Chapter-15- LIFE ON THE EARTH
The biosphere includes all the living components of the earth. It consists of all plants and
animals, including all the micro-organisms that live on the planet earth and their
interactions with the surrounding environment.
Most of the organisms exist on the lithosphere and/or the hydrosphere as well as in the
atmosphere. There are also many organisms that move freely from one realm to the other.
Life on the earth is found almost everywhere. Living organisms are found from the
poles to the equator, from the bottom of the sea to several km in the air, from
freezing waters to dry valleys, from under the sea to underground water lying below the
earth’s surface.
ecology
is the study of the earth as a ‘household’, of plants, human beings, animals and microorganisms.
They all live together as interdependent components.
ecology is the study of the earth as a ‘household’, of plants, human beings, animals and
micro-organisms. They all live together as interdependent components.
ecological systems- The interactions of a particular group of organisms with abiotic
factors within a particular habitat resulting in clearly defined energy flows and material cycles
on land, water and air.
Ecological adaptation-
Different types of ecosystems exist with varying ranges of environmental conditions where
various plants and animal species have got adapted through evolution.
Types of Ecosystems-
Terrestrial ecosystem- can be further be classified into ‘biomes’.
1. a biome can be defined as the total assemblage of plant and animal species interacting
within specific conditions. These include rainfall, temperature, humidity and soil
conditions. Some of the major biomes of the world are: forest, grassland, desert and tundra
biomes.
Aquatic ecosystems- can be classed as marine and freshwater ecosystems. Marine ecosystem
includes the oceans, estuaries and coral reefs. Freshwater ecosystem includes lakes,
ponds, streams, marshes and bogs
Structure and Functions of Ecosystems-
The structure of an ecosystem involves a description of the available plant and animal
species.
From a structural point of view, all ecosystems consist of abiotic and biotic
Factors
. Abiotic factors include rainfall, temperature, sunlight, atmospheric humidity, soil
conditions, inorganic substances (carbon dioxide, water, nitrogen, calcium, phosphorus,
potassium, etc.).
Biotic factors include the producers, the consumers (primary, secondary, tertiary) and
the decomposers.
producers include all the green plants, which manufacture their own food through
photosynthesis.
The primary consumers include herbivorous animals like deer, goats, mice and all planteating
animals. The carnivores include all the flesh-eating animals like snakes, tigers and lions.
Certain carnivores that feed also on carnivores are known as top carnivores like hawks and
mongooses.
Decomposers are those that feed on dead organisms (for example, scavengers like
vultures and crows), and further breaking down of the dead matter by other decomposing
agents like bacteria and various micro- organisms.
Two types of food-chains are recognised:
Grazing food-chain, the first level starts with plants as producers and ends with carnivores as
consumers at the last level, with the herbivores being at the intermediate level. There is a loss
of energy at each level which may be through respiration, excretion or decomposition. The
levels involved in a food- chain range between three to five and energy is lost at each level.
A detritus food-chain is based on autotrophs energy capture initiated by grazing animals
and involves the decomposition or breaking down of organic wastes and dead matter
derived from the grazing food-chain.
Types of Biomes- There are five major biomes — forest, desert, grassland, aquatic and altitudinal
biomes
Biogeochemical Cycles
The sun is the basic source of energy on which all life depends. This energy initiates
life processes in the biosphere through photosynthesis, the main source of food
and energy for green plants.
Out of the total solar insolation that reaches the earth’s surface, only a very small
fraction (0.1 per cent) is fixed in photosynthesis
Life on earth consists of a great variety of living organisms. These living organisms
exist and survive in a diversity of associations. Such survival involves the presence of
systemic flows such as flows of energy, water and nutrients.
balance of the chemical elements is maintained by a cyclic passage through the
tissues of plants and animals. The cycle starts by absorbing the chemical elements
by the organism and is returned to the air, water and soil through decomposition.
These cycles are largely energised by solar insolation. These cyclic movements
of chemical elements of the biosphere between the organism and the environment
are referred to as biogeochemical cycles.
.There are two types of biogeochemical cycles : the gaseous and the sedimentary cycle.
In the gaseous cycle, the main reservoir of nutrients is the atmosphere and the ocean.
In the sedimentary cycle, the main reservoir is the soil and the sedimentary and other
rocks of the earth’s crust.
The Water Cycle
All living organisms, the atmosphere and the lithosphere maintain between
them a circulation of water in solid, liquid or gaseous form referred to as the water or
hydrologic cycle
The Carbon Cycle
Carbon basic elements of all living organisms.
The carbon cycle is mainly the conversion of carbon dioxide. This conversion is initiated by
the fixation of carbon dioxide from the atmosphere through photosynthesis.
Such conversion results in the production of carbohydrate, glucose that may be converted to
other organic compounds such as sucrose, starch, cellulose, etc. Here, some of the
carbohydrates are utilised directly by the plant itself.
During this process, more carbon dioxide is generated and is released through its leaves or roots
during the day. The remaining carbohydrates not being utilised by the plant become part of
the plant tissue. Plant tissues are either being eaten by the herbivorous animals or get
decomposed by the micro- organisms.
The herbivores convert some of the consumed carbohydrates into carbon dioxide for release into
the air through respiration.
The micro-organisms decompose the remaining carbohydrates after the animal dies. The
carbohydrates that are decomposed by the micro-organisms then get oxidised into carbon.
The Oxygen Cycle
Oxygen is the main by-product of photosynthesis. It is involved in the oxidation
of carbohydrates with the release of energy, carbon dioxide and water.
The cycling of oxygen is a highly complex process. Oxygen occurs in a number
of chemical forms and combinations. It combines with nitrogen to form nitrates
and with many other minerals and elements to form various oxides such as the iron
oxide, aluminium oxide and others.
Much of oxygen is produced from the decomposition of water molecules by sunlight
during photosynthesis and is released in the atmosphere through transpiration and
respiration processes of plants.
The Nitrogen Cycle
Nitrogen is a major constituent of the atmosphere comprising about seventy-nine
per cent of the atmospheric gases.
It is also an essential constituent of different organic compounds such as the amino
acids, nucleic acids, proteins, vitamins and pigments.
Only a few types of organisms like certain species of soil bacteria and blue green algae
are capable of utilising it directly in its gaseous form.
Generally, nitrogen is usable only after it is fixed. Ninety per cent of fixed nitrogen
is biological.
The principal source of free nitrogen is the action of soil micro-organisms and
associated plant roots on atmospheric nitrogen found in pore spaces of the soil.
Nitrogen can also be fixed in the atmosphere by lightning and cosmic radiation. In the
oceans, some marine animals can fix it.
After atmospheric nitrogen has been fixed into an available form, green plants can
assimilate it.
Herbivorous animals feeding on plants, in turn, consume some of it.
Dead plants and animals, excretion of nitrogenous wastes are converted into
nitrites by the action of bacteria present in the soil.
Some bacteria can even convert nitrites into nitrates that can be used again by green
plants. There are still other types of bacteria capable of converting nitrates into free
nitrogen, a process known as denitrification
Other Mineral C y c l e s
phosphorus, sulphur, calcium and potassium.
They usually occur as salts dissolved in soil water or lakes, streams and seas.
Mineral salts come directly from the earth’s crust by weathering where the soluble
salts enter the water cycle, eventually reaching the sea.
Other salts are returned to the earth’s surface through sedimentation, and after weathering,
they again enter the cycle.
All living organisms fulfill their mineral requirements from mineral solutions in their
environments. Other animals receive their mineral needs from the plants and animals they
consume.
After the death of living organisms, the minerals are returned to the soil and water
through decomposition and flow.
Ecological Balance
Ecological balance is a state of dynamic equilibrium within a community of organisms
in a habitat or ecosystem. It can happen when the diversity of the living organisms remains
relatively stable.
Gradual changes do take place but that happens only through natural succession. It can
also be explained as a stable balance in the numbers of each species in an ecosystem. This
occurs through competition and cooperation between different organisms where population
remains stable.
This balance is brought about by the fact that certain species compete with one another
determined by the environment in which they grow. This balance is also attained by the fact
that some species depend on others for their food and sustenance. Such accounts are
encountered in vast grasslands where the herbivorous animals (deer, zebras, buffaloes, etc.)
are found in plenty. On the other hand, the carnivorous animals (tigers, lions, etc.) that are not
usually in large numbers, hunt and feed on the herbivores, thereby controlling their
population.
In the plants, any disturbance in the native forests such as clearing the forest for shifting
cultivation usually brings about a change in the species distribution.
This change is due to competition where the secondary forest species such as
grasses, bamboos or pines overtakes the native species changing the original forest
structure. This is called succession.
Biomes Subtypes Regions Climatic
Characteristic
Soil Flora and Fauna
Forest A.
1.
2.
B.
C.
Tropical
Equatorial
Deciduou
s
Temperat
e Boreal
A1. 10° N-S
A2. 10°- 25° NS
B. Eastern
North
America,
N.E. Asia,
Western
and Central
Europe
C. Broad belt
of Eurasia
and North
America
(parts of
Siberia,
Alaska,
Canada and
Scandinavia
)
A1. Temp. 20-
25°C,
evenly
distributed A2.
Temp. 25-30°C,
Rainfall, ave.
ann. 1,000mm,
seasonal
B. Temp. 20-30°
C,
Rainfall evenly
distributed 750-
1,500mm,
Well- defined
seasons and
distinct winter.
C. Short moist
moder- ately
warm summers
and long cold
dry winter; very
A1. Acidic,
poor in
nutrients
A2. Rich in
nutrients
B. Fertile, enriched
with
decaying
litter
C. Acidic and
poor in
nutrients,
thin soil
cover
A1. Multi-layered
canopy tall and
large trees
A2. Less dense,
trees of medium
height; many
varieties coexist.
Insects,
bats, birds and
mammals are
common
species in both
B. Moderately
dense broad
leaved trees.
With less
diversity of
plant species.
Oak, Beach,
Maple etc. are
Desert A. some common
B.
C.
D.
Hot and
Dry desert
Semi arid
desert
Coastal
desert
Cold
A.
B.
C.
S a h a r a
, K a l a h a r
i ,
Marusthali
, Rub-el-
Khali
Marginal
A. Temp. 20 -
45°C. B. 21 -
38°C.
C. 15 -
35°C. D. 2
- 25°C
A-D Rainfall is less
Rich in
nutrients with
little or no
organic matter
A-C. Scanty
vege- tation;
few large m a m
m a l s , insects,
reptiles and
birds
D. Rabbits, rats,
Social