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					Chapter 22 Ecosystems and the Biosphere 22-1 Energy Transfer  In an ecosystem, energy flows from the sun to autotrophs and then to other organisms  Autotrophs make their own food (plants and some bacteria and protists) Producers  Most producers are plants  Photosynthesis: plants use carbon dioxide, water, and solar energy to make glucose. (Oxygen is a byproduct)  6 CO2 + 6 H2O + solar energy  C6H12O6 + 6 O2 Chemosynthesis  Some species of bacteria can produce carbohydrates from inorganic molecules  Example: bacteria found along hydrothermal vents in the ocean Measuring Productivity  Gross primary productivity: the rate that producers in an ecosystem capture energy  Biomass: organic material  Only energy stored as biomass is available to other organisms Net Primary Productivity  The rate at which biomass accumulates in an ecosystem Can vary greatly in different ecosystems Influenced by light, temperature, and precipitation Consumers  Organisms that get their energy by eating other organisms  Also called heterotrophs (“other feeders”)  Examples: animals Herbivores  Consumers that eat only producers (plant eaters)  Examples: rabbits, deer, cows, sheep, grasshoppers Carnivores  Consumers that eat only other consumers (meat eaters)  Examples: coyote, bobcat, shark, alligator, hawk, owl, snakes Omnivores  Consumers that eat both plants and animals  Examples: humans, bears, pigs, gorillas, rats, raccoons, some insects Detritivores  Consumers that feed on dead organisms, animal waste, or fallen leaves and branches  Examples: vultures, maggots, carrion beetles, earthworms Decomposers  Consumers that break down dead organisms in an ecosystem (returns nutrients to soil, water, and air)  Examples: fungi and bacteria Energy Flow  Cellular respiration: breaking down food to yield energy  C6H12O6 + 6 O2  6 CO2 + 6 H2O + energy  Cells use glucose and oxygen to produce carbon dioxide, water, and energy Food Chain A sequence in which energy is transferred from one organism to the next as each organism eats another organism  Represents one strand of a food web Food Web  Shows many feeding relationships that are possible in an ecosystem DDT  Dichloro-Diphenyl-Trichloroethane  Pesticide once used to prevent mosquitoes from transmitting malaria to humans  Contaminated zooplankton small fish large fish  eagles and ospreys Biomagnification  DDT became more concentrated as it moved up the food chain  Caused eggshell thinning in eagles and ospreys  Banned in 1972, but is still present in some ecosystems  Migratory birds are exposed to DDT in other countries that still use it Trophic Levels  Refers to each step in the transfer of energy through a food chain or a food web  Each time energy is transferred, some energy is lost and less energy is available to the next trophic level Energy Pyramid Energy Loss  Since so much energy is lost at each level, there are fewer organisms at the higher trophic levels  Ecosystems rarely have more than 4-5 trophic levels Quantity of Energy Transfers  10% of the total available energy at one trophic level is transferred to the next level  Higher trophic levels contain less energy and can support fewer organisms 22-2 Ecosystem Recycling  Biogeochemical cycles: The movement of water, minerals, and elements through the environment  Examples: the water, carbon, nitrogen, and phosphorus cycles The Water Cycle  Water is a renewable resource because it is circulated through the water cycle  The water cycle is the continuous movement of water between Earth and the atmosphere Global Water Distribution  97% of Earth’s water is saltwater  3% is freshwater, but most of it is frozen as icecaps or glaciers  Less than 1% is available as liquid freshwater Watershed  An area of land drained by a river  Pollution anywhere in a watershed can pollute a river The Carbon Cycle  A process by which carbon is cycled between the atmosphere, land, water, and organisms  Carbon is present in all living things Short-term cycle  Consumers eat producers and obtain carbon from the carbohydrates  Some of the carbon is released back into the atmosphere as a byproduct of cellular respiration Long-term cycle  Carbonates (found in bones, shells, & coral) do not break down easily  Calcium carbonate deposits form limestone  Limestone is one of the largest carbon sinks on Earth Fossil Fuel  When living organisms die, their remains still contain carbon  Over time, the remains of ancient organisms changed into coal, oil, and natural gas Humans and the Carbon Cycle  When we burn fossil fuels, we release carbon dioxide into the atmosphere  Increased levels of carbon dioxide contributes to global warming The Carbon Cycle The Nitrogen Cycle  The process by which nitrogen is cycled between the atmosphere, bacteria, and other organisms  The atmosphere is 78% nitrogen, yet most organisms (including humans) cannot use it until it has been “fixed” Nitrogen-Fixing Bacteria  Legume plants, such as soybeans and clover, have root nodules that contain nitrogen-fixing bacteria  The bacteria “fixes” the nitrogen into a usable form All Life is Interconnected  All organisms need nitrogen to build proteins  The bacteria alter the atmospheric nitrogen for plants to use  Animals obtain the nitrogen they need when they eat plants Decomposers  Bacteria break down wastes and dead organisms to return nitrogen to the soil  Some of the nitrogen is transformed into a gas and is returned to the atmosphere The Nitrogen Cycle The Phosphorus Cycle  The movement of phosphorus from the environment to organisms and then back to the environment  This cycle is very slow  Phosphorus moves from phosphates in rock to living organisms and eventually to the ocean Phosphates  When rocks erode, they release phosphates into the soil and water  Plants absorb phosphates through their roots  Phosphates are also added to the soil when organisms die and decompose The Phosphorus Cycle Fertilizers  Fertilizers contain both nitrogen and phosphorus  Fertilizers can enter an aquatic ecosystem through runoff  Excess nitrogen and phosphorus in an aquatic ecosystem can result in an algal bloom Artificial Eutrophication  Sewage and fertilizer runoff enter lakes and ponds and causes an algal bloom  When the algae dies, the decomposition from bacteria uses most of the oxygen and the fish suffocate and die 22.3 Terrestrial Ecosystems  Biomes: very large terrestrial ecosystems that contain specific kinds of plants and animals  Biomes are influenced by climate and altitude Climate & Altitude  Climate: the temperature and precipitation of an area over a long period of time  Altitude: refers to the elevation above sea level Biomes  Each biome is made up of many different types of ecosystems.  There are seven major biomes: tundra, taiga, temperate deciduous forest, temperate grassland, desert, savanna, and tropical rainforest Biomes of the World Tundra  A cold biome located across northern North America, Europe and Asia  The ground is permanently frozen at a depth of 10-36 inches (trees can't grow)  Receives little precipitation and a very short growing season (2 months) Common Plants & Animals of the Tundra  Plants: grasses, sedges, mosses, and lichens  Animals: caribou, musk ox, lemmings, snowshoe hares, snowy owls, arctic fox Taiga  A forested biome dominated by conifers (pine, fir, hemlock, and spruce)  Needles are specialized leaves that help the trees survive the long, cold winters Common Plants & Animals of the Tiaga  Plants: evergreen trees  Animals: lynx, moose, bears, wolves, great gray owls Temperate Deciduous Forest  Characterized by trees that lose their leaves in the Fall  Variable temperatures and moderate precipitation Common Plants & Animals of the Temperate Deciduous Forest  Plants: beech, maple, oak, hickory, sycamore, elm, birch  Animals: white-tailed deer, raccoons, foxes, squirrels, great-horned owls Temperate Grasslands  Regions that are dominated by grasses and have variable temperatures  Found in the interior of continents  Also called prairies, steppes, pampas, and veldt Common Plants & Animals of the Temperate Grassland  Plants: various grasses (a lot has been turned into farmland!)  Animals: pronghorn, prairie dogs, meadowlark, bison Deserts  Areas that receive less than 25 cm of rainfall per year  Most deserts are hot, but there are also cold deserts  Desert vegetation is sparse and has a waxy coating that prevents water loss Rain Shadow Effect Common Plants & Animals of the Desert  Plants: cacti and succulents  Animals: lizards, scorpions, jack rabbits, roadrunners, kit fox, snakes, burrowing owls Savannas  Tropical or Subtropical grasslands with scattered trees and shrubs  Has alternating wet and dry seasons Common Plants & Animals of the Savanna  Plants: various grasses, few trees, shrubs  Animals: wildebeest, zebras, gazelles, giraffe, lions, cheetahs, elephants Tropical Rain Forests  Areas near the equator that have a warm, wet climate and a year-round growing season  Most biodiversity is found in tropical rainforests Common Plants & Animals of the Tropical Rain Forest  Plants: trees, epiphytes, understory plants  Animals: parrots, jaguar, monkeys, insects, sloth, snakes, lizards (contains 1/5 of all known species) 22-4 Aquatic Ecosystems  Water covers ¾ of Earth  97% of all water on our planet is saltwater  3% is freshwater (less than 1% is liquid freshwater!) Ocean Zones  Photic Zone: the part of the ocean that receives light  Aphotic Zone: the cold, dark depths where sunlight doesn’t reach The Intertidal Zone  The area that includes the beaches, tidal pools, and waves  Organisms are adapted to the rise and fall of the tides Tides  Tides are the cyclic rising and falling of Earth's ocean surface caused by the tidal forces of the moon and the sun acting on the oceans High and Low Tides During the day, the Earth rotates 180 degrees in 12 hours. The moon, meanwhile, rotates 6 degrees around the earth in 12 hours. The moon's rotation and its gravitational pull mean that any given coastal city experiences a high tide approximately every 12 hours Spring Tide  When the sun and moon are aligned, there are exceptionally strong gravitational forces, causing very high and very low tides which are called spring tides, though they have nothing to do with the season. Neap Tides  During the moon's quarter phases the sun and moon work at right angles, causing the bulges to cancel each other. The result is a smaller difference between high and low tides. The Neritic Zone  The most productive zone in the ocean  Upwelling refers to currents that carry nutrients up from the bottom  Coral reefs, plankton, sea turtles, fish, squid, etc. are found in this zone Coral Reefs  Limestone ridges built by coral polyps  Very diverse ecosystem  Corals are invertebrates that only live in shallow tropical seas Threats to Coral Reefs  Coral reefs are fragile  Divers cut pieces of coral to sell  Also threatened by oil spills, pollution, sewage, pesticides, and silt runoff The Oceanic Zone  Nutrient levels are lower in this zone  Deep sea organisms have reduced skeletons and slower metabolism Threats to the Oceans  OVERFISHING!  Trawl nets entangle and kill many animals  Industrial waste, sewage, solid waste, oil spills, toxic chemicals Hydrothermal Vents  Areas that release water that is rich in minerals and can exceed 750 °C  Chemosynthetic bacteria uses hydrogen sulfide (H2S) to make their own food  Many organisms along a vent get their food directly from the bacteria Estuaries  Areas where freshwater rivers and streams flow into the sea  Examples: bays, salt marshes, mud flats  Receive a lot of light and nutrients  Important breeding grounds for many species Freshwater Zones  Freshwater contains less than .005 % salt (NaCl)  Examples: lakes, ponds, streams, & rivers Lakes and Ponds  Eutrophic: rich in organic matter and vegetation  Oligotrophic: contains little organic matter Rivers  Bodies of water that flow down a gradient Headwaters: where a river begins (usually as a mountain stream) As a river flows down a mountain, it becomes wider, warmer, slower, and has less oxygen Streams  Tributaries that flow into larger bodies of water  Faster flowing streams are highly oxygenated and contain more benthic macroinvertebrates