduced
because of the different structure and form of
the waves and their much greater force. Distance
from the earthquake epicentre, the presence of
inlets and headlands, the gradient of the
continental slope, shoreline elevation, the
presence of dunes and other vegetation, and
density of habitation and infrastructure seem to
explain most of the variation.

PROS AND CONS OF REHABILITATION AND RESTORATION
Both reefs and mangroves will recover naturally once a
stress has been removed, but this can be slow; for example,
the reefs most seriously damaged by the tsunami may take
five to ten years to recover. New growth of coral colonies and

S Wells

In the front line

mangrove trees, and recruitment of coral larvae and
mangrove seedlings, is balanced by erosion and breakdown
from both human-induced and natural stresses. The
chronic human impacts faced by these ecosystems are
tending to slow recovery, and the highest priority is to
reduce and eliminate these stresses. It is tempting to try to
speed recovery of an ecosystem by active restoration, or
repair. However, this is rarely totally successful because of
the difficulties involved in re-establishing full biodiversity
and ecological processes:

1 Mangrove restoration is relatively simple and
large areas of new forest are being created using
volunteers and local labour. However, achieving a
mangrove forest with a full complement of
biodiversity is a more complex and long-term
process, and it is questionable whether any
programmes have yet achieved this.

O Reefs, involving numerous species with very
different life histories and poorly understood
growth and reproductive characteristics, are
more difficult to restore. Many attempts have
been made using a variety of techniques. Most
methods are costly and require considerable
skill, and there are few examples of successful
sustainable reef restoration over large areas.

CORAL REEF AND MANGROVE MANAGEMENT IN THE
FUTURE

Investing in environmentally sustainable management
and development of the coast will be more cost effective
than restoring human livelihoods and ecosystems after a
catastrophe. The relatively small amount of damage
inflicted on coral reefs and mangroves by the
2004 tsunami demonstrated the resilience of these
ecosystems to natural disturbance, but the worldwide
public concern generated also revealed our awareness of

their vulnerability.

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The devastation recently wrought by hurricanes
and tropical storms testifies to the priority that
must be accorded to the maintenance and
enhancement of the resilience of natural coastal
barriers such as reefs and mangroves.
Post-tsunami and hurricane reconstruction
efforts provide an opportunity to introduce and
expand good coastal management practices.
These may indeed help to mitigate damage from
future tsunamis but, since these are infrequent
events, the more important consequence is
mitigation of the impacts of the more certain, but
gradual, changes due to global warming.
Short-term, small-scale rehabilitation progr-
ammes should not take precedence over
activities directed at the root causes of the
decline in reef and mangrove health. Key tools
include integrated coastal management, marine
protected areas, and monitoring and assessment
for adaptive management.

Governments, civil society and the private sector
must recognize that, as with other benefits, there
is a price to pay for maintaining these eco-
systems. However, this is much lower than the
benefit received. For example, the estimated
average operational management cost of a
marine protected area is US$775 per km’, or less
than 0.2 per cent of the estimated global value of
a square kilometre of reef or mangrove.

Many of the world’s wealthiest nations have
jurisdiction over these ecosystems - more than
30 per cent of reefs are in countries classified as
highly developed. They also have strong links
with less developed countries struggling with
their management. Political will and concerted
action are needed - coral reefs and mangroves
are in the front line, and calling for attention.

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In the front line

Global status of reefs and

mangroves

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DISTRIBUTION
Of the 177 countries in the world, rather less than half (44
per cent] have tropical coral reefs and about half have
mangroves. Our knowledge of the distribution of coral reefs
and mangroves is now relatively good, as a result of regional
and global mapping programmes using navigational charts,
satellite imagery and aerial photography, as well as more
detailed field surveys.

Both ecosystems occur principally in the tropics,
with South-East Asia a major centre. Distribution between

Fig. 1: Area of coral reefs and mangroves

Coral reefs

M
Behar: 284 300 km?

167 000 km?

Tropical and
subtropical forests
23 300 000 km?

Coral reefs and mangroves are among the world’s rarest
ecosystems. Reefs cover an estimated 284 300 km’, or just 1.2 per
cent of the world’s continental shelf area (Spalding et al., 2001).
The total area of mangrove forest is less certain but is even
smaller, estimated at between 167 000 km’ [Valiela et al., 2001)
and 181 000 km* [Spalding et al., 1997]. As a comparison, tropical
and subtropical forests cover 23.3 million km’, an order of
magnitude larger (Millennium Ecosystem Assessment, 2005].

Mangroves and tropical coral reefs

countries is very unequal. Australia and Indonesia each
have about 50 000 km’ of reef and account for nearly 35 per
cent of the world’s reefs, and Indonesia alone has 23-25 per
cent of the world’s mangroves. In general, other countries
have less than 10 000 km’ of reef and less than 1 000 km‘? of
mangroves (Spalding et al., 1997; 2001).

STATUS
The coastal biome, which makes up only 4 per cent of the

Fig. 2: Distribution of tropical coral reefs and mangroves

Coral reefs

Pacific

South-East
Asia

Indian Ocean
& Middle East

Atlantic &
Caribbean

Mangroves
South &
South-East
Asia
Americas
West Africa
Australia
Indian Ocean
& Middle East

0 10 20 30 40 50
per cent

In the front line

planet's total land area, is home to one-third of the world’s
population, and this population is predicted to double over
the next 15 years. In many countries, such as island nations
and those with inhospitable and arid interiors, humankind
lives almost entirely on the coast. With the exception of
some isolated atolls, all reefs and mangroves lie adjacent to
the coast; more than half these ecosystems occur within 25
km of urban centres inhabited by 100 000 or more people
(Millennium Ecosystem Assessment, 2005). Not
surprisingly, the health and extent of both reefs and
mangroves have declined dramatically over the last century.

Trends in reef health are well documented as
assessments are carried out at regular intervals, through
Numerous monitoring programmes, the results of which
are published in the biennial Status of the World's Reefs
Reports (Wilkinson, 2004), the regional World Resources
Institute's Reefs at Risk reports (Burke and Maidens, 2004;
Burke et al., 2002) and many national reports.

Results from monitoring programmes indicate that
about 30 per cent of the world’s reefs are seriously
damaged, with possibly no pristine reefs at all remaining,
and it has been predicted that 60 per cent of reefs will be
lost by 2030 (Wilkinson, 2004). Using information on existing
and potential threats to reefs in 1998, the World Resources
Institute suggested that 27 per cent of all reefs are
potentially at high risk and a further 31 per cent are at
medium risk of damage (Bryant et al., 1998]. More recent
regional predictions, using the same method, paint an even
more disturbing picture. A 2000 analysis estimated that
human activities potentially threaten 88 per cent of the
reefs of South-East Asia, with 50 per cent at ‘high’ or very
high’ risk and only 12 per cent at low risk (Burke et al.,
2002).

As yet there are no equivalent global mangrove

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Q 200 400 600 800 1,000 km

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70°w

Carysfort Reef, the largest and most luxuriant reef in the Florida
Keys, United States, in 1975 (higher) and 2004 [lower] showing the
catastrophic decline of living coral cover.

Reefs at risk in the Caribbean

Nearly two-thirds of reefs in the Caribbean are potentially at risk
from human activities, according to a 2004 report, with over 40 per
cent at ‘high’ or ‘very high’ risk, and about 28 per cent at low risk
(Burke and Maidens, 2004). In this region, elkhorn (Acropora
palmata] and staghorn (A. cervicornis) corals have undergone
massive die-offs (Gardner et al., 2003).

60°W

Total Observed change in percent

Threat Index coral cover across the Caribbean
| © Low 1977-2001
* Medium 60
e High a
* Very high 2 50
°
°o
ro 40
8
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4 10
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1977 1981 1985 1989 1993 1997 2001

Year

Coordinate System: Geographic
Source: WRI (2004) Reefs at Risk in the Caribbean

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R Dustan

P Dustan

Y Latypov

assessments, but several studies have shown this
ecosystem to be as much at risk as coral reefs. The
amount of mangrove lost varies widely among countries
but, where data are available, mangroves are on a
declining trend. An estimated 35 per cent of mangrove
forest has disappeared in the last two decades (Valiela et
al., 2001), and some countries have lost 80 per cent of
cover (Spalding et al., 1997). The average annual rate of
disappearance [or conversion to other forms of land use]
is estimated at 2.1 per cent, with the greatest rate of loss
in the Americas (3.6 per cent). The annual rate of loss of
Mangroves thus exceeds the rate of disappearance of
tropical rainforests (0.8 per cent) (Valiela et al., 2001).
Estimates for some locations suggest that rates of
mangrove loss may be as high as 50 per cent a year
(Alongi, 2002).

Over the last few decades there have been major
changes in the appearance and quality of reefs and
mangroves, the result of a combination of many ‘drivers’ or
threats. These have both direct and indirect impacts that
often trigger an escalating series of problems.

Many reefs, for example, are undergoing a shift from
a coral-dominated to an algal-dominated state. Corals have
been disappearing as a result of bleaching, disease, storm
damage and a range of human activities, including
overfishing, use of destructive fishing gear, anchor damage
and pollution. At the same time, algae have increased as
herbivores and grazers, such as sea urchins and some fish
species, that keep them in control have declined through
disease and overfishing. Algae have further increased as a
result of nutrient pollution. Where coral cover has started to
increase there are indications that the so-called
framework-building corals (e.g. Acropora, Montastrea) that
once dominated are being replaced by corals that contribute

The brown seaweed Chnoospora overgrowing branching corals.

In the front line

Fig. 3: Area of mangrove lost to human activities
(per cent]

Land
reclamation

Other

Shrimp
Diversion of culture

freshwater

Fish
culture

Forests use

Source: Valiela et al., 2001

little to the main structure of the reef (e.g. Agaricia) (Hughes
et al., 2003; Knowlton, 2001).

Degradation of mangroves leads to long-term
changes in the ecology of large areas of coastline. In
particular, conversion of mangroves to shrimp farms, and
the subsequent aeration and use of fertilizers, alters the
composition and structure of the soil. Eventually ponds
are abandoned, sometimes after only two to ten years, as
they are no longer suitable for production (Stevenson,
1997}. There is little chance of mangrove regeneration in
the remaining barren lands. Leading causes of mangrove
forest loss and degradation are conversion for
aquaculture, use of mangroves for timber for
construction and other functions, and for fuelwood and
charcoal, conversion to rice paddies, and freshwater
diversion and coastal development for tourism and other
purposes [Valiela et al., 2001).

THREATS

Overexploitation and destructive fishing

Many commercial fish species, such as rabbitfish
{Siganidae], feed on algae, and their removal can result in
excessive algal overgrowth of corals. Removal of
‘keystone’ species (those that play a particular role in an
ecosystem) - such as triggerfish which prey on sea
urchins —- may be the cause of urchin population out-
breaks which further degrade corals through bioerosion.
Dynamite, small-mesh nets and nets that are dragged
over the seabed, although illegal in many countries, are
still used and cause widespread physical damage as well
as removing or killing immature fish and other species of
no commercial value.

Habitat loss

Mangroves can be completely wiped out when forests are
cleared for salt production operations, for industrial,
residential and tourism development, or, particularly, for
aquaculture. In contrast, coral reefs generally suffer from

UNEP.

In the front line

In Honduras, shrimp farms have progressively transformed the coast of the Gulf of Fonseca since the early 1970s. Although there were still large
areas of mangrove in 1987, by 1999 the only substantial forests were in protected areas such as Estero Real Nature Reserve (UNEP, 2005a].

a gradual decline in quality rather than a sudden
disappearance. However, mining for corals for use as
building materials can eliminate, or reduce to rubble,
large areas of reef. Although coral mining is illegal or
regulated in most countries, it is still having a major
impact in India, the Maldives, Sri Lanka and Tanzania
(Wilkinson, 2004).

Land-based sources of pollution

More than 77 per cent of the pollutants entering the oceans
originate on land, and 44 per cent of these pollutants come
from improperly treated wastes and run-off (Cicin-Sain et
al., 2002). The nutrient content of the oceans has increased
dramatically in recent years as a result of fertilizer and other
agricultural run-off, sewage and aquaculture waste.
Nutrients such as nitrogen and phosphorus deplete oxygen
in the water and promote the growth of algae on reefs
(Hughes et al., 2003).

Many coastal development activities, such as
residential, tourist, industrial and port development, involve
land reclamation and dredging which invariably results in
sediment being stirred into the water column.
This reduces light penetration, may directly smother corals
and can damage mangroves. Construction activities inland,
agriculture and deforestation, and poor management also
contribute to increased sediment.

10

Disease

Coral diseases, rarely recorded until the 1970s, have had
a catastrophic effect on reefs, particularly in the
Caribbean, affecting 100 hard and soft coral species in 54
countries. The cause is still largely unknown, although

Sediment plume in Monte Cristi National Park, Dominican Republic.
Inland deforestation is causing sediment run-off on to nearby coral
reefs. As a result, coral cover tends to be low compared with other
less impacted areas.

71°45'W 71°30'W

GHB Mangrove

JF
Protected area
- International boundary
Ses GC Sf

UNEP-WCMC

A W Bruckner

Coral attacked by black-band disease.

both fungi and bacteria have been identified as pathogens
in two cases (Porter, 2001; UNEP-WCMC, 2003). There are
indications that abrasion of massive corals through tourist
activities may make corals more susceptible to disease
(Hawkins et al., 1999).

Climate change

There is now general consensus that extreme storm events
are becoming more frequent, and sea levels and
sea surface temperatures are rising as a result of global
warming. Reefs are already suffering from bleaching events
that have increased significantly since 1975. In the
Caribbean bleaching events are predicted to become an
annual event as current sea surface temperatures are in the
upper temperature threshold for coral survival (Gardner et
al., 2005; Hughes et al., 2003). Tropical storms are forecast
to become even more frequent and/or more intense
(Trenberth, 2005), and this will compound the problem,
causing more damage to both reefs and mangroves and
resulting in shorter recovery times between events (Hughes
et al., 2003).

The change on reefs from coral to algal dominance,
and from framework-building species to non-framework
species, may also compromise their ability to keep pace with
rising sea levels (Bellwood et al., 2004; Gardner et al., 2003).

In the front line

Fishing with dynamite in the Philippines.

Furthermore, by 2100, rates of calcification (the
process by which calcium is formed) on reefs may have
decreased by 17-35 per cent of pre-industrial levels as a
result of high levels of dissolved carbon dioxide in the
oceans [these are now 380 parts per million (ppm),
compared with 280 ppm two centuries ago). This will cause
weakening of coral skeletons and slower growth rates,
making reefs even less effective as breakwaters (Feeley et
al., 2004; Kleypas et al., 1999).

Other threats

Individual tourists, tourist boats and anchors may have only
a minor impact, but over time and in large numbers the
impact becomes significant (Hawkins et al., 1999; Zakai and
Chadwick-Furman, 2002). Spills of oil and toxic chemicals,
and dumping of other wastes, cause localized impacts to
both reefs and mangroves. The introduction of alien species
is a threat to marine ecosystems that is growing rapidly with
increased shipping and susceptibility in systems degraded
by other stresses. Marine plants and animals can be
transported immense distances on the hulls of vessels or in
ballast water. Non-indigenous sessile species have been
introduced to reefs in Guam via ships’ hulls, and other alien
species are spreading on the reefs of Hawaii, outcompeting
native species (Eldredge, 2003).

11

"Thomas Heeger

In the front line

Value of ecosystem services

The Millennium Ecosystem Assessment (Millennium
Ecosystem Assessment, 2005) defines four categories of
ecosystem services:
] provisioning - e.g. food, medicines,
construction materials
4 regulating - e.g. protection of shorelines,
water quality maintenance
Q cultural - e.g. tourism, spiritual beliefs
_] supporting — e.g. maintenance of basic life
support systems.
Coral reefs and mangroves provide benefits under all four
categories.

Reduction of beach erosion

from storm surges and waves

Formation of beaches and islands

Ecosystem services Coral reefs Mangroves
REGULATING Protection of beaches and coastlines Protection of beaches and coastlines from

storm surges, waves and floods
Reduction of beach and soil erosion
Stabilization of land by trapping sediments
Water quality maintenance

Climate regulation

Nursery habitats

PROVISIONING Subsistence and commercial fisheries Subsistence and commercial fisheries
Fish and invertebrates for the Aquaculture
ornamental aquarium trade Honey
Pharmaceutical products Fuelwood
Building materials Building materials
Jewellery and other decoration Traditional medicines
CULTURAL Tourism and recreation Tourism and recreation
Spiritual and aesthetic appreciation Spiritual - sacred sites
SUPPORTING Cycling of nutrients Cycling of nutrients

Nursery habitats

Techniques for valuing ecosystem services are still
relatively new and untested, and the results of such
calculations must be interpreted with care. Putting
a monetary value on an ecosystem, however, can help to
demonstrate why its survival is important (IUCN/TNC/
World Bank, 2004; Turner et al., 2003). Economic values
can be calculated from the cost of the products (e.g. fish]
and services [e.g. tourism) derived from an ecosystem, or
from the cost of replacing a service [e.g. building
seawalls where natural storm protection has been lost).

12

There is, however, no single agreed total value for all
coral reefs or all mangroves, or even for the different
services provided by these ecosystems. Values vary
according to:

(4 The location - e.g. reefs that are major tourist
destinations will have a higher value in terms of
diving and other reef-related activities than
those where tourism has not been developed.

(4 The length of time being considered and
whether a prediction for the future is involved

C Ravilious

(e.g. all reefs are potentially of value for diving

tourism but some may have no value at present).
(1 The ‘beneficiaries’ of the service, since some

people will place a higher value on it than others.
{) The method used and the assumptions made.

Furthermore, it is hard to calculate the economic value
of the aesthetic and ethical benefits of ecosystems, or of
the service some ecosystems provide through cycling
nutrients. Estimates of the ‘total’ economic value of an
ecosystem thus vary considerably and there is a risk
that using this approach underestimates the
ecosystem’s social benefits and overall importance. This
means that it is not always wise to use ecosystem
valuations for policy making and investment decisions
(IUCN/TNC/World Bank, 2004). For example, the
apparent higher value assigned to mangroves than coral
reefs [see Fig. 4) should not be interpreted to mean that
they have a higher management priority. It is also true
that many of the activities that bring benefits, such as
fishing and tourism, also damage reefs and mangroves,
and only careful management will allow the full values
to be materialized.

However, if these limitations are taken into
account, an economic valuation can help to demonstrate
the major role that reefs and mangroves play in the lives
of many people. Studies to date have shown that most
benefit comes from provisioning services [i.e. fisheries
and, for mangroves, timber and fuelwood), cultural
services [tourism] and regulating services {shore
protection).

The total annual economic value of reefs has
been estimated at between US$100 000 and US$600 000
per km? (Cesar et al., 2003; Constanza et al., 1997) and
the value of mangroves even higher, at more
than US$900 000 per km? (Constanza et al., 1997).
Figures are, however, very variable as some national
estimates show:

(4 Sri Lanka's coral reefs have been valued at
between US$140 000 and US$7.5 million per

km* over a period of 20 years (Berg et al., 1998).

“In American Samoa, mangroves, which cover less
than 0.5 km’, have an estimated value

of US$104 000 per km? [total value of about

US$50 million a year) and reefs, which cover 222

km’, are estimated at US$14 300 per km’ (total

value of US$318 million a year) (Spurgeon and

Roxburgh, 2005).

{1 In Thailand, very high values of US$2.7 million

In the front line

Fig. 4: Economic value of the main ecosystem
services of coral reefs (billion US$)

10 -

8

6

4

w
oe a
gx OG re
iS os a O)
= x 2s a2) =
Re GE & &
fea)

Source: Cesar et al., 2003

to US$3.5 million per km? have been calculated
for mangroves (Sathirathai and Barbier, 2001).

Some of the variation can be explained by the location of
the ecosystem. The value of reefs and mangroves for
shore protection (often measured per linear kilometre}
depends on the activities under way or planned along a
particular stretch of coast. In Indonesia, reefs have been
valued as follows (Cesar, 1996):

(4 Reefs adjacent to sparsely populated areas
where agriculture is the main activity: US$829
per km, based on the value of agricultural
production that would be lost if there were no
protection.

OU Reefs adjacent to areas of high population
densities: US$50 000 per km, based on the cost
of replacing housing and roads if coastal
protection were lost.

(1 Reefs in areas where tourism is the main use:
US$1 million per km, based on the cost of
maintaining sandy beaches.

Similar values have been obtained for the Caribbean,
varying from US$2 000 to US$1 million, with the highest
values in areas heavily developed for tourism (Burke and
Maidens, 2004).

There are also several methods for valuing
mangroves. The storm protection value of mangroves in
Sri Lanka (before the tsunami) was put at US$7 700 per
km? a year using a linear value [UNEP/GPA, 2003). A study
in Indonesia, in a different approach, calculated the
erosion control value of mangroves as being equivalent to
S$600 per household per year (Ruitenbeek, 1992).

13

In the front line

Regulating services - shoreline

protection

Although reefs and mangroves form natural barriers
along the coast and thus inevitably provide some
protection to the shore, there is surprisingly little
scientific data to back this up. Most of the evidence is
observational and anecdotal, and relates to normal wave

energy and storms. The calm lagoons inside reefs and
behind mangroves are immediately evident on tropical
coastlines. Fishers use these sheltered waters as
navigation routes and for fishing, particularly during
bad weather or the rough season monsoons. Holiday
makers and tourists benefit from the sheltered waters
for numerous recreational activities. The breakwater
role of reefs is emphasized by the importance accorded
to the channels through them. These allow safe passage
to the lagoon and shore for fishing, navigation and
recreational activities, particularly in bad weather, a
significance recognized by both coastal communities
and port authorities.

Coastal communities are often aware of the
particular protection afforded by mangroves. In India
(Dahdouh-Guebas et al., 2005) and the Philippines
(Walters, 2004), villagers tell of how they have been
protected from cyclones and typhoons in locations where
mangroves are intact, but suffer where mangroves have
been converted to shrimp farms or otherwise lost. In

14

Hotel built behind mangroves, Kenya.

Orissa, India, a powerful cyclone in 1999 and associated
waves caused extensive damage and human mortality,
but communities protected by mangrove belts were less
affected [Mangrove Action Project, 2005]. In Viet Nam,
mangroves have been observed to limit damage from
cyclone waves and tsunamis and are said to have led to
large savings on the costs of maintaining sea dykes (Ha,
2003; Tri et al., 1996).

In southern India, the distinct differences
between the Gulf of Mannar and Palk Bay, caused by the
protection provided by reefs, have led to these seas being
equated with men and women by local villagers. The
former is considered ‘male’ because waves hit the reef
and subside in force before they reach the shore. The
latter is considered ‘female’ because waters are
generally calmer, but, if disturbed by storms, cause
greater damage due to the lack of a reef. Fishing
communities on Pamban, an area lying between the two
seas, still remember the 1964 cyclone that washed away
one village, while those behind reefs survived
(Whittingham et al., 2003). Further north, in Chidambaran
District the shore protection role of mangroves is
recognized by local people where a 113 km’ forest is used

SH Grady

as a sacred grove and is traditionally known in Tamil as
Alaithi Kadukal, which means the forest that controls the
waves’ (WWF, 2005).

Both reefs and mangroves also play a role in the
accretion of coastlines. Reefs produce sand that forms
and replenishes sandy beaches and islands, the sediment
accumulating when corals and other calcified organisms
break down after their death. Mangroves help to stabilize
coastal land, by trapping sediment washed down in rivers
or from more general run-off. Remains of rows of
mangroves planted to stabilize the coast by early
generations of Maoris can still be seen in New Zealand
(Vannucci, 1997).

The role of reefs as breakwaters is also
demonstrated by the many artificial structures that are
being installed for shoreline protection in locations with
no natural reefs. These often have a negative impact, in
terms of creating unwanted longshore drift, but they
nevertheless show how reef-type barriers influence wave
action, even being installed to improve surfing conditions
(Jackson et al., 2002).

Although the general buffering capacity of reefs
and mangroves thus seems obvious, the mechanical
processes involved are complex, and the extent to which
they provide shore protection compared with man-made
barriers and other natural features is not yet fully
understood. Furthermore, the reef and mangrove
ecosystems are themselves damaged by events such as
storms and tsunamis. Hurricanes, for example, can
reduce coral cover significantly [Gardner et al., 2005).
Mangroves can be destroyed or seriously degraded by
hurricanes, through defoliation and uprooting by the
wind, erosion of the shoreline by waves and burial under
sediment. In 1999 Hurricane Mitch destroyed 97 per cent
of the mangroves of Guanaja, one of the Bay Islands in
Honduras [Cahoon and Hensel, 2002). Thus the buffering
capacity of both ecosystems is a balance between their
resilience and their vulnerability, with many factors
involved. A healthy coral reef or mangrove, in the absence
of human impact, acts as a self-repairing breakwater,
with growth in equilibrium with the erosion caused by
waves, storms and other processes.

WIND-GENERATED WAVES AND STORMS

The waves normally seen on the ocean are generated by
wind, and have most of their energy in the surface waters.
The reef flat (the zone of a reef extending seaward across
the lagoon) and the reef crest (the seaward edge of the reef
flat] absorb most of a wave's force, often up to or more than
90 per cent (Brander et al., 2004; Lugo-Fernandez et al.,
1998; Roberts and Suhada, 1983). The greater the width of

In the front line

reef flat between the reef edge and the shore, the more
wave energy is lost. In Egypt, for example, the reef flat and
reef crest of the fringing reef off the tourist resort of
Hurghada dissipate wave energy considerably, protecting
marinas and beaches (Frihy et al., 2004).

S Wells

The lagoon behind the fringing reef here in northern Zanzibar
provides a shallow sheltered area where many activities can be
undertaken.

The amount of energy reduction also depends on
the extent of fragmentation of the reef, as a continuous
reef acts more as a breakwater than a reef that is broken
by channels. The state of the tide and the depth of water
over the reef — at low tide a reef affords more protection —
and whether it ‘plunges’ on to or ‘spills’ over the reef top
also play a role (Gourlay, 1994; Kabdali and Turker, 2002).
Quantifying what the reduction in wave energy may mean
in terms of shore protection is more difficult. !n Sri Lanka,
however, it has been estimated that with current rates of
erosion and assuming that 1 kilometre of reef protects 5
kilometres of shoreline, 1 km* of coral reef can prevent
2 000 m? of erosion a year (Berg et al., 1998).

Mangroves dissipate the energy and size of waves as
a result of the drag forces exerted by their multiple roots and
stems. Wave energy may be reduced by 75
per cent in the wave’s passage through 200 metres
of mangrove {Massel et al., 1999] but, as with coral
reefs, other factors also have an influence, including coastal
profile, water depth and bottom configuration. One study
suggested that a 1.5-km belt of mangrove may be able to
reduce entirely a wave one metre high (Mazda et al., 1997).

15

A Baird

the front line

Large boulder coral washed up on an Aceh beach following the
tsunami of December 2004.

TSUNAMIS

Compared with a wind-generated wave, a tsunami has a
much longer wave length and the wave energy is
distributed throughout the entire water column and is
on a much greater scale. As a tsunami approaches the
shore and water depth decreases, the wave height
increases dramatically as energy is converted to
surface layers, this effect being more pronounced on
gradually shallowing shores {Kowalik, 2004; Mojfeld
et al., 2000). Tsunamis can cause substantial damage
at locations protected from wind-generated waves, as
they tend to accelerate through channels and up inlets,
rapidly increasing in height. They can also be reflected
off obstacles and travel in different directions [Yeh et
al., 1994]. It is thus perhaps not surprising that
the roles of reefs and mangroves as buffers in the

June, 2002 rs

11°27'0"N

Pichavaram
Sanctuary

11°24'0"N

79°43'0"E

2004 tsunami, and
varied considerably.

the damage they received,

Despite initial fears, both ecosystems were less
badly damaged than expected even on reefs in Aceh,
Indonesia, which were within 300 km of the epicentre
(Baird et al., 2005). In Thailand, of 175 reef sites surveyed
on the Andaman coast after the tsunami,
more than 60 per cent had little or no damage; 13 per
cent were seriously damaged, however. Shallow reefs on
wave-exposed islands and shorelines were most
vulnerable, as were the northernmost coast and offshore
islands (Phongsuwan and Brown, in press). At some sites,
differences were even more localized: at Patong Bay,
Phuket, reefs in the south were badly damaged but those
in the north were almost untouched, a pattern that was
reflected in the destruction on land (Edwards, 2005).
Post-tsunami surveys in Thailand and Aceh show
that most damage was in the form of overturning of
poorly attached boulder corals, breakage of branching
corals, and smothering of the reef with sediment (Baird
et al., 2005; Phongsuwan and Brown, in press).
Much greater damage was sustained by reefs directly
affected by the earthquake. Reef flats, with once diverse
coral communities, have been permanently uplifted
above the high water mark in many coastal areas of
Aceh and the Andaman and Nicobar islands {B. Brown,
pers. comm.).

An analysis by UNEP/GRID of more than 50 sites
affected by the tsunami, using pre- and post-satellite
imagery, indicated that there was greater coastal
flooding behind coral reefs (Chatenoux and Peduzzi,
2005), perhaps because channels through the reef
accelerated the flow. The same result was found in Aceh

January, 2005

UNEP-WCMC

Karitturai :
chaverum fo

11°24'0"N

Nadupalaiyam o

Many parts of the coast of Tamil Nadu in India were severely hit by the tsunami. Three villages behind the mangroves in Pitchavaram
Sanctuary survived whereas the two in front were lost (Danielsen et al., 2005; Kathiresan and Narayanasamy, 2005). This could, however,
have been due to the reduced force of the wave, as the continental slope drops to deep waters much more sharply here, compared with areas

further south which suffered greater damage (Wood, 2005].

16

UNEP-WCMC

Mangroves Mangroves

sy *
? ie

In the front line

2004 (Post tsunami)

coastal damage

04-23 4 5’km

The once extensive mangroves around Banda Aceh in Sumatra, Indonesia, an area which suffered devastating damage and loss of life in the
tsunami, had been largely replaced by shrimp farms, covering 360 km* (UNEP, 2005b]). Although loss of mangroves could have contributed to
the destruction, the area was also very close to the epicentre of the tsunami, and thus vulnerable to substantial impact.

(Baird et al., 2005), and studies on the Queensland coast
of Australia have also shown that historically tsunamis
have breached the Great Barrier Reef through passes in
the reef (Knott, 1997).

Some studies have suggested that, in certain
locations, reefs did provide protection. In Sri Lanka, at
Hikkaduwa where the reefs are in a better condition than
many in the country — and are protected in a marine park -
the tsunami caused damage to a distance of only 50 metres
inland and waves were only 2-3 metres high. At Peraliya,
just 3 km to the north but where the reefs have been
extensively affected by coral mining, waves were 10 metres
high, and damage and flooding occurred up to 1.5 km inland
(Fernando et al., 2005, Liu et al., 2005). Detailed analysis of
these areas is still needed, as other factors may also be
involved. Dunes were particularly important in providing
protection in Sri Lanka [Liu et al., 2005).

Initially, there were many observations suggesting
that mangroves both dissipated the force of the tsunami
and caught the debris washed up by it, and thus helped to
reduce damage [|UCN, 2005). In several cases, mangroves
were also instrumental in saving lives by preventing
people caught in the backwash of the wave from being
pulled out to sea. However, as with coral reefs,
subsequent studies showed that the benefit of mangrove
protection was rather variable. In India, bathymetry and
coastal profile were most important in determining the
impact, but less erosion was observed in the Andamans
behind mangroves than where there were no mangroves
(Department of Ocean Development, 2005).

A survey of 24 lagoons and estuaries along the
south-west, south and south-east coasts of Sri Lanka
which suffered the greatest damage showed that where
good quality mangrove communities occurred there was
little destruction to the coast, and the mangroves
themselves were not badly harmed. However, forests
dominated by less typical mangrove species [i.e. those
that had been degraded in the past and were no longer

dominated by genera such as Sonneratia or Rhizophora)
were damaged [Dahdouh-Guebas et al., 2005). It therefore
seems that the ‘quality’ of the mangrove forest contributes
in large measure to its buffering capacity, in addition to its
size and the extent of regrowth if it had previously been
cleared. Tree density may certainly be important: one
study indicated that a 100 metre-wide belt of mangroves,
with trees at a density of 30 per 100 m’, would be sufficient
to reduce the flow pressure from a tsunami by as much as
90 per cent (Hiraishi and Harada, 2003).

Analyses of satellite images of a large number of
tsunami-impacted sites do not show clear correlations
between the presence of mangroves and reduced
shoreline damage (Chatenoux and Peduzzi, 2005; Wood,
2005). In many cases the locations where mangroves have
been reported to have helped protect the shoreline were
out of the main path of the wave, or were adjacent to
deeper water, and thus less susceptible to serious
damage. These findings demonstrate the importance, in
developing predictive models, of carefully analysing every
aspect of a site, both at the broad scale where satellite
imagery can be useful and through detailed field surveys
and on-the-ground studies.

The general picture emerging since the tsunami
is that reefs and mangroves were not the main factor
influencing the extent of damage on the coastline.
Nearshore bathymetry and coastline profile are probably
the key factors determining the force of a wave at any
particular coastal location. Shores adjacent to deep
water tended to be less affected than those next to
shallow sloping shelves, regardless of the presence or
absence of reefs. The shape of the coastline is also
influential, with headlands often providing protection
while bays and inlets act as funnels, restricting and
focusing the force of a wave. More research is required
before it will be possible to predict where, and in what
way, a reef or mangrove will help to reduce the impact of
a tsunami.

17

In the front line

Other ecosystem services

OTHER REGULATING SERVICES

Climate and global carbon cycle

Emissions of carbon dioxide from fossil-fuel combustion and
land-use changes are the leading cause of the build-up of
greenhouse gases. Forests, as well as crops, soil and other
organic matter, take up carbon [carbon sequestration) and
help to reduce the rate of global warming. Mangroves fix and
store significant amounts of carbon (Alongi, 2002) and they
play an important role in carbon sequestration, currently
absorbing an estimated 25.5 x 10° tonnes of carbon a year
(Ong, 1993).

Although reefs play an important role in the carbon
budget, contributing 7-15 per cent of global calcium
carbonate production, they do not help with carbon
sequestration. Sedimentary carbonates, including corals,
coralline algae and the shells of other marine organisms,
are the largest reservoir of carbon on Earth, and so
fluctuations in the global calcium carbonate budget
influence atmospheric carbon dioxide concentration.
However, the chemistry of the system is such that although
the oceans themselves are a ‘sink’ (i.e. they take up carbon
dioxide), reefs are ‘sources’ or net producers of carbon
dioxide, albeit on a small scale in terms of the global carbon
budget, through the process of calcification (Suzuki and
Kawahata, 2004).

Water quality

Mangroves are capable of absorbing pollutants such as
heavy metals and other toxic substances (Lacerda and
Abrao, 1984), as well as nutrients and suspended matter
(Ewel et al., 1998). This makes them natural wastewater
filters, preventing many pollutants from reaching deeper
water (Robertson and Phillips, 1995; Tann and Wong, 1999).

CULTURAL SERVICES

Tourism

Coral reefs add significantly to the value of coastal tourism,
supporting activities such as scuba diving, snorkelling and
glass-bottom boat operations. They also contribute to the
formation of white sandy beaches. Tourism is the world’s
largest industry, with 694 million international tourist
arrivals generating revenues of over US$500 billion in 2003.
The tourism industry is a major employer and source of
foreign exchange and is growing rapidly; it is expected to
reach 1.6 billion arrivals by 2020. Beach-based leisure

18

« cm
ee I Mangrove

ss @ Coral Reef
ra = Dive Centres

S Coordinate System:
(. Geographic

Source: Is
UNEP-WCMC datasets

af
MEXICO 4 (2005)
# t

GUATEMALA 88°wW s6;w HONDURAS

The number of dive operators along the Meso-American Barrier
Reef has increased dramatically in recent years, reflecting the
growth of this leisure activity. In 2000, reef divers - numbering
about 3.6 million - made up 10 per cent of all tourists to the
Caribbean. Divers, however, contributed 17 per cent of tourism
revenue, spending about US$2 100 per trip, compared with
US$1 200 for tourists in general. It has been estimated that in 2000
the net annual benefits from diver tourism in the Caribbean
amounted to US$2.1 billion, with US$625 million being spent
directly on diving on reefs (Burke and Maidens, 2004).

tourism constitutes a large, and possibly the fastest
growing, sector. In Egypt, for example, the tourism sector as
a whole accounts for more than 11 per cent of gross
domestic product (GDP), and coral reefs have been central
to the extremely rapid development of beach-based and
diving tourism in south Sinai since the 1990s; this area now
accounts for some 25 per cent of tourism’s contribution to
national GDP (Jobbins, 2004).

The 2004 tsunami brought home the economic
value of coastal and reef-based tourism, since this is vital to
the economies of the Maldives, Sri Lanka and Thailand. In
Sri Lanka, coastal tourism contributed about US$20 million
a year to the national economy in the mid-1990s (Berg et al.,
1998). A study in 2003 of the reefs of the Phi Phi Islands in
Thailand, subsequently heavily damaged by the tsunami,
valued them at US$624 300/km* a year for tourism and

A mangrove boardwalk for tourists on Wasini Island in southern
Kenya, managed by a local women's group, generates several
thousand dollars a year which are used for maintaining the
boardwalk and for community development activities (IUCN, 2004).

recreation, with a total value of US$205 million a year
(Seenprachawong, 2003). This provides a major incentive
for careful management of the reefs post-tsunami, to
ensure that they recover rapidly and continue to provide
tourism benefit.

Mangroves are not traditionally thought of as tourist
attractions or suitable sites for recreation, but this is
changing fast with the realization that this ecosystem
provides a fascinating educational experience and also
harbours a range of unusual species that can be easily
observed once boardwalks have been installed. Visits to
mangroves and birdwatching tours are now generating
significant revenue for local communities.

PROVISIONING SERVICES

Fisheries and other marine products

Coral reefs and mangroves support numerous different
types of fishery: artisanal, commercial and recreational;
food, curios and souvenirs, bait, and items for decoration;
and fish, lobsters, crabs, molluscs, sea cucumbers and
many other species. However, much of the harvesting of
these species, as well as of species taken for non-food
purposes, is unsustainable, and current economic benefits
may thus be short term.

Of the estimated 30 million small-scale fishers in
the developing world, most are dependent to some extent
on coral reefs for food and livelihood. In the Philippines,
more than 1 million small-scale fishers depend directly on
coral reefs for their livelihood. The productivity of the
fisheries sector (shrimp, lobster, conch and other high-

In the front line

valued species] in Belize, Honduras and Mexico is directly
dependent on the health of the adjacent barrier reef, the
longest in the hemisphere. Sustainable annual catches of
fish from reefs vary from 0.2 to 30 tonnes/km’, with an
average of 5 tonnes/km? (Jennings and Polunin,1995).
Depending on the value of the fish, reef fisheries are thus
potentially worth US$15 000-150 000/km‘’ a year, based on
catch values of US$1-10 per kg [Talbot and Wilkinson, 2001).
Reef fisheries in South-East Asia generate some US$2.4
billion a year (Burke et al., 2002), and in the Caribbean
US$310 million a year (Burke and Maidens, 2004).

There is now a global market for reef species.
Commercial reef fisheries are a major source of
employment and foreign exchange, supplying export
markets and retailers around the world, as well as the
restaurant and hotel industries. The live reef fish trade
supplies restaurants throughout South-East Asia with
products from the Pacific and Indian Oceans (Hughes et al.,
2003). Tuna fisheries, such as those in the Maldives and
Lakshadweep, are often supported by reef-based bait
fisheries, and tuna themselves depend in part on reefs for
their food (Whittingham et al., 2003). Reef-based
recreational fisheries generate over US$100 million
annually (Cesar et al., 2003).

A large proportion of fish and invertebrates in the
aquarium trade comes from coral reefs, shipped to the 1.5-
2 million people in Europe and North America who have
aquaria. Sri Lanka, for example, earns about US$5.6 million
a year exporting reef fish to about 52 countries, an activity
that supports directly and indirectly around 50 000 people.
Large quantities of corals, shells, starfish, pufferfish and
other species are used in the curio trade. Reef-based

Some estimates suggest that reefs contribute up to 25 per cent of
the annual total fish catch in developing countries, providing food
for 1 billion people [Cesar et al., 2003).

19

S Wells

P Scott

In the front line

The high-value, low-volume nature of the aquarium trade means
that it could provide a livelihood for many people if carefully
managed: a kilo of aquarium fish was worth nearly US$500 in 2002,
compared with a kilo of food fish which sold for about US$6
(Wabnitz et al., 2003).

curios provide significant export revenue, but the souvenir
trade is largely unregulated and the benefits from it may be
short term.

Mangroves are important as breeding and nursery
areas for fish and prawns that form the basis of major
fisheries [Bann, 1997; Sasekumar et al., 1992]. Annual
commercial fish harvests from mangroves have been
valued at from US$6 200 per km’ in the United States to
US$60 000 per km’ in Indonesia (Bann, 1997). An estimated
75 per cent of the commercially caught prawns and fish in
Queensland, Australia, depend on mangroves for part of
their lives and on nutrients exported from the mangroves to
other ecosystems (Horst, 1998]. The annual market value of
seafood from mangroves has been put at US$7 500-
167 500/km* [Millennium Ecosystem Assessment, 2005).
With fish catches averaging 1.3-8.8 kg an hour, a 400-km’
managed mangrove forest in Matang, west Malaysia,
supports a fishery worth US$100 million a year
(US$250 000/km‘*/year). Many commercial shrimp fisheries
are dependent on mangrove-fringed coastlines and
estuaries including those in Central America and East
Africa. In the Gulf of Panama, the fisheries for shrimps and
fish generate an estimated US$95 000 per kilometre of
coastline (Talbot and Wilkinson, 2001).

Mangrove forest products

Several mangrove species provide high-quality
commercial timber, used for building and for making
newsprint, matchsticks and matchboxes. Mangroves are

20

also used in large quantities locally for house, boat and
jetty construction. Mangrove timber is particularly
valuable for construction as it is resistant to rot and to the
boring activities of many marine invertebrates. Wood
from several mangrove species has a high calorific value
and is thus of value both directly as fuelwood and as
charcoal. Mangrove wood was used as fuel in many of the
early train engines in India, and it is still widely used in
kilns to make lime [often using live corals from adjacent
reefs). The Matang mangroves in Malaysia provide
forestry products [timber and charcoal) with a value of
US$30 000/km‘/year, and totalling US$10 million a year
(Talbot and Wilkinson, 2001).

Mangroves provide a variety of traditional products.
Tannins from mangroves were used to coat and preserve
wood, nets and other fishing gear, as well as being used as
a dye for cloth. In several countries, mangrove leaves
provide fodder for cattle and goats. Mangrove forests have
long been an important source of honey and beeswax.
Avicennia germinans in Florida in the United States is
particularly valued, as the bees that use this species make
high-quality honey, and large quantities were produced
until the late 1800s when progressive loss of the best
forests led to a decline in production. Honey has been
gathered from mangroves on a subsistence basis in
numerous countries, and, with a renewed interest in this
product, the activity is being developed on a small-scale
commercial basis in many places (Horst, 1998).

Pharmaceuticals

Marine organisms often contain pharmaceutically active
compounds, many of the source species coming from reefs.
Reef organisms have provided an HIV treatment and a
painkiller, while a large part of current cancer drug
research focuses on coral reef species (Millennium
Ecosystem Assessment, 2005]. A study in Indonesia
estimated that mangroves provide a potential net benefit of
US$1 500 per km? (US$15/hectare) for medicinal plants
(Ruitenbeek, 1992].

SUPPORTING SERVICES

The waters around mangroves are generally rich in
nutrients, as a result of the organic matter produced by the
trees and plants themselves, and also from the sediment
that is trapped around the roots. Mangroves produce about
1 kg litter/m? annually, which forms the basis of a complex
food chain and some of which is exported with the tide. As
a result mangroves support an abundant and productive
marine life, and often act as spawning areas, as well as
nursery areas, sheltering juveniles of species that spend
their adult lives in other ecosystems such as coral reefs and
seagrass beds (Mumby et al., 2004).

In the front line

What happens when ecosystem

services are lost?

Just as it is hard to calculate accurately the economic value
of different ecosystems, it is equally difficult to predict the
cost to society of losing their various services. It was thought
that the bleaching event of 1998 in the Indian Ocean would
have a major impact on tourism and fisheries. It was
estimated, for example, that Tanzania would potentially
suffer a direct loss of US$20 million from tourism revenue
(Westmacott et al., 2000a). However, neither sector
underwent the expected decline: tourism fluctuated but
probably more as a result of worldwide political and
economic changes; while fisheries are still in decline largely
because of overexploitation.

Both the 1997 bleaching and the 2004 tsunami were
single, if acute, events, and reefs and mangroves are
expected to recover from damage incurred. A more typical
scenario is of reefs and mangroves undergoing steady
decline. Ecosystems that can no longer provide their full
ecological services have a social and economic ‘cost’ to
humanity, which can be felt in areas or situations many
miles away. Ultimately, therefore, degradation of coral reefs
and mangroves will cause loss of fishing and tourism
revenue and other forms of livelihood, loss of export
earnings, malnutrition due to lack of protein, increased
coastal erosion, and destruction from storms and
catastrophic natural events.

It is predicted that, for example, over a 20-year
period, blast fishing, overfishing and sedimentation in
Indonesia and the Philippines could lead to a net economic
loss of US$2.6 billion and US$2.5 billion respectively for
these two countries (Burke et al., 2002). In the Caribbean,

coral reef degradation continuing through to 2050 could
reduce benefits from fisheries, dive tourism and shore
protection by a predicted total of US$350 million to US$870
million over that period (Burke and Maidens, 2004).

LOSS OF REGULATING SERVICES

The impact of the loss of the protective functions of
coral reefs and mangroves is already being felt in
some countries. Parts of Sri Lanka, India, Indonesia
and the Maldives, where coral mining and collection
has almost eliminated some reefs, have already
seen Serious erosion.

In Sri Lanka, erosion on the south and west coasts
now averages an estimated 40 cm a year, considered to be
partly due to damage to reefs. Some US$30 million has
already been spent on breakwaters and other constructions
to curtail this, and it has been estimated that the cost of
replacing the coastal protection provided by these reefs
would be US$246 000-836 000 per km (Berg et al., 1998). A
hotel in West Lombok, Indonesia, spent an average of
US$125 000 a year over a seven-year period restoring its
250-metre-long beach, which had been eroded largely
because of offshore coral mining [Riopelle, 1995).

Modelling and predictions of the impact of the loss
of natural shore protection provide dire warnings. Modelling
of the changes in wave energy striking some island
shorelines in the Seychelles (Sheppard et al., 2005)
indicates that wave energy has recently doubled as a result
of sea level rise, loss of corals from reef flats due to
bleaching, and changes in reef crest profiles and wave

21

=
S
x
1S)
ly
wy

S Westmacott

In the front line

In the Maldives, a reef flat adjacent to the capital of Male was filled
using coral rubble and causing sedimentation of nearby reefs.
Their degradation was partly responsible for reduced shore
protection and extensive flooding in 1987, which resulted in 20-30
per cent of the new infill being lost. Subsequently, artificial
breakwaters of concrete tetrapods were installed at a cost of
US$10 000 per metre (or US$10 million per kilometre} (Brown,
1997}. Not only was this expensive, but it did not prevent serious
flooding during the tsunami.

regime. The models predict that, over the next decade, it
will double again as a result of further damage to coral
reefs. The consequences of this will depend on the shore’s
composition, but there will almost certainly be increased
erosion on sandy shores.

In the Caribbean, more than 15 000 km of shoreline
could experience a 10-20 per cent reduction in protection
from waves and storms by 2050 as a result of coral reef
degradation (Burke and Maidens, 2004). The economic
costs to Australia from a degraded Great Barrier Reef as a
result of the predicted impact of global warming have been
put at US$2.5 billion to US$6 billion over 19 years [(Hoegh-
Guldberg and Hoegh-Guldberg, 2004).

Loss of mangroves causes saltwater intrusion and
deterioration of groundwater quality, as well as the
disappearance of the filtering mechanism provided by the
roots and the ecological characteristics of this ecosystem.

Mangroves play a sufficiently important role in the
global carbon cycle that it has been estimated that the loss
of 35 per cent of the world’s mangroves [Valiela, 2001) over
the last two decades has resulted in the release of large
quantities of stored carbon, thus further contributing to the
greenhouse effect (Cebrian, 2002).

LOSS OF PROVISIONING SERVICES

The degradation of reefs and mangroves is already having a
major impact on the livelihoods of thousands of coastal

22

communities in the tropics, through loss of earnings and
food security. Both overexploitation and habitat deterioration
(particularly of nursery areas which causes disruptions to
marine productivity) are leading to reduced catches in most
tropical regions. For the Caribbean, it is predicted that, in the
absence of reef degradation, fisheries production in 2015
could be 100 000 tonnes, with a revenue of US$310 million.
However, with the reef degradation that is projected to
occur, production may be 30-45 per cent less [60 000-70 000
tonnes), and revenue only US$140 million (Burke and
Maidens, 2004).

LOSS OF CULTURAL SERVICES

Scuba divers specifically look for coral reefs with rich live
coral, high fish and invertebrate diversity and clear water. In
the long term, degradation of reefs will reduce their value to
the tourist industry. Reefs will provide less interesting diving
and snorkelling, poorer sport fishing and, where erosion has
taken hold, less attractive beaches. For the Caribbean, it is
predicted that, if reefs undergo no further deterioration, net
benefits from scuba diving could grow to US$5.7 billion by
2015. If reef health deteriorates further, however, dive
revenue could amount to only US$5.4-5.6 billion,
representing a future ‘loss’ of 2-5 per cent (Burke and
Maidens, 2004). Already it is widely believed in Florida,
United States (although data are lacking) that the decline in
reef quality is partly responsible for the shift from high-
value, low-volume tourism to budget travellers; this reduces
revenue and potentially, if large numbers are involved,
further contributes to the degradation of the reefs [T.
Agardy, pers. comm.]).

RA Patzner/University of Salzburg

The commercially important rainbow parrotfish Scarus guacamaia
in the Caribbean depends on mangroves as a juvenile but lives on
reefs as an adult. It is far less common on reefs with no adjacent
mangroves, and is one of probably many species that are declining
from loss of habitat as well as overfishing (Mumby, et al., 2004).
Local extinctions have been reported where mangroves have been
cleared, as at Glover's Atoll in Belize (A. Edwards, pers. comm.].

UNEP/Topham

In the front line

Natural recovery - or rehabilitation
and restoration

Although our instinct is to repair or restore something
that has been damaged, there is often an argument for
allowing natural recovery. There are, indeed, many
examples of reefs and mangroves recovering from a
major impact such as a hurricane without human

intervention. Although recovery may seem slow, natural
regeneration increases the likelihood that the ecosystem
will return to what it was before.

The many chronic, long-term impacts now
affecting these ecosystems often slow the rate of
recovery. On reefs, for example, the shift from a coral-
dominated to an algal-dominated ecosystem means that
new coral recruits are quickly outnumbered and those
that settle often have little chance of survival. The focus
now needs to be on removing the causes of this
imbalance, and eliminating stresses in order to
encourage natural recovery of damaged ecosystems
(Edwards and Clark, 1998; Cahoon and Hensel, 2002).

However, there may be certain situations or
conditions when active intervention is necessary or
beneficial, for example where an ecosystem has
particularly high economic value or scientific interest.

Mangrove restoration.

There are two terms in common use: restoration’, which
means that all the key ecological processes and functions
and all the former biodiversity are re-established; and
‘rehabilitation’ which means that most, but not all, are re-
established. Most experience so far with reefs and
mangroves is in terms of rehabilitation.

Mangrove rehabilitation can be relatively simple
since comparatively few species are involved. However,
rehabilitation of reefs is more complex because coral
reproductive biology and growth rates are still poorly
understood, many species are involved and the
techniques are complex and expensive, requiring scuba-
diving and other special equipment and materials. Reef
rehabilitation projects have so far been largely
experimental and have involved only small areas (less
than 100 m’). A careful evaluation of the methods
available must be undertaken to determine feasibility and
cost effectiveness before any attempt at rehabilitation is
made. Research into coral reef restoration is currently
under way through the GEF/World Bank Coral Reef

23

In the front line

Targeted Research and Capacity
Management project (Edwards, 2004).
Reefs and mangroves comprise different comb-
inations of species and occur in a variety of physical
conditions and locations. These factors, combined with the
type and scale of damage suffered, will affect recovery
processes and thus any decisions about rehabilitation.

Building for

CORAL REEFS

Reefs will generally recover provided there is an adequate
supply of larvae of corals, fish and invertebrates, and as
long as chronic disturbances such as sediment, pollution
and overfishing are minimized. Recovery involves two
processes: the settlement of larvae which then develop
into new coral colonies; and growth of the remaining coral
colonies and fragments. Both processes are affected by
the prevailing environmental conditions and by the extent
of the damage. New coral growth and recolonization of
fish populations will start to occur within one to two years
of a damaging event or the end of damaging activities.

Coral larvae require hard surfaces, preferably
coral rock or coralline algae, for settlement, and so
seaweeds, sediment and debris on the seabed will reduce
coral recruitment. However, coral spawning can take
place quite normally after a natural event such as a
hurricane. For example, in Guam, after a typhoon, coral
spawning took place at the normal time and even broken
coral fragments were seen to spawn.

Coral growth rates are highly variable,
depending on the species, the location of the colony on
the reef, the geographical location of the reef and
environmental conditions. Branching corals grow
relatively fast (10-20 cm a year) but are easily broken by
waves and storms. Massive corals grow very slowly (5-
25 mm a year) but may survive for hundreds of years;
colonies more than 1 000 years old have been found.
The reef as a whole grows more slowly than its
individual corals, as it is constantly being eroded, and
upward growth on reef flats is only about 4 mm a year,
while deeper reef thickets grow at about 10 mm a year.
The breakdown of coral skeletons results from either
mechanical damage or from ‘bio-eroders’, which
include sea urchins that graze on fine algae on the
surface of corals and abrade them in the process, and
sponges that bore into corals and weaken their
structure.

The speed of a reef’s recovery from major
damage thus depends on the balance between the
growth of coral colonies and their erosion. Recovery
time is generally a matter of decades (10-50 years) and
is longer on reefs subject to other long-term stresses,
although the process of recovery can start in as little as

24

two years. Natural recovery of mined reefs in the
Maldives has been particularly slow (Clark and
Edwards, 1994]. Reefs in marine parks in eastern
Indonesia, which had previously suffered from long-
term dynamite fishing, show little sign of recovery after
seven years, despite good water quality and larval
recruitment. The vast quantities of broken rubble act as
‘killing fields’ for juvenile corals, abrading or burying
the newly settled recruits (Fox et al., 2003). Reefs that
suffered light damage from the 2004 tsunami in
Thailand are predicted to take only three to five years to
recover; those that received greater damage may take
five to ten years. However, the rates of recovery will
depend on whether the reefs suffer other impacts in the
coming years, particularly bleaching which has
occurred several times in Thailand in the past
(Phongsuwan and Brown, in press).
The main approaches to rehabilitation of coral
reefs are (Westmacott et al., 2000b):
J Increasing the area of substrate for settlement
of coral larvae by installing artificial surfaces,
e.g. concrete blocks, wrecks or other purpose-
designed structures. Stabilizing or removing

A major industry has developed in recent years to build artificial
reefs, such as this ‘Reefballs’ breakwater, to replace the original
natural reefs and create new amenity value, Although the costs of
such structures are decreasing, this approach is expensive, and
not feasible for large areas; most importantly, an artificial
structure such as this will never replace all the ecosystem
services of a natural reef. Before investing in potentially risky
‘engineering’ solutions to reef restoration, it is essential to seek
advice from scientists and other experts.

www.reefball.org

J Harris

Reef restoration projects are under way in many areas, as here in
the Solomon Islands. The tsunami gave fresh impetus to such
projects but they will need careful assessment. Experience to date
suggests they are appropriate only at the scale of tens to at most
hundreds of square metres, for example on reefs damaged by
shipping or used by tourists.

loose or soft substrate, such as coral fragments
and seaweeds, can also help, but this procedure
requires care and expert help. New surfaces
can be created by passing an electric current
through metal to cause deposition of calcium
carbonate (electrolysis). This requires
considerable financial and human investment,
and the long-term impact of the current in the
water is not known.

“I Transplanting coral fragments or colonies from
healthy reefs to damaged reefs or to artificial
substrates. Many species survive transplantation
provided environmental factors are favourable,
but the process requires significant labour, and
transplanted fragments are easily dislodged by
waves and human disturbance, or can easily be
buried or smothered. In addition, there is a risk of
damaging healthy reefs by removing corals from
them. Coral fragments can also be transplanted
to a protected site and ‘grown out [or ‘farmed’] to
a certain size before being used for rehabilitation
(Epstein et al., 2003).

Q ‘Repairing’ the reef: Under some circumstances,
it is possible to cement pieces of reef, or even
coral colonies, together, using glue, special
cements, plastic or other binding agents.

In the front line

MANGROVES

Mangrove regeneration is affected by the patterns of
damage [e.g. broken branches, impact from debris,
sediment disturbance] and by the characteristics of the
area. After storms and impacts such as a tsunami,
sediment scouring leaves inorganic substrates that are
difficult for mangroves to colonize. Sediment turnover may
also expose and/or dump onto existing mangroves material
in which there has been long-term accumulation of heavy
metals, hydrocarbons and other contaminants that inhibit
seedling establishment and survival [Ellison and
Farnsworth, 1996; Cahoon and Hensel, 2002). As with reefs,
for effective recovery it is essential that the causes of the
damage are eliminated. Even when disturbance is reduced,
the altered soil conditions {e.g. increased acidity where
aquaculture was previously carried out) and limited natural
dispersal of many mangrove species mean that natural
recovery can be very slow.

Most mangrove species produce propagules that
are relatively easy to collect and plant and, in the right
conditions, growth is fast. Restoration projects usually
involve the direct planting of propagules (particularly for
Rhizophora spp.) in the recovery area, although
seedlings and saplings can be grown up in advance in
nurseries. The exact technique to be used will depend on
the species involved, whether the soil needs treatment
(for example to reduce acidity) or physical reworking (to
create a suitable grain size], the season, the
developmental stage of the propagules and the
resources available. Replanting is generally most
successful in relatively sheltered areas, but is also
carried out in more exposed areas where the main aim is
control of soil erosion (Stevenson, 1997).

Partly because of the ease with which propagules
can be replanted, many mangrove restoration schemes
have been undertaken, often as a forestry production
initiative. Replanting schemes in Matang, Malaysia (Chan,
1996}, Thailand (Fast and Menasveta, 2003) and East Africa
(Kairo et al., 2001) have been successful, although
rehabilitated mangroves often lack their full biodiversity
and ecological processes (Ellison, 2000). Many of the Asian
countries affected by the 2004 tsunami have embarked on
ambitious replanting programmes which are nevertheless
a first step. Indonesia, for example, has initiated a four-
year operation to plant 150 000 hectares of mangroves
along the coast of Aceh where 300 000 hectares of
mangroves were destroyed. Such programmes will require
careful monitoring and assessment if full restoration is to
be achieved. There is some evidence that greater success
in recovering the biodiversity is achieved when the
replanting is carried out in association with integrated
aquaculture systems (Ellison, 2000).

25

Cancun Travel Online

In the front line

Mangoves and coral reefs on
tropical coastlines of the future

Devastating as they were, the tsunami of December 2004
and recent tropical storms have sent a clear message that
investing in environmentally sound development and
sustainable management of the coastal environment will,
in the long run, be more cost effective than restoring
human lives and ecosystems after a catastrophe. Tsunamis
are relatively rare events compared with hurricanes and
cyclones — fewer than 100 tsunamis were recorded over the
last 300 years in the Indian Ocean [Dahdouh-Guebas et al.,
2005; Department of Ocean Development, 2005) compared
with three tropical cyclones a year (Dahdouh-Guebas et al,
2005). Evidence for the shore protection benefits of coral
reefs and mangroves is currently less for tsunamis than it
is for storms. This, however, does not lessen the urgency -
the devastation recently wrought by hurricanes and
typhoons testifies to the priority that must be accorded to
shore protection measures, of which maintenance of
natural coastal barriers such as reefs and mangroves
must be among the first.

There are no simple management models for
mangroves or reefs. The variability of these ecosystems
means that a good understanding of local characteristics
is essential. In the case of mangroves, even though a
common feature is their regular inundation by the sea, the
extent of this inundation and the tidal regime vary greatly
as do their species composition and the chemical and
microbial characteristics of the soils, all of which affect
their resilience and ability to recover.

MAINTAINING REGULATING SERVICES
Human activities that weaken reefs and make them less
effective breakwaters must be regulated or halted as a

26

matter of urgency, and alternative livelihoods found for
those dependent on the activities that cause damage.
Good coastal planning can considerably reduce
vulnerability to natural disasters, as well as help
safeguard other regulatory services such as water quality
maintenance. Full implementation of the UNEP Global
Programme of Action on Land-based Sources of Pollution
will go a long way towards helping to maintain the
regulating services of reefs and mangroves.

MAINTAINING PROVISIONING SERVICES

The sustainable exploitation of reef and mangrove
fisheries and other resources is a recognized global
priority. There are some success stories, such as the
harvesting of mangrove timber over a 20-30 year rotation
period in Bangladesh, Malaysia and Thailand. Much
greater attention must, however, be paid to fisheries
management. Techniques and approaches are well
developed but often poorly implemented. The FAO Code of
Conduct for Responsible Fisheries enshrines many of
these, including elimination of destructive fishing gear,
establishing no-take areas, and emphasizing the need for
management plans, developed with the full involvement
of fishers and users, that are fully enforced. In Sri Lanka,
where 80-95 per cent of the fishing fleet was destroyed in
areas affected by the 2004 tsunami, there was an
opportunity to introduce measures, such as reduction of
overcapacity, to ensure sustainability. However, in the
rush to provide humanitarian aid, fishing gear and boats
have been distributed in large numbers and without
consideration of the long-term future. This demonstrates
the need for a much greater understanding by the public
and decision makers of the management requirements of
nearshore tropical fisheries.

Thirty years ago, Cancun in Mexico, lying at the top of the great
Meso-American Reef System, was a small fishing village. Since
then, it has grown to a resort that receives more than 3.5 million
visitors annually, on top of its 650 000 residents, and has suffered
considerable environmental problems, particularly in the form of
numerous hurricanes, such as Ivan in 2004 (left) and Emily and
Wilma in 2005. In 2001, Guidelines for Low-Impact Tourism were
produced for the state of Quintana Roo (Molina et al., 2001). These
aim to ensure that further tourism development, particularly in the
Costa Maya to the south of Cancun, will avoid many of the existing
problems, and will contribute to the sustainable development of
this region without increasing its vulnerability.

UNEP.

ATK:
1 Mangrove
Ramsar Site

89°0'E

88°30'E Sajnakhali Sanctuary

__!n the front line

Sundarbans East WS

f0P5520:- 30).-40)) 50) +
— eee KI |

89°30'E 90°0'E

The Sundarbans, lying at the southern end of the Ganges River and straddling the border between India and Bangladesh, is the largest
continuous area of mangrove in the world. The area provides a livelihood for more than 300 000 people, protects them from cyclones and tidal
waves and is an important source of revenue for both countries through commercial timber which is harvested on a 20-year felling cycle. The
total extent - some 6 050 km? (Spalding et al., 1997) - has not changed significantly in the last 25 years, although there are concerns that
forest quality may be declining. The relative success of the Sundarbans Is largely due to its management which has been aimed at taking
advantage of the mangroves’ provisioning and regulatory ecosystem services. It has been managed as a commercially exploited reserved
forest since 1875; wildlife sanctuaries and national parks protect key biodiversity areas, and the area is both a World Heritage and a Ramsar
site. Since the 1970s, the Sundarbans has also been managed as a protective belt against storm damage.

MAINTAINING CULTURAL SERVICES
The vulnerability of the tourism industry to natural events
was made very clear by recent hurricanes as well as the
2004 tsunami. Maintaining the ecosystems on which the
industry depends is thus of paramount importance to
both governments and the private sector. The
International Ecotourism Society (Halfpenny, 2002), the
Convention on Biological Diversity (CBD, 2004), the
Center for Environmental Leadership in Business
(CELB/CORAL/ |HEI/TOI, 2004) and others have produced
guidelines to promote sustainable tourism. Political will
and individual commitment are now needed to ensure
their implementation.

Although many coastal
traditionally valued the ecosystems on which they depend,
much of this understanding has been eroded. The growing

communities have

recognition of the role of communities in the stewardship of
natural resources, and the numerous examples of how this
can be successful, will help to ensure that the cultural
services of reefs and mangroves continue to be valued.

ESSENTIAL MANAGEMENT TOOLS

There is no shortage of guidelines, codes of practice and
information on how to manage reefs and mangroves but
there is there is still a notable lack of commitment to
using and implementing them. The UNEP Regional Seas
Programme is among the organizations trying to reverse
this, by helping countries to work together to protect
these ecosystems, recognizing that success involves
transboundary action, regional co-operation and clear
demonstration of successful approaches (see for example
UNEP 2004). Key management approaches that must be

27

In the front line

promoted include integrated coastal management (ICM),
marine protected areas (MPAs), and improved resilience
and adaptive management.

Integrated coastal management

Coastal development is often ad hoc and based on
numerous unconnected small decisions, or, where plans
exist, may be illegal as a result of poor enforcement of
regulations (Kay and Alder, 2005). National and local ICM
programmes can go a long way to improving coastal
management. The links between impacts on the coast and
watershed management need to be recognized. Plans
should take into account soils, topography and the need to
protect vulnerable ecosystems. Areas needing
rehabilitation must be identified, as well as areas where
construction should be restricted or banned.

In particular, the construction industry must
respect environmental principles [such as set-back
regulations], and ensure that pollution and sedimentation
are minimized through measures such as the use of silt
curtains, and building in the dry rather than the wet
season. Incorporating knowledge of coastal processes
and applying best management practices for beaches,
lagoons, coastal vegetation, energy, sewage treatment,
solid waste and wastewater into planning and
infrastructure are essential. Construction behind reefs
will need particular care, not only to prevent damage to
these ecosystems, but to reduce future shoreline damage
if channels through the reef do indeed increase
vulnerability to flooding. Environmental impact assess-
ment legislation, now in place in most countries, must be
enforced as a matter of urgency.

The ICM approach Is fully recognized in the 12
guiding principles that were drawn up at a meeting in
Cairo in February 2005 by the UNEP Asian Tsunami
Disaster Task Force, in collaboration with the UNEP Co-
ordination Office of the Global Programme of Action for
the Protection of the Marine Environment from Land-
based Activities and other organizations (UK Department
for Environment, Food and Rural Affairs, the Food and
Agriculture Organization of the United Nations, the United
Nations Educational, Scientific and Cultural Organization,
IUCN, and WWF). Known as the Cairo Principles, these are
aimed at helping to ensure environmentally sound post-
tsunami reconstruction programmes, and are being
implemented through an Action Plan (UNEP/GPA, 2005).

THE CAIRO PRINCIPLES
Overarching principle
1 Reduce the vulnerability of coastal comm-
unities to natural hazards by establishing a
regional early warning system and applying

28

construction set-backs, green belts and other
no-build-areas.
Priority technical measures

2 Promote early resettlement with provision for
all basic livelihood needs.

3 Enhance the ability of natural ecosystems to
provide protection by conserving, managing and
restoring wetlands, mangroves, seagrass beds,
and coral reefs, and by seeking alternative
sustainable sources of building materials.

4 Promote design that is cost-effective and
consistent with best practices, favouring soft
engineering solutions to coastal erosion control.

5 Respect traditional access and uses of the
shoreline.

6 Adopt ecosystem-based management measures;
promote sustainable fisheries management;
encourage low-impact aquaculture.

7 Promote sustainable tourism.

How to apply the principles

8 Secure commitments from governments and
international organizations to abide by the
principles.

9 Ensure public participation.

10 Make full use of tools such as strategic
environmental assessment, spatial planning and
environmental impact assessment.

11 Monitor the progress and impact of recon-
struction.

12 Disseminate good practices and lessons learnt
as they emerge.

Marine protected areas

There is growing evidence that reefs within MPAs recover
faster from catastrophes than those that are unprotected.
The abundant fish populations in Hikkaduwa National
Park, Sri Lanka, showed little change as a result of the
2004 tsunami, although unprotected reef sites appear to
have suffered losses (MPA News, 2005]. Reefs in the
Indian Ocean that were well managed or remote from
human impact tended to recover more rapidly from the
1998 bleaching; reefs under anthropogenic stress
recovered poorly, if at all (Wilkinson, 2004).

Many more MPAs are needed. Currently, some 685
protected areas contain mangroves, covering about 9 per
cent of the total area of mangrove (Spalding et al., 1997),
and 660 MPAs contain coral reefs. There is no global
estimate of how much reef is protected (Spalding et al.,
2001), but in the Caribbean an estimated 20 per cent of
reefs lie within MPAs (Burke and Maidens, 2004). Many
MPAs need to be larger and to be made part of carefully
designed networks to ensure that connected ecosystems

T Heeger

Fig. 5: Management effectivenes of Caribbean
MPAs [per cent]

Good
Partial 6%
13%

Inadequate
48%

Unknown
33%

Most marine protected areas urgently need improved
management. Of 285 MPAs assessed in the Caribbean in 2004, only
6 per cent were considered to be effectively managed [Burke and
Maidens, 2004).

Mu Koh Surin National Park in Thailand, gazetted in 1981 and
covering 135 km, is an ICRAN demonstration site and has a good
track record of effective management. The December 2004
tsunami largely destroyed tourism and the park's infrastructure on
the islands, as well as sea gypsy villages, but there were no
fatalities. The coral reefs, which were especially healthy with high
biodiversity before the event [see above], were being surveyed at
the time of the tsunami, permitting first-hand accounts. Trees
were knocked onto the reefs, along with large amounts of
sediment. A survey was carried out two months later and
remarkably little damage had occurred: reefs had an average of 75
per cent live coral cover, and some had 90 per cent, the sediment
had gone, and there were already signs of some coral regeneration
in damaged areas (Comley et al., 2005).

are protected [not only representative sites), as well as
resilient ecosystems, such as reefs identified as resisting
or recovering quickly from bleaching [Grimsditch and
Salm, 2005). This is essential if species dependent on
different ecosystems at different stages of their life cycles
are to be protected, and the full range of ecosystem
services maintained.

In the front line

Improved resilience and adaptive management

Natural disasters have affected humans and the
environment since the beginning of time — but both have
the ability to regenerate and adapt to the impact of such
events and the new circumstances that may arise as a
result of them. This capacity to absorb recurrent
disturbances such as storms and floods is called
‘resilience’.

Already two-thirds of the coastal disasters
recorded each year are associated with extreme weather
events. The growing populations on, and rapid
development of, the coastal zone guarantee that we will
see an increase in economic, social and environmental
damage in the future caused by the associated reduction
in human and ecosystem resilience. The conventional
approach has been to try to reduce the damage and
eliminate change but a new thinking is developing. A far
better approach may be to promote the conditions that
improve resilience and also learn to adapt to the resulting
changes [Adger et al., 2005). Careful planning and
adaptive management can greatly reduce the impact of
large disturbances.

The rapid response of global, regional and
national monitoring programmes to the tsunami
demonstrated their value in providing essential
information for management. Guidelines for Rapid
Assessment and Monitoring of Tsunami Damage to Coral
Reefs were produced within ten days [ICRI/ISRS, 2005)
and disseminated by the UNEP Coral Reef Unit to the
various international and UN agencies conducting
environmental assessments in the region. Expert surveys
were also quickly initiated with assistance from the
Global Coral Reef Monitoring Network (GCRMN) and the
regional Coral Reef Degradation in the Indian Ocean
(CORDIO) programme.

FINANCING THE FUTURE

Reefs and mangroves clearly provide significant benefits
and services to humankind, many of which have a high
economic value. Governments, civil society and the
private sector must recognize that, as with other benefits,
there is a price to be paid for maintaining these
ecosystems. The cost is, however, generally much lower
than the benefit received.

Although costs are hugely variable depending on
the location, size and type of management, average
annual operational management costs of US$775 per km*
have been estimated for MPAs (Balmford et al., 2004).
This is significantly less that the estimated global values
of ecosystems: US$100 000-600 000 per km’ per year in
the case of reefs and possibly more for mangroves. Basic
annual operating costs for MPAs can be as low as

29

In the front line

Fig. 6: Area of the world’s coral reefs and mangroves lying within the waters of countries in relation to those
countries’ position on the UN Human Development Index (left) and their GDP per capita (right) {per cent)

80

Coral reefs
60 Mangroves
40
20
0

Low Medium High
HDI HDI HDI

100
GH Coral reefs

Mangroves

80
60
40

20

< US$ 9 000 > US$ 9 000
per capita GDP per capita GDP

Many of the world’s wealthiest nations have jurisdiction over reefs and mangroves, either in their own coastal waters or in those of their
territories. Over 30 per cent of the world's reefs lie in countries that are classified as highly developed, with a GDP per capita of more than
US$9 000. Australia, France, New Zealand, the United Kingdom and the United States directly influence about 25 per cent of reefs and a
significant proportion of mangroves. Furthermore, most of these countries are either sources of tourists to reef countries or have other
strong economic links with them and potentially could provide much greater financial and technical support. A higher proportion of
mangroves are found in the poorer countries, but nevertheless more than 10 per cent are found in highly developed countries.

US$200 000-600 000, as in the case of Belize and the
Seychelles (Lutchman, 2005).

There are vast untapped sources of funds and
financing mechanisms, ranging from fishery and tourism
revenues and taxes, to royalties and fees from offshore
mining and mineral exploitation, to voluntary donations
and government aid (Spergel and Moye, 2004). Studies

30

have indicated, for example, that tourists are willing to
pay more than US$50 extra per holiday and divers US$25
more per dive if these result in high-quality reefs
(Westmacott et al., 2000a; Burke and Maidens, 2004). It
seems a small price to pay for the future survival of these
small, priceless ecosystems.

A Cornish

In the front line

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33

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In the front line

Shoreline protection and other
ecosystem services
from mangroves and coral reefs

The tragic and devastating consequences of the Asian tsunami, December 2004,
and the hurricanes and cyclones of 2005 were a wake up call for the global
community, dramatically drawing attention to the dangers of undermining the
services that coastal ecosystems provide to humankind.

This report has gathered lessons that have been learnt since these events that
will be relevant to future management of the coasts in the context of severe
weather events and other potential consequences of global warming. More than
ever it is essential to consider the full value of ecosystem services - that is the
benefits that people derive from ecosystems - when making decisions about
coastal development.

The publication aims to help decision and policy makers around the world
understand the importance of coastal habitats to humans, focusing on the role of
coral reefs and mangroves. As well as coastal protection, it also addresses the
huge range of other benefits provided by these ecosystems and the role that they
can play in coastal development and in restoring livelihoods for those suffering
from the effects of extreme events.

www.unep.org
United Nations Environment Programme
P.0. Box 30552, Nairobi, Kenya
Tel: +254 (0) 20 621234
Fax: +254 (0) 20 623927
Email: cpiinfo@ unep.org
Website: www.unep.org

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