IB Biology HL - Ecology

A soecies is a group of organisms that can potentially interbreed to produce fertile, viable offspring.

Organisms resulting from cross-breeding of two different, but closely related species. They are reproductively sterile.

A population is a group of organisms of the same species living in the same area at the same time

Community is a group of populations living together and interacting with each other within a given area.

Habitat is the environment in which a species normally lives, or the location of a living organism.

Ecosystem is a community and its abiotic environment (habitat).

Ecology is the study of the relationship between living organisms, or between living organisms and their environment.

• 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

It is the method used to determine the presence of two species within a given environment.

A quadrat is a rectendular frame of known dimensions that can be used to establish population densities. Quadrats are placed inside a defined area, either in random or designed arrangement. The number of individuals of a given species is either counted or estimated via percentage coverage. The sampling process is repeated many times to gain the representative data set.

In each quadrat, the presence or absence of each species is identified, allowing for the number of quadrats where both species were present to be compared against the total number of quadrats.

It is an effective method to count plants and sessile animals, but not motile organisms.

Chi square test can be used to test for association between the presence of both species.

Sunlight (in rare cases the producers are chemoautotrophic bacteria).

1. 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)

2. Primary consumers feed on plants (second trophic level)

3. Further consumers may occupy subsequent trophic levels.

The position that the organism occupies within a feeding sequence.

A graphical representation of the linear feeding relationships between species in a community.

Chemical energy produced by an organism can be converted into kinetic, electrical or even light energy, but it is accompanied by an energy loss in the form of evolved heat.

Living organism cannot turn the heat into other forms of usable energy, so it is lost from the ecosystem. That is why ecosystems require a continuous influx of energy from an external source, such as sun.

Typically, energy transformations are ~10% efficient, with about 90% of available energy being lost between trophic levels (the exact values depend on the certain organism’s ability to efficiently capture and use energy).

Most energy is lost to the organism - either used in respiration, released as heat, excreted in faeces or unconsumed.

Consequently, hugher trophic levels strore less energy as carbon compounds and have less biomass. It is because the subsequent trophic levels receive less and less energy from feeding, so they have to eat more to obtain sufficient nutrients. It also causes them to expend more energy hunting for food. Eventually, when the energy required to hunt orey exceeds the energy available from the food eaten, the trophic level becomes unviable - this is why the number of trophic levels is limited.

The tital mass of a group of organisms - consisting of the carbon compounds contained in cells and tissues.

A graphical representation of the amount of energy at each trophic level of a food chain, expressed in units of energy per area per time.

The carbon cycle is a biogeological cycle whereby carbon is exchanged between the different spheres of the Earth (atmosphere, litosphere, hydrosphere and biosphere)

• carbon dioxide from the atmosphere dissolves in water

• some of it remains as dissolved gas, the remainder combines with water to form carbonic acid (CO2 + H2O <—> H2CO3)

• carbonic acid dissociates to form hydrogen carbonate ions (H2CO3 <—> HCO3- + H+)

• this conversion also releases H+ ions, which is why pH changes when CO2 is dissolved in water (it becomes more acidic)

• autotrophs absorb both dissolved CO2 and HCO3- ions and use them to produce organic compounds

• when HCO3- ions come into contact with the rocks and sediments on the ocean floor and aquire metal ions, forming calcium carbonate and limestone

• living animals also combine HCO3- with calcium to form calcium carbonate that they use to build exoskeletons (e.g. corals) and shells. When the organism dies and settles to the sea floor, these hard components may become fossilized in limestone

• 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

Carbon fluxes describe the rate of exchange of carbon between various carbon sinks (litosphere - earth crust, hydrosphere - oceans, atmosphere - air, biosphere - organisms)

Nope. Estimations are made and usually they involve large uncertainties fur to variety of sources and the size of fluxes.

1. 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

2. Natural events

   • forest fires release CO2 + loss of trees decreases the rate of photosynthesis

   • vulcanic eruptions release CO2

3. 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