IB DP Biology Topic 4: 4.3 Carbon cycling: Study Notes

4.3  Carbon Cycling

Essential Idea:
Continued availability of carbon in ecosystems depends on carbon cycling

Understandings:

  • Autotrophs convert carbon dioxide into carbohydrates and other carbon compounds
  • In aquatic ecosystems carbon is present as dissolved carbon dioxide and hydrogen carbonate ions
  • Carbon dioxide diffuses from the atmosphere or water into autotrophs
  • Carbon dioxide is produced by respiration and diffuses out of organisms into water or the atmosphere
  • Methane is produced from organic matter in anaerobic conditions by methanogenic archaeans and some diffuses into the atmosphere or accumulates in the ground
  • Methane is oxidised to carbon dioxide and water in the atmosphere
  • Peat forms when organic matter is not fully decomposed because of acidic and/or anaerobic conditions in waterlogged soils
  • Partially decomposed organic matter from past geological eras was converted into either coal or into oil and gas that accumulates in porous rocks
  • Carbon dioxide is produced by the combustion of biomass and fossilised organic matter
  • Animals such as reef-building corals and mollusca have hard parts that are composed of calcium carbonate and can become fossilised in limestone

Applications:

  • Estimation of carbon fluxes due to processes in the carbon cycle
  • Analysis of data from air monitoring stations to explain annual fluctuations

Skills:

  • Construct a diagram of the carbon cycle
4.3.U1  Autotrophs convert carbon dioxide into carbohydrates and other carbon compounds.
  • State the role of photosynthesis in the carbon cycle.
4.3.U2  In aquatic ecosystems carbon is present as dissolved carbon dioxide and hydrogen carbonate ions.
  • Outline the process that converts CO2 to hydrogen carbonate ion in water, leading to a reduction of the pH in the water.
4.3.U3  Carbon dioxide diffuses from the atmosphere or water into autotrophs.
  • State that in diffusion, molecules move from an area of higher concentration to an area of lower concentration. 
4.3.U4  Carbon dioxide is produced by respiration and diffuses out of organisms into water or the atmosphere.
  • ​State that carbon dioxide is a waste product of aerobic cellular respiration.​
  • State that carbon dioxide diffuses out of cells into the atmosphere or water.
4.3.U5  Methane is produced from organic matter in anaerobic conditions by methanogenic archaeans and some diffuses into the atmosphere or accumulates in the ground.
  • Outline the role of methanogenic archaea in the transformation of organic material into methane.
4.3.U6  Methane is oxidized to carbon dioxide and water in the atmosphere.
  • State that methane is oxidized to carbon dioxide in the atmosphere.
4.3.U7  Peat forms when organic matter is not fully decomposed because of acidic and/or anaerobic conditions in waterlogged soils.
  • Define peat.
  • Outline formation of peat.
4.3.U8  Partially decomposed organic matter from past geological eras was converted either into coal or into oil and gas that accumulate in porous rocks.​
  • Outline formation of coal.
  • Outline formation of oil and natural gas.
4.3.U9  Carbon dioxide is produced by combustion of biomass and fossilized organic matter.
  • Define combustion.
  • State the products of a combustion reaction.
  • State sources of fuel for a combustion reaction. ​​
4.3.U10  Animals such as reef-building corals and Mollusca have hard parts that are composed of calcium carbonate and can become fossilized in limestone.
  • State that hard shells, such as in mollusk and coral, are made of calcium carbonate.
4.3.A1  Estimation of carbon fluxes due to processes in the carbon cycle.
  • List seven flux processes in the carbon cycle.
  • State the unit of measure for carbon flux values.  ​
4.3.A2  Analysis of data from air monitoring stations to explain annual fluctuations.​
  • Sketch a graph of the annual fluctuation in atmospheric carbon dioxide concentration.
  • Explain the annual fluctuation in atmospheric carbon dioxide concentration in the northern hemisphere.
4.3.S1  Construct a diagram of the carbon cycle.
  • Draw a diagram of the terrestrial carbon cycle.
  • Draw a diagram of the aquatic carbon cycle.
  • Define pool and flux.
4.3.NOS  Making accurate, quantitative measurements-it is important to obtain reliable data on the concentrations of carbon dioxide and methane in the atmosphere.​
  • Explain why accurate measurements of CO2 and methane in the atmosphere are important.
  • Outline how data on concentration of atmospheric CO2 and methane are collected.

​4.3 carbon cycle

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In the Carbon Cycle we will look at how carbon is one of the most important elements that are recycled in an ecosystem. We will see how Inorganic carbon dioxide in the atmosphere is trapped or fixed as organic carbon compounds during photosynthesis.

​This unit will last 3 days


​Essential idea:

  • Continued availability of carbon in ecosystems depends on carbon cycling.

Nature of science:

  • Making accurate, quantitative measurements—it is important to obtain reliable data on the concentration of carbon dioxide and methane in the atmosphere. (3.1)
    • Explain why accurate measurements of CO2 and methane in the atmosphere are important.
    • Outline how data on concentration of atmospheric CO2 and methane are collected.
Understanding

4.3.U1 Autotrophs convert carbon dioxide into carbohydrates and other carbon compounds

  • State the role of photosynthesis in the carbon cycle.​
Autotrophs absorb carbon dioxide from the atmosphere and convert it into carbohydrates, lipids, and all the other carbon compounds that they require. This has the effect of reducing the carbon dioxide concentration of the atmosphere

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4.3.U2 ​In aquatic ecosystems carbon is present as dissolved carbon dioxide and hydrogencarbonate ions.

  • Outline the process that converts CO2 to hydrogen carbonate ion in water, leading to a reduction of the pH in the water.

Carbon dioxide dissolves in water and some of it will remain as a dissolved gas, however the remainder will combine with water to form carbonic acid  (CO2 + H2O  ⇄  H2CO3)​

  • Carbon dioxide is soluble in water – can remain in water as dissolved gas or can combine with water to form carbonic acid (H2CO3)
    • Carbonic acid can dissociate to form hydrogen and hydrogen carbonate ions (H+ and HCO3-) -> explains how CO2 can reduce the pH of water
  • Dissolved CO2 and hydrogen carbonate ions are absorbed by aquatic plants / other autotrophs that live in water
    • Use them to make carbohydrates and other carbon compounds

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4.3.U3 ​Carbon dioxide diffuses from the atmosphere or water into autotrophs.

  • State that in diffusion, molecules move from an area of higher concentration to an area of lower concentration.

Autotrophs, such as all plants and algae, convert inorganic carbon dioxide into organic compounds via photosynthesis. These organic compounds include the carbohydrates, lipids and proteins required by the organism for survival​A

Autotrophs use CO2 in the production of carbon compounds by photosynthesis or other processes. – Reduces the concentration of CO2 inside autotrophs and sets up a concentration gradient between cells in autotrophs and the air/water around

  • CO2 diffuses from the atmosphere or water into autotrophs
  • In land plants – occurs in the stomata in the underside of leaves
  • Aquatic plants – entire surface of leaves / stems usually permeable to CO2 (diffusion can be through any part of the plant)

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4.3.U4 Carbon dioxide is produced by respiration and diffuses out of organisms into water or the atmosphere

  • State that carbon dioxide is a waste product of aerobic cellular respiration.​
  • State that carbon dioxide diffuses out of cells into the atmosphere or water.

All organisms may produce the chemical energy (ATP) required to power metabolic processes via the process of cell respiration​

  • CO2 is a waste product of aerobic cell respiration – produced in all cells that carry out aerobic cell respiration. Can be grouped according to trophic level:
    • Non-photosynthetic cells in produces (eg root cells)
    • Animal cells
    • Saprotrophs (eg fungi that decompose dead organic matter)
  • CO2 produced by respiration diffuses out of cells and passes into the atmosphere or water that surrounds the organism

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4.3.U5 ​Methane is produced from organic matter in anaerobic conditions by methanogenic archaeans and some diffuses into the atmosphere or accumulates in the ground.

  • ​Outline the role of methanogenic archaea in the transformation of organic material into methane​

Methane is produced widely in anaerobic environments – it is a waste product of a type of anaerobic respiration

3 groups of anaerobic prokaryotes involved:

  • Bacteria that convert organic matter into mixture of organic acids, alcohol, hydrogen, and carbon dioxide
  • Bacteria that use organic acids and alcohol to produce acetate, carbon dioxide, and hydrogen
  • Archaeans that produce methane from carbon dioxide, hydrogen and acetate do this by two chemical reactions:
    • CO2 + 4H2 -> CH4 + 2H20
    • CH3COOH -> CH4 + CO2

Archaeans in this group are methanogenic – they carry out methanogenesis in many anaerobic environments:

  • Mud along shores / in bed of lakes
  • Swamps, mires, mangrove forests and other wetlands where soil or peat deposits are waterlogged
  • Guts of termites and of ruminant mammals like cattle / sheep

Landfill sites where organic matter is in wastes that have been buried
Some methane produced by archaeans is released into the atmosphere
Methane produced from organic waste in anaerobic digesters is not allowed to escape is instead burned as a fuel

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4.3.U6 ​Methane is oxidized to carbon dioxide and water in the atmosphere.

  • State that methane is oxidized to carbon dioxide in the atmosphere.

When methane is released into the atmosphere as a result of anaerobic reactions, it only persists for ~12 years. Methane will be naturally oxidised to form carbon dioxide and water  (CH4 + 2 O2  →  CO2 + 2 H2O)

  • Monatomic oxygen and highly reactive hydroxyl radicals are involved in methane oxidation

4.3.U7  Peat forms when organic matter is not fully decomposed because of acidic and/or anaerobic conditions in waterlogged soils.

  • Define peat.
  • Outline formation of peat.

In many soils, saprotrophic bacteria and fungi will decompose dead organisms and return nutrients to the soil for cycling. This decomposition process requires oxygen (cell respiration is required to fuel digestive reactions)

  • Peat forms when organic matter is not fully decomposed because of anaerobic conditions in waterlogged soils
    large quantities of organic matter accumulate and become compressed to form a dark brown acidic material called peat
  • Dead leaves from plants is eventually digested by saprotrophic bacteria and fungi
  • Saprotrophs obtain oxygen for respiration from airspaces in soil
  • In some environments, water cannot drain out of soils – become waterlogged and anaerobic
  • Saprotrophs can’t thrive – dead organic matter isn’t fully decomposed
  • Acidic conditions tend to develop – further inhibiting saprotrophs and methanogens that might break down the organic matter
  • Large quantities of partially decomposed organic matter have accumulated in some ecosystems and become compressed to form a dark brown acidic material called peat
  • Conditions go from being aerobic to being anaerobic.
  • Becomes more and more acidic -> methanogens cannot work any longer. (The methanogens are releasing carbon dioxide which is what causes the water to become more acidic)

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4.3.U8 ​Partially decomposed organic matter from past geological eras was converted either into coal or into oil and gas that accumulate in porous rocks.

  • Outline formation of coal.
  • Outline formation of oil and natural gas.

Oil (i.e. petroleum) and natural gas form as the result of the decay of marine organisms on the ocean floor​

  • Carbon / some carbon compounds are chemically stable and can remain unchanged in rocks for hundreds of millions of years
  • Large deposits of carbon from past geological eras – a result of incomplete decomposition of organic matter. Burial in sediments became rock
    • Coal formed when deposits of peat are buried under other sediments. Peat is compressed/heated – turns into coal.
    • Oil and natural gas formed in the mud at bottom of seas and lakes. Conditions usually anaerobic so decomposition is often incomplete. More mud/other sediments are deposited, partially decomposed matter is compressed/heated. Chemical changes occur – produce complex mixtures of liquid carbon compounds or gases. -> crude oil and natural gas. Methane forms the largest part of natural gas.

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4.3.U9 Carbon dioxide is produced by the combustion of biomass and fossilized organic matter.

  • Define combustion.
  • State the products of a combustion reaction.
  • State sources of fuel for a combustion reaction. ​​
When organic compounds rich in hydrocarbons are heated in the presence of oxygen, they undergo a combustion reaction. This reaction is exergonic (produces energy) and releases carbon dioxide and water as by-products
The carbon dioxide is typically released into the atmosphere, increasing the concentration of the gas in the ai
  • If organic matter is heated to ignition temp. in the pressure of oxygen – will set light and burn. -> Oxidation reactions called combustion
    • Products of combustion are CO2 and H2O
  • Biomass: total mass of a group of organisms (dry mass)
    • Units of grams/meter squared (g/m^2) = g m^-2 -> land and terrestrial; g m^3 -> aquatic
  • One way that carbon enters the atmosphere

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4.3.U10 Animals such as reef-building corals and mollusca have hard parts that are composed of calcium carbonate and can become fossilized in limestone.

  • State that hard shells, such as in mollusk and coral, are made of calcium carbonate.

Some animals like Molusca have hard body parts composed of calcium carbonate (CaCO3).

Hard corals that build reefs (exoskeletons by secreting calcium carbonate)

When these animals die, soft parts are decomposed quickly. IN acid conditions, calcium carbonate dissolves but in neutral/alkaline conditions, it is stable and deposits of it from hard animal parts can form on the sea bed.. In shallow tropical seas calcium carbonate is deposited by precipitation in the water – result is limestone rock.

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Application

4.3.S1 Estimation of carbon fluxes due to processes in the carbon cycle. (Carbon fluxes should be measured in gigatonnes.)

  • List seven flux processes in the carbon cycle.
  • State the unit of measure for carbon flux values.  ​

Carbon fluxes describe the rate of exchange of carbon between the various carbon sinks / reservoirs. There are four main carbon sinks – lithosphere (earth’s crust), hydrosphere (oceans), atmosphere (air), biosphere (organisms)

The rate at which carbon is exchanged between these reservoirs depends on the conversion processes involved:

  • Photosynthesis – removes carbon dioxide from the atmosphere and fixes it in producers as organic compounds
  • Respiration – releases carbon dioxide into the atmosphere when organic compounds are digested in living organisms
  • Decomposition – releases carbon products into the air or sediment when organic matter is recycled after death of an organism
  • Gaseous dissolution – the exchange of carbon gases between the ocean and atmosphere
  • Lithification – the compaction of carbon-containing sediments into fossils and rocks within the Earth’s crust (e.g. limestone)
  • Combustion – releases carbon gases when organic hydrocarbons (coal, oil and gas) are burned as a fuel source

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4.3.S2 ​Analysis of data from air monitoring stations to explain annual fluctuations​

  • Sketch a graph of the annual fluctuation in atmospheric carbon dioxide concentration.
  • Explain the annual fluctuation in atmospheric carbon dioxide concentration in the northern hemisphere.

Atmospheric CO2 concentrations have been measured at the Mauna Loa Observatory (in Hawaii) since 1958 by Charles Keeling. From these continuous and regular measurements a clear pattern of carbon flux can be seen:

  • CO2 levels fluctuate annually (lower in the summer months when long days and more light increase photosynthetic rates)
  • Global CO2 trends will conform to northern hemisphere patterns as it contains more of the planet’s land mass (i.e. more trees)
  • CO2 levels are steadily increasing year on year since the industrial revolution (due to increased burning of fossil fuels)
  • Atmospheric CO2 levels are currently at the highest levels recorded since measurements began
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Data is now being regularly collected at a variety of field stations globally, using standardised measurement techniques

  • All stations show a clear upward trend in atmospheric CO2 concentrations year on year, with annual fluctuations
  • Different monitoring stations may have slightly different trends due to seasonal variations and the distribution of local vegetation

Analysing Carbon Data
Carbon data can be plotted and analysed using the online database at CDIAC (Carbon Dioxide Information Analysis Centre)

  • This website stores data on atmospheric CO2 levels, which can be imported into an Excel spreadsheet in order to graph

How to use the CDIAC database:

  • Access the CDIAC website (click on the link to redirect)
  • Click on ‘Atmospheric Trace Gases and Aerosols’ (under ‘Data’ tab at top of page)
  • Select ‘Carbon dioxide’ from the list of greenhouse gases
  • Choose a monitoring station / network (e.g. Scripps Institution of Oceanography Network)
  • Download data from a particular site (e.g. South Pole, Antarctica)
  • Paste data of interest into an Excel spreadsheet to produce a graphical display (e.g. Jan 2000 – Dec 2007)
Skill

4.3.S1 Construct a diagram of the carbon cycle.

  • Draw a diagram of the terrestrial carbon cycle.
  • Draw a diagram of the aquatic carbon cycle.
  • Define pool and flux.

The carbon cycle is a biogeochemical cycle whereby carbon is exchanged between the different spheres of the Earth. The four spheres are the atmosphere (air), lithosphere (ground), hydrosphere (water / oceans) and biosphere (living things). Carbon is exchanged between a variety of forms, including:

Atmospheric gases – mainly carbon dioxide (CO2), but also methane (CH4)
Oceanic carbonates – including bicarbonates dissolved in the water and calcium carbonate in corals and shells
As organic materials – including the carbohydrates, lipids and proteins found in all living things
As non-living remains – such as detritus and fossil fuels

​D
etails include

  • interaction of living organisms and the biosphere through:
    • photosynthesis – atmospheric carbon dioxide –> organisms
    • cell respiration – organisms –> atmospheric carbon dioxide
    • fossilization – carbon-containing molecules –> fossil fuels
    • combustion – carbon-containing organisms & fossil fuels –> atmospheric carbon dioxide
    • sedimentation – carbon-containing molecules –> mineral deposits
    • volcanoes – carbon-containing mineral deposits –> atmospheric carbon dioxide
  • recall of quantitative data is not required
 

Carbon Cycle Animation

 

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Ecosystem

Table of Contents

What is Ecosystem?

  • The communication between the living life form and the non-living environment is called Ecosystem.

Ecosystem – Structure and Function

  • Interaction of biotic and abiotic parts brings about a physical structure that is normal for every kind of Ecosystem.
  • Identification and portrayal of plant and creature species of an ecosystem provides its species composition.
  • Distribution of various species vertically possessing diverse levels is called stratification.
  • The parts of the ecosystem are believed to work as a unit:
    • Productivity
    • Decomposition
    • Energy stream
    • Nutrient cycle

Description of pond as an ecosystem

  • The abiotic parts incorporate all broke down organic and inorganic substances and the rich soil store at the base of the lake.
  • The sunlight based information, cycle of temperature, length of the day, regulates the rate of capacity of the whole lake.
  • The producer (autotrophic) incorporates phytoplankton, some green growth (algae) and the gliding, submerged and peripheral plants found on edge of the lake.
  • The consumers are spoken to by zooplankton, swimming freely and basal staying animals.
  • The decomposers are the bacteria, fungi particularly inexhaustible at the base of the lake.

Basic events (in terms of function) in an Ecosystem

  • Conversion of inorganic into a natural material (Photosynthesis) with the help of producers
  • Autotrophs being consumed by heterotrophs
  • Decomposition and mineralization of the dead natural matter to discharge them back to be used again by the autotroph
  • There is unidirectional stream of vitality towards the higher trophic levels and its dispersal and loss as warmth to the earth

Fig: Pond Ecosystem (above) and Terrestrial Ecosystem (below)

Productivity

Primary Productivity

  • The measure of biomass or natural matter created per unit range over a time frame by plants amid photosynthesis
  • It is expressed as weight (g-2) or vitality (kcal m-2)
  • The rate of biomass generation is called productivity
  • Gross primary productivity (GPP): is the rate of creation of natural matter amid photosynthesis.
  • Net primary productivity:
    • A significant measure of vitality is used by plants while respiration
    • Gross primary productivity minus loss through respiration (R) is the net primary productivity.
    • GPP – R = NPP
    • Net primary productivity is the accessible biomass for the utilization to heterotrophs (herbivore and decomposers)

Secondary Productivity

Secondary Productivity is characterized by the rate of arrangement of new natural matter by the consumer.

Decomposition

  • Earthworm is said to be “farmer’s friend”
  • Breakdown the intricate natural matter
  • Loosening of the soil helps in air circulation and passage of root
  • The decomposers decompose complex natural matter into inorganic substances such as nutrients, water, and carbon dioxide, called decomposition
  • Remains of dead plants, for example, leaves, flowers, bark remains of dead animals, including fecal matter, constitute the detritus
  • The procedure of decomposition is finished in following steps:
    • Fragmentation: Breakdown of debris by detritivore (earthworm) into smaller and simpler particles
    • Leaching: Inorganic supplements that are water solvent go down into the horizon of the soil and get hastened as inaccessible salts
    • Catabolism: Bacterial and parasitic enzymes debase waste into basic inorganic substances
    • Humification: Accumulation of amorphous substances that are dark in color is called Humus

The significance of humus

  • High imperviousness to microbial activity
  • Undergo deterioration at a moderate rate
  • Being colloidal in nature, it serves as a repository for supplements
  • Mineralization: The humus is further broken down by a few microorganisms and inorganic supplements get released

Factors that affects rate of Decomposition

  • Decomposition is generally a process that needs oxygen
  • Detritus rich in lignin and chitin has a moderate rate of decomposition
  • Detritus rich in substances that are soluble in water like sugar and nitrogen has quicker decomposition
  • Temperature and soil dampness are most vital climatic element that regulates decomposition
  • Warm and sodden environment support decomposition

Anaerobiosis, dryness and, low temperature restrain decomposition.

Energy Flow in Ecosystem

  • Except for remote ocean aqueous ecosystem, the sun is the main source of vitality for all ecosystems on earth
  • Less than half of occurrence solar radiation is Photosynthetically Active Radiations. (PAR)
  • Plants catch 2-10 % of PAR and utilized as a part of photosynthesis
  • All living beings rely on upon the producers, either specifically or by implication
  • Flow of energy in the ecosystem is unidirectional i.e. vitality is exchanged from producer to consumers
  • Energy exchange is not supreme, and unconstrained unless vitality is degraded it can not be exchanged. At the point when vitality is exchanged starting with one trophic level then onto the next, a significant amount of vitality is lost as warmth to the earth.
  • Only 10% of vitality is exchanged from one trophic level to other

Fig: Energy flow (10% of energy is transferred at successive trophic levels)

Food Chain

  • Grazing food chain: it moves from producers through herbivore to meat eater (carnivores)

Fig a: Grazing Food Chain

  • Detritus food chain: Begins with dead natural matter (detritus) and go through detritus feeding life forms in soil to living beings nourishing on detritus-feeders

Fig b: Detritus Food Chain

  • In oceanic ecosystem GFC is the significant channel for energy flow
  • In terrestrial ecosystems a much bigger portion of vitality flows through the detritus food chain than through GFC
  • Many different food chains are normally interconnected e.g. a particular herbivore of one food chain may become food of carnivores in other food chains. Such interconnected grid of food chains is called food web
  • Trophic level: A gathering of living beings independent of their size having same source of vitality or comparative food propensity constitute a trophic level
  • Standing crop: every trophic level has a specific mass of living material at a specific time called as the standing crop
  • The standing crop is measured as the mass of living creatures (biomass) or the number in a unit region
  • The number of trophic levels in a food chain is confined by 10% flow of vitality, less measure of vitality accessible to the last trophic level

Ecological Pyramid

An ecological pyramid (additionally called energy pyramid, trophic pyramid, or now and again food pyramid) is a graphical representation intended to demonstrate the biomass or bio efficiency at each trophic level in any given ecosystem. The trophic structure and capacity of progressive trophic levels, i.e. Producers → Herbivores → Carnivores, might be indicated graphically by methods called ecological pyramids where the first or producer level constitutes the base of the pyramid and the progressive levels, the levels making the pinnacle. Ecological pyramids were first introduced by Charles Elton (1927) and are, in this manner, additionally called Eltonian pyramids. Ecological pyramids are of three general sorts:

  • Pyramid of Energy
  • Pyramid of Numbers
  • Pyramid of Biomass

Pyramid of Energy

The energy pyramid or the pyramid of energy portrays the general way of the ecosystem. Amid the stream of energy from living forms to other, there is a significant loss of energy as warmth. In primary producers such as the autotrophs, there is more measure of energy accessible. The minimum energy is accessible in the tertiary consumers. Along these lines, the shorter food chain has more measure of energy accessible even at the most elevated trophic level.

  • The energy pyramid is constantly upright and vertical
  • This pyramid demonstrates the stream of energy at various trophic levels
  • It portrays, the energy is least at the most astounding trophic level and is greatest at the most reduced trophic level
  • At each trophic level, there is progressive loss of energy as warmth and breath, etc.

Fig. a: Pyramid of Energy

Pyramid of Numbers

The pyramid of numbers portrays the relationship as far as the quantity of producers, herbivores and the carnivores at their progressive trophic levels are concerned. There is an abatement in the quantity of people from the lower to the higher trophic levels. The number pyramid differs from one ecosystem to another ecosystem. There are three forms of the pyramid of numbers:

  • Upright pyramid of number
  • Partly upright pyramid of number and
  • Inverted pyramid of number

Upright Pyramid of Number
Such a sort of pyramid number is found in the grassland and aquatic ecosystem, in these ecosystems there are various little autotrophs which bolster lesser herbivores which thus bolster littler number of carnivores and henceforth this pyramid is upright.

Fig. b: Upright Pyramid of Number

Partly Upright pyramid of Number

It is found in the woodland ecosystem where the quantity of producers are lesser in number and bolster a more prominent number of herbivores and which thus bolster a less number of carnivores.

Fig. c: Partly Upright Pyramid of Number

Inverted Pyramid of Number

Such a sort of ecological pyramid is seen in parasitic food chain where one primary producer bolsters various parasites which bolster all the more hyperparasites.

Fig. d: Inverted pyramid of number

Pyramid of Biomass

The pyramid of biomass is more central, they speak of the quantitative connections of the standing crops. In this pyramid, there is a slow decline in the biomass from the producers to the higher trophic levels. The biomass here is gathered from every bolstering level and are then dried and weighed. This dry weight is the biomass and it speaks to the measure of energy accessible as a natural matter of the life forms. In this pyramid, the net dry weight is plotted to that of the producers, carnivores, herbivores, and so on.

There are two sorts of pyramid of biomass, they are:

  • Upright pyramid of biomass and
  • Inverted pyramid of biomass.

Upright Pyramid of Biomass

Such a case happens when the bigger net biomass of producers maintain a little weight of consumers.

For Example: Forest ecosystem.

Fig. e: Upright Pyramid of Biomass

Inverted Pyramid of Biomass

Such a case happens when the producer’s smaller weight supports the larger weight of consumers. For example: Aquatic ecosystem.

Fig. f: Inverted Pyramid in an Aquatic Ecosystem

Limitations of Ecological Pyramids

  • It does not consider similar species having a place with at least two trophic levels
  • It expect a basic food chain, it never exits in nature
  • It does not oblige food web
  • Saprophytes are placed in ecological pyramids

Ecological Succession

  • The slow and genuinely unsurprising change in the species piece of a given zone is called Ecological Succession
  • Structure and composition of the group always show signs of change because of changing natural condition
  • This change is efficient and successive, parallel with the adjustments in the Physical Environment
  • All the progressions lead at long last to a group that is in close harmony with the earth and that is called Climax Community
  • During succession, a few species colonize and territory and their populations turn out to be increasingly various, though populations of different species decay and even vanish
  • The whole sequences of groups that progressively change in a given zone are known as sere
  • The individual transitional groups are named as seral stages
  • In the progressive seral organizes there is an adjustment in the diversity of species of life forms, increase in number of species and aggregate biomass

Primary Succession:

Primary succession that begins where no living life forms are there- these could be ranges where no living creature ever existed might be an uncovered rock or new water body.

Secondary Succession:

Secondary succession that begins in regions that some way or another, lost all the living beings that existed there.

  • Primary succession happens in:-
    • newly cooled magma
    • bare rock
    • newly made lake or repository
  • Secondary succession starts in ranges where regular biotic groups have been devastated, for example,
    • In deserted homestead lands
    • Burned or cut woodland,
    • land that has been overflowed
  • Since some soil or silt is available, secondary succession is quicker than primary succession

Succession in plants

  • Based on the way of living space – whether it is water or it is in extremely dry regions succession of plants is called hydrarch or xerarch
  • Hydrarch succession happens in water territories and the successional arrangement progress from hydric to a mesic condition
  • Xerarch succession happens in dry territories and the arrangement advance from xeric to mesic conditions
  • Both hydrarch and xerarch successions prompt to medium water conditions (mesic) – neither excessively dry (xeric) nor excessively wet (hydric)

Xerarch Succession: Succession in bare rock:

  • The species that attacks exposed territory are known as pioneer species
  • In primary succession on exposed rock, the pioneer species to be grown is the lichen
  • Lichen secretes corrosive materials to break down the rock, leading to weathering and soil development
  • The small quantity of soil prompts to the development of bryophytes (greeneries)
  • The greeneries accelerate the procedure of soil aggregation by catching wind-blown particles
  • Lichen greenery carpet gives reasonable substratum to the germination of seeds of herbaceous plants
  • Gradually more soil is aggregated and herbaceous species clear a path for the intrusion of bushes took after by trees
  • The climax group is by and large ruled by trees

Fig a: Xerarch Succession on Bare Rock

Hydrarch (succession in aquatic environment)

  • The pioneer species in primary succession in water are phytoplankton
  • Zooplanktons
  • Sub consolidated plant organize. (established hydrophytes)
  • Sub combined and free-gliding plant stage
  • Reed-swamp stage
  • Marsh-meadow stage
  • Shrub stage
  • Trees
  • The climax again would be the backwoods
  • All the succession whether occurring in water or ashore continues to a comparable climax group – the mesic

Fig b: Hydrarch Succession Stages

Nutrient Cycling

  • Organism needs consistent supply of supplements to develop, divide, and regulate different body capacities
  • Standing state: the sum nutrients, for example, carbon, calcium, phosphorus, nitrogen, and so on present in soil at any given time
  • Nutrient cycling: The development of nutrient components through the different part of an ecosystem is called nutrient cycling.
  • Alternate name of nutrient cycling is Biogeochemical Cycle
  • Nutrient cycles are of two sorts:
    • Gaseous Cycle
    • Sedimentary Cycle
  • The store for vaporous kind of nutrient cycle (nitrogen, carbon) exists in the environment
  • The store for sedimentary cycle (sulfur, phosphorus) is Earth’s covering
  • Environmental variables like soil, pH, dampness, temperature regulate the rate of arrival of nutrient into the climate
  • The capacity of the repository is to meet the shortage which happens because of unevenness in the rate of efflux and influx

Fig: Nutrient Cycle

Ecosystem – Carbon cycle

  • Carbon constitutes 49 % of dry weight of living being
  • Out of aggregate worldwide carbon:
    • 71 % carbon was discovered broke down in the sea
    • About 1 % in the climate
  • 4 X 1013 kg of carbon is settled in the biosphere by photosynthesis, every year.
  • Large measure of carbon came back to the climate as CO2 through respiratory processes of producers and consumers.
  • Decomposers return back the CO2 to the reservoir through the process of decomposition.
  • Some measure of Carbon is lost to silt and expelled from the flow.
  • Burning wood, backwoods fire, ignition of natural matter, fossil fuel, volcanic exercises are extra hotspots for discharging CO2 to air.

Fig: Carbon Cycle

Influence of human activity on Carbon cycling

  • Massive blazing of fossil fuel for vitality and transport
  • Rapid deforestation
  • Increased the rate of arrival of CO2 into the air

Ecosystem Phosphorus cycle

  • Phosphorus is a noteworthy constituent of nucleic acids, cellular membranes and cell vitality exchange system, adenosine triphosphate (ATP)
  • Animals require phosphorus to make shells, teeth, and bones.
  • Reservoir pool of phosphorus is the stone, which contains phosphorus as phosphates
  • During rock weathering, a little measure of phosphates broke up in soil arrangement and are consumed by the underlying foundations that are the roots of the plants
  • Herbivore and different animals get the natural type of phosphorus from plants
  • The dead life forms and waste products are deteriorated by phosphate-solubilizing bacteria discharging phosphorus

Fig: Phosphorus Cycle

How phosphorus cycle differs from carbon cycle?

  • There is no respiratory arrival of phosphorus into the air
  • Atmospheric contributions of phosphorus through precipitation are quite small
  • Gaseous trade of phosphorus amongst life form and environment are immaterial

Ecosystem Services

Fig: Ecosystem Services

  • The results of ecosystem procedures are named as Ecosystem services
  • Healthy woods ecosystems sanitize air and water
  • Mitigate dry spells and surge
  • Cycle supplements
  • Generates ripe soil
  • Provide natural life territory
  • Maintain biodiversity
  • Pollinate crops
  • Provide capacity site for carbon
  • Provides spiritual, social and aesthetic qualities

PAR: Photosynthetically Active Radiation
GAP: Gross Primary Productivity
NPP: Net Primary Productivity
DFC: Detritus Food Chain
GFC: Grazing Food chain

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