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ECOSYSTEM 
Created by: 
Kush Sehgal 
Class XII science 
Roll number : 29 
Session: 2014- 
2015
What Is 
Ecosystem 
An ecosystem is a community 
of living organisms (plants, 
animals and microbes) in 
conjunction with the nonliving 
components of their environment 
(things like air, water and 
mineral soil), interacting as a 
system.
Niche v/s habitat 
Habitat: 
The natural home or 
environment of an animal, 
plant, or other organism. 
Niche: 
A role taken by a type of 
organism within its 
community.
Biotic Factors 
Biotic components 
These are the living things that shape an ecosystem. 
A biotic factor is any living component that affects another organisms, 
including animals that consume the organism in question, and the living food that the 
organism consumes. 
Example : 
a fresh water 
ecosystem 
showing prey 
and a predator
More About Biotic 
Components 
Biotic components are contrasted to abiotic components, which are non-living 
components of an organism's environment, such as temperature, 
light, moisture, air currents, etc. Biotic components usually include:
Abiotic factors 
In biology and ecology, abiotic components include physical conditions and non-living 
resources that affect living organisms in terms of growth, maintenance, 
and reproduction. Resources are distinguished as substances or objects in the 
environment required by one organism and consumed or otherwise made unavailable 
for use by other organisms. 
Component degradation of a substance by chemical or physical processes, 
e.g. hydrolysis. All non-living components of an ecosystem is called abiotic 
components.
productivity 
I n ecology, pr oduct ivit y or pr oduct ion r ef er s t o 
t he r at e of gener at ion of biomass in an ecosyst em. 
I t is usually expr essed in unit s of mass per unit 
sur f ace (or volume) per unit t ime, f or 
inst ance gr ams per squar e met r e per day (g m-2 d-1). 
The mass unit may r elat e t o dr y mat t er or t o t he 
mass of car bon gener at ed. Pr oduct ivit y 
of aut ot r ophs such as plant s is called pr imar y 
pr oduct ivit y, while t hat of het er ot r ophs such 
as animals is called secondar y pr oduct ivit y.
Producers, Consumers and 
Decomposers 
Pr oducer s, i.e. aut ot r ophs: e.g. plant s, t hey 
conver t t he ener gy [f r om phot osynt hesis (t he 
t r ansf er of sunlight , wat er , and car bon dioxide int o 
ener gy), or ot her sour ces such as hydr ot hermal 
vent s] int o f ood. 
Consumer s, i.e. het er ot r ophs: e.g. animals, t hey 
depend upon pr oducer s (occasionally ot her 
consumer s) f or f ood. 
Decomposer s, i.e. det r it ivor es: 
e.g. f ungi and bact er ia, t hey br eak down chemicals 
f r om pr oducer s and consumer s (usually dead) int o
ENERGY FLOW 
Food chain 
A linear sequence of links in a food web starting from species that are called 
producers in the web and ends at species that are called decomposers in the web. A 
food chain also shows how the organisms are related with each other by the food 
they eat. A food chain differs from a food web, because the 
complex polyphagous network of feeding relations are aggregated into tropic species 
and the chain only follows linear monophagous pathways.
Types of food chain 
Grazing food chain - The gr azing f ood chain begins 
wit h t he phot osynt het ic f ixat ion of light , car bon 
dioxide, and wat er by plant s (pr imar y pr oducer s) 
who pr oduce sugar s and ot her or ganic molecules. 
Once pr oduced, t hese compounds can be used t o 
cr eat e t he var ious t ypes of plant t issues. Pr imar y 
consumer s or her bivor es f orm t he second link in 
t he gr azing f ood chain. 
Detrital food chain - The det r it us f ood chain 
dif f er s f r om t he gr azing f ood chain in sever al 
ways:t he or ganisms making it up ar e gener ally 
smaller (like algae, bact er ia, f ungi, insect s, &
Ecological succession 
Ecological 
succession is the 
observed process of 
change in 
the species structu 
re of an ecological 
community over time. 
The time scale can 
be decades (for 
example, after a 
wildfire), or even
Primary succession is one of two types of 
biological and ecological succession of plant 
life, occurring in an environment in which new 
substrate devoid of vegetation and usually 
lacking soil, such as a lava flow or area left 
from retreated glacier, is deposited.
Secondary succession is one of the two types 
of ecological succession of plant life. As opposed to 
the first, primary succession, secondary succession is 
a process started by an event that reduces an already 
established ecosystem to a smaller population of 
species.
Nutrient cycle 
A nut r ient cycle (or ecological r ecycling) is t he 
movement and exchange of or ganic 
and inor ganic mat t er back int o t he pr oduct ion of 
living mat t er . The pr ocess is r egulat ed by f ood 
web pat hways t hat decompose mat t er int ominer al 
nut r ient s. Nut r ient cycles occur wit hin ecosyst ems. 
Ecosyst ems ar e int er connect ed syst ems wher e 
mat t er and ener gy f lows and is exchanged as 
or ganisms f eed, digest , and migr at e about . Miner als 
and nut r ient s accumulat e in var ied densit ies and 
uneven conf igur at ions acr oss t he planet . 
Ecosyst ems r ecycle locally, conver t ing miner al 
nut r ient s int o t he pr oduct ion of biomass, and on a
C a r b o n c y 
The car bon cycle is ct h le e 
biogeochemical cycle by which car bon is 
exchanged among t he biospher e, 
pedospher e, geospher e, hydr ospher e, 
and atmospher e of t he Ear t h. 
The global carbon budget is t he balance of t he 
exchanges (incomes and losses) of 
car bon bet ween t he car bon r eser voir s 
or bet ween one specif ic loop (e.g., 
atmospher e ↔ biospher e) of t he car bon 
cycle. An examinat ion of t he car bon
Phosphorus cycle 
The phosphorus cycle is the biogeochemical cycle that describes the 
movement of phosphorus through the lithosphere, hydrosphere, 
and biosphere. Unlike many other biogeochemical cycles, 
the atmosphere does not play a significant role in the movement of 
phosphorus, because phosphorus and phosphorus-based compounds are 
usually solids at the typical ranges of temperature and pressure found on 
Earth. The production of phosphine gas occurs only in specialized, local 
conditions. 
On the land, phosphorus (chemical symbol, P) gradually becomes less 
available to plants over thousands of years, because it is slowly lost in 
runoff. Low concentration of P in soils reduces plant growth, and slows soil 
microbial growth - as shown in studies of soil microbial biomass
Ecosystem | class 12 | cbse

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Ecosystem | class 12 | cbse

  • 1. ECOSYSTEM Created by: Kush Sehgal Class XII science Roll number : 29 Session: 2014- 2015
  • 2. What Is Ecosystem An ecosystem is a community of living organisms (plants, animals and microbes) in conjunction with the nonliving components of their environment (things like air, water and mineral soil), interacting as a system.
  • 3. Niche v/s habitat Habitat: The natural home or environment of an animal, plant, or other organism. Niche: A role taken by a type of organism within its community.
  • 4.
  • 5. Biotic Factors Biotic components These are the living things that shape an ecosystem. A biotic factor is any living component that affects another organisms, including animals that consume the organism in question, and the living food that the organism consumes. Example : a fresh water ecosystem showing prey and a predator
  • 6. More About Biotic Components Biotic components are contrasted to abiotic components, which are non-living components of an organism's environment, such as temperature, light, moisture, air currents, etc. Biotic components usually include:
  • 7. Abiotic factors In biology and ecology, abiotic components include physical conditions and non-living resources that affect living organisms in terms of growth, maintenance, and reproduction. Resources are distinguished as substances or objects in the environment required by one organism and consumed or otherwise made unavailable for use by other organisms. Component degradation of a substance by chemical or physical processes, e.g. hydrolysis. All non-living components of an ecosystem is called abiotic components.
  • 8.
  • 9.
  • 10. productivity I n ecology, pr oduct ivit y or pr oduct ion r ef er s t o t he r at e of gener at ion of biomass in an ecosyst em. I t is usually expr essed in unit s of mass per unit sur f ace (or volume) per unit t ime, f or inst ance gr ams per squar e met r e per day (g m-2 d-1). The mass unit may r elat e t o dr y mat t er or t o t he mass of car bon gener at ed. Pr oduct ivit y of aut ot r ophs such as plant s is called pr imar y pr oduct ivit y, while t hat of het er ot r ophs such as animals is called secondar y pr oduct ivit y.
  • 11. Producers, Consumers and Decomposers Pr oducer s, i.e. aut ot r ophs: e.g. plant s, t hey conver t t he ener gy [f r om phot osynt hesis (t he t r ansf er of sunlight , wat er , and car bon dioxide int o ener gy), or ot her sour ces such as hydr ot hermal vent s] int o f ood. Consumer s, i.e. het er ot r ophs: e.g. animals, t hey depend upon pr oducer s (occasionally ot her consumer s) f or f ood. Decomposer s, i.e. det r it ivor es: e.g. f ungi and bact er ia, t hey br eak down chemicals f r om pr oducer s and consumer s (usually dead) int o
  • 12.
  • 13. ENERGY FLOW Food chain A linear sequence of links in a food web starting from species that are called producers in the web and ends at species that are called decomposers in the web. A food chain also shows how the organisms are related with each other by the food they eat. A food chain differs from a food web, because the complex polyphagous network of feeding relations are aggregated into tropic species and the chain only follows linear monophagous pathways.
  • 14. Types of food chain Grazing food chain - The gr azing f ood chain begins wit h t he phot osynt het ic f ixat ion of light , car bon dioxide, and wat er by plant s (pr imar y pr oducer s) who pr oduce sugar s and ot her or ganic molecules. Once pr oduced, t hese compounds can be used t o cr eat e t he var ious t ypes of plant t issues. Pr imar y consumer s or her bivor es f orm t he second link in t he gr azing f ood chain. Detrital food chain - The det r it us f ood chain dif f er s f r om t he gr azing f ood chain in sever al ways:t he or ganisms making it up ar e gener ally smaller (like algae, bact er ia, f ungi, insect s, &
  • 15.
  • 16. Ecological succession Ecological succession is the observed process of change in the species structu re of an ecological community over time. The time scale can be decades (for example, after a wildfire), or even
  • 17. Primary succession is one of two types of biological and ecological succession of plant life, occurring in an environment in which new substrate devoid of vegetation and usually lacking soil, such as a lava flow or area left from retreated glacier, is deposited.
  • 18.
  • 19. Secondary succession is one of the two types of ecological succession of plant life. As opposed to the first, primary succession, secondary succession is a process started by an event that reduces an already established ecosystem to a smaller population of species.
  • 20.
  • 21. Nutrient cycle A nut r ient cycle (or ecological r ecycling) is t he movement and exchange of or ganic and inor ganic mat t er back int o t he pr oduct ion of living mat t er . The pr ocess is r egulat ed by f ood web pat hways t hat decompose mat t er int ominer al nut r ient s. Nut r ient cycles occur wit hin ecosyst ems. Ecosyst ems ar e int er connect ed syst ems wher e mat t er and ener gy f lows and is exchanged as or ganisms f eed, digest , and migr at e about . Miner als and nut r ient s accumulat e in var ied densit ies and uneven conf igur at ions acr oss t he planet . Ecosyst ems r ecycle locally, conver t ing miner al nut r ient s int o t he pr oduct ion of biomass, and on a
  • 22. C a r b o n c y The car bon cycle is ct h le e biogeochemical cycle by which car bon is exchanged among t he biospher e, pedospher e, geospher e, hydr ospher e, and atmospher e of t he Ear t h. The global carbon budget is t he balance of t he exchanges (incomes and losses) of car bon bet ween t he car bon r eser voir s or bet ween one specif ic loop (e.g., atmospher e ↔ biospher e) of t he car bon cycle. An examinat ion of t he car bon
  • 23.
  • 24. Phosphorus cycle The phosphorus cycle is the biogeochemical cycle that describes the movement of phosphorus through the lithosphere, hydrosphere, and biosphere. Unlike many other biogeochemical cycles, the atmosphere does not play a significant role in the movement of phosphorus, because phosphorus and phosphorus-based compounds are usually solids at the typical ranges of temperature and pressure found on Earth. The production of phosphine gas occurs only in specialized, local conditions. On the land, phosphorus (chemical symbol, P) gradually becomes less available to plants over thousands of years, because it is slowly lost in runoff. Low concentration of P in soils reduces plant growth, and slows soil microbial growth - as shown in studies of soil microbial biomass