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Fundamental niche
The niche potential of a species, if competitive
exclusion and resource partitioning were non-existentent
realized niche
The actual niche of a species bc competition is a thing
specialist species
animals that require specific resources
generalist species
species that can live in many different enviromentents and can eat many types of food
ecosystem engineer
species that modify the environment so that other organisms rely on the changes to survive
trophic cascade
A ripple effect across trophic levels caused by changes at one level.
Removing a top predator can increase herbivores, reduce plants, and alter habitat structure, erosion, and nutrient cycling.
(reciprocal changes in other pops)
indicator species
one whose presence/absence/health reveals environmental conditions.
Sensitive species can signal pollution or oxygen stress before broader ecosystem damage is obvious
species sensitive to certain enviromental conditions
invasive species
introduced species may outcompete natives.
Common invasive traits include fast growth, rapid reproduction, high dispersal, tolerance of many conditions, broad diets, association with humans, and prior invasion success.
generalists and usually outcompete specialists
Commensalism
+/0
One benefits while one is unaffected
Parasitism
-/+
One is benefitting while one is being harmed
Mutualism
+/+
Both benefit
Predation
1 organism gains energy from another (hunter/predator eats prey)
Intraspecific competition
Competition of resources between the same species
Interspecific competition
competition b/w different species
Competition Exclusion principle
if 2 different species in the same territory start to fill the same niche, they will compete for the same resources and one willl lose
Resource partitioning
Different species use the same resource in different ways to reduce comp
temporal partitioning
use same resource at different times
spatial partitioning
using diff areas of shared habitat/resouce
Tropical rainforest
Most diverse biome
high precipitation and heat
Nutrient-poor soil decaying matter quickly sucked up becuase of a lot of vegetation
Morphological partitioning
species evolve different structures to use the same resource differently
different resouces based on evolved body features
savannah/ tropical grasland
small shrubs
Temperate grassland
richest soil
cooler temps
less biodiverse
Tundra
Permafrost frozen ground
cold desert
short growing season
temperare decidious forest
all four seasons
oak hickory trees
moderat rainfall
Aquatic biomes
characteristics: salinity (marine biome-salt/freshwater-no salt)
factors: pH & light availability- light is needed for photoautotrophs (photoplankton are primary consumers of surface)
Freshwater & layers of lake
no salt & drinking water
Litoral layer: shallow water with emergent plants (1st layer)
wetlands
area w soil submerged in water for at least part of the year
lessens floods
Estuaries
Where the river meets the sea (transition zone)
high productivity (plant growth)
Intertidal zone
marine
Fluctuating tides (narrow band of coastline b/w high & low tide)
organisms must be adapted to survive
Disolved oxygen
Amount of oxygen available in the water
Cold water= holds more oxygen
Warm water = less oxygen (release)
Running stream holds more oxygen (colder)
eutrophication often causes low-oxygen “dead zones”: decomposition increases and oxygen drops.
Biological oxygen demand
how much oxygen is needed
Amt of D.O. used by aerobic microrganisms
More organic matter = greater BOD
Human impact - sediment pollution
turbitity = measure of dissolved/suspended solute
Light cant penetrate → less productivity
Eutrophication
Excessive richness of nutrients in a lake or water
due to runoff from the land, which causes a dense growth of plant life & death of animal life from lack of oxygen.
unoff brings nutrients and silt, but fertilizer pollution can dramatically accelerate algae growth and deplete oxygen
Carbon sinks
largest carbon sink: ocean (hydrosphere)
Lithosphere - sediments/soil
Biosphere- vegetation (3rd largert)
sink/reservior: stores more while source releases more
Carbon cycle
Photosynthesis removes CO2 from air or water and stores it in organic molecules.
Cellular respiration returns CO2 to air or water.
Decomposition releases CO2, and can release methane in low-oxygen environments.
Combustion of biomass or fossil fuels rapidly releases CO2.
Solutions- increase biomes and plant trees
Nitrogen cycle