Nutrient Cycles
- Elements are taken up by producers (plants) / stored as organic matter
- Passed on across trophic level / consumer digest and absorb food / stored as organic matter
- Decomposers decay detritus and excretory products / return inorganic ions to environment / taken up by producers
- Warm temp / higher enzyme activity / faster decomposition
Table 9-14-1: Use of nutrients in plants and animals
PLANTS | ANIMALS | |
CARBON | Organic substances / lipids / proteins / ATP / chlorophyll | Organic substances / lipids / proteins / ATP / chlorophyll |
NITROGEN | - Amino acid / nucleotide synthesise - In RNA, DNA, proteins, ATP | - Amino acid / nucleotide synthesise - In RNA, DNA, proteins, ATP |
IRON | - In cytochromes / ETC - Needed for enzymes such as catalase to work - Synthesis of chlorophyll | - In cytochromes / ETC - Needed for enzymes such as catalase to work - Part of Hb |
IODINE | Contained in thyroxine (hormone) | |
MOLYBDENUM | Nitrate reductase / reduces nitrates during synthesis of amino acids |
Carbon Cycle
- Producers, consumers, decomposers
- Add CO2 to the air by respiration
- Carbon is stored in tissues as organic matter (carbohydrates, lipids, proteins)
- Carbon is passed along food web by feeding
- Plants remove CO2 from air by photosynthesis
- Animals excrete carbon as waste products
- Decomposers decay detritus and excretory products / add carbon to soil
- Detrivores digest detritus to small pieces / large surface area
- Saprophytes digest smaller detritus by
- Extracellular digestion by secreting enzymes
- Absorb resulting nutrients across plasma membrane
- Releases inorganic matter (CO2, H2O, mineral ions) into soil
- Fossil fuels
- Combustion releases CO2 into air
- Fossilisation of carbon atoms in organic compounds in dead remains (plants, animals) and excretory products (animals)
- Respiring organisms must not die to release stored carbon / differs from other cycles
Respiration, Photosynthesis and CO2
- Photosynthesis takes up more CO2 than is released by respiration
- CO2 concentration
- Higher at night than at daylight; light-dependent reaction cannot take place
- Peaks at winter time due to high oil consumption; low rate of photosynthesis due to cooler temp, shorter day length, loss of leaves
- Variation in a graph due to wind mixing CO2 with the surrounding air
- Graph should show conc over whole area rather over a specific area
- Rate of photosynthesis and respiration are balanced in a rain forest
- Forests grow for a long time and have stored lots of carbon in their tissues, other plants have stored carbon as cellulose and lignin
- Forests grow for a long time and have stored lots of carbon in their tissues, other plants have stored carbon as cellulose and lignin
Nitrogen Cycle
- *processes involved in restoring nitrate conc in soil after cultivation is abandoned
1) Assimilation (→Building up organic molecules)
- Plants take up NITRATE NO3/AMMONIA NH3 from the soil by active transport
- Used to synthesis amino acids / synthesise proteins / new cells and tissues
- Primary consumers feed on plants
- Proteins are digested into amino acids and absorbed
- Amino acids synthesise new proteins
- Nitrogen is passed along the trophic level through the food web
2) Ammonification*
- Detritus/leaves from plants/excretion from animals/dead animals
- Broken down by saprotrophs/decomposition
- Releases ammonia (NH3)/ammonium ions (from decay)
- Ammonia dissolves in H2O → NH3 + aq → NH4+
3) Nitrification*
- Ammonium NH4+ / nitrite NO2-
- Nitrite / nitrate
- By aerobic nitrifying bacteria eg. include:
- (Nitrosomonas, Nitrosospira, Nitrosococcus, and Nitrosolobus - which are bacteria that convert ammonia to nitrites),
- (Nitrobacter,Nitrospina, and Nitrococcus - which are bacteria that convert nitrites (toxic to plants) to nitrates )
4) Denitrification
- Removal of nitrogen from NO2 (nitrite)- and NO3 (nitrate)- to make N2(g)
- By anaerobic denitrifying bacteria eg. include:
- Thiobacillus denitrificans, Micrococcus denitrificans, and some species of Serratia, Pseudomonas, and Achromobacter.
5) Nitrogen Fixation*
- N2(g) is converted to nitrates by lightning N2(g) + O2 → NO3-
- NITROGEN GAS IS CONVERTED TO NH3/NH4+
- By Haber process: N2(g) + H2 → ammonia NH3
- //used to make fertilisers / added to soil / leakage of ions into river
- By Nitrogen-fixing bacteria by anaerobic nitrogenase. There are 2 types of nitrogen fixing bacteria:
- Live free in soil (non-symbiotic) bacteria, including the cyanobacteria (or blue-green algae) Anabaena, Azotobacter, Beijerinckia, and Clostridium;
- Mutualistic (symbiotic) bacteria such as Rhizobium, living in the nodules of leguminous plants, and Spirillum lipoferum, associated with cereal grasses.
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