Final Chapters 17,18,19,20 Flashcards
To prepare and get a B for ENV 220 final
What is a food web?
Summary of the feeding interactions within a community
Community portrait based on feeding relationships
Depicted with arrows that point in the direction of energy flow
What is ecology?
The scientific study of interactions between organisms and their environment.
Scientific method
The basis for scientific inquiry.
- Ask a question
- Do research
- Form a hypothesis
- Perform experiments
- Analyze data and form a conclusion
- Record results
Scale and manipulation
The changes to environments that occur over large spatial of temporal scales.
Levels of ecological organization
- Biosphere - This is where all living things on Earth live.
- Biomes - A large naturally occurring community of flora and fauna occupying a major habitat.
- Ecosystem - A biological community of interacting organisms and their physical environment.
- Community - All the people living in a particular area or place: “local communities”.
- Populations - A particular section, group, or type of people or animals living in an area or country.
- Species - This is the most basic unit of biological organization.
The 9 biomes
- Tropical Rainforests
- Tropical Dryforests
- Tropical Savannas
- Deserts
- Mediterranean Woodlands and Shrublands
- Temperate Grasslands
- Temperate Forests (Old Growth)
- Boreal Forests (Taiga)
- Tundras
Tropical Rainforests
- Most occur within 10o latitude of the equator.
- Little temperature variation.
- Annual rainfall between 80 and 160 inches and occurs evenly throughout the year.
- Quickly leaches soil nutrients.
- Well developed, tall (up to 260 ft) canopy.
- increasingly exploited for foods and medicines.
Tropical Dryforests
- Most occur between 10o and 25o latitude of the equator.
- Climate is more seasonal than tropical rainforests.
- Alternates between very dry (winter) season and wet season.
- Soils are richer in nutrients, but rain pulses make it vulnerable to erosion.
- shares many animal and plant species with tropical rainforests.
- Heavily settled by humans for dry season.
Tropical Savannas
- Tropical grasslands at ground level.
- Most occur north and south of tropical dryforests within 10o and 20o of the equator.
- Climate alternates between wet and dry seasons.
- Wet season is shorter and dryer than tropical dry forests.
- Droughts in dry season lead to lightning-caused fires; maintains grasslands with scattered mature trees.
- Soils have low water permeability with impermeable subsoils; helps persist as grassland.
Deserts
- Occur in major bands at 30o N and S latitude of the equator.
- Occupy about 20% of Earth’s land.
- Water loss usually exceeds precipitation.
- Soil is extremely low in organic matter.
- influenced by plant/animal activity.
Mediterranean Woodlands and Shrublands
- Also called chaparral.
- Occur in all continents expect Antarctica.
- Climate is cool/moist in fall, winter, and spring; and hot and dry in summer.
- Fragile soils with moderate fertility.
- Plants/animals adapted to drought/low nutrients.
- Fire-resistant plants.
- long history of human intrusion and clearing for agriculture.
Temperate Grasslands
- Midwest prairies - “sea of grass.”
- Largest biome in North America.
- Annual rainfall between 15 - 40 in. with periodic droughts.
- Winters are cold and dry with most rainfall in summer.
- Soils are extremely nutrient rich and deep.
- Dominated by herbaceous vegetation.
- Fertile farmlands due to fertilizer addition.
Temperate Forests (Old Growth)
- Occur between 40o and 50o latitude of the equator.
- Annual rainfall up to 120 in.
- Moderate variations in temperature.
- Fertile soils.
- Dominated by deciduous plants (longer growing seasons), conifers (redwoods).
- High biomass production; high wood accumulation.
- Many major human pops center on once old growth forests; Tokyo, Berlin, London, New York, Chicago.
Boreal Forests (Taiga)
- Occur only in northern hemisphere.
- Covers 11% of Land area.
- Thin acidic soils, low in fertility.
- Extreme climates have permafrost subsoils.
- Large temperature variation with cold, dry climate.
- Dominated by evergreen conifers.
- High animal density.
- Low levels of human intrusion.
Tundras
- Covers most lands north of Arctic Circle
- Cool dry climate with short summers.
- 7 to 23 inches of rain.
- Low decomposition rate, resulting in peat.
- Netlike soil surface.
- Mostly mosses and dwarf trees.
- Low human intrusion but for oil as of recent.
The Hydrologic Cycle
- 71% of Earth’s surface covered in water.
- Oceans contain 97%.
- Polar icecaps and glaciers contain 2%
- Freshwater lakes, streams, and groundwater contain <1%.
- Non-static distribution of water.
- Solar energy drives cycle.
1. Evaporation: water turns to gas and rises into the atmosphere.
2. Condensation: clouds form.
3. Precipitation: water rains down to Earth. Then evaporates again, is consumed by organisms, joins ground water, or joins surface water.
Turnover time
Amount of time it takes for entire volume of water of a reservoir to be renewed.
Evolution
Variation in phenotype of individuals in a population results from both genes and environment. Random processes (genetic drift), differences in survival and reproduction can effect it.
Natural selection
The result of differences in survival and reproduction among phenotypes.
What is the broadest (most inclusive) of the levels of ecological organization?
Biosphere
Keystone Species
Keystone species exert strong effects on their community structure, despite low biomass
What two examples did she use for keystone species (chap 17)
Fish (power California Roach and Steelhead Trout experiment)
Power’s Experiment:
- Set up enclosures/exclosures
- Predatory fish enclosed in one treatment
- Predatory fish excluded in another treatment
Snail:Lubchenko Lubchenko observed in tide pools:
◦Tide pools with green alga densities had snail densities
◦Pools w/ snail densities were dominated by red alga
◦In absence of snails, green alga competitively displaces red alga
What is a introduced species?
Introduced species:
those that humans intentionally or accidentally move from the species’ native locations to new geographic regions
Sometimes called non-native, exotic, alien
Example:
Exotic species have dramatic impacts on communities because they were outside the evolutionary experience of local prey populations
◦Lake Victoria (E. Africa) harbored one of the greatest conc. of fish species in the world
◦Nile Perch (Lates nilotica) exotic fish predator
Since introduced decline in species diversity.
Why is a keystone species important?
A keystone species is important because it has great significance in promoting species diversity.
What are strong interactions?
Paine (1980):
◦Suggested feeding activities of a few species may have a dominant influence on community structure – called these influential trophic relations strong interactions
◦Suggested criterion for strong interaction is degree of influence on community structure and not quantity of energy flow
What is a ecosystem?
all of the organisms living in and area and the physical environment with which those species interact
What is primary production?
Production of biomass (organic matter) via fixation of energy by autotrophs in an ecosystem.
Rate of primary production: Amount of energy fixed over a given period of time
Gross primary production (GPP): Total amount of energy fixed by autotrophs
◦Net primary production (NPP): Amount of energy leftover after autotrophs have met their metabolic needs; what you see as plant biomass
Types of Trophic Levels
Primary Producers (Plants) Primary Consumers (Herbivores and detritivores) Secondary consumers(Carnivores that comsume herbivores and detritivores) Tertiary, Quaternary (harder carnivores) Top Predators (Apex Predators)
Evapotranporation
Rosenzweig :
◦moisture and temperature influence rates of primary production
◦relationship between annual net primary production and annual actual evapotranspiration (AET)
◦AET: Amount of water that evaporates (from surfaces) and transpires (from plants) off a landscape
AET is affected by both temperature and precipitation
Cold ecosystems (e.g. tundra) and dry ecosystems (e.g. deserts) tend to have low AET
What is soil fertility?
Variation in soil fertility can explain differences in terrestrial primary production
◦Shaver and Chapin found arctic (tundra) net primary production was twice as high on fertilized plots as unfertilized plots
Limits on nutrient availability in freshwater?
Freshwater primary productivity is usually limited by nutrient availability
◦Several studies have found quantitative relationship between phosphorus and phytoplankton biomass
◦Several studies support generalization that nutrient availability (esp. phosphorus) controls rate of 1° prod. in freshwater ecosystems
Thiik adding fertilizer will increases biomass taking away fertilizer decreases. Graneli Baltic sea.
How Do Consumers Influence Production?
Bottom-Up Controls ◦Influences of physical/chemical factors of an ecosystem ◦e.g. temperature, nutrients, light Top-Down Controls ◦Influences of consumers ◦HSS (1960): the earth is green ◦Carpenter et al.: influence of predators on lake primary production propagate through the food web Ex: apex predator down
Lake Production and Trophic Cascades
Carpenter et al. (1985) : Trophic Cascade Hypothesis
◦Effects of predators on prey that alter abundance, biomass or productivity across more than one link in the food web
◦Predators can influence ecosystem properties (1° prod) through effects on intermediary trophic levels
◦Piscivores (fish that eat fish) and planktivorous (eat phytoplankton) most important
◦Can cause significant deviations in primary productivity in lake ecosystems
Trophic Cascade Hypothesis:
- Piscivores reduce planktivorous fish directly by eating them
- Piscivores then indirectly increase populations of large zooplankton and indirectly reduce phytoplankton biomass
Lake Trophic Cascade experiment
Carpenter and Kitchell
◦Reduction in planktivorous fish populations led to reduced rates of primary production, via:
In absence of planktivorous minnows, predaceous invertebrates became more numerous and ate smaller herbivorous zooplankton….
…resulted in abundant, large herbivorous zooplankton that ate phytoplankton, biomass and rate of primary production declined
…..
Trophic Dynamic View of Ecosystems defention
Lindeman (1942):
◦ Ecosystem concept is fundamental to the study of
energy transfer within an ecosystem
◦ Suggested grouping organisms within an ecosystem
into trophic levels
Each feeds on level immediately below
As energy is transferred from one trophic level to
another, energy is degraded
◦ Among the first ecologists to
quantify the flux of energy
through an (lake) ecosystem
Trophic Dynamic View of Ecosystems defention 2nd law of thermodynamics
2nd Law of Thermodynamics: ◦ As energy is transferred from one trophic level to another, energy is degraded ◦ Results in/from: Limited ability to consume and assimilate food source Consumer respiration Waste production Heat production Low ecological efficiency – percentage of energy in biomass that is transferred to biomass in next higher trophic level; varies from 5-20%, usually ~10%
Ecological Pyrimad
Ecological Pyramids:
◦ Seen in numbers, biomass, production
◦ Results from energy losses at each successive energy transfer
◦ Also called an “Eltonian pyramid”
◦ The amount of energy available to top consumers is small
compared to that of lower level consumers (=herbivores)
Reasons for decline in energy flow
This decline in the amount of available energy
explains why:
◦ Top level consumers (whales, hawks) require so much
geographic territory to get enough food
◦ Most food chains are limited to 4-5 levels – not enough
energy to support more
◦ Are no non-human predators of large predators (lions,
eagles)
biomass of these predators is not sufficient to support
another trophic level
Ecosystem Energetics and Human Nutrition
How do lessons about energy flow apply to human nutrition?
Eating producers instead of consumers requires less photosynthetic productivity and reduces the impact on the environment
It takes at least 10 lbs. of corn 1 lb. beef
Energy Flow in A Temperate Deciduous Forest: An Energy Budget
Most energy flowing through ecosystem is lost to heat, respiration, evapotranspiration
NPP was <1% of the input of solar energy
◦99% of solar energy unavailable for use by a second trophic level
As energy losses between trophic levels accumulate, eventually there is insufficient energy left to support a higher trophic level
◦Consumers lose significant energy to respiration
◦Only ~10% of energy transferred to next successive level
Energy flows, nutrients cycle
Nutrient Cycles (3 types)
Nitrogen Cycle, Phosphorous cycle, and Carbon cycle
Define Nutrients and Nutrients cycle
elements required for the development, maintenance and reproduction of organisms Ex: C, P, N, K, Fe
Nutrient cycle – use, transformation movement and reuse of nutrients
Phosphorous significance
Biological/Ecological Significance:
◦forms phospholipids, nucleic acids, ATP
Phosphorus forms
Forms:
◦Not very abundant in the biosphere
◦Primarily found as phosphate (PO4)
◦Available to living things after decomposition of phosphate-containing organic matter
Reservoirs:
◦Global phosphorus cycle does not include substantial atmospheric component (unlike C, N) – no gaso
Phosphorous Resivors
◦Largest quantities found in mineral deposits and marine sediments – also mined for fertilizer
◦Much phosphorus to rivers, ocean sediments
◦Slowly released in terrestrial and aquatic ecosystems via weathering of rocks
◦Human activity has moved cycle:
land freshwater ecosystems
Nitrogen cycle signifigance
Biological/Ecological Significance
◦amino acids (proteins), nucleic acids, chlorophyll, hemoglobin
◦of high ecological importance, scarce
Nitrogen resivors
Largest pool is in the oceans
◦Includes major atmospheric pool, but only one way to bioavailability - N2
◦Human activity has moved cycle: land atmosphere
Nitrogen forms and fluxes
Forms and Fluxes:
◦Only nitrogen fixers can use atmospheric supply directly - N2 reduced to ammonia (NH3) in an energy-demanding process
Once N is fixed it is available to organisms
◦Ammonification: upon death & decomposition, N can be released by fungi and bacteria as NH4 (ammonium)
◦Nitrification: Ammonium (NH4) nitrate (NO3) by bacteria
NH4, NO3 are used directly by bacteria, fungi, plants
◦Denitrification: NO3N2 (via anaerobic respiration by specific bacteria)
Carbon cycle signifigance
Biological/Ecological Significance
◦Component of all organic molecules, also CO2
◦Important biologically as well as atmospheric forms to climate
◦Moves between organisms and atmosphere through the reciprocal processes of photosynthesis and respiration