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Ecology The scientific study of the relationships among living organisms and the interaction they have with the environment Part 1: Organisms and Their Relationships Part 2: Flow of Energy in an Ecosystem Part 3: Cycling of Matter Day 1 Organisms and Their Relationships First, let’s review: What is a “Living Thing”? 1. 2. 3. 4. 5. 6. Composed of cells. Complex organization patterns Use energy. Have stable internal conditions. Grow and change. Reproduce Biotic and Abiotic Factors Biotic • The living factors in an organism’s environment Abiotic • The nonliving factors in an organism’s environment Biotic or Abiotic? (Make a Venn Diagram with your group) • • • • • • • • • • • • • Whale Clock Water Fish Paper Glass Aluminum Wooden Ruler Sand Clouds Corpse Snail Steak • • • • • • • • • • • • • Pork Chops Salad Bread Plant Hair Finger Nails Pipe Cotton Fabric Wool Gold Plastic Grapes Air Levels of Organization We have covered very small living things. Just to review, let’s start with the cell… Cell Tissues Organs Organisms Population Biological Community Ecosystem Biome Biosphere Levels of Organization • Organism: An individual • Population: Organisms of a single species that share the same geographic location • Community: A group of interacting populations (different species) that occupy the same area at the same time. Levels of Organization • Ecosystem: A community and all of the abiotic factors that affect it. • Biome: A large group of ecosystems that share the same climate and have similar types of communities. • Biosphere: All biomes together; the Earth Community Interactions • Competition: More than one organism uses a resource at the same time. • Predation: The act of one organism consuming another organism for food. • Symbiosis: The close relationship that exists when two or more species live together. Symbiotic relationships • Mutualism: When both organisms benefit (ex. Lichen = photosynthetic algae and fungus) Algae provides food (sugar) for the fungus Fungus provides algae with water • Commensalism: One organism benefits, while the other is neither helped nor harmed. • Parasitism: One organism benefits at the expense of the other. Ecosystem Interactions • Habitat: An area where an organism lives • Niche: The role or position that an organism has in its environment Day 2 Flow of Energy in an Ecosystem Flow of Energy in an Ecosystem • Autotroph: An organism that collects energy from sunlight or inorganic substances to produce food. (Producer) • Heterotroph: An organism that gets its energy requirements by consuming other organisms. (Consumer) Different types of Heterotrophs • Herbivore: Eats only plants – (Deer, rabbits, grasshoppers, etc.) • Carnivore: Prey on other heterotrophs – (Wolves, lions, cats, etc.) • Omnivore: Eat both plants and animals – (Bears, humans, mockingbirds, etc.) • Detritivore: Eat fragments of dead matter – (Worms, organisms on stream bottoms, fungi) Models of Energy Flow • Trophic Levels: Each step in a food chain or food web. – Autotrophs always make up the first trophic level in ecosystems. – Heterotrophs make up the remaining levels Models of Energy Flow • Food chains: A simple model that shows how energy flows through an ecosystem Models of Energy Flow • Food webs: Show flow of energy through many interconnected food chains How many connections can we make? Activity: Deadly Links (In your IntNB, record the following) • Objective: To understand how food (energy) moves through an ecosystem and to understand the phenomonon called “biological magnification.” • My assigned role in this food chain is ____________. Now that you have completed the activity… Explain in your interactive notebook: 1) What happened to the animals at each level of the food web 2) Summarize your understanding of biological magnification Warm-up Activities • Flow of Energy in an Ecosystem question 4 (121) • do page 123-125 • Do page 129-130 Models of Energy Flow (page 121) • Ecological pyramids: A diagram that can show the relative amounts of energy, numbers of organisms, or biomass at each trophic level in an ecosystem. – Biomass: The total mass of living matter at each trophic level Activity #2 (page 129-130) • DDT in Real Life Day 3 Cycling of Matter Cycling of Matter • Cycles in the Biosphere – Natural processes cycle matter through the atmosphere – The exchange of matter through the biosphere is called the biogeochemical cycle. • Bio: Involves living things • Geo: Geological Processes • Chemical: Chemical Processes The Water Cycle Solar Energy Precipitation Movement of clouds by wind Evaporation Precipitation Transpiration from plants Percolation in soil The Water Cycle • Most precipitation falls into the ocean • Over land – approximately 90% of the water evaporates – 10% transpires (evaporated) from plants • Only about 2% of water is retained in a reservoir – i.e., a glacier, ice cap, aquifer or lake Carbon and Oxygen Cycles CO2 in atmosphere Burning Cellular Respiration Photosynthesis Plants, Algae & Cyanobacteria Higher level Consumers Wood & Fossil Fuels Primary Consumer Detritivores (soil microbes & others) Detritus Carbon and Oxygen Cycles Classified in two groups • Short term cycles • Long term cycles Carbon and Oxygen Cycles 1) Short term cycle – Autotrophs use CO2 for Photosynthesis ____________. – Heterotrophs produce CO2 during ________ Cellular Respiration __________. Carbon and Oxygen Cycles 2) Long term cycle: a) Fossil Fuels – – – Organic matter is buried and converted to peat, coal, oil or gas deposits. 5.5 billion tons are burned annually 3.3 billion tons stay in the atmosphere, the rest dissolves in sea water* http://www.ucar.edu/ (The National Center for Atmospheric Research) Carbon and Oxygen Cycle b) Calcium Carbonate (CaCO3) – Marine animals use Carbon to build skeleton – They fall to the bottom of the ocean, creating limestone rock. Carbon and Oxygen Cycles c) Atmosphere (atm) • 21% Oxygen (O2) is found in the atm – – – very reactive element that combines with other elements and disappear from the atmosphere. Some of the O2 is converted into Ozone (O3) in higher atm Ozone absorbs damaging UV radiation from the sun. Carbon and Oxygen Cycles d) Green house effect • Carbon dioxide (CO2) is a greenhouse gas and traps heat in the atmosphere. • 30% more CO2 in air today than 150 years ago due to human activity (burning of fossil fuels) • The atm has not held this much Carbon for at least 420,000 years http://www.ucar.edu/ (The National Center for Atmospheric Research) Nitrogen Cycle Nitrogen in atmosphere Plants Assimilation Nitrogen – fixing bacteria in root nodules of legumes Denitrifying Nitrates bacteria Decomposers (aerobic & anaerobic bacteria and fungi) Ammonification Ammonium (NH4+) Nitrogen – fixing bacteria in soil (NO3-) Nitrifying bacteria Nitrites (NO2-) Nitrogen Cycle Nitrogen is 78% of atmosphere Most is unusable. – – nitrogen gas (N2) is made of 2 strongly bonded atoms. Lots of energy needed to break these bonds, such as produced by lightning or fires Little Nitrogen on land or sea – – Bacteria can release nitrogen from organic material Bacteria can also release nitrogen from organic material back into the atm Nitrogen is a key element in proteins and DNA. Pl an kt on ea d M in no w er Pi ck er el N ee dl ef M is er h ga ns er du ck C or m or an t Sh ee ps h W at Warm-up: What does your DDT graph tell you? 30 25 20 15 10 DDT in ppm 5 0