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Natural vegetation expresses the whole environment (climate,
topography, geology and soil) and hence studies of vegetation
composition leading to production of flora can form
a basis for land use. In contrast to the area, Pakistan
has a very diverse flora including roughly 6,000 plant
species of flowering plants.
Climate and
Topography
The type of the flora of Pakistan as a rule depends
on the climate, soil and topography which incessantly
varies as one travels from sea level to the Northern
Pakistan. On the basis of temperature, Pakistan is roughly
divided into following four zones:
1. Tropical very hot and winterless.
2. Subtropical hot with a cool winter.
3. Temperate with a warm summer and a
pronounced winter.
4. Arctic with a short summer and long
severe winter.
The mean annual temperature of Pakistan exceeds 25°C
over the whole country with the exception of hilly areas.
The diurnal range of temperature does not appear to
have a significant effect on vegetation provided tolerable
limits are not over-stepped. High diurnal ranges of
temperature are found in the central Indus plains and
parts of Quetta and Kalat Divisions. The highest mean
annual diurnal range of 4°C has been recorded for
Kalat. The annual diurnal range is usually below —9.5°C
in the Himalayan areas.
Rainfall
The mean annual rainfall ranges from less than 50 mm
to 125 mm in Pakistan. The variation in annual rainfall
from year to year is an important factor for plant growth.
It is apparent over most of Pakistan that the length
of dry season determines the type of vegetation found.
Except for a small area which is humid and perhumid
(1.5%) and a little larger area (8.5%) in the submontane
region which is dry, subhumid and wet, the rest of Pakistan
is arid (72%) and semi-arid (18%).
Topography
Few countries have such a diversity of the terrain
as found in Pakistan. It stretches from the Arabian
Sea on the west to the wild of Tibet in Central Asia.
Beginning at the sea level the country rises to 8,611
m. at K-2 in the Karakoram mountains, the second highest
peak in the world. Large alluvial plains are the creation
of the river Indus. A large area of Pakistan was desert
and this untamed land came under cultivation by a well-established
canal system, but as a result some of the land has become
waterlogged. The waterlogging accompanied by alkalinity
and salinity poses a serious problem in those areas.
Floristic Regions
As a result of diversity in the climate and the terrain
a number of distinct floristic elements are found in
Pakistan. However, Pakistan can be divided into four
floristic regions: the first floristic region is called
as Saharo-Sindian or Sudanian region. The flora of this
region is predominantly tropical or subtropical type
and, in fact, an extension of North African desert,
Sahara. In
Pakistan this Saharo-Sindian flora stretches from
the desert of Sind, Punjab deserts in the coastal plains
and southern Baluchistan, foothills in NWFP and even
penetrates the Himalayan range along the river Indus.
Floristically this region is of great interest. The
most distinctive is the flora of the tidal swamps found
along the coast of Sind and Baluchistan. This is dominated
by various species of mangroves viz. Avicennia marina,
Aegiceras corniculata and Rhizophora and Ceriops species.
Pakistan this Saharo-Sindian flora stretches from
the desert of Sind, Punjab deserts in the coastal plains
and southern Baluchistan, foothills in NWFP and even
penetrates the Himalayan range along the river Indus.
Floristically this region is of great interest. The
most distinctive is the flora of the tidal swamps found
along the coast of Sind and Baluchistan. This is dominated
by various species of mangroves viz. Avicennia marina,
Aegiceras corniculata and Rhizophora and Ceriops species.
The second floral region in Pakistan is usually called
as Irano-Turanian region. It includes northern Baluchistan
and upper Waziristan, on one side, and the portion of
upper Hazara, Chitral, Gilgit, portion of Baltistan
in the northern regions of Pakistan, on the other.
The most interesting and distinctive flora in Baluchistan
of Irano-Turanian region is called the “juniper
tracts”. Under this head may be included the vegetation
from 2,000 to 3,000 m. and embraces the country around
Ziarat, the Pu range and the Zarghun range near Quetta.
The flora of Gilgit, upper Hazara, upper Chitral, Astor
and Skardu in the eastern Irano-Turanian subregion is
very interesting. The areas are drier and less tropical.
Due to the diversity in local topography and climate,
particularly of rainfall, the flora varies from place
to place.
The third and perhaps the most interesting region is
called as Sino-Japanese region. The territory of this
region in Pakistan is narrow and lies between 33°
-35°NL. Part of Kashmir, upper Murree hills, parts
of Hazara and Chitral are included in it.
The last and the smallest region of our flora is known
as the South Asian region. In Pakistan, the territory
of this region lies in the extreme southeast part and
lies between 27° —28° NL and includes
Nagar Parker and the area of Rann of Kuch. The flora
of Nagar Parker is quite different from its adjoining
areas due to its higher rainfall. The average annual
rainfall is as high as 24”. Flora is dominated
by mostly Saharo-Sindian elements.

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