introduction to ecology chapters 52. figure 50.3 rachel carson

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Introduction to Ecology Chapters 52

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  • Slide 1
  • Introduction to Ecology Chapters 52
  • Slide 2
  • Figure 50.3 Rachel Carson
  • Slide 3
  • Ecology Ecology the study of interactions between organisms and the environment Biotic living components of an ecosystem (ex. animals and plants) Abiotic - nonliving components of an ecosystem (ex. soil, air, and water)
  • Slide 4
  • Species distribution Interactions between organisms and the environment limit the distribution of species. What affects the distribution of species? Dispersal limits (range expansions and species transplants) Behavior and habitat selections Biotic factors (other species) Abiotic factors (temperature, water, sunlight, wind, rocks/soil, and climate)
  • Slide 5
  • Figure 50.7 Spread of the African honeybee in the Americas since 1956
  • Slide 6
  • Figure 50.11 Solar radiation and latitude
  • Slide 7
  • Figure 50.12 What causes the seasons?
  • Slide 8
  • Figure 50.14 How mountains affect rainfall
  • Slide 9
  • Figure 50.18 Zonation in a lake
  • Slide 10
  • Figure 50.22 Zonation in the marine environment
  • Slide 11
  • Figure 50.24 The distribution of major terrestrial biomes
  • Slide 12
  • Figure 50.10 A climograph for some major kinds of ecosystems (biomes) in North America
  • Slide 13
  • POPULATION ECOLOGY CHAPTER 53
  • Slide 14
  • POPULATION CHARACTERISTICS Population organisms of the same species in the same area Density number of individuals in a given area (example: 1200/m 2 ) Dispersion pattern of spacing among individuals
  • Slide 15
  • Measuring Size Quadrant method used for stationary organisms Mark and recapture used for mobile organisms
  • Slide 16
  • Patterns of Dispersion Clumped individuals aggregated in patches (most common) Uniform evenly spaced individuals Random unpredictable, patternless
  • Slide 17
  • Patterns of dispersion within a populations geographic range
  • Slide 18
  • DEMOGRAPHY Demography is the study of factors that affect populations Age structure relative number of individuals of each age Birthrate or fecundity number of offspring born during a certain time period Death rate number of individuals who die in a certain time period Generation time average span between birth of individuals and the birth of their offspring Sex ratio proportion of individuals of each sex
  • Slide 19
  • Life tables used to determine how long, on average, an individual of a given age could be expected to live Cohort group of individuals of same age Survivorship curve a plot of the numbers in a cohort that are alive at each age
  • Slide 20
  • Life Table for Belding Ground Squirrels (Spermophilus beldini) at Tioga Pass, in the Sierra Nevada Mountains of California
  • Slide 21
  • Idealized survivorship curves
  • Slide 22
  • LIFE HISTORIES Life history traits that affect an organisms schedule of reproduction and death Life histories vary greatly Salmon travel to ocean to mature and then back to stream to reproduce Some oaks cannot reproduce until they are at least 20 years old Semelparity or big bang reproduction produce numerous offspring and then die Iteroparity or repeated reproduction produce fewer offspring over many seasons
  • Slide 23
  • An example of big-bang reproduction: Agave (century plant)
  • Slide 24
  • There is a trade-off between reproduction and survival Female red deer who are reproductive have a greater chance of dying Larger brood sizes increase mortality rate
  • Slide 25
  • Cost of reproduction in female red deer on the Island of Rhum, in Scotland
  • Slide 26
  • Probability of survival over the following year for European kestrels after raising a modified brood
  • Slide 27
  • POPULATION GROWTH N = Change in population size B = # births during time interval (birth rate) D = # deaths during time interval (death rate) t = time interval N/t = B D Per capita birthrate (b)= # offspring produced per time by an average member of population Ex. 46 births/year in pop of 1000 so b = 46/1000 = 0.046 Birth rate = Expected # births/year for pop (B): B=bN Ex. B = 0.046 x 500 = 23 births/year (where N = 500)
  • Slide 28
  • Per capita death rate (m)= # deaths per time by an average member of population Ex. 22 deaths/year in pop of 1000 so m = 22/1000 = 0.022 Death rate = Expected # deaths/year for pop (D): D=mN Ex. D = 0.022 x 500 = 11 deaths/year (where N = 500) Maximum per capita growth rate (r max ) N/t = bN mN (birthrate death rate) r = b m N/t = r max N (exponential growth rate) dN/dt = r max N (calculus version)
  • Slide 29
  • If a population is growing, r is positive. If a population is declining, r is negative. Zero population growth occurs when r = 0 Exponential growth maximum population growth rate Intrinsic rate of increase is the maximum population growth rate, r max Exponential growth is: dN/dt = r max N
  • Slide 30
  • Population growth predicted by the exponential model
  • Slide 31
  • Example of exponential population growth in nature
  • Slide 32
  • Carrying capacity (K) maximum population size that a particular environment can support with no net increase or decrease Logistic Growth incorporates the effect of population density on r max, allowing it to vary from r max under ideal conditions to zero as carrying capacity is reached.
  • Slide 33
  • When N is small compared to K, the per capita rate of increase is high. (N = pop size) When N is large and resources are limiting, the per capita rate of increase is small. When N = K, pop stops growing. For logistic growth: N/t = r max N (K-N/K)
  • Slide 34
  • Population growth predicted by the logistic model
  • Slide 35
  • How does the logistic curve fit real populations? Some populations closely follow the S-shaped curve. Other populations do not. Low numbers may hurt a population (rhinos) Populations may overshoot the carrying capacity and then drop below K.
  • Slide 36
  • How well do these populations fit the logistic population growth model?
  • Slide 37
  • Strategies K-selected populations (density dependent) organisms that are likely to be living at density near the limit imposed by the environment (K) r-selected populations (density indepedent) organisms that are likely to be living in variable environments in which populations fluctuate or in open habitats where individuals are likely to face little competition
  • Slide 38
  • Characteristicsr-selectedK-selected Maturation timeShortLong LifespanShortLong Death rateOften highUsually low #offspring/episodeManyFew # reproductions/ lifetime Usually oneOften several Timing 1 st reproductionEarly in lifeLate in life Size of offspring/eggsSmallLarge Parental carenone Often extensive
  • Slide 39
  • POPULATION LIMITING FACTORS Limiting factors factors that limit population growth Density dependent factors death rate rises or birth rate falls with increasing pop density Disease Predation Competition Lack of food Lack of space Density independent birth rate or death rate that does not change with pop density Climate
  • Slide 40
  • Decreased survivorship at high population densities
  • Slide 41
  • Long-term study of the moose (Alces alces) population of Isle Royale, Michigan
  • Slide 42
  • Extreme population fluctuations
  • Slide 43
  • Population cycles in the snowshoe hare and lynx
  • Slide 44
  • Human population growth
  • Slide 45
  • Demographic transition in Sweden and Mexico, 1750-1997
  • Slide 46
  • Age-structure pyramids for the human population of Kenya (growing at 2.1% per year), the United States (growing at 0.6% per year), and Italy (zero growth) for 1995
  • Slide 47
  • Annual percent increase in global human pop (data from 2005). Sharp dip in 1960 due mainly to famine in China that killed 60 million people.
  • Slide 48
  • Infant mortality and life expectancy (from 2005)
  • Slide 49
  • COMMUNITY ECOLOGY CHAPTER 54
  • Slide 50
  • COMMUNITIES Communities different populations living within the same area What factors are most significant in structuring a community?
  • Slide 51
  • INTERACTIONS Interspecific interactions occur between different populations within a community Coevolution a change in one species acts as a selective force on another species, and counter-adaptation by the second species, which may cause a selective force on the 1 st species.
  • Slide 52
  • Predation (+/-) Lion hunting, killing, and eating a zebra Parasitism (+/-) Ticks sucking blood of human Competition (-/-) Fighting over resources Commensalism (+/0) Birds feeding on insects which bison flush out of grass Mutualism (+/+) Legumes with nitrogen fixing bacteria Herbivory (+/-) Insects eating plants Disease (pathogens) (+/-) Bacteria, viruses, protists, fungi, and prions
  • Slide 53
  • Figure 53.x2 Parasitic behavior: A female Nasonia vitripennis laying a clutch of eggs into the pupa of a blowfly (Phormia regina)
  • Slide 54
  • Figure 53.9 Mutualism between acacia trees and ants. The ants live in the hollow thorns and sting other pests.
  • Slide 55
  • Predation Cryptic coloration camouflage Aposematic coloration when animals with effective chemical defenses are brightly colored as a warning
  • Slide 56
  • Figure 53.5 Camouflage: Poor-will (left), lizard (right)
  • Slide 57
  • Figure 53.6 Aposematic (warning) coloration in a poisonous blue frog
  • Slide 58
  • Figure 53.x1 Deceptive coloration: moth with "eyeballs"
  • Slide 59
  • Mimicry an organisms mimic another Batesian mimicry a harmless species mimics a harmful or unpalatable species Mullerian mimicry two or more aposematically species resemble each other
  • Slide 60
  • Figure 53.7 Batesian mimicry: the hawkmoth larva resembles a snake
  • Slide 61
  • Figure 53.8 Mllerian mimicry: Cuckoo bee (left), yellow jacket (right)
  • Slide 62
  • Competition Competitive exclusion principle two species with similar needs for the same limiting resources cannot coexist in the same place. Could lead to extinction of one species Ecological niche ecological role; the sum total of the organisms use of biotic and abiotic resources
  • Slide 63
  • Resource partitioning sympatric (geographically overlapping) species consume slightly different foods or use resources in slightly different ways. Character displacement characteristics are more divergent in sympatric populations compared to geographically isolated (allopatric) populations
  • Slide 64
  • Figure 53.3a Resource partitioning in a group of lizards
  • Slide 65
  • Figure 53.2 Testing a competitive exclusion hypothesis in the field
  • Slide 66
  • Figure 53.3bc Anolis distichus (left) perches on sunny areas and Anolis insolitus (right) perches on shady branches.
  • Slide 67
  • What controls community structure? Species diversity Food webs Dominant species Keystone species Foundation species
  • Slide 68
  • Figure 53.21 Which forest is more diverse?
  • Slide 69
  • Species Diversity Species diversity considers the following: Species richness number of different species Species relative abundance proportion each species represents of the total individuals in community
  • Slide 70
  • Dominant species most abundant or highest biomass Ex. American Chestnut was dominant before 1910, but chestnut blight killed all in N. America Invasive species can become dominant Keystone species a predator that makes an unusually strong impact on community structure Keystone predators maintain higher species diversity by reducing the densities of strong competitors, such that the competitive exclusion of other species does not occur Ex. Removing Piaster decreased species diversity. Without piaster, mussels overpopulated and excluded other species,
  • Slide 71
  • Figure 53.14b Testing a keystone predator hypothesis
  • Slide 72
  • Figure 53.14a Testing a keystone predator hypothesis
  • Slide 73
  • Figure 53.15 Sea otters as keystone predators in the North Pacific Without sea otters, sea urchins do well and eat kelp. Kelp forests are being destroyed. Otters are being eaten by killer whales.
  • Slide 74
  • Foundation species - cause physical changes to environment Ex. beaver dam, black rush (grass) helps prevent salt build up in soil of marshes
  • Slide 75
  • Slide 76
  • Bottom-up or Top-down Controls Bottom-up = influence from lower to higher trophic levels Mineral nutrients control the plants, which control the herbivores, which then controls the predators Top-down = influence from higher to lower trophic levels Predators limit herbivores, which in turn limits plants, which affects soil nutrients
  • Slide 77
  • DISTURBANCES Disturbances are events such as fire, storms, drought, or human activities that damage communities. Can create opportunities for other species Human disturbance is not always negative Yellowstone fire in 1988 killed old forest, but new plants quickly grew in its wake Dynamic equilibrium hypothesis species diversity depends on the effect of disturbance on the competitive interactions of populations.
  • Slide 78
  • Figure 53.16 Routine disturbance in a grassland community
  • Slide 79
  • Figure 53.18x2 Forest fire
  • Slide 80
  • SUCCESSION Ecological succession transitions in species composition over time Primary succession when succession begins in an area that is virtually lifeless and has no soil. Lichens and mosses are usually the first macroscopic photosynthesizers Can slowly dissolve rock to make soil, which takes thousands of years
  • Slide 81
  • Figure 53.18x1 Large-scale disturbance: Mount St. Helens
  • Slide 82
  • Figure 53.19 A glacial retreat in southeastern Alaska
  • Slide 83
  • Table 53.2 The Pattern of Succession on Moraines in Glacier Bay
  • Slide 84
  • Secondary succession occurs where an existing community has been cleared by some disturbance that leaves soil intact (example fire or volcanoes erupting) Typically pioneer species are r-selected (high birthrates and dispersal)
  • Slide 85
  • Figure 53.18 Patchiness and recovery following a large-scale disturbance
  • Slide 86
  • ECOSYSTEMS Chapter 55
  • Slide 87
  • FOOD WEBS and TROPHIC LEVELS Autotrophs Producers make own food Heterotrophs Primary consumers = herbivores = eat producers Secondary consumers = carnivores = eat primary consumers Tertiary consumers = carnivores = eat secondary consumers Detritivores (decomposers) = eat detritus (nonliving organic material and dead remains)
  • Slide 88
  • Figure 54.1 An overview of ecosystem dynamics
  • Slide 89
  • Section 3-2 A Food Web
  • Slide 90
  • Figure 54.2 Fungi decomposing a log
  • Slide 91
  • Production rate of incorporation of energy and materials into the bodies of organisms Consumption metabolic use Decomposition breakdown of organic material into inorganic
  • Slide 92
  • ENERGY FLOW IN ECOSYSTEMS Most solar radiation is absorbed, reflected, or scattered in the atmosphere of Earth. Only a very small portion of sunlight is used by algae, bacteria, and plants for photosynthesis
  • Slide 93
  • Primary productivity amount of light energy converted to chemical energy by autotrophs in an ecosystem in a given time period Gross primary productivity (GPP) total primary productivity (not all of this energy is stored in autotrophs because autotrophs use energy for respiration) Net primary productivity (NPP) NPP = GPP R Where R = the amount of energy used in respiration
  • Slide 94
  • C 6 H 12 O 6 + 6O 2 6CO 2 + 6H 2 O Gross primary productivity results from photosynthesis Net primary productivity is the difference between the yield of photosynthesis and the consumption of fuel in respiration Respiration Photosynthesis
  • Slide 95
  • Primary productivity J/m 2 /yr (energy measured per area per unit time) g/m 2 /yr (biomass added per area per unit time) Seasonal changes and available nutrients can limit primary productivity
  • Slide 96
  • Figure 54.3 Primary production of different ecosystems
  • Slide 97
  • Figure 54.4 Regional annual net primary production for Earth
  • Slide 98
  • Limiting nutrient the nutrient that must be added to increase primary productivity Example: nitrogen or phosphorus are often limiting in aquatic systems (especially in the photic zone) Secondary productivity rate at which an ecosystems consumers convert chemical energy into their own new biomass
  • Slide 99
  • Figure 54.9 Nutrient addition experiments in a Hudson Bay salt marsh
  • Slide 100
  • Figure 54.11 An idealized pyramid of net production
  • Slide 101
  • ECOLOGICAL PYRAMIDS Pyramid of productivity ~10% rule - ~10% of energy at one level transfers to next level Where does the energy go?
  • Slide 102
  • Figure 54.10 Energy partitioning within a link of the food chain
  • Slide 103
  • Pyramid of biomass standing crop biomass (total dry weight) Some aquatic systems show inverted pyramids because zooplankton consume phytoplankton quickly Productivity still upright
  • Slide 104
  • Figure 54.12 Pyramids of biomass (standing crop)
  • Slide 105
  • Figure 54.13 A pyramid of numbers
  • Slide 106
  • NUTRIENT CYCLING Biogeochemical cycles involve both abiotic and biotic components
  • Slide 107
  • Figure 54.16 The water cycle
  • Slide 108
  • Figure 54.17 The carbon cycle
  • Slide 109
  • CARBON CYCLE Carbon dioxide in atmosphere is lowest in summer in N. hemisphere and highest in winter. More plants in summer = less CO 2 in atmosphere Dissolved CO 2 makes carbonic acid (H 2 CO 3 )
  • Slide 110
  • Increased burning of fossil fuels has increased CO 2 levels, which leads to global warming. Carbon dioxide absorbs much of the reflected infrared radiation = greenhouse effect. Without the greenhouse effect, temperature would be 18C.
  • Slide 111
  • Figure 54.26 The increase in atmospheric carbon dioxide and average temperatures from 1958 to 2000 (readings taken from Mauna Loa, Hawaii)
  • Slide 112
  • Global Warming A number of studies predict CO 2 will double by end of 21 st century. Will cause a predicted 2C average global temp increase Historically, a 1.3 C would make world warmer than any time in past 100,000 years. Poles probably most affected and polar ice melting may change our coastlines!
  • Slide 113
  • Figure 54.18 The nitrogen cycle
  • Slide 114
  • NITROGEN CYCLE Plants cannot use N 2 (gas). Nitrogen fixing bacteria convert nitrogen gas into a form of N that plants can use: ammonium (NH 4 + ) or nitrate(NO 3 - ). Nitrogen fixing bacteria can live in the soil or in plants called legumes (mutualism). Legumes include beans, alfalfa, and soy. Denitrifying bacteria convert nitrate back into nitrogen gas. Without nitrogen fixing bacteria, plants could not get the nitrogen they need and would die. All life on earth depends on these bacteria.
  • Slide 115
  • Figure 54.19 The phosphorous cycle
  • Slide 116
  • PHOSPHORUS CYCLE Phosphorus is often the limiting nutrient in lakes. Sewage and runoff provide excess phosphorus. This can cause eutrophication. This is when a lake develops a high productivity, which is supported by high rates of nutrient cycling. This leads to algal blooms, which can suffocate the lake.
  • Slide 117
  • Figure 54.8 The experimental eutrophication of a lake
  • Slide 118
  • Figure 54.24 Weve changed our tune
  • Slide 119
  • BIOLOGICAL MAGNIFICATION Nonbiodegradable substances become more concentrated in increasing, successive trophic levels. The biomass at any given level is produced from a much larger biomass ingested from the level below. Example: DDT caused birds of prey to lay eggs with thin shells.
  • Slide 120
  • Figure 54.25 Biological magnification of DDT in a food chain
  • Slide 121
  • Chlorinated Hydrocarbons Include DDT, agent orange, PCBs (polychlorinated biphenyls) They are persistent (i.e., they persist in the environment for several years) They are non-polar (i.e., water-hating) They bioaccumulate (i.e., they concentrate in the fat of organisms, and their concentration increases as one moves up the food chain) They are causing a toxic effect at low concentrations
  • Slide 122
  • Agent Orange was a defoliant used during the Vietnam War. Agent Orange is an herbicide that was used during the Vietnam War to strip the land of vegetation making it easier for the US troops to see the opposing forces and also to deplete their food supply. Dioxin is a very toxic chemical within Agent Orange. Dioxin is believed to be the cause of so much damage and has been linked to many cancers and birth defects.
  • Slide 123
  • Dioxin (part of Agent Orange)
  • Slide 124
  • OZONE DEPLETION Ozone (O 3 ) provides a protective barrier to UV light. Chlorofluorcarbons react with O 3 and reduce it to O 2, which makes holes in the layer. Largest hole over Antarctica. Chlorofluorcarbons come from refrigerants, propellants in aerosol cans, and in some manufacturing processes.
  • Slide 125
  • Figure 54.27a Erosion of Earths ozone shield: The ozone hole over the Antarctic
  • Slide 126
  • Figure 54.27b Erosion of Earths ozone shield: Thickness of the ozone layer