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Organismal Ecology
includes physiological, evolutionary, & behavioral ecology
Population Ecology
focuses on factors affecting population size over time
studies populations in relation to their environment
Community Ecology
examines the effect of interspecific interactions on community structure & organization
Ecosystem Ecology
emphasizes energy flow & chemical cycling between organisms & the environment
Landscape Ecology
exchanges of energy, materials, & organisms across multiple ecosystems
Global Ecology
examines the influence of energy & materials on organisms across the biosphere
Earth’s climate varies by
latitude & season; changing rapidly
Climate
long-term prevailing weather conditions in an area
Physical Components of Climate
sunlight
temperature
precipitation (rainfall, snow, ice)
wind
Solar energy determines
temperature variation
circulation of air
circulation of water
evaporation of water
Latitudinal variation determines
angle of sun
which varies sunlight intensity
which causes season variation (temperature/precipitation)
The tilt of the Earth causes
incidental sunlight & creates the season variation
Solar radiation causes
global patterns of air circulation & precipitation
Pattern of air circulation & precipitation
wet warm air rises over equator, due to temperature
as air cools & expands in upper atmosphere, rain falls over equator
dry cold air masses return to Earth, absorb water from land (30°); deserts
as air cools & expands in upper atmosphere, rain falls over land (60°)
Surface winds are named by
the direction they originate from
Tradewinds
northeasterly, southeasterly - blow towards equator
Westerlies
west-east winds 30° N/S to 60° N/S - blow towards poles
Large bodies of water moderate
the climate of nearby land
Mountains influence air flow
over land & affect climate in the area
Windward Side
warm air cools as it rises up the mountain
releases moisture on windward side
Leeward Side
cool dry air descends down mountain
it warms as it descends; picking up any moisture from land
creates a rain shadow on leeward side; arid region
Every 1000m increase in elevation
drops temp 6°C
equal to change at different latitudes
Every environment on Earth is characterized by a
mosaic of small-scale differences in abiotic & biotic factors that influence the distribution & abundance of organisms
Global Climate Change
directional change to global climate
lasts three decades or more
Why is global climate change happening?
increasing carbon dioxide
deforestation - trees take CO2 out of the atmosphere
burning fossil fuels - adds CO2 to the atmosphere
What are signs of global climate change?
wind patterns shifting
precipitation patterns shifting
global temperature has increased
extreme weather events have increased
Current range & predicted ranges (American Beech)
beech needs to move 4-6 miles/year to remain in favorable climate
has only moved 0.12 miles since ice age
Seeds can travel by many mechanisms to
spread to further range
The distribution of terrestrial biomes is controlled by
climate & disturbance
Biomes are
major life zones
Terrestrial Biomes
climate is major factor
precipitation & temperature
northern vs. southern hemispheres
vertical layering - important feature
Distant Biomes
similar environments create convergent evolution
Cacti in North America & Euphorbs in African deserts
convergent evolution, analogous features
Hawaiian Islands
tourist area is leeward side
Disturbance (terrestrial biomes)
an event that changes a community
fire, flood, hurricane
human activity (MAJOR THREAT): pollution - global warming, urban areas - habitat loss/fragmentation, farms - habitat loss/fragmentation
Climograph
plots the annual mean in temperature & precipitation in a region
Aquatic Biomes
less latitudinal variation than terrestrial biomes
marine biomes average salt concentration of 3%
oceans make up largest biome - 70% Earth
What is the average salt concentration of freshwater biomes?
< 0.1%
Freshwater biomes influenced by
surrounding terrestrial biome
patterns of water
speed of water
Many aquatic biomes are stratified into zones defined by
light penetration
temperature
depth
Pelagic Zone
“open sea”
open water area; not close to shore
has photic & aphotic zones
Upper photic zone (pelagic)
sufficient light for photosynthesis
most organisms live in photic zone
abundant sunlight
Lower aphotic zone (pelagic)
receives little light; sunlight is sparse
extensive zone, but little life found there
abyssal zone - 2000 to 6000m
Benthic Zone
bottom zone - deep or shallow water
organic or inorganic sediment at bottom
benthos are communities of organisms living there
detritus falls from productive surface waters = food source
Littoral Zone
area near shore
submerged plants final area
Limnetic Zone
deeper water past shore
within photic zone
Intertidal Zone
area between high tide/low tide
Neritic Zone
from low tide to continental shelf
Oceanic Zone
everything else; divided into three parts
Thermocline
in oceans & lakes
temperature boundary separates warm & upper lower cold H2O
Turnover
mixes oxygenated water of surface & nutrient rich water of bottom
tropical lowland lakes & ocean have year round mixing of water
temperate lakes undergo semiannual mixing of water
Aquatic Biome Characterization
physical environment (light penetration; temperature; depth)
chemical environment (salinity; oxygen concentration; nutrient density)
geologic features
photosynthetic organisms (autotrophs)
heterotrophs
human impact
Biotic factors that affect the distribution of organisms
predation
herbivory
competition
mutualism
parasitism
abiotic factors that affect the distribution of organisms
temperature
water
oxygen
salinity
sunlight
soil
Most abiotic factors vary in
space & time
Population ecology determines how
biotic & abiotic factors influence population density, dispersion, & demography
Population
a group of individuals of single species living in same general area
described by boundary & size
Density
number of individuals per unit area or volume within set boundary
ex: number of E. coli in a test tube; number of oak trees in a park
Dispersion
pattern of spacing among individuals within their boundary
environmental & social factors influencing spacing
Demography
study of birth/death/migration/vital rates of a population over time
Population size (density) can be estimated by
extrapolation from small samples
Mark-Recapture Method
capture organism
tag (mark) organism
release tagged organism (s = number tagged & released)
scientists recaptured a 2nd sample of individuals (n)
note how many are marked (x) in 2nd sample
estimated population size (N = sn/x)
Images of animals can be used
to identify animals - spot patterns, fin shapes, etc.
Density is the result of
interplay between processes that add or remove individuals from a population
birth = adds
immigration = adds
death = removes
emigration = removes
Clumped Dispersion
individuals aggregate in patches
most common pattern of dispersion
influenced by 1. resource availability 2. mating behavior 3. group predator defense
Uniform Dispersion
individuals are evenly distributed
influenced by 1. social interactions 2. territoriality
Random Dispersion
pattern of each individual is independent of other individuals
not influenced by 1. strong attractions 2. strong repulsions
uncommon in nature
Life Tables
summarize demographic information
age specific summary of 1. survival rates 2. reproductive rates
follow the fate of a cohort
same aged group followed from birth-death
tracks proportion of cohort that survives from one age group to the next
males usually ignored; females produce offspring
population is viewed as females producing new females (offspring)
Survivorship Curve
graphic way to represent data in life table
three types - Type I, Type II, Type III
most species are intermediate to these curves
Type I Survivorship Curve
large mammals, few offspring, care for young
low death rates early & mid life; deaths increase in older age
Type II Survivorship Curve
rodents, invertebrates, annual plants
constant death rate over organism’s life span
Type III Survivorship Curve
produce large numbers of offspring; little/no care
high death rates in young, lower death rate of survivors
Reproductive Rates
counts number of females in age group
counts average number of female offspring produced by females
age specific reproductive rates vary considerably by species
overharvesting can lead to population collapse
Exponential Population Growth
describes population increase under idealized conditions
dN/dt = the rate at which the population is increasing in size at each moment in time
N = current population size
r = constant; the intrinsic rate of increase/growth
r = the per capita (per individual) rate at which an exponentially growing population increases in size at each instant in time
Exponential population growth cannot be
sustained for very long in any population
Carrying Capacity
a more realistic population model limits growth by incorporating K
K = maximum population size the environment can support
varies with abundance of limiting resources
food, shelter, refuge from predators, nesting sites, etc.
Logistic Population Growth Model
produces a sigmoid curve
individuals are added to population most rapidly at N = K/2
when N approaches K, growth rates slow down
births decrease; deaths increase
when N=K, the population stops growing
Logistic Population Growth Model Importance
useful as a starting point for thinking about how populations grow & constructing more complex models
important for predicting how population will recover from small size, estimating sustainable harvest rates for wildlife populations, determining critical size at which animals may go extinct
Life history traits are products of
natural selection
Life History
traits that affect an organism’s schedule of reproduction & survival
why we should not overharvest or overfish
Key Components of Life History
when an organism reaches sexual maturity
how often the organism reproduces
how many offspring are produced per reproductive episode
Semelparity
semel = once & parere = to beget
Big Bang reproduction
produce once then die: salmon
in hostile environment, adult & offspring likely to die
Iteroparity
iterare = to repeat & parere = to beget
repeated reproduction
produce offspring multiple times while fertile
in dependable environment, both adult & offspring tend to survive
Life histories represent an
evolutionary resolution of conflicting demands
limited resources mandate trade-offs between investment in reproduction & survival
Categorizing the diversity of life history based on variables of logistic equation
K-selection
r-selection
K-selection
selection for traits that are advantageous at high densities
operates in populations living near limits imposed by resources (carrying capacity)
competition among individuals of population is strong
r-selection
selection for traits that are advantageous at low densities
maximizes intrinsic rate of increase r
competition among individuals of population is weak
Density-Dependent factors regulate
population growth
Mechanisms of Density-Dependent Regulation
competition for resources
disease
predation
territoriality
intrinsic factors
toxic wastes
Competition for Resources (density-dependent regulation)
plants are stuck where they are
use of fertilizers on crops to increase yield
Disease (density-dependent regulation)
more dense populations spread diseases more easily
less resources, more stressed physiologically, get sick
Predation (density-dependent regulation)
dense population, prey is more abundant, may be selected
Territoriality (density-dependent regulation)
when space is resource of competition
surplus of non-breeding males is a sign
Intrinsic Factors (density-dependent regulation)
physiologic factors that regulate population size, even with resources
Toxic Wastes (density-dependent regulation)
as density increases, so do toxins, alcohol for yeasts
global warming, etc. for humans
No population can
increase indefinitely (humans are no exception)
Age structure diagrams can (pyramids)
help predict a population’s growth trends
Ecological Footprint
summarizes aggregate land & water area needed to sustain a person, city, or nation (provides all resources one consumes & absorbs all the waste one generates)
Types of Lakes
oligotrophic
eutrophic
Types of Wetlands
marsh
bog
swamp