Concept of biome and their distribution
Biomes are large regions of earth that have
similar or common vegetation and climatic conditions. They play a crucial role
in sustaining life on Earth. They are defined by their soil, climate, flora and
fauna. Biomes have distinct biological communities that have been formed in
response to a shared physio-chemical climate. Biomes are seen to even spread
across continents. Thus, it can be observed that a biome is a broader term than
habitat. Any biome can comprise a variety of habitats. Factors such as
temperature, light, water availability determine what type of organisms and
adaptations are observed in a biome (Fig. 11.4).
• Location, Geographical position (Latitude,
Longitude)
• Climate and physiochemical environment •• Predominant plant and
animal life
• Boundaries between biomes are not always
sharply defined. Transition or transient zones are seen as in case of grassland
and forest biomes. (Fig. 11.5)
Aquatic Biomes: They occupy about 71% of
the biosphere. The aquatic biome is home to millions of aquatic
organisms like fishes. The climate of coastal zones are influenced by aquatic
bodies. (Fig. 11.6).
·
Freshwater (Lakes, ponds, rivers)
·
Brackish water (Estuaries / Wetlands)
·
Marine (Coral reefs, pelagic zones and abyssal zones)
These are large communities of plants and
animals that occupy a distinct region. They
include grassland, tundra, desert, tropical
rainforest, and deciduous and coniferous forests. Terrestrial biomes are
distinguished
primarily by their
predominant vegetation, and are mainly determined by climate, which in turn,
determines the organisms inhabiting them. These include the keystone species
and indicator species which are unique to their respective biomes. The
terrestrial biomes are a source of food, O2 and act as CO2 sink, apart from the
climate regulatory role. (Fig. 11.7).
Tundra biome, Taiga biome, Grassland biome,
Alpine biome, Forest biome and Desert biome.
• This is the almost treeless plain in the
northern parts of Asia, Europe and North America.
•• Winters are long with little daylight, Summers
are short, with long daylight hours.
• Precipitation is less than 250 mm per year.It
is a zone of permafrost.
• Dwarf willows, birches, mosses, grasses,
sedges are the flora here.
• Reindeer, arctic hare, musk ox, lemmings are
important Tundra herbivores. Some important carnivores are the arctic fox,
arctic wolf, bobcat and snowy owl. Polar bears live along coastal areas.
• Because of the severe winters, many of the
animals are migratory. For example, the many shore birds and waterfowl such as ducks and geese, nest in the Tundra
during the summer and migrate south for the winter.
•Extremely cold climate
•Low biotic diversity
•Simple vegetation structure
•Limitation of drainage
•Short season of growth and reproduction
•Energy and nutrients in the form of dead
organic material
•Large population oscillations
• The Taiga is 1300-1450 km wide zone south of
the Tundra.
• This area has long and cold winters.
• Summer temperature ranges from 10⁰ C to 21⁰ C.
• Precipitation ranges about 380-1000 mm
annually.
• The Taiga is a forest of coniferous trees such
as spruce, fir and pine. This is a major source for the logging industry.
• Important migratory herbivores include moose, elk, deer and
reindeer. Moose and reindeer migrate to the Taiga for winter and to the Tundra
for summers. The common smaller mammals are herbivorous squirrels, snowshoe
hare and predatory pine martens. Important predators include the timber wolf,
grizzly bear, black bear, bobcat and wolverines. (Fig. 11.8).
• Grasslands occur in temperate and in the
tropical regions.
• They have hot summers, cold winters, and
irregular rainfall.
• Often they are characterized by high winds.
• The low irregular rainfall is the factor which
makes the difference between a temperate deciduous forest and a temperate
grassland.
• Herbivores like antelope, bison, wild horse,
jack rabbit, ground squirrel and prairie dogs are abundant.
• Predators include coyotes, foxes, hawks and
snakes.
• In India, fauna of grasslands includes
Elephant, Gaur, Rhino, Antelope.
• Flora of grasslands include purple needle
grass, wild oats, foxtail, ryegrass and buffalo grass (Fig. 11.9).
• The alpine zone (zone between timber line and
snow zone) includes in the descending order, a sub-snow zone immediately below
the snow zone, a meadow zone in the centre and a shrub zone which gradually
merges into the timber zone.
• The snow zone of Himalayas lies over 5100m
above mean sea level and alpine zone exists at a height of 3600m. From an
ecological view point, the zone above the limits of tree growth (timber line)
exhibits extreme environmental conditions which greatly influence the biota of
this region.
• Alpine zone of Himalayas is characterized by
sparseness of animal groups. Many invertebrates of alpine zone are predatory
and occur in lakes, streams and ponds. Among fishes, amphibians and vertebrates
are totally lacking and reptilian fauna is greatly impoverished.
• Flora of alpines includes alpine phacelia,
bear grass, bristlecone pine, moss campion, polylepis forest, pygmy bitterroot,
and wild potato.
Forest is a broad term used to describe areas
where there are a large number of trees (Fig. 11.10). The forest biomes
include a complex assemblage of different kinds of biotic communities. The
major forest biomes are the Tropical forests and the Temperate forests.
Tropical forest
• They occur near the equator
(between latitudes 23.5⁰
at north and 23.5⁰
at south).
• The major characteristic of tropical forests
is their distinct seasons. Only two seasons are present (rainy and dry). Winter
is absent. The length of daylight is about 12 hours and varies little.
• The average annual temperature ranges between
20° C and 25° C.
• Precipitation is evenly distributed throughout
the year with annual rainfall exceeding 2000 mm.
• Soil is nutrient-poor and acidic.
Decomposition is rapid and soils are subject to heavy leaching.
• Tree canopy is multilayered and continuous,
allowing little light penetration.
• Flora is highly diverse: one square kilometer
may contain as many as 100 different tree species. Trees are 25-35 m tall, with
buttressed trunks and shallow roots, mostly evergreen, with large dark green
leaves. Common vegetation are orchids, bromeliads, vines (lianas), ferns,
mosses, and palms.
• They are characterized by the greatest
diversity of fauna which includes birds, bats, small mammals, and insects.
Based on the seasonal distribution of rainfall,
the types of tropical forests are
• Evergreen rainforest: no dry season.
• Seasonal rainforest: short dry period in a
very wet tropical region.
• Semi evergreen forest: longer dry season (the
upper tree storey consists of deciduous trees, while the lower storey is still
evergreen).
• Moist/dry deciduous forest (monsoon): the length of the
dry season increases further as rainfall decreases (all trees are deciduous).
More than half of earth’s tropical forests have already been destroyed.
• These forests occur in eastern North America,
northeastern Asia and western and central Europe
• Have well-defined seasons with a distinct
winter. Moderate climate and a growing season of 140-200 days during 4- 6
frost-free months distinguish temperate forests.
• Annual temperature varies from -30° C to 30°
C.
• Precipitation (750- 1500 mm) is distributed
evenly throughout the year.
• Soil is fertile, enriched with decaying
litter.
• Canopy is moderately dense and allows light to
penetrate, resulting in well-developed and richly diversified understorey
vegetation and stratification of animals.
• Flora is characterized by 3 -4 tree species
per km2. Trees have broad leaves that are lost annually such as oak, hickory,
beech, hemlock, maple, basswood, cottonwood, elm, willow, and spring-flowering
herbs.
• Fauna consists of squirrels, rabbits, skunks,
birds, deer, mountain lion, bobcat, timber wolf, fox, and black bear.
Based on seasonal distribution of rainfall, the
types of temperate forests are
• Moist conifer and evergreen broad-leaved
forests: wet winters and dry summers.
• Dry conifer forests:
dominate higher elevation zones; low precipitation.
• Mediterranean forests: precipitation is concentrated
in winter (<1000 mm /year).
• Temperate coniferous forests : mild winters,
high annual precipitation (> 2000 mm /year).
• Temperate broad-leaved rainforests: mild, frost-free
winters, high precipitation (> 1500 mm/year), evenly distributed throughout
the year.
Only scattered remnants of original temperate
forests remain today.
• Deserts cover about one fifth of the earth's
surface and occur where rainfall is >500 mm/year.
• Rainfall is usually very low and/or
concentrated in short bursts between long rainless periods. Evaporation rates
regularly exceed rainfall rates.
• Soils are course-textured, shallow, rocky or
gravely with good drainage and have no subsurface water. The finer dust and
sand particles are blown elsewhere, leaving heavier pieces behind. Sand dunes
are common.
• Mean annual temperatures range from 20-25° C.
The extreme maximum ranges from 43.5 - 49° C. Minimum temperatures sometimes
drop to -18° C. Based on the temperature range, deserts can be Hot deserts and
Cold deserts.
• Hot deserts such as the Sahara of North Africa
and the deserts of the southwestern U.S., Mexico, Australia and India (Thar
desert) occur at low latitudes.
• Hot deserts have a considerable amount
of specialized vegetation (xerophytes), aloe, agave, Opuntia species,
Euphorbia royleana as well as specialized vertebrate and
invertebrate animals.
• Soils often have abundant nutrients because
they need only water to become very productive and have little or no organic
matter.
• Only animals which can tap available water or
capable of storing sufficient water and withstand the heat can survive in the
desert. The animals include small nocturnal (active at night) carnivores. The
dominant animals are burrowers and have cursorial, fossorial and saltatorial
adaptations.
• The animals stay inactive in protected
hideaways during the hot day and come out to forage at dusk, dawn or at night,
when the desert is cooler.
• The dominant animals of warm deserts are
reptiles and small mammals. The Indian Spiny-tailed
lizard, the blackbuck, the white-footed fox are the common fauna of the Thar deserts. There
are also insects, arachnids and birds (Fig. 11.11).
• Cold deserts are characterized by cold
winters with snowfall and high overall rainfall throughout the winter and
occasionally over the summer.
• They occur in the Antarctic, Greenland and the
Nearctic realm, parts of USA and in parts of western Asia and the Ladakh region
in India.
• They have short, moist, and moderately warm
summers with fairly
long, cold winters. The mean winter
temperature is between -2° C and 4° C and the mean summer temperature is
between 21° C and 26° C.
• Winters receive quite a bit of snow. The mean
annual precipitation ranges from 150-250 mm.
• The soil is heavy, silty and salty.
• Widely distributed animals are jack rabbits,
kangaroo rats, kangaroo mice, pocket mice, grasshopper mice, antelope and
ground squirrels.
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