Biology 1010 Lecture Notes
Unit 4. Introduction to Ecology
This page was last updated April 7, 2003
Key terms and phrases
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population, community, ecosystem, biosphere
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biodiversity, species richness
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abiotic vs biotic factors
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exponential growth models, logistic growth models, demographic models;
rate of increase, carrying capacity; r-selected species, k-selected species
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Laws of thermodynamics; entropy
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Energy flow, nutrient cycles
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Net and gross primary productivity; net and gross secondary productivity;
energy pyramids
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nitrogen-fixation, nitrification, denitrification
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Introduction
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observation--members of a species are not uniformly distributed over the
world; groups of species sometimes seem to occur together
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leads to the concepts of populations, communities, ecosystems, biomes
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raises the questions of what are the major influences on the distribution
of species and do communities form integrated units (Gaia hypothesis in
its broadest form)
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in this unit we are concerned with what are the factors that give rise
to the structure of ecosystems
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role of abiotic factors
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physical/chemical factors
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types
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for each physical chemical factor there is a certain limit range of values
that can be tolerated by individuals and by members of a species; within
this range there is a certain optimum where the individual or species does
the best; each individual or species has a particular set of abiotic factors
it can tolerate, these define the boundaries of its theoretical habitat;
niche refers to the way organisms uses the habitat and the resources therein
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island biogeography
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geographic barrier blocks movement of organisms
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size of island affects the number of habitats
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dynamic between colonization and extinction
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environmental catastrophes (meteorites, volcanic eruptions, free O2) can
severly limit the numbers of individuals
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role of biotic factors
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competition within or between species for a limiting resource
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scramble (exploitative) vs interference competition
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competitive exclusion principle, resource partitioning and character displacement;
realized niches; Darwinian evolution
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predation and parasitism
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food chains and food webs
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prey defenses
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chemical defenses--secondary metabolites in plants, poisons and toxins
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camouflage
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mimicry and warning coloration
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commensalism and mutualism
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keystone species--predator that promotes diverisity
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which is more important?
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Global systems
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Aquatic systems
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pelagic systems
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geologic/geographic profile
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continental shelf--less than 200 meters
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continental slope
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abyssal plain--average around 3000 meters
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physical/chemical profile
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light and temperature profiles; thermocline
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nutrient levels; upwelling
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biological profile
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euphotic zone
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phytoplankton (ultraplankton)
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zooplankton
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fish
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numbers of organisms
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deeper waters
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benthos
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abyssal plain
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hydrothermal vents
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neritic and littoral systems
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physical/chemical conditions
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light and temperature
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tides
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wave action
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nutrient status
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biological conditions
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Terrestrial systems
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controlled primarily by moisture
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latitudinal variation
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topographic factors
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biological interactions/trends in biodiversity
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Ecosystem dynamics--population growth
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general ideas
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birth, death, immigration, emigration
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techniques
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census
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mark and recapture
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proportional areas
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models
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exponential models; rate of increase
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doubling time in bacterial cultures
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human population growth, r = 1.4%, P = 6 billion
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logistic models and the carrying capacity
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basic features
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components of the carrying capacity
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r-selection and K-selection
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what is the carrying capacity of the Earth for humans?
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demographic models
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mortality; age-dependent mortality
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fertility; age-dependent fertility; total fertility; replacement fertility
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survivor curves
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type I--almost all live until reach old age then die rapidly
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type II--equal chance of dying at any age
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type III--most mortality in newborns; after certain age there is a good
chance of surviving
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examples
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humans with high infant mortality
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previous example with 0 infant mortality
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previous example with replacement rate fertility
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population momentum
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Ecosystem dynamics--ecosystem function
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introduction--life support systems
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application to spaceship Earth
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Basic rules governing everything
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matter is neither created nor destroyed
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First Law of Thermodynamics--the amount of energy does not change, only
the form
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Second Law of Thermodynamics--the quality (usefulness) of the energy decreases
with every change
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version two--entropy increases in closed systems
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implications
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Energy flow in ecosystems
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light driven systems
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initial input = sunlight
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solar constant = 1360 Watts/m2 (0.325 kcals/m2/sec); equivalent to about
5 million kcals/m2/year (because of day-night cycles)
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about 30% of the energy is reflected back into space and another 20% absorbed
by the air, bringing the total to 2.5 million kcals/m2/year; value less
at the poles because of the spherical shape of the Earth
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plants and algae absorb a small fraction of the light (roughly 30% in forests
and lakes, much less in deserts); an even smaller fraction of the light
absorbed (usually about 2%) is converted to chemical energy through photosynthesis--this
is referred to as gross primary productivity (maximum less than 15,000
kcals/m2/year)
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plants and algae first use the converted energy to battle entropy (referred
to as respiratory losses); anything left over can be used for growth and
reproduction--the left over is referred to as net primary production
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grazers (herbivores) eat a fraction of the plant material (clearly they
can't eat it all) and assimilate some of the ingested energy; the assimilated
energy is used first to battle entropy; anything left over is available
for growth and reproduction (net secondary productivity)
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assimilation efficiency depends on the type of food (seed, stem, flower,
etc)
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net production efficiency depends on the metabolism of the herbivore
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ecological efficiency is defined as consumer productivity/prey productivity;
in terrestrial systems usually estimated as about 10%, somewhat higher
in aquatic systems
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predators eat a fraction of the herbivores and assimilate some of the ingested
energy (usually a higher percentage than herbivores get from their food);
energy is used to first battle entropy, then for growth and reproduction
(net tertiary productivity)
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some questions
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how long can food chains be?
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short in terrestrial systems, longer in aquatic systems
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what about all of the unassimilated material?
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detritus food chains and the role of bacteria
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what happens to all of the heat and and all of the light absorbed by the
Earth?
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must eventually be lost to space or the Earth would melt
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basic mechanisms of heat transfer: conduction, convection, radiation;
only radiation applicable
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what does this imply about life-support systems for space-flight?
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what kinds of yields would be necessary to sustain human life? how
much volume would that take?
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how do space ships solve the heat problem?
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chemically-driven systems
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relatively rare accept near vents
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basic on the production of ATP and organic molecules by chemoautotrophs;
otherwise similar to what happens in light
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where does the energy come from? i.e., why is the center of the Earth hot?
recall famous debate between Lord Kelvin and Darwin
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Element cycling in ecosystems and globally
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most important elements: CHNOPS
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carbon
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functions in organisms
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major pools of carbon
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connections between the pools
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biological cycle
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mineralogical/geological cycle
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problems
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increasing CO2 in the atmosphere could lead to climate change
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shortage of fossil fuels
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oxygen
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functions in organisms
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major pools: water, O2 in the air, oxygen in inorganic molecules
and minerals (carbon dioxide, silicates, oxides, etc.), oxygen in organic
molecules
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connections: photosynthesis, respiration (electron chains)
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problems
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nitrogen
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functions in organisms
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major pools: N2 in the air, ammonium ions, nitrate ions, and nitrite
ions in water and soil, nitrogenous compounds in organisms
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connections
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nitrogen fixation by bacteria and cyanobacteria
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N2 converted to ammonium by nitrogenase; energy expensive
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nitrogenase usually can only work in the absence of oxygen
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nitrogen in organic wastes usually converted first to ammonia (ammonification)
then to nitrite then to nitrate (nitrification) which can be used by plants
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some nitrate is converted to N2 again in the process of denitrification
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problems
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aquatic pollution--eutrophication
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lake dynamics and phytoplankton blooms
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eutrophication
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other water pollution problems
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NOx compounds and smog
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phosphate
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functions in organisms
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major pools: PO4 ions in soil and water, organisms, detritus, phosphate
rocks
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connections: uptake, ingestion, decomposition, binding at low and high
pH
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pesticide cycling
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definitions
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biological amplification
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genetic pesticides
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Prospects
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summary of current problems
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population growth
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energy requirements
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carbon dioxide increases and global warming
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air and water pollution
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