IB Biology: Ecology
19 flashcards · Other · by Gabrielle Wong
Species: group of organisms capable of producing fertile offspring together, have similar morphological characteristics, and a common gene pool
Some limitations to this definition include: hybrid species infertility geographical separation Species -> Population -> Community -> Ecosystem
Population: group of members of a species living together
Species -> Population -> Community -> Ecosystem
Community: members of different species living and interacting together
Species -> Population -> Community -> Ecosystem
Ecosystem: the interaction of biotic and abiotic elements of the envrionment
Species -> Population -> Community -> Ecosystem
Autotroph: able to produce own food (usually through the process of photosynthesis)
Examples: grass, algae, trees, certain types of bacteria
Heterotroph: must obtain food by consuming it
Examples: zooplankton, fish, insects
Saprotoph: a consumer and decomposer, releasing digestive enzymes to speed up the brocess of decay
Examples: bacteria, funghi
Detrivore: a consumer and decomposer that feeds on non-living organic matter such as leaves and carcasses
Examples: earthworms, wood lice, dung beetles
Trophic levels: feeding levels for organsisms
Trophic levels are: Producer Primary consumer Secondary consumer Tertiary Consumer Apex Predator
Biomass: The total amount of dry organic matter that is found in an ecosystem or area
Biomass can be used to measure the rate of photosynthesis :D
Pyramid of energy: graphic model to illustrate the flow of energy through an ecosystem, each level is 10-20% of the level before it
Rules of heat and energy: heat can't be created or destroyed, only converted only 10-20% of an organism's energy is available when consumed (not all of an organism is consumable, cellular respiration, death and decay)
Greenhouse effect: ability to retain heat and warmth without sunlight
The problem is the enchanced greenhouse effect, not the greenhouse effect itself, which is important for life on earth
Greenhouse gases: Gasses that trap outgoing long wavelength radiation (heat) in the atmosphere. These include carbon dioxide and water vapor, and to a smaller effect, methane and nitrogen oxides. As a result, they warm the earth through the absorption and re-radiation of heat
The concentration of CO2 in the atmosphere is now at over 400 ppm Not all greenhouse gases have the trapping power - methane, for instance, is over 86x more powerful than CO2
Carbon cycle: movement of carbon in the ecosystem
See visual in study aids
Carbon sequestration: trapping of carbon
The storage of carbon shells and sediment in limestone is an example of carbon sequestration.
Formation of peat: peat is acidic/waterlogged soil made of at least 30% dead organic matter It forms in spongy, anaerobic conditions like wetlands
Formation of methane: produced by cows when they burp due to archaea and metabolism of food
Formation of coal: formed through the partial decomposition of peat
compression of peat with sediment increased pressure exposure to higher temperatures lithification
Formation of oil and gas: geological transformations form over many years
dead reamins produce silt lipids decompose less and form keorgen geological transformations eventually lead to oil and/or natural gas