Chapter 24 Lecture Outline See separate PowerPoint slides for all figures and tables preinserted into PowerPoint without notes. Copyright © 2016 McGraw-Hill Education. Permission required for reproduction or display. 1 Global Ecology and Human Interferences 2 Points to ponder • What is an ecosystem and what are its biotic components? • What are energy flow and chemical cycling in an ecosystem? • What are the two major ecosystems on earth? • Describe the three types of terrestrial ecosystems and the two types of aquatic ecosystems. • Compare and contrast food webs and food pyramids. • What is a biogeochemical cycle? • What is a reservoir and an exchange pool? 3 Points to ponder • Explain the water, carbon, nitrogen, and phosphorus cycles. • What human activities interfere with these cycles? • What problems are we creating by altering these pathways? • What is biomagnification and why is mercury a concern? 4 24.1 The Nature of Ecosystems The nature of ecosystems • Biosphere – the regions of the Earth’s waters, crust, and atmosphere inhabited by living organisms • Ecosystem – a place where organisms interact with each other and their environment – – Terrestrial: several distinct types based on temperature and waterfall Aquatic: freshwater and marine 5 24.1 The Nature of Ecosystems Terrestrial ecosystems • Forests – dominated by trees • • • • Tropical rain forest Coniferous forests (taiga) Temperate deciduous forests Grasslands – dominated by grass • • Tropical grasslands Temperate grasslands (prairie) 6 24.1 The Nature of Ecosystems Terrestrial ecosystems • Deserts – characterized by lack of available moisture • • Tundra Deserts 7 24.1 The Nature of Ecosystems Terrestrial ecosystems Figure 24.1 The distribution of the major terrestrial biomes. 8 24.1 The Nature of Ecosystems Aquatic ecosystems • Marine • • • • • Seashores Oceans Coral reefs Estuaries Freshwater • • • • Lakes Ponds Rivers Streams 9 24.1 The Nature of Ecosystems Aquatic ecosystems Figure 24.2 Examples of freshwater and saltwater ecosystems. Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. a. c. b. d. a: © Francois Gohier/Photo Researchers; b: © The McGraw-Hill Companies, Inc. Carlyn Iverson, photographer; c: © David Hall/Photo Researchers; d: © Vol. 121/Corbis RF 10 24.1 The Nature of Ecosystems Components of an ecosystem • Abiotic components – nonliving environment • Biotic components - living components • • Autotrophs – producers Heterotrophs – consumers • Herbivores – feed on plants and algae • Carnivores – feed on other animals • Omnivores – eat both plants and animals • Detritus feeders – feed on decomposing organic matter 11 24.1 The Nature of Ecosystems Components of an ecosystem • Niche – the role an organism plays in an ecosystem such as how it gets its food, what it eats, and how it interacts with other organisms 12 24.1 The Nature of Ecosystems Biotic components of an ecosystem Figure 24.3 The biotic components of an ecosystem. 13 24.1 The Nature of Ecosystems Energy flow and chemical cycling • Energy flow • It begins and continues when producers absorb solar energy. • Energy flow occurs as nutrients pass from one population to another. • This energy is converted to heat that dissipates into the environment. • Only a portion of energy is passed to organisms as they consume one another. 14 24.1 The Nature of Ecosystems Energy flow and chemical cycling • Chemical cycling • Inorganic nutrients are returned to producers from the atmosphere or soil. • Chemicals recycle within and between ecosystems. 15 24.1 The Nature of Ecosystems Energy flow and chemical cycling Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. solar energy heat producers consumers inorganic nutrient pool heat Figure 24.4 Energy flow and chemical cycling in an ecosystem. energy heat decomposers nutrients 16 24.1 The Nature of Ecosystems Fate of food energy taken in by an herbivore Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Heat to environment growth and reproduction Energy to carnivores Energy to detritus feeders Figure 24.5 The fate of food energy taken in by an herbivore. © George D. Lepp/Photo Researchers, Inc. 17 24.2 Energy Flow Energy flow • Food web – describes who eats whom • Grazing food web • Detrital food web • Trophic levels – composed of all organisms that feed at a particular link in the food chain • Producers, primary consumers, and secondary consumers 18 24.2 Energy Flow Energy flow • Ecological pyramid – reflects the loss of energy from one trophic level to another • Only about 10% of the energy of one trophic level is available to the next trophic level 19 24.2 Energy Flow Food webs Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Autotrophs Herbivores/Omnivores Carnivores owls nuts birds hawks leaf-eating insects deer foxes leaves chipmunks rabbits skunks snakes detritus mice mice a. death death Figure 24.6 Food webs illustrate ecological relationships. fungi and bacteria in detritus b. death invertebrates carnivorous invertebrates salamanders shrews 20 24.2 Energy Flow An example of a food pyramid Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. top carnivores 1.5g/m2 carnivores 11g/m2 herbivores 37g/m2 producers 809g/m2 Figure 24.7 The influence of trophic level on biomass. 21 24.3 Global Biogeochemical Cycles Biogeochemical cycles • Biogeochemical cycles are pathways by which chemicals circulate through an ecosystem. 1. Water cycle 2. Carbon cycle 3. Nitrogen cycle 4. Phosphorus cycle 22 24.3 Global Biogeochemical Cycles Biogeochemical cycles • Reservoir – fossil fuels, minerals in rocks, and sediments in oceans contain inorganic nutrients that are limited in availability • Exchange pools – atmosphere, soil, and water are ready sources of inorganic nutrients 23 24.3 Global Biogeochemical Cycles Biogeochemical cycles Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Reservoir • fossilfuels • mineral in rocks • sediment in oceans Exchange Pool • atmosphere • soil • water Community Figure 24.8 The cycling of nutrients between biotic communities and biogeochemical reservoirs. 24 24.3 Global Biogeochemical Cycles Water cycle • Water evaporates from bodies of water, land, and plants, and returns when water falls on land to enter the ground, surface waters, or aquifers. 25 24.3 Global Biogeochemical Cycles Water cycle • Human activities that interfere • • • Withdrawing water from aquifers Clearing vegetation from the land and building structures that prevent percolation and increase runoff Adding pollutants to water such as sewage and chemicals 26 24.3 Global Biogeochemical Cycles Water cycle Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. 3 transpiration from plants and evaporation from soil H2O in Atmosphere 2 precipitation over land transport of water vapor by wind lake 1 evaporation from ocean 2 precipitation to ocean 5 fresh water runoff 6 aquifer Ocean I ce 4 Groundwaters Figure 24.9 The hydrologic (water) cycle. 27 24.3 Global Biogeochemical Cycles Carbon cycle • CO2 is exchanged between the atmosphere and living organisms. • Plants incorporate atmospheric CO2 into nutrients through photosynthesis, providing food for themselves and other organisms. • CO2 is returned to the atmosphere through respiration. 28 24.3 Global Biogeochemical Cycles Carbon cycle Figure 24.10 The carbon cycle. 29 24.3 Global Biogeochemical Cycles Carbon cycle • Human activities that interfere • Burning of fossil fuels and the destruction of forests are adding CO2 to the atmosphere faster than it is being removed. • CO2 and other gases (N2O and CH4) are being emitted due to human activities. • These gases are called greenhouse gases because they trap heat; this contributes to global warming. 30 24.3 Global Biogeochemical Cycles Global warming and climate change Figure 24.11 Global warming and climate change. 31 24.3 Global Biogeochemical Cycles Nitrogen cycle • 78% of the atmosphere is nitrogen gas (N2) but plants cannot use this form. • Nitrogen-fixing bacteria convert nitrogen gas to ammonium (NH4+), which can be used by plants. • Nitrifying bacteria convert ammonium to nitrate (NO3-). • Bacteria convert nitrate back to nitrogen gas through a process called denitrification. 32 24.3 Global Biogeochemical Cycles Nitrogen cycle Figure 24.12 The nitrogen cycle. 33 24.3 Global Biogeochemical Cycles Nitrogen cycle • Human activities that interfere • We add nitrogen fertilizers that run off into lakes and streams, causing major fish kills by eutrophication. • Burning of fossil fuels - It puts nitrogen oxides and sulfur dioxide into the atmosphere, where they combine with water vapor to form acids that return to earth as acid deposition. - It results in nitrogen oxides and hydrocarbons that react with one another to produce smog. 34 24.3 Global Biogeochemical Cycles Thermal inversions and smog • During a thermal inversion, pollutants are trapped near the Earth. – The air does not circulate, so pollutants can build up to dangerous levels. Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. cooler air cool air warm air a. Normal pattern cool air warm inversion layer cool air b. Thermal inversion Figure 24.14 Thermal inversions. 35 24.3 Global Biogeochemical Cycles Nitrogen cycle Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. a. c. b. a: © Larry Lee Photography/Corbis RF; b: © Oxford Scientific/Photolibrary/Getty Images; c: © Sue Baker/Photo Researchers Figure 24.13 The effects of acid deposition. 36 24.3 Global Biogeochemical Cycles Phosphorus cycle • Phosphate ions become available to living organisms by the slow weathering of rocks. • Phosphate is a limiting nutrient in ecosystems. Figure 24.15 The phosphorus cycle. 37 24.3 Global Biogeochemical Cycles Phosphorus cycle • Human activities that interfere • Runoff of phosphate due to fertilizer and discharge from sewage treatment plants results in eutrophication. • Sources of water pollution - Point sources are the easily identifiable sources. Nonpoint sources cannot be specifically identified (e.g., runoff). 38 24.3 Global Biogeochemical Cycles Biomagnification of mercury • • • • Emissions of mercury into the environment can lead to serious health effects for humans, fish, and wildlife. There is widespread mercury contamination in streams, wetlands, reservoirs, and lakes throughout most of the U.S. Bioaccumulation occurs when an organism accumulates a contaminant such as mercury faster than it can eliminate it. Mercury enters ecosystems at the base of the food chain and increases in concentration as it moves up higher trophic levels. 39 24.3 Global Biogeochemical Cycles Sources of water pollution Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Sources of Water Pollution acidic water from mines sediments Leading to Cultural Eutrophication Oxygen-demanding waste Biodegradable organic compounds (e.g., sewage, wastes from food-processing plants, paper mills, and tanneries) Plant nutrients Nitrates and phosphates from detergents, fertilizers, and sewage treatment plants Sediments Enriched soil in water due to soil erosion Thermal discharges Heated water from power plants city crop dusting industrial wastes barnyard wastes biomedical wastes Health Hazards Disease-causing agents Synthetic organic compounds Bacteria and viruses from sewage and barnyard waste (causing, for example, cholera, food poisoning, and hepatitis) suburban development Pesticides, industrial chemicals (e.g., PCBs) fertilizer runoff Inorganic chemicals and minerals Acids from mines and air pollution; dissolved salts; heavy metals (e.g., mercury) from industry Radiation Radioactive substances from nuclear power plants, medical and research facilities sewage treatment plant oil pollution nuclear reactor Figure 24.16 Some sources of surface water pollution. 40
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