individual
one organism (elk)
population (pop.)
group of individuals of the same species (elk herd)
community
all living organisms in an area
ecosystem
all living and nonliving things in an area (plants, animals, rocks, soil, water, etc.)
biome
the plants and animals found in a given region - determined by climate (tropical rain forest)
biosphere
the region of our planet where life resides, the combination of all ecosystems on Earth
competition
organisms fighting over a resource like food or shelter; limits pop. size since there are fewer resources available and few organisms can survive
predation
one organism using another for energy source (hunter, parasites, even herbivores)
mutualism
relationship that benefits both organisms (coral reef)
commensalism
relationship that benefits one organism and doesn't impact the other (birds nest in trees)
parasitism
an interaction in which one organism lives on or in another organism
herbivores
plant eaters - eat plants for energy (giraffe and tree)
true predators
carnivores - kill and eat prey for energy (leopard and giraffe)
parasites
use a host organism for energy, often without killing the host & often living inside host (mosquitoes, tapeworms, sea lamprey)
parasitoids
lay eggs inside a host organisms; eggs hatch and larvae eat host for energy (parasitic wasps, bot fly)
symbiosis
any close and long-term interaction between two organisms of different species
resource partitioning
different species using the same resource in different ways to reduce competition
temporal partitioning
using resources at different times (wolves and coyotes hunting at different times, night vs day)
spatial partitioning
using different areas of a shared habitat (different length roots)
morphological partitioning
using different resources based on different evolved body features
biome characteristics
Latitude (distance from equator) determines temperature & precipitation which is why biomes exist in predictable patterns on earth
tropical rainforest
nutrient-poor soil - high competition from so many different plant species
boreal forest
nutrient-poor soil - low temp. and low decomposition rate of dead organic matter
temperate forest
nutrient-rich soil - lots of dead organic matter; leaves & warm temperature/moisture for decomposition
shifting biomes
as earth's climate changes, biomes shift in location
salinity
how much salt there is in a body of water, determines which species can survive and usability for drinking (fresh water vs. estuary vs. ocean)
depth
influences how much sunlight can penetrate and reach plants below the surface for photosynthesis
flow
determines which plants & organisms can survive, how much O2 can dissolve into water
temperature (aquatic biomes)
warmer water holds less dissolved O2 so it can support fewer aquatic organisms
delta and flood plains have ___________
fertile soil because rivers have high O2 due to flow mixing water and air and they also carry nutrient-rich sediments
lake
a standing body of fresh H2O (key drinking H2O source)
littoral
shallow water with emergent plants
limnetic
where light can reach (plants can photosynthesize) - no rooted plants, only plankton
profundal
too deep for sunlight (no photosynthesis)
benthic
murky bottom where inverts (bugs) live, nutrient-rich sediments
wetland
area with soil submerged/saturated in water for at least part of the year, but shallow enough for emergent plants
benefits of wetland
Stores excess water during storms, lessening floods
Recharges groundwater by absorbing rainfall into soil
-Roots of wetland plants filter pollutants from water draining through
-Highly plant growth due to lots of water & nutrients (dead organic matter) in sediments
estuaries
areas where rivers empty into the ocean (mix of saltwater and freshwater) - high productivity (plant growth) due to nutrients in sediments deposited in estuaries by rivers
salt marsh
estuary habitat along coast in temperate climates, breeding ground for many fish and shellfish species
mangrove swamps
estuary habitat along coast of tropical climates; mangrove trees with long, stilt roots stabilize shoreline and provide habitat for many species of fish and shellfish
what coral reefs are
warm shallow waters beyond the shoreline; most diverse marine biome on earth
mutualistic relationship between coral and algae in a coral reef
coral takes CO2 out of the ocean to create calcium carbonate exoskeleton (the reef) and provides CO2 to the algae; algae live in the reef and provide sugar (energy) to the coral through photosynthesis
why coral and algae rely on each other in a coral reef
Coral couldn't survive without energy from algae, algae need the home of the reef and CO2 from the coral
intertidal zones
narrow bands of coastline between high tide and low tide; organisms must be adapted to survive crashing waves and direct sunlight/hear during low tide (ex: barnacles, sea stars, crabs that can attach themselves to rocks); different organisms are adapted to live in different zones
open ocean
low productivity/area as only algae & phytoplankton can survive in most of ocean; so large though, that lagae and phytoplankton of ocean produce a lot of earth's O2 and absorb a lot of atmospheric CO2
photic zone
area where sunlight can reach (photosynthesis)
aphotic zone (abyssal)
area too deep for sunlight (no photosynthesis)
the carbon cycle is _________
the movement of molecules containing carbon (such as CO2, glucose, CH4) between sources and sinks.
what happens during the carbon cycle?
Some steps are quick (e.g., fossil fuel combustion) while others are slow (e.g., sedimentation and burial), leading to an imbalance in carbon storage among different reservoirs or sinks.
the atmosphere important in the carbon cycle because ________
The atmosphere is a key carbon reservoir. Increasing levels of carbon in the atmosphere contribute to global warming.
carbon sink
reservoir that take in more carbon than it releases (ocean, plants, soil)
carbon source
reservoir that releases more carbon than it takes in (ff combustion, animal agriculture, deforestation)
photosynthesis _________
removes CO2 from the atmosphere and converts it to glucose (biological form of C and stored chemical energy in for of sugar) and is a CO2 sink
cellular respiration
done by plants and animals to release stored energy, uses O2 to break glucose down and release energy, and is a CO2 source by adding it to the atmosphere
direct exchange
CO2 moves directly between the atmosphere and the ocean by dissolving into and out of ocean water at the surface, this happens very quickly and in equal directions, balancing levels of CO2 between the atmosphere and the ocean; because of direct exchange, increasing atmosphere CO2 also increases ocean CO2, leading to ocean acidification
burial
slow, geological process that stores C in underground sinks like sedimentary rock or fossil fuels, takes longer for burial than extraction and combustion
sediments
bits of rock, soil, organic matter
sedimentary rock
sediments compressed by pressure from overlying rock layers or water
fossil fuels (ff)
coal, oil and natural gas are formed from fossilized remains of organic matter, carbon sink
extraction and combustion
digging up or mining ffs & burning them as energy source; releases CO2 into atmosphere (carbon source), takes longer for burial than extraction and combustion
nitrogen cycle
movement of N containing molecules between sources and sinks/reservoirs
nitrogen reservoirs
they hold N for relatively short period of time compared to C cycle (plants, soil, atmosphere)
main N reservoir
atmosphere
nitrogen (N)
critical plant and animal nutrient
nitrogen fixation
process of N2 gas being converted into biologically available (useable by plants) NH3 (ammonia) or NO3- (nitrate)
bacterial fixation
certain bacteria that live in the soil, or in symbiotic relationship with plant root nudules convert N2 into ammonia (NH3)
synthetic fixation
ff combustion converts N2 gas into ammonia (NH3)
assimilation (N)
plants and animals taking in N and incorporation it into their body
ammonification
soil bacteria, microbes and decomposers converting waste and dead biomass back into NH3 and returning it to the soil
nitrification
conversion of NH4 into nitrite (NO2-) and then nitrate (NO3) by soil bacteria
denitrification
conversion of soil N (NO3) into nitrous oxide (N2O) gas which returns to the atmosphere
nitrogen effects on climate
N2O (nitrous oxide) is a greenhouse gas which warms the earth's climate
ammonia volatilization
excess fertilizer use can lead to NH3 gas entering atmosphere
leaching
nitrates (NO3) being carried out of the soil by water
synthetic fertilizer use leads to nitrates leaching leading to _________
eutrophication
phosphorus cycle
movement of P atoms and molecules between sources and sinks/reservoirs; very slow compared to C/H2O/N cycles
major phosphorus sink
rocks and sediments containing P minerals
major natural source of P
weathering of rocks that contain P minerals
weathering
wind and rain breaking down rocks over time
synthetic sources of P
mining phosphate minerals and adding to products like synthetic fertilizers and detergents/cleaners
assimilation and excretion/decomposition (P)
P is absorbed by plant roots and assimilate into tissues; animals assimilate P by eating plants or other animals
sedimentation (P)
phosphate doesn't dissolve very well into water; much of it forms solid bits of phosphate that fall to the bottom as sediment
geological uplift
tectonic plate collision forcing up rock layers that form mountains; P cycle can start over again with weathering and release of P from rock
what is eutrophication?
an excess of N and P in the water
how does eutrophication lead to algae growth?
the excess N and P cause algae to grow rapidly, covering the water surface
what are the consequences of algae growth in eutrophication?
algae block sunlight, leading to the death of plants below the water surface
how does eutrophication affect O2 levels in water?
bacteria decomposing dead algae take up O2, leading to lower O2 levels that can kill aquatic animals
what positive feedback loop is created in eutrophication?
bacteria decomposing dead aquatic animals further take up O2 levels, creating a cycle of O2 depletion
eutrophication can occur from ______
fertilizer runoff, human/animal waste contamination
water cycle
movement of H2O (in different states) between sources and sinks; energy from the sun drives the H2O cycle
biggest H2O sink
ocean
transpiration
process plants use to draw groundwater from roots up to their leaves
evapotranspiration
amount of H2O that enters the atmosphere from transpiration and evaporation combined - both processes are driven by energy from the sun
infiltration
water trickling through soil down into groundwater aquifers
permeable
able to let water pass through
primary productivity (pp)
rate that solar energy is converted into organic compounds via photosynthesis over a unit of time
high pp
high plant growth —> lots of food and shelter for animals; ecosystems with high PP are more biodiverse
net primary productivity (npp)
the amount of energy (biomass) leftover for consumers after plants have used some for respiration
respiration loss (rl)
plants use up some of the energy they generate via photosynthesis by doing cellular respiration
gross primary productivity (gpp)
the total amount of sun energy that plants capture and convert to energy (glucose) through photosynthesis