Carbon cycling PDF

Title Carbon cycling
Course Biology SL
Institution International Baccalaureate Diploma Programme
Pages 4
File Size 56.6 KB
File Type PDF
Total Downloads 96
Total Views 160

Summary

Biology SL
Topic 4.3
carbon, role of autotrophs, carbon dioxide, aquatic ecosystems, methane, peat, fossil fuels, biomass, limestone...


Description

Carbon cycling

Topic 4.3

Biology SL

Carbon ➢ Life on Earth is referred to as carbon-based life ➢ The biosphere refers to all the places where life is found and the lithosphere refers to all the places where rocks are found ➢ Cycling involves how the carbon atoms are incorporated into dierent molecules

Role of autotrophs ➢ Photosynthetic autotrophs take carbon dioxide from the atmosphere and convert it into carbohydrates In its inorganic form, carbon isn’t usable as a food source by the autotrophs



or by any consumer, but sugars (organic form of carbon) are ■

Fructose, galactose, starch, cellulose are all made by glucose



Other organic compounds, like lipids and amino acids, are also made of glucose ●

Glucose is the starting point in this case, since other elements, such as nitrogen, must be added to it

Carbon dioxide ➢ Absorbed by photosynthetic autotrophs and is turned into organic compounds ➢ Consumers eat the producers and use the carbon compounds ➢ Consumers and decomposers respire and release carbon dioxide back into the environment

Carbon in aquatic ecosystems ➢ Carbon dioxide can be absorbed by water ➢ Organisms that live in the water produce cc through cell respiration ➢ As the carbon dioxide is dissolved in the water, it forms and acid The pH of water decreases and carbon dioxide increases



CO2 + H2O ⇒ H2CO3 (carbonic acid) -

➢ HCO3 is an inorganic molecule which participates in the carbon cycle +

H2CO3 + H ⇒ HCO3 ○

-

(hydrogen carbonate ion)

Carbon can be absorbed in this form by organisms

➢ Carbon by carbon sequestration can turn into: ○

Methane, limestone, peat, fossil fuels

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Carbon cycling

Topic 4.3

Biology SL

Methane ➢ Some organisms are capable of living in anaerobic conditions, such as methanogenic archaeans ➢ When these methanogenic archaeans metabolise food, they produce methane instead of carbon dioxide, as a waste gas ➢ They’re also common in wetlands where they produce marsh gas, which can sometimes glow at night ➢ Methane forms slowly and large quantities can be trapped in the ground ➢ Methane is a very potent greenhouse gas ➢ It can be burnt in oxygen to form carbon dioxide CH4 + 2O2 ⇒ 2H2O + CO2 ➢ Methane is the main ingredient in the fossil fuel we call natural gas ➢ The carbon found in methane was borrowed from a carbon dioxide molecule that was removed from the atmosphere millions of years ago during photosynthesis ○

Methane formed and accumulated underground



Through burning, the carbon is returned to the atmosphere as carbon dioxide ■

The problem is that the burning is very fast, but the formation very slow

Peat

➢ Peat is an organic substance that consists of partially decomposed plant material ○

It’s a heterogeneous mixture of many things



At least 30% of its dry mass has to be composed of dead organic material

➢ Used as fossil fuel ➢ It’s a kind of waterlogged soil found in certain types of wetlands ➢ The low pH hinders decomposition ○

Anaerobic conditions are created



Certain types of microorganisms grow, but microorganisms that would help in the decomposition of plant material are prevented from growing

➢ It takes a long time to form and it isn’t considered to be a renewable source of energy ➢ Wetlands are an important part of the ecosystem and a habitat for unique species ➢ Pollen trapped in deep layers of the bogs can provide evidence of what the climate was like in the past

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Carbon cycling

Topic 4.3

Biology SL

➢ When left in the correct conditions, partially decomposed peat can be further transformed into coal

Fossil fuels ➢ When organic compounds are trapped under sediments over a long time, fossil fuels can form ○

Sediments are layers of dead organisms that weren’t fully decomposed usually formed at the sea bottom

➢ The carbon-rich deposits are under huge pressure and exposed to high temperatures ○

These 2 factors cause chemical transformations associated with lithification ■

Lithification is the transformation of sediments into solid rock

➢ The term fossil fuel refers to the fact that the source of energy in the fuel comes from partially decayed once-living organisms that died millions or hundreds of millions years ago ○

Theyäre considered to be a non-renewable source of energy

➢ Such ideal conditions have existed in a few parts of the world ○

If favourable geological changes occur the compounds can be trapped and later extracted

Biomass ➢ The dried dung of domesticated animals can be burnt and used for various purposes ➢ Fresh, wet dung can be mixed with other refuse from a farm and put into a large container where methane-producing microorganisms will decompose and ferment he material to produce flammable methane gas ➢ Plant material is fed to microorganisms that ferment it and in the process release ethanol ○

Ethanol is added to gasoline for vehicles and contributes to a reduction in gasoline use

➢ The burning of any biomass still releases carbon dioxide into the atmosphere but unlike fossil fuels, the carbon dioxide from biofuels was removed from the atmosphere by plants just a few months/years before the biofuel was used

Limestone ➢ The organisms that build coral reefs are called coral polyps and they absorb 2 ions from seawater to build the reef: 3

Carbon cycling

Topic 4.3



Hydrogen carbonate ions



Calcium ions

Biology SL

➢ When combined, molecules of calcium carbonate are formed -

2+ Ca + 2HCO3 ⇒ CaCO3 + CO2 + H2O

➢ As these organisms die, their shells are deposited on the bottom of the sea and they accumulate in sediments ○

When the sediments go through the process of lithification, they form limestone

➢ The process of taking carbon out of the environment and “locking it up” in a substance for an extended period of time is called carbon sequestration ○

When it happens naturally, it is called biosequestration ■

This is one way in which balance is maintained in the carbon cycle

➢ When limestone is used, some of the carbon is released back into the atmosphere as carbon dioxide cancelling out the biosequestration

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