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species distribution
range of area that a species occupies
Island biogeography theory
hat larger, less isolated islands support more species.
dispersal
the movement of individuals or gametes away from their original location
dispersal limitations
behavior
environment
biotic + abiotic components, everything in an organisms surroundings
biotic
living components of the environment
abiotic
non-living components of the environment
abiotic limits
temperature
biotic limit
herbivory, competition
continuous gradient
physically continuous
patchy gradient
patches span range of environmental conditions
biome
a region experiencing similar environmental condition, therefore containing a similar core set of species
temperature
increase at low latitudes because they receive more solar radiation
decreases at high elevation
precipitation
decreases at mid latitudes because of Hadley cell air
increases at high elevation on windward side of mountains
Hadley cell step 1
tropical air heats up, moisture rises and air cools
Hadley cell step 2
cooler air precipitates moisture as rain in tropic
Hadley cell step 3
rising air is displaces either north or south, creating winds and air transport
Hadley cell step 4
transported air begins to cool down and sink
Hadley cell step 5
dry air falls in mid-latitudes
oceans
buffer climate, so climate extremes are strong in the interior of continents
ecosystems
all the organism in a place and the environment
ecosystem ecology
typically focuses on systems thinking, and abstracting away the complexity of what happens within it, meaning less focus on population and communities
photosynthesis
solar energy is captured by formation of C bonds in compounds that are stored in organismal bodies
respiration
metabolic reaction release chemical energy, and in doing so return carbon to the environment
energy used directly for metabolism
gross primary production
the energy obtained from sunlight by autotrophic organisms
net primary production
all the energy available to other organisms from autotrophs
NPP equation
NPP = GPR - R
climate drivers of NPP
water availability is a limit on productivity
extreme temperatures limit productivity
energy flow
consumption of living tissue and organisms
ecological efficiency
fraction of energy later available to other organisms growth
assimilation fraction
fraction of energy used by an organism for growth and respiration
trophic pyramid
distribution of energy across trophic levels
trophic cascade
an effect of energy flow due to a change in the biomass of one trophic level
bottom up control
amount of limiting resources determine energy avail to producers which in turn limit other trophic levels
top down control
amount of top predators/ consumer determines energy flows of prey, which in turn limit other trophic levels
sociometabolism
metabolism of human accounting for bodily energy use and also indirect consumption through appropriation of ecosystems ad well as other energy sources
residence time equation
residence time = stock/flux into subject
net flux
when fluxes in are not equal to the fluxes out
types of stocks
sink and source
sink
a stock that is increasing due to net flucx
source
a stock that is decreasing due to net flux
nitrogen cycle I
nitrogen reaches animals and plants→ nitrogen expanses animal and plants through decomposer microbes
nitrogen fixation
bacteria convert nitrogen gas to ammonium or amonia for the rest of the ecosystem to use
nitrogen cycle II
humans increase nitrogen inputs via industrial nitrate fertilizers
humans increase nitrogen inputs from atomostphere to land via acid rain
acid rain
nitric acid and other compounds
haber-bosch process
production of nitrate from nitrogen gas using catalysts, hydrogen, and high pressure/ temperature
nitrogen fixing crops
an alternative to fertilizer
phosphorus cycle
most phosphorus available to life boringly comes from phosphate rock weathering, restored slowly as new phosphate rock is formed
rock weathering
method of introducing phosphorus to ecosystem
Dust transport
Dust particles, once airborne, can be carried by winds to various distances from the source region and deposited back onto the surface somewhere downstream
greenhouse gas
absorb infrared radiation and re-emit infrared radiation, trapping more of it in the atmosphere instead of allowing it to radiate to space
greenhouse gas examples
carbon dioxide, nitrous oxide, methane, ozone, water vapor
fossil fuel burning
direct emissions of carbon to the atmosphere
land use change
through chains how humans use land and therefore how the carbon cycle operates in those locations, we change carbon emissions
human impacts on carbon cycle
land use change and fossil fuel burning
climate models
link data to physical processes and enable predicting future climates
positive feedback
X changes, causing Y to change, causing X to change further- a destabilizing feedback
negative feedback
X chabges, causinf Y to change, causing X to change back toward its original value- a stabilizing feedback
positive feedback examples
ice feedback, vegetation feedback, cloud feedback
ice feedback
warmin = polar ice melting = lower albedo = more sunlight absorbed =. more warming
vegetation feedback
warming = more tree mortality = more CO2 in atomostphere =. more warming
cloud feedback 1
warming = more high elevation clouds = more infrared radiation absorbed = more warming
negative feedback examples
radiation feed back and cloud feedback
radiation feedback
warming = more infrared radiation
(heat) emitted = more cooling
cloud feedback 2
warming = more tropical atlitude
clouds = more sunlight reflected to space = more cooling
representative concentration pathway
reflect trajectories of population growth, economic development, and carbon efficiency of the economy with respect to using carbon
phenology
changes in timing of seasonal events relating to organisms
disease
a harmful condition affecting an individual, sometimes reducing its growth, survival, or reproduction
biological pest control
uses natural enemies like predators, parasites, or pathogens to manage pests
parasite
an organism that feeds on cell contents/tissues/fluids of a host while in to on the host organism; harm but usually do not kill the host organism. Generally much smaller than the host, but can also live outside the host organism
pathogen
an organism or virus that causes disease(not neccesarilty living on/in a host)
hyperparasites
parasites that live off of other parasites
contact transmission
direct movement from one host to another. indirect contact is also possible
vehicle transmission
indirect movement from one host to another via aerosols, water, dust, etc. also via side stage in an environmental reservior
vector transmission
indirect movement from one host to another via another biological host species
metapopulation
many patches, each with populations, linked by immigration/emigration of individuals
environmental reservior
locations where pathogenic species live when not parasitizing a host
biotic reservior
locations where pathogenic species live when parasitizing a host
ozonic disease
one that typically has non-human biotic reserviors but which can jump to a human host
SIR model of disease spread
factors in susceptible, infectious, and recovered(or dead) populations when an epidemic occurs
epidemic
when the number of infections individuals starts to rapidly increase(dI/dt > 0)
SIR equation
dI/dt =. beta * S * I - m * l
indigenous science
bodies of observations, oral and written knowledge, innovations, techniques, etc. developed by indigenous people passed from generation to generation
forest gardens
a non-plowed, year round tree dominated agricultural system common in central america
cultural landscape
maintained by regular actions that promote/ discourage certain species
fire
long tradition of indigenous management of landscapes by regular burning to promote habitat for food plant, game animals, ect.
pyromes
fire dependent biomes
pyrome examples
savanna, chaparral, and coniferous forests
regeneration
post-fire germination
flammability
dead tissue accumulates and promotes fire spread, compete by killing ones neighbors and survive better, or resprout first
serotiny
reproductive parts survive fire and open/germinate immediately after a fire- compete by having highest colonization or dispersal rate
anthrome
human-modified landscape
biotic homeogenization
overtime ecological communities increase in similarity over time
human appropriation
how much of the production humans use for their own benefit
protected area
humans set aside land or water areas for more restricted set of human uses
dispersal corridors
promote persistence of a species metapopulation across its multiple patches
translocation/ assisted migration
human moves genotypes of a species to new location, helping support climate adaptation and is also time/money-intensive