autotrophs - synthesize their own organic molecules from simple inorganic substances using energy derived from sunlight (photosynthesis) or oxidation (chemosynthesis); producers
heterotrophs - obtain organic molecules from other organisms
consumers - ingest organic molecules from living or recently killed organisms
herbivores - consume plant matter
carnivores - consume animal matter
omnivores - consume both plants and animals
scavengers - consume dead and decaying carcasses
detritivores - ingest organic molecules found in the non-living remnants of organisms (e.g. detritus, humus)
saprotrophs - release digestive enzymes and then absorb the external products of digestion (decomposers)
mixotrophes - some unicellular organisms ocassionally use both forms of nutrition, depending on the resource availability
The supply of inorganic nutrients on Earth is finite, so the chemical elements are constantly recycled.
autotrophs obtain inorganic nutrients from air, water and soil and convert them into organic compounds
heterotrophs ingest the organic compounds and use them for growth and resporation, releasing inorganic byproducts
when organisms die, saprotrophs decompose the remains and free inorganic materials into the soil
the return of inorganic materials to the soil ensures the continual supply of raw materials for the autotrophs
Energy enters most ecosystems as sunlight and is converted into chemical energy by the producers in photosynthesis. This chemical energy is stired in carbon compounds (organic molecules) and is transferred to heterotrophs when they feed on plants (producers are the first trophic level)
Primary consumers feed on plants (second trophic level)
Further consumers may occupy subsequent trophic levels.
methanogens are archaean microorganisms that produce methane (CH4) as a metabolic by-product in anaerobic conditions (wetlands, marine sediments, digestive tracts of ruminants animals
acetic acid —> methane + carbon dioxide
CH3COO- + H+ —> CH4 + 2H2O
carbon dioxide + hydrogen —> methane + water
CO2 + 4H2 —> CH4 + 2H2O
Methane can either accumulate under the ground or diffuse into the atmosphere
Mathane persists in the atmosphere for ~12 years and naturally oxidizes to form carbon dioxide and water
CH4 + 2O2 —> CO2 + 2H2O
This is why methane levels in the atmosphere are not very large, even though significant quantities are being produced
saprotrophic bacteria in soil decompose dead organisms and return nutrients to the soil (this process requires oxygen, as the cell resporation is meeded to fuel digestive reactions)
waterlogged regions lack oxigenated air spaces - anaerobic conditions
organic acids are produced in anaerobic respiration, resulting in acidic conditions
saprotrophs cannot function effectively on anaerobic/acidic conditions, preventing decomposition and forming peat
when deposits of peat are copressed under sediments, heat and pressure force out impurities and remove moisture
remaining material has a high carbon concentration and undergoes chemical transformation to produce coal
they are formed as the result of the decay of marine organisms on the ocean floor
sediments (clay, mud) are deposited on top of the organic matter, creating anoxic conditions to prevent decomposition
burial and compaction causes the organic material to be heated and hydrocarbons are formed
hydrocarbons form oil and gas, which are forced out of the source rock and accumulate in porous rocks, such as sandstone
this process takes millions of years
Climate conditions
rates of photosynthesis are highers in summer seasons (more daulight)
oceanic temperatures determine how much carbon is stored in the water
events like El Niño and La Niña change the rate of carbon flux between ocean and atmosphere
melting of polar ice caps results in the decomposition of frozen detritus
Natural events
forest fires release CO2 + loss of trees decreases the rate of photosynthesis
vulcanic eruptions release CO2
Human activity
deforestation
increased numbers of ruminant lifestock (e.g. cows) = higher levels of methane
burning fossil fuels
Atmospheric gases that absorb and emit long-wave (infrared) radiation, thereby trapping and holding heat within the atmosphere. They collectively make up < 1% of the Earth’s atmosphere
water vapour
CO2
methane
nitrogen oxides (from vehicles and some bacteria)
ability to absorb long-wave radiation - gases that have a greater capacity to absorb long-wave radiation will have a greater warming impact per molecule
concentration in the atmosphere - determined by the rate of release and persistence within the atmosphere
A natural process whereby the atmosphere acquires the ability to trap and retain heat. It ensures that the Earth maintains the moderate temperature needed by organisms to maintain life processes (homeostasis) and that the temperature differences between night and day are not too big and rapid.
incoming radiation from the sun is a shorter wave radiation (UV and visible light)
the surface of the Earth absorbs short-wave radiation and re-emits it at a longer wavelength (IR - heat)
greenhouse gases absorb and re-radiate this longer wave rafiation and hence retain the heat within the atmosphere
more frequent and extreme weather conditions (heat waves, cyclones, tropical storms)
some areas will become more drought affected and some will become more prone to periods of heavy rainfall
changes to circulating ocean currents - longer El Niño (warming) and La Niña (cooling) events
oceans are a major carbon sink and absorb ~33% of all human produced (antrophomorphic) CO2
CO2 solubility is temperature-dependent (more soluble when cooler), so the higher the temperature the less CO2 will be absorbed
when ocean absorbs CO2, some of it remains as dissolved gas and some is chemically modified
CO2 can combine with water to form H2CO3, which dissociates into H+ ions and CO3^2-
H+ ions lower the ocean pH (acidification) and combine with free carbonate ions (Ca^2+) to form hydrogen carbonate
with less free carbonate ions in water, marine organism are less able to produce calcium carbonate (via calcification) used to form exoskeletons and shells
it threatens the vaiblity of coral reefs and molluscs
since the start of industrial revolution ocean pH has dropped from 8.2 to 8.1 (~30% increase in acidity), and if currentbconditions continue, it is predicted that oceanic pH could fall to 7.8 by the end of the century