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Rapid population increases and changes in lifestyle
have contributed to the degradation of wetland ecosystems due to increased
exploitation of surface and groundwater. In Jordan, groundwater extraction
for urban needs increased from around 2 million m3 in 1979 to around 25
million m3 in 1993 (Fariz and Hatough-Bouran 1998) while an additional
25 million m3 per year was used for irrigated agriculture. As well as
water extraction, pollution and impacts from refugee camps in the area
have led to the deterioration and drying up of the Azraq wetlands natural
reserve (Fariz and Hatough-Bouran 1998). As a consequence tourism in Azraq
has declined. In the eastern part of the Arabian Peninsula, many of the
date palm oases and natural freshwater springs have been lost in the past
two decades (Bundy, Connor and Harrison 1989).
By far the most serious wetland change in West Asia over the past three
decades has occurred in the lower Mesopotamian marshlands, where serial
satellite images confirm a loss of around 90 per cent of the area of lake
and marshlands (UNEP 2001). This loss may be attributable in part to the
large number of dams now present on upstream parts of the Tigris- Euphrates
system, but appears to be primarily a result of major hydrological engineering
works in southern Iraq, notably the completion of the Major Outfall Drain
(or 'Third River') which diverts water to the head of the Gulf. However,
despite some negative impacts of damming on indigenous biodiversity, the
loss of some habitats such as wetlands has been offset by the creation
of large artificial habitats elsewhere in the region. For example, the
630 km2 Assad Lake in Syria on the Euphrates River is considered an important
site for migratory and wintering birds in West Asia.
The rapid decline of the lower Mesopotamian marshlands
represents one of the most significant environmental events to have occurred
globally during the past 30 years. Loss of such an important habitat illustrates
the pressures on wetlands in the region, which are likely to intensify in
future as demand for water continues to increase.
Food self-sufficiency policies in the region have resulted in the cultivation
of marginal lands for irrigated intensive agriculture. This has strained
water resources and caused salinization, with negative effects on freshwater
biodiversity. The breakdown of traditional systems of resource management
has also had a major impact on biodiversity. For example, the traditional
Al-Hema system, which facilitated the sustainable use of rangelands and
other natural resources by setting aside large reserves during times of
stress (Abu-Zinada and Child 1991, Daraz 1985) was abandoned in the 1960s
in the Arabian Peninsula and Mashriq countries. While about 3 000 hema
reserves existed in Saudi Arabia in 1969, only 71 were still in existence
under various degrees of protection in 1984 and only nine were on the
1997 Protected Areas list (WCPA 2000).
Coastal and marine biodiversity is threatened by several human activities
including pollution (oil spills, industrial and domestic discharges into
the sea), physical alteration of habitats (sand dredging and landfills),
climate variability and alien species introduced by ballast water (ROPME
1999, UNEP/MAP 1999). The extent of mangroves has been decreasing along
the shores of the Gulf over the past 30 years due to unplanned coastal
development to the extent that only 125-130 km2 of mangrove patches remain.
In Saudi Arabia, more than 40 per cent of the Gulf coastline has been
reclaimed and almost 50 per cent of the mangroves lost (Sheppard, Price
and Roberts 1992). In the Arabian Peninsula seas, about 20 000 km2 of
coral reefs or 7.9 per cent of the total area of world corals have been
exposed to bleaching due to increases in sea water temperature caused
by El Niņo (UNDP, UNEP, World Bank and WRI 2000). It is feared that global
warming will intensify this phenomenon. In the Mashriq sub-region many
marine species, including Mediterranean monk seals, marine turtles and
marine sponges, are threatened by the continuous deterioration of coastal
water quality due to sedimentation, nutrient discharge and eutrophication
(Lakkis 1996, Tohme 1996).
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