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Ecology The Biosphere Population Ecology Community Ecology Ecosystems Introduction to Ecology and the Biosphere Chapter 50 Abiotic Factors of the Biosphere  Climate – Water/Rainfall – Temperature  Rocks and Soil – Particle size – pH  –Light –Wind –Mineral composition Periodic Disturbances – Catastrophic events: fire, flood, earthquake, etc. Global Climate Patterns  Determined by: – input of solar energy • Shape of earth—latitudinal variation • 23.5° tilt of earth’s axis—seasonal variation – earth’s movement in space Global Air Circulation, Precipitation, and Winds Local and Seasonal Effects on Climate  Proximity to bodies of water – Oceanic currents along continental coasts – Large inland bodies of water—lakes  Topographic features – Mountain ranges Rain Shadows Seasonal Turnover of Lakes/Ponds  Lake stratification and biannual mixing – Temperature – Density water densest at 4°C, it sinks below water that is warmer or colder Chapter 52 Population Ecology Overview: Earth’s Fluctuating Populations  To understand human population growth, we must consider general principles of population ecology Population ecology = study of populations relative to environment, including environmental influences on density and distribution, age structure, and population size  Population = group of individuals of a single species living in the same general area  Density and Dispersion Density is the number of individuals per unit area or volume  Dispersion is the pattern of spacing among individuals within the boundaries of the population  – Environmental and social factors influence spacing of individuals in a population Clumped distribution may be influenced by resource availability (living in groups increases the effectiveness of hunting, spreads the work of protecting and caring for young) Uniform distribution may be influenced by social interactions such as territoriality Random distribution—the position of each individual is independent of other individuals Demography Study of theory and statistics behind population growth and decline  N = size of the population  Demographic Statistics Birth rate = number of offspring produced per time period  Death rate = number of deaths per time period  Sex ratio = proportion of males and females in a population  Generation time = time needed for individuals to reach reproductive maturity  Demographic Statistics  Age structure = statistic that compares the relative number of individuals in the population from each age group Copyright © 2002 Pearson Education, Inc., publishing as Benjamin Cummings   Immigration rate = rate at which individuals relocate into a given population Emigration rate = rate which individuals relocate out of a give population Demographic Statistics These statistics together determine the size and growth rate of a given population  Population Growth = (Births + immigration) - (deaths + emigration)  If birth rates are greater than death rates:     Fictional "Tribbles" from Star Trek: Defining characteristic of the Tribbles is their extreme reproductive rate. Over half of a Tribbles metabolism is devoted to reproduction, allowing them to bear a litter of young every twelve hours. With an average litter of ten, a single Tribble can therefore create a population of 1,771,561 within three days, and an amazing 304,481,639,541,400,000,000 ,000,000,000,000,000,000,00 0,000,000,000,000,000,000,0 00 in thirty days! Population Growth Short generation time = faster rate of population growth Population Growth and Size  Biotic potential = maximum growth rate of a population given unlimited resources, unlimited space, and lack of competition or predators – Rate varies from species to species  Carrying capacity = maximum number of individuals that a population can sustain in a given environment without destroying the habitat Limiting Factors Control Population Sizes  Density-dependent factors come into play when population approaches and/or passes the carrying capacity – Food supplies, waste products, populationcrowding diseases  Density-independent factors have nothing to do with the population size – Floods, droughts, earthquakes, other natural disasters and weather conditions Population Growth   Exponential Growth = population grows as if there are no limitations as to how large it can get (biotic potential) A population increases slowly at first (the "lag phase") and then grows increasingly rapidly as time passes (the "log phase"). When numbers are low, a doubling does not produce much addition to the population, but as numbers increase, each successive doubling adds larger and larger increments. Population Growth  Logistic Growth = population growth slows to zero and population size tends to stabilize because of environmental resistance (limiting factors) Exponential growth can be represented by the following equation: dN/dt = rN where:  – dN/dt is the instantaneous rate of change in population size – r is the intrinsic rate of increase of the population – N is population size at any given point in time   The S-shaped (sigmoid) curve that shows the effect of environmental resistance upon population growth can be represented by the following equation, often referred to as the logistic equation: dN/dt = rN (K-N) / K where K is the carrying capacity (maximum value of N for a given set of environmental conditions) Point of Maximum growth (K/2) Carrying Capacity Population size (N) 2,000 dN dt = 1.0N 1,500 Exponential growth K = 1,500 Logistic growth 1,000 dN dt = 1.0N 1,500 – N 1,500 500 0 0 10 5 Number of generations 15 Life History Strategies  K-selected populations are of a roughly constant size whose members have low reproductive rates. – Offspring require extensive postnatal care until sufficiently matured (humans)  R-selected populations experience rapid growth – Offspring are numerous, mature rapidly, and require little postnatal care (bacteria) Predator-Prey Cycling   Many populations undergo boom-andbust cycles Boom-and-bust cycles are influenced by complex interactions between biotic and abiotic factors Community Ecology Chapter 53 Interactions Between Populations of Different Species Interspecific interactions—occur b/w populations of different species  Coevolution—a change in one species acts as a selective force on another species  Interactions Between Populations of Different Species  Predation (+/–)—consumption of one organism by another – Predator eats prey – Parasitism (+/–)—specialized predator (parasite) lives on/in its host, not killed immediately • Endoparasitism—live inside host (tapeworms/viruses) • Ectoparasitism—live on surface of host (mosquitoes/aphids) – Herbivory (+/–)—herbivores consume plants Plant Defenses Against Hebivores  Physical defenses – thorns, hooks/spines on leaves  Chemical defenses – Make plant distasteful or poisonous • Morphine from opium poppy • Nicotine from tobacco Animal Defenses Against Predators  Behavioral defenses – Alarm cries – Distraction displays  Cryptic coloration/shape (camouflage) – Blend in with environment – Asposematic coloration • Red/black; yellow/black  Mechanical/chemical defenses – Quills, spines, and other similar structures – Toxins—distasteful or poisonous • Monarch butterfly stores toxin of milkweed as larvae • Poisonous toads secrete toxin Animal Defenses Against Predators  Mimicry—prey resembles species that cannot be eaten – Batesian mimicry: Imitate color patterns or appearance of more dangerous organisms  Mimicry can be used to lure prey – Snapping turtle wriggles tongue like a worm to attract and capture small fish Interspecific Competition (–/–)  Competition occurs when 2 or more populations overlap in their niches – Limiting resources • Food • Space • Mates  Generally, one will out-compete the other Competitive Exclusion Principle  Two species cannot coexist in a community if their niches are identical Competition in Nature   Two possible Outcomes 1. Weaker competitor becomes extinct 2. One or both species may evolve enough to use a different set of resources Competition cannot operate for long periods of time Resource Partitioning Evolution Drives Reduced Niche Overlap 12 10 8 6 4 2 0 12 Number of individuals Population 1 Population 2 10 8 6 4 2 0 2 4 6 8 10 12 14 16 18 20 2 4 6 8 10 12 14 16 18 20 Height of nesting site in apple trees Character Displacement Joseph H. Connell Study Symbiotic Relationships  Non-Beneficial – Parasitism (+/–)—host harmed  Beneficial – Commensalism (+/0)—one partner benefits while not harming the other • Cattle egrets—egrets eat ectoparasites/cattle are groomed – Mutualism (+/+)—both partners benefit • Lichens-association b/w fungus and algae • Nitrogen-fixing bacteria and legumes Community Structure Predators can moderate competition among its prey species  Keystone species can alter the whole community  Effects of a Keystone Predator:Sea Star (Pisaster) 20 15 With Pisaster Without Pisaster 10 5 68 19 69 19 70 19 71 19 72 19 67 19 66 19 65 19 64 19 63 0 19 Number of Species Present 25 Year Community Structure Introduction of a species (exotic species) into a community can have drastic affects on the existing community members  Habitats that are more varied can support a more diverse community  – provides more ecological niches Nonequilibrium and Disturbances in a Community  Storms, fire, floods, droughts, overgrazing, or detrimental human activities: – Remove organisms – Alter resource availability Create opportunities for new species that have not previously occupied the habitat  Humans are the biggest disturbance  – Logging, agriculture, overgrazing Ecological Succession  Primary succession – Begins in a virtually lifeless area where soil has not formed – Lichens and mosses colonize first – Soil gradually forms and small plants and shrubs take root  Secondary succession – Occurs where an existing community has been cleared by some disturbance that leaves soil in tact – Earliest plants to recolonize are often those that grow from wind-blown or animal-borne seeds Ecological Succession Competition among early species shape the succession of an area  Tolerance to abiotic conditions determines early species  Ecosystems Chapter 54 Trophic Relationships  Ecosystems divided into trophic levels (feeding levels) – Primary producers—autotrophs (mostly photosynthetic) – Primary consumers—herbivores – Secondary consumers—carnivores that eat herbivores – Tertiary consumers—carnivores that eat other carnivores – Detrivores—consumers that eat dead or decaying matter Food Webs  Feeding relationships woven into elaborate interconnections between species Energy Flow in Ecosystems Each level in a food web contains a different quantity of stored chemical energy  When consumers eats producers or 2 consumers eat 1 producers, some energy is lost in the each transfer from one level to the next  – Gross primary productivity= [total chemical energy generated by producers] – Net primary productivity= [total chemical energy – respiration by plants] Pyramid of Net Productivity: 10% of energy at each level converted to new biomass Pyramids of Standing Crop Biomass Sharp decrease in biomass at successively higher levels Small crop of 1 producers support larger crop of 1 consumers Pyramid of Numbers: In higher trophic levels, the small amount of biomass contained in a few organisms Biogeochemical Cycles Chemical elements available only in limited amounts  Movement of essential elements between the biotic and abiotic environment  Carbon Cycle  Nitrogen Cycle  Phosphorus Cycle  Water Cycle  * Carbon Cycle Human Impacts  Greenhouse Effect – Increase of atmospheric CO2 • Combustion of fossil fuels • Burning of wood from deforestation – Increase in numbers of C3 plants in areas previously inhabited by C4 plants – Increase in global temperature * Nitrogen Cycle Human Impacts  Agricultural effects – Cultivation—turns up soil and increases rate of decomposition of organic matter; Releases more nitrogen – Harvesting removes nitrogen from ecosystem – Adding industrially synthesized fertilizers to soil has resulted in doubling globe’s supply • Excess nitrogen leeches into soil and into rivers, streams, and lakes and ground water— – high amounts are toxic to aquatic organisms and humans – Algal blooms in lakes speed up eutrophication * Phosphorus Cycle Water Cycle The human population is disrupting chemical cycles throughout the biosphere  As the human population has grown, our activities have disrupted the trophic structure, energy flow, and chemical cycling of many ecosystems Nutrient Enrichment  In addition to transporting nutrients from one location to another, humans have added new materials, some of them toxins, to ecosystems Agriculture and Nitrogen Cycling Agriculture removes nutrients from ecosystems that would ordinarily be cycled back into the soil  Nitrogen is the main nutrient lost through agriculture; thus, agriculture greatly impacts the nitrogen cycle  Industrially produced fertilizer is typically used to replace lost nitrogen, but effects on an ecosystem can be harmful  Contamination of Aquatic Ecosystems     Critical load for a nutrient is the amount that plants can absorb without damaging the ecosystem When excess nutrients are added to an ecosystem, the critical load is exceeded Remaining nutrients can contaminate groundwater and freshwater and marine ecosystems Sewage runoff causes cultural eutrophication, excessive algal growth that can greatly harm freshwater ecosystems Acid Precipitation   Combustion of fossil fuels is the main cause of acid precipitation North American and European ecosystems downwind from industrial regions have been damaged by rain and snow containing nitric and sulfuric acid 4.6 4.3 4.6 4.3 4.6 4.3 4.1 Europe North America 4.6 5.0 5.3 5.4 5.3 5.3 5.2 5.2 5.5 5.2 5.5 5.6 5.4 5.2 5.3 5.3 5.5 6.0 5.9 5.5 5.3 5.2 5.3 5.4 5.4 5.3 5.0 5.05.1 4.9 5.4 5.1 6.3 5.7 5.6 4.9 5.4 5.3 5.0 5.2 5.4 5.1 5.5 5.2 4.8 5.3 4.5 4.6 4.7 5.4 5.2 5.15.0 4.8 4.7 5.2 4.5 4.6 4.8 4.3 4.5 4.5 5.2 4.9 5.5 4.5 5.6 4.5 4.5 4.6 4.9 4.7 4.7 4.3 4.4 4.5 4.6 5.1 4.7 4.6 4.5 4.7 5.4 4.5 4.1 4.4 5.3 5.3 4.8 4.4 4.4 4.6 4.3 4.6 4.6 4.6 4.5 4.4 4.5 4.7 4.5 4.5 4.5 4.7 4.7 4.6 4.8 4.6 5.4 4.6 4.8 4.6 4.5 5.0 4.5 4.5 4.7 4.8 4.9 4.5 4.6 4.5 Field pH 4.5 4.7 5.0 4.7 4.8 4.7 4.7 5.0 4.8 5.1 4.7 5.3 4.7 4.7 5.2–5.3 5.0 5.4 4.7 4.6 4.7 4.9 5.1–5.2 4.8 4.7 4.8 5.3 4.8 4.9 5.0–5.1 4.8 4.7 4.9–5.0 4.9 4.8 4.7 5.6 6.1 5.2 5.7 5.0 5.0 5.1 5.1 5.7 5.1 5.0 5.0 4.8 4.7 4.7 4.7 4.9   By the year 2000, acid precipitation affected the entire contiguous United States Environmental regulations and new technologies have allowed many developed countries to reduce sulfur dioxide emissions 4.8–4.9 4.7–4.8 4.6–4.7 4.5–4.6 4.4–4.5 4.3–4.4 <4.3 Toxins in the Environment  Concentration of PCBs Herring gull eggs 124 ppm  Lake trout 4.83 ppm Smelt 1.04 ppm Zooplankton 0.123 ppm Phytoplankton 0.025 ppm  In some cases, harmful substances persist for long periods in an ecosystem One reason toxins are harmful is that they become more concentrated in successive trophic levels In biological magnification, toxins concentrate at higher trophic levels, where biomass is lower Atmospheric Carbon Dioxide  One pressing problem caused by human activities is the rising level of atmospheric carbon dioxide Rising Atmospheric CO2  Due to the burning of fossil fuels and other human activities, the concentration of atmospheric CO2 has been steadily increasing The Greenhouse Effect and Global Warming The greenhouse effect caused by atmospheric CO2 keeps Earth’s surface at a habitable temperature  Increased levels of atmospheric CO2 are magnifying the greenhouse effect, which could cause global warming and climatic change    Life on Earth is protected from damaging effects of UV radiation by a protective layer or ozone molecules in the atmosphere Satellite studies suggest that the ozone layer has been gradually thinning since 1975 Ozone layer thickness (Dobson units) Depletion of Atmospheric Ozone 350 300 250 200 150 100 50 0 1955 1960 1965 1970 19751980 1985 19901995 2000 2005 Year (Average for the month of October)  Destruction of atmospheric ozone probably results from chlorine-releasing pollutants produced by human activity Chlorine atoms Chlorine from CFCs interacts with ozone (O3), forming chlorine monoxide (CIO) and oxygen (O2). O2 Chlorine O3 CIO O2 Sunlight causes Cl2O2 to break down into O2 and free chlorine atoms. The chlorine atoms can begin the cycle again. Sunlight CIO Cl2O2 Two CIO molecules react, forming chlorine peroxide (Cl2O2).  Scientists first described an “ozone hole” over Antarctica in 1985; it has increased in size as ozone depletion has increased October 1979 October 2000
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                            