Open systems in which both energy and matter can enter and exit. This Systems only allow the exchange of energy.
Closed Systems
Systems where only energy is able to pass in and out
Sunlight
The principal source of energy that sustains most ecosystems
Exceptions to Sunlight as the Principal Energy Source
Ecosystems in caves
Below the levels of light penetration in oceans
Flow of Chemical Energy Through Food Chains
Chemical energy passes to a consumer as it feeds on an organism that is the previous stage in a food chain
Construction of Food Chains and Food Webs
Arrows indicate the direction of transfer of energy and biomass
Supply of Energy to Decomposers
Carbon compounds in organic matter come from dead organisms (faeces, dead parts of organisms, dead whole organisms)
Autotrophs
Organisms that use external energy sources to synthesize carbon compounds from simple inorganic substances
Energy Source in Photoautotrophs and Chemoautotrophs
Light and oxidation reactions, respectively
Heterotrophs
Organisms that use carbon compounds obtained from other organisms to synthesize the carbon compounds that they require
Cell Respiration
Release of energy in both autotrophs and heterotrophs by oxidation of carbon compounds
Trophic Levels
Producer
Primary consumer
Secondary consumer
Tertiary consumer
Decomposers and Detritus Feeders
Not usually considered to be part of food chains
Primary Production
Accumulation of carbon compounds in biomass by autotrophs
Secondary Production
Accumulation of carbon compounds in biomass by heterotrophs
Carbon Cycle Diagrams
Illustrate how carbon is recycled in ecosystems by photosynthesis, feeding, and respiration
Combustion
Release of carbon dioxide into the atmosphere during combustion of biomass, peat, coal, oil, and natural gas
Open Systems
Ecosystems are open systems where energy and matter can be exchanged
Sunlight in Ecosystems
Sunlight is the initial source of energy that sustains most ecosystems, as it is needed to produce glucose in photosynthesis.
Plants, eukaryotic algae, and cyanobacteria carry out photosynthesis and are referred to as producers or autotrophs.
Heterotrophs use the sunlight indirectly and are also dependent on it
Ecosystems With Limited Sunlight
Life is usually adapted to the decreased amount of energy available.
In marine and freshwater ecosystems, light must pass through water to reach producers, and transmission is not 100%.
In deep-sea ecosystems, the source of energy often originates from bacteria which can use sulfides as a source of energy.
Flow of Energy
Energy enters as light, flows as nutrients through the food chains, and usually leaves as heat
Recycled Nutrients
Carbon
Nitrogen
Phosphorus
Decomposers
1. Supplied with energy from carbon compounds in dead organic matter such as faeces, shed exoskeletons, and dead plant material
2. Secrete digestive enzymes into dead organic matter and digest it externally by absorbing the products of digestion
Saprotrophs
Break down complex insoluble carbon compounds into soluble ones, recycling dead matter which would otherwise build up
Organisms
Autotrophs
Heterotrophs
Photoautotrophs
Chemoautotrophs
Consumers
Saprotrophs
Photoautotrophs
Use sunlight as an energy source. A small amount of solar radiation that reaches the Earth is absorbed by chloroplasts
Chemoautotrophs
Use sulfur, hydrogen sulfides, iron sulfides, hydrogen, or ammonia as sources of energy that can be oxidized to release energy for synthesizing carbon compounds
Iron Oxidizing Bacteria
Use Fe2+ ions and oxidize them to Fe3+ ions. The electrons from this reaction are used to drive energy production (ATP) processes in the cell membrane
Trophic Levels
Offer a way of classifying organisms by their feeding relationships within the same ecosystem. Energy transformations in living organisms are never 100% efficient, commonly being 10-20%.
Energy Loss Reasons
Not ingested (eaten)
Not digested or assimilated
Excreted
Lost as heat from respiration
Heat Energy
Lost to the environment in both autotrophs and heterotrophs due to conversion of chemical energy to heat in cell respiration
Heat energy is unusable to organisms and is lost from ecosystems
Heat resulting from cell respiration makes living things warmer, passing from hotter to cooler bodies and eventually lost to the abiotic environment
Energy Forms
Chemical energy (ATP) produced by an organism through cellular respiration can be converted into electrical energy during nerve impulse transmission, light energy in bioluminescence, or kinetic energy during muscle contractions
Elements required by living organisms
Carbon
Hydrogen
Oxygen
Nitrogen
Phosphorus
Magnesium
Calcium
Manganese
Copper
Sodium
Potassium
Nitrogen Cycle
1. Nitrogen from the air or in organic matter is converted to ammonia and ammonium, then to nitrates, which can be assimilated by plants
2. Decomposers break down the body parts of dead organisms, converting the nutrients into a more usable form
Energy Transfers
Not 100% efficient, so heat is produced both when ATP is produced in cell respiration and when it is used in cells.
Food Chains and Biomass
At each successive stage in food chains there are fewer organisms or smaller organisms, so there is less biomass, but the energy content per unit mass is not reduced.
Ecosystems as Carbon Sinks and Sources
If photosynthesis exceeds respiration, there is a net uptake of carbon dioxide.
If respiration exceeds photosynthesis, there is a net release of carbon dioxide.
Recycling of Chemical Elements
All chemical elements required by living organisms are recycled in ecosystems.
Aerobic Respiration and Photosynthesis
Dependence of aerobic respiration on atmospheric oxygen produced by photosynthesis, and of photosynthesis on atmospheric carbon dioxide produced by respiration.
Energy Flow and Pyramids
Energy flow can be represented using pyramids of energy.
Construction of energy pyramids involves calculating the percentage energy transfer from producers to primary consumers, drawing the pyramid to scale, and labeling each trophic level.