16/09/2014 Ecology Biology 20 Study of the interactions between organisms and their physical environment and with each other. Equilibrium in the Biosphere Biosphere the part of the earth that is inhabited by organisms . 3 parts: 1 Lithosphere Land 2 Hydrosphere water 3 Atmosphere The gasses that surround the Earth. Living vs. Non-living There are two factors which make up the biosphere. Biotic Factors Living components of the biosphere plants and animals… Abiotic Factors Non-living components of the biosphere minerals, water, weather... 1 16/09/2014 Interactions Within the Biosphere Levels of Organization Abiotic vs Biotic When a non-living factor affects a living factor. i.e. The weather affecting a living organism Biotic vs. Biotic When a living factor affects another living factor. i.e. Two organisms fighting for the same food. Biotic vs. Abiotic Abiotic vs. Abiotic Levels of organization Cell Tissue Organ System Hierarchical Levels within the Biosphere Biosphere World Ecosystem Lake or River Organism Population Community Lots of different species of organisms Ecosystem Community Population Lots of same species of fish Organism Fish Biome Biosphere 2 16/09/2014 Important Definitions Population: group of individuals of the same: species, place & time Community: populations of all species in an area Ecosystem: community and its biotic and abiotic factors Interactions Biome: large scale ecosystems Can be found around the world tundra, grassland General Terms Autotroph Producer Photosynthesis Light energy used to make organic compounds (glucose) Done by chloroplast containing organisms (plants, algae) Chemosynthesis Energy released by chemical reactions to make a sugar Oxidizing hydrogen sulfide or methane Done by bacteria in extreme environments (deep sea vents, hot springs) More General Terms More General Terms Heterotroph Herbivore Consumer A Primary consumer eats a producer A Secondary consumer eats a primary consumer A Tertiary consumer eats a secondary consumer… An organism that only eats plants. Rabbit, squirrel Carnivore An organism that only eats animals. Wolf, Lion, Tyrannosaurus Rex Omnivore An organism that eats both plants and animals. Bear, Human 3 16/09/2014 More General Terms Scavenger An organism that feeds on dead organisms or the wastes of organisms. Vulture, Seagull, Decomposer An organism that breaks down organic wastes and the remains of dead organisms into simpler compounds such as: carbon dioxide ammonia Water Food chains Input energy Biogeochemical Ecosystems are OPEN SYSTEMS. Energy and matter can flow in and out of system Food Chain A linear illustration that represents the step sequence of who eats whom in the biosphere. used to show: energy transfers Two Types Cycles Grazer: plant, herbivore, carnivore Detritus: organic waste, scavengers, decomposers Energy Lost 4 16/09/2014 Food chains Food Chain Characteristics: Energy is transferred from organism to organism Each time energy is transferred about 90% is lost as heat or used for life processes Lost as heat during cellular respiration, stored in an unusable form, metabolized by the organism itself for ATP to live Note that: the arrow points at the eater the arrows separate trophic (eating) levels Trophic Levels Trophic level: how far an organism is from the original energy source Plants – first trophic level Original energy is from the sun When an organism is ingested by another, energy is transferred Plant – mouse – owl Producer – primary consumer – secondary consumer (top carnivore) T1 – T2 – T3 5 16/09/2014 Food Webs What would happen if we relied on deer for our food? In reality, a consumer relies on more than one food source If one source is scarce, consumer can eat more of something else Food web: a series of interlocking food chains Food Web ABCD represent different trophic levels. Level D represents the decomposers more accurately represents energy pathways who eats whom… really 6 16/09/2014 Laws of Thermodynamics Biosphere requires a constant flow of energy Energy flows one way through the biosphere following basic scientific principles called the laws of thermodynamics Laws of Thermodynamics First Law Second Law Energy can be changed in form, but not created or destroyed. (Law of conservation of energy) Any energy change results in loss of energy as heat Energy input = Energy Output Energy input desired energy + waste energy 7 16/09/2014 Energy Flow About 10% of the energy is transferred from one trophic level to the next. During any change, some of the energy is lost as waste energy or heat. Applied to an ecosystem, as energy flows through the community there is energy loss at each trophic level. Much of this loss is in the form of heat which is lost when food molecules are broken down in the cells. There would be less energy loss in the community if consumers only fed on producers Ecological Pyramids Ecological pyramids illustrate the energy loss through the trophic levels Solar radiation transformed in plants Plants create chemical energy Plant eaten by consumer Energy lost at each transformation Higher trophic level = less energy available Number of trophic levels limited b/c of loss of energy 8 16/09/2014 Ecological Pyramids In ecological pyramids, Base -the producer populations Next Level - the primary consumers Higher levels and above -the secondary, tertiary etc. Ecological Pyramids Energy Pyramids Three types: Numbers: total number of organisms in each trophic levels Biomass: mass of dry tissue of organisms at each trophic level shows how mass decreases as you move up the food chain Energy: based on energy produced at each trophic level 9 16/09/2014 Pyramid of Numbers Pyramid of Biomass 10 16/09/2014 Human Interference in the Ecosystem Pesticides used to kill pests mosquitoes - malaria Example DDT: dichloro diphenyl trichloroethane developed as a biological weapon in WWII 1950’s - used as a pesticide for insects pesticides in food chain accumulate at each level causes loss of diversity. DDT also affects human populations found in breast milk came from sprayed crops animals that ate crops Banned in Canada and US in 1970’s Not banned in other areas - Mexico, Central America Continues to be produced as a cheap pesticide in poorer nations 11 16/09/2014 Biological amplification Pesticide concentration builds up at the top level of the pyramid toxins accumulate in fatty tissue not released in wastes Magnifies each time you move up higher trophic level - higher concentration Biogeochemical Cycles Cycling of Organic Matter 12 16/09/2014 Cycling of Organic Matter The materials used in building the bodies of living organisms are limited to the atoms and molecules that make up the planet. There is no alternative source of matter. Therefore, to maintain life on Earth, matter must be recycled. Cycling of Organic Matter Food is organic matter. Every time you eat, organic matter that was once part of other living things passes into your body. Through the process of digestion, complex organic molecules are broken down into simpler molecules. Cells use these simple molecules to build the complex molecules that become part of your own structure. Cycling of Organic Matter Decay After death, decomposer organisms make the materials available to other living things. Decomposers break down the organic matter in dead bodies and feces into small, inorganic molecules 13 16/09/2014 Properties of Water All living things need water Water can be found in the biosphere in three states Properties of Water 1. Solid (snow or ice) 2. Liquid 3. Gas ( vapour) Water is continuously entering and leaving living systems Properties of Water Water: a Polar molecule Water molecules have a positive pole and a negative pole causing water molecule to be a polar molecule Properties of Water The attraction between opposing charges of different molecules create a special hydrogen bond. Hydrogen bonds pull water molecules together Polar molecule – a molecule that has a positive and a negative end 14 16/09/2014 Biogeochemical Cycles Matter can neither be created or destroyed It cycles through the biosphere. As it cycles, it follows certain characteristic pathways These pathways are called “Biogeochemical Pathways” Biogeochemical Cycles A biogeochemical pathway can be defined as the complex cyclical transfer of nutrients ... from the environment to an organism and back to the environment. There are 3 major cycles to understand Carbon/Oxygen Cycle Bio = Life Nitrogen Cycle Geo = Earth Phosphorus Cycle The Carbon Cycle Also called the Carbon-Oxygen Cycle. Refers to the flow of CO2 through the biosphere. The Carbon Cycle The main part of this cycle involves the interrelation between cellular respiration and photosynthesis. 15 16/09/2014 Photosynthesis Cellular Respiration The Carbon Cycle Carbon dioxide is also released by the activities of : Volcanoes Glucose + O2 CO2 + H2O Automobiles Combustion of any source Uplifting and weathering The Carbon Cycle 16 16/09/2014 Reservoirs for Carbon Organic Carbon - Organic carbon is held in the bodies of all living things. - All living things die, and decomposition eventually returns the carbon to the cycle in inorganic form. - There is one important exception to this rule: Some ecosystems such as bogs, store huge quantities of carbon in organic form. Reservoirs for Carbon Inorganic Carbon When Carbon is not in organic form it may be found in three main reservoirs. 1. The Atmosphere 2. The Ocean 3. Earth’s Crust - Peat Human Impact on the Carbon Cycle Human have modified the global carbon cycle by: Mining fossil fuels and burning them, releasing carbon from organic reservoirs faster than normal. Humans are also increasing the amount of carbon dioxide in the inorganic reservoir by clearing away vegetation in order to build or farm. The Nitrogen and Phosphorus Cycles Oceans can hold only so much carbon dioxide 17 16/09/2014 The Nitrogen Cycle The complex cycling of nitrogen between organisms and the environment. The air is 79% nitrogen. The main component of most fertilizers is a nitrogen compound. Nitrogen and Animals Nitrogen is also needed for the construction of proteins and nucleic acids Muscle tissue Hair Bones Nitrogen and Plants Nitrogen is a chemical that plants need to grow well. Nitrates are a group of nitrogen containing compounds that are readily absorbed by the roots of plants Nitrogen Usage Nitrogen is usually utilized in life in the form of nitrates. There are 2 main ways atmospheric nitrogen can be converted into useful forms. 1) Lightning 2) Bacteria Cell parts DNA RNA 18 16/09/2014 Method #1 -- Lightning Lightning can force nitrogen and oxygen together to form nitrates these will fall with precipitation and be absorbed by plant roots. The plants will change these into their own proteins. Animals eat the plants and reorganize those proteins into the ones they need. Method #2 -- Bacteria These can convert atmospheric nitrogen into nitrates. Nitrogen-fixing bacteria can also be found in small lumps called nodules on the roots of legumes. Legumes can utilize atmospheric nitrogen Legumes are members of the bean family and include: Clover and Alfalfa… Legumes 19 16/09/2014 Nitrogen and decomposers After an organism dies, it decays. Decaying matter which contains nitrogen produces ammonia. Ammonia will degrade into nitrites. Nitrites will degrade into nitrates. The nitrates will now re-enter the cycle. Bacteria Some bacteria will actually convert the nitrates back into atmospheric nitrogen. Denitrifying bacteria. These bacteria do not need oxygen -- anaerobic respiration. 20 16/09/2014 Denitrification Atmospheric pool of nitrogen Lightning the process in which nitrates are converted to nitrites and then to nitrogen gas Fertilizers 1 2 3 4 5 6 7 8 9 10 11 12 Nitrogen-fixing bacteria in root nodules of legumes Atmospheric pool of nitrogen Nitrogen-fixing bacteria in root nodules of legumes Fertilizers Soil nitrate Nitrate take up by plant roots Plant and animal proteins Dead organisms Decomposers Nitrate bacteria Nitrate bacteria Denitrifying bacteria Lightning 21 16/09/2014 a Atmospheric nitrogen b Lightning causes oxygen to react with nitrogen c Rain dissolves the oxides of nitrogen that are formed d Fertilizer e Soil f Nitrogen-fixing plants (legumes) g Plants use nitrate to make protein h Plants are eaten by animals i Excretion j Death k Bacterial decomposition of nitrates to nitrogen Phosphorus Cycle Phosphorus is a nutrient required by all living things. Component of bones and teeth DNA ATP Phosphorus Cycle is simpler than the carbon or nitrogen cycles because it does not involve movement through the atmosphere. The Phosphorus Cycle Phosphorus is used in only one important inorganic form… Phosphate Ion (PO43-) Plants absorb this through their roots. After plants incorporate phosphorus... it is transferred through the food chain it is eventually returned to the soil. excretions of animals actions of decomposers. 22 16/09/2014 The Phosphorus Cycle Two methods of P recycling: geological (abiotic Long-term cycle) living organisms (biotic short-term cycle) Long Term Cycle Most common form: a part of rocks Properties: soluble - dissolve in water Phosphates dissolve in water—erosion (weathering) carries them from land to streams and rivers and then finally to the oceans Oceans sediments may be thrust upward (uplifting) and once again form land through geological activity The Phosphorus Cycle Long Term Cycle The weathering of rocks gradually adds phosphorus to the soil and to the waterways. 23 16/09/2014 Short Term Cycle Short Term Cycle Phosphates in water also enter the food chain through photosynthetic organisms Decomposition of dead organisms soluble phosphates are absorbed by plants and used during photosynthesis Plants are eaten by animals Phosphorous Cycle 24 16/09/2014 Roles in Ecosystems Each organism has its own place within an ecosystem. Ecological niche – an organism’s role in an ecosystem, consisting of its place in the food web, its habitat, its breeding area and time of day at which it is most active. Roles in Ecosystems Each species in an ecosystem tends to have a different niche, a different role to play. This helps to reduce competition between species. E.g. Even if two species eat the same food they are not in competition because they may: Live in different places Eat at different times Roles in Ecosystems E.g. Owls and hawks feed on many of the same organisms, but occupy distinctly different niches. Owls hunt down prey with in forests Hawk hunt down prey in grassland and open fields Owls are active during dusk and at night Hawk hunt by daylight Competition is further reduced because owls and hawks nest in different areas. 25 16/09/2014 Competition for Niches When a new species enter an ecosystem, it causes a disturbance because it comes into competition for a niche with one or more of the species already in the ecosystem. Exotic species – species that are not native to an ecosystem The introduction of new species happens naturally. Animals are mobile and can move from one ecosystem to another. Introduction of Exotic species The introduction of new species by humans to an ecosystem is one of the main causes of species depletion and extinction, second only to habitat loss. Problems with introducing Exotic Species: No natural population controls ( predators or diseases) Native species may not be able to compete for space, food or reproductive sites. Prey organisms may not have defense mechanisms. 26 16/09/2014 Introduction of Exotic species The actual number of introduced species that have established themselves in Canada is well over 300 species. Supporting Biodiversity in Terrestrial Ecosystems Limiting Factors in Terrestrial Ecosystems 27 16/09/2014 Limiting Factors Terrestrial ecosystems are ecosystems that are found anywhere on Earth that is not covered by water. Despite their many differences in each terrestrial region biotic and abiotic factors are interdependent. These factors can limit the size of populations and can also determine the number of species that survive in each ecosystem. Abiotic Factors that can limit Terrestrial ecosystems: 1. Soil 2. Available Water 3. Temperature 4. Sunlight Soil The quality and amount of soil are critical factors in determining the size and health of the plant community and the biodiversity of an ecosystem. Soil Soil pH Humans have been contributing to higher levels of acidity in many soils by burning fossil fuels. Burning of fossil fuels release sulphur dioxide and nitrogen oxides into the air which fall to earth as acid deposition. Acid deposition – the process by which sulphur dioxide and nitrogen oxides in the atmosphere form acidic compounds and fall to Earth’s surface. (Acid rain is an example of acid deposition) 28 16/09/2014 Available Water The amount of available water in an ecosystem help determine the size and health of populations and the biodiversity of an ecosystem. Sunlight The amount of sunlight determines what plants will grow in an ecosystem. In ecosystems around the equator receive more or less the same amount of daily sunlight. Regions at more southern or northern latitudes experience changes in the amount of sunlight during different times of the year. Temperature Temperature affects both biotic and abiotic factors. Temperature can vary significantly throughout the year in an ecosystem. Taiga In a forest, the amount of sunlight varies from the top of the canopy to the forest floor. In Taiga biomes, the mature trees are mostly conifers like spruce and pine These trees can only support certain types of birds that have tough beaks for cracking open cones and nuts 29 16/09/2014 Taiga Taiga Year-round, these trees block the sunlight from reaching the forest floor This determines the types of plants that can grow below the canopy In the Taiga, we see shade loving plants like shrubs, mosses and ferns Due to the low growth on the forest floor, nesting animals are only successful if they are suitably camouflaged These plants then determine which primary consumers exist in this ecosystem Deer and moose Deciduous Forests Have higher temperatures and precipitation than Taiga Also have more humus Decaying plant and animal matter These conditions lead to a richer soil and support growth of deciduous trees 30 16/09/2014 Deciduous Forests Spring: sun can reach all the way to forest floor Summer: Canopy is full, so very little sun gets to the understorey. This is ok, because the understorey had the chance to grow in the spring and is already mature Resulting in support for a diverse range of organisms Deciduous Forests Lots of leaf litter Many different insects Full understorey Moose and deer Leafy canopy Variety of birds and climbing mammals Limiting factors of Aquatic Ecosystems Limiting Factors in Aquatic Ecosystems Like terrestrial ecosystems, aquatic ecosystems are limited by abiotic factors: 1. Chemical environment 2. Light levels 3. Temperature 31 16/09/2014 Chemical environment 1. The type of water: Freshwater Saltwater Chemical environment 2. Chemical environment The amount of oxygen dissolved in the water. The amount of dissolved oxygen depends on: Temperature (warmer water holds less) Pressure (more oxygen dissolved at sea level than mountain streams) 3. Any other dissolved substance E.g., Naturally occurring minerals, and organic pollutants. And the amount of salt and other substances dissolved in the water (more salt, less oxygen) 32 16/09/2014 Light Levels and Temperature Light and temperature in an aquatic ecosystem may vary over the course of the year (seasonal changes), But these factors are also affected by the depth of the water. Depending on the depth of the body of water the amount of light available, the temperature and oxygen levels can all vary. This will have a significant impact on what organisms you can find. Littoral Zone the area extending out from the lakeshore to the point where you can no longer find plants rooted. Most productive part of the lake. High amount of sunlight. Zones within Aquatic Ecosystems Littoral Limnetic Profundal Limnetic zone the area of a lake or pond in which there is open water and sufficient light for photosynthesis to occur. Most common form of organism in the zone is plankton (small autotrophic and heterotrophic microorganisms. 33 16/09/2014 Profundal zone the region of a lake beneath the limnetic zone, in which there is insufficient light for photosynthesis to occur. Most of the time only sources of nutrients in the zone are dead plants and animals that fall from the limnetic zone. Low oxygen due to bacteria decomposing dead organic matter. No sunlight, no photosynthesis. Lake Ecosystems 1. Oligotrophic Changes in Lake Ecosystems Lakes are typically deep and cold. Nutrient levels are low limiting size of producer populations. Limited numbers of only a few kinds of organisms. Water usually very clear. 34 16/09/2014 Lake Ecosystems 2. Eutrophic Eutrophication Lakes are generally shallow and warmer. In general oligotrophic lakes gradually become eutrophic over time and eventually filling in and becoming dry land. Very good supply of nutrients. This process is call eutrophication. Many species of photosynthetic organisms. Water is often murky. Eutrophication Eutrophication 35 16/09/2014 Eutrophication Eutrophication Human sometimes accelerate eutrophication by adding nutrients to lakes: Human wastes Fertilizers Household and Industrial products Thermal energy 36