Living organisms require?nutrients?from their?environments?for?growth?and other processes (e.g. reproduction)
These nutrients are then?returned?to the environment when organisms produce?waste?or?die?and?decompose
This is due to the waste products and dead organisms being?digested?(decomposed) by?microorganisms
The?products?of this decomposition are available to?plants?as?nutrients?in the?soil
These plants can then sustain organisms in higher trophic levels (consumers)
In?stable?communities, the processes that?remove?nutrients (e.g. plant growth) are?balanced?by the processes that?return?these nutrients (e.g. decomposition of dead plants and animals)
This means these nutrients are constantly being?cycled?in ecosystems
Two examples of these nutrient cycles are:
The?nitrogen?cycle
The?phosphorous?cycle
The nitrogen cycle
The nitrogen cycle shows how nitrogen is recycled in ecosystems
Plants and animals require nitrogen in order to produce?proteins?and?nucleic acids?(DNA and RNA)
About 78% of the atmosphere is actually?nitrogen gas?but plants and animals?cannot?access the nitrogen in this gaseous form
Instead, they rely on certain?bacteria?to convert the nitrogen gas into?nitrogen-containing compounds, which can be taken up by plants
The nitrogen cycle shows this conversion, as well as how the nitrogen in the nitrogen-containing compounds is then passed between trophic levels or between living organisms and the non-living environment
The role of bacteria in the nitrogen cycle
There are?four?key processes in the nitrogen cycle that are carried out by?different types of bacteria
Nitrogen?fixation:
Atmospheric nitrogen gas is converted into nitrogen-containing compounds
This biological nitrogen fixation is carried out by?nitrogen-fixing bacteria?such as?Rhizobium
The bacteria convert nitrogen into?ammonia,?which forms?ammonium ions?(in solution) that can then be used by?plants
These nitrogen-fixing bacteria are found inside the?root nodules?(small growths on the roots) of?leguminous?plants such as peas, beans and clover
The bacteria have a?symbiotic?(mutually beneficial) relationship with these plants - the bacteria provide the plants with nitrogen-containing compounds and the plants provide the bacteria with organic compounds such as carbohydrates
Ammonification:
Nitrogen compounds in?waste products?(e.g. urine and faeces) and?dead organisms?are converted into?ammonia?by?saprobionts?(a type of decomposer including some fungi and bacteria)
This ammonia forms?ammonium ions?in the soil
Nitrification:
The ammonium ions in the soil are converted by?nitrifying bacteria?into nitrogen compounds that can be used by plants, known as?nitrates
Initially, nitrifying bacteria such as?Nitrosomonas?convert ammonium ions into?nitrites
Different nitrifying bacteria such as?Nitrobacter?then convert these nitrites into?nitrates
Denitrification:
Denitrifying bacteria use?nitrates?in the soil during?respiration
This process produces?nitrogen gas, which returns to the?atmosphere
This process occurs in?anaerobic?conditions (when there is little or no oxygen available, such as in waterlogged soil)
The nitrogen cycle
The phosphorus cycle
The phosphorus cycle shows how phosphorus is recycled in ecosystems
Plants and animals require phosphorus in order to produce certain biological molecules such as?phospholipids?(for cell membranes),?nucleic acids?(DNA and RNA) and?ATP
The phosphorus cycle includes the following processes:
Phosphorus?in?rocks?is slowly released into the soil and into water sources in the form of?phosphate ions?(PO?3?) by the process of?weathering?(the slow breaking down and erosion of rocks over time)
Phosphate ions are taken up from the soil by?plants?through their?roots?or absorbed from water by?algae
Phosphate ions are transferred to?consumers?during?feeding
Phosphate ions in?waste products?and?dead organisms?are released into the soil or water during?decomposition?by?saprobionts
The phosphate ions can now be taken up and used once again by producers or may be trapped in?sediments?that, over very long geological time periods may turn into phosphorus-containing?rock?once again