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level: Level 1

Questions and Answers List

level questions: Level 1

QuestionAnswer
variant on human population growth (population size, how resources are used, meeting necessities, valuation of ecological services, lack of knowledge)supply and demand
maximal rate a population can increase when there are no limits on its rate of growth (unlimited resources = unlimited growth)biotic potential
limiting factors that act together to limit growth of a populationenvironmental resistance
carrying capacity = maximum population size that a specific environment can handle/carryK
consume/use more to keep up, an unsustainable addictionaffluenza
anything we get from the living or nonliving environment to meet wants and needsresources
not to run out within human time scale (ex. direct solar energy)perpetual resources
renewed fairly rapidly by the sun directly or indirectlypotentially renewable resources
rate a potentially renewable resource can be used indefinitely without reducing supply (ex. forest, fresh h2o, fresh air, fertile soil)sustainable yield
exhaustible resourcesnonrenewable resources
exceed renewable resource replacement rate (potentially renewable resources changed to nonrenewable or unusable)environmental degradation
everything is a sum of its parts (do not completely understand function of species in a system)reductionist view
based on limited knowledge (uncertainties)quotas, harvests, etc.
has inputs but no outputs (high salt and mineral deposits)terminal lake
single interconnected system, connected by matter and energyearth
anything that has mass and takes up spacematter
how useful a matter resource is, based on availability and concentrationmatter quality
organized, concentrated, dilute, near surfacehigh quality matter
disorganized, dilute or dispersedlow quality matter
capacity to do work and transfer heatenergy
measurement of usefulness of energy to do workenergy quality
organized, concentrated, great ability to perform useful workhigh quality energy
disorganized, dispersed, little ability to do useful worklow quality energy
matter can neither be created nor destroyed by natural physical and chemical changes, but transferred/changed from one form to anotherlaw of conservation of matter
energy can neither be created nor destroyed, energy input = energy output **does not apply to nuclear chargeslaw of conservation of energy (1st law of thermodynamics)
energy quality is lost when converted from one form to anothersecond law of energy (2nd law of thermodynamics)
autotrophs, first trophic levelproducers
trophic levels greater than first (2-4/5 maximum)consumers
decomposers/detritus feeders (recyclers)detritivores
sequence of who eats or decomposes whom in a system, determines how energy moves through the systemfood web/chain
transfer of chemical energy (creates biomass)the currency of life
truest representation of energy available in an ecosystempyramid of energy
rate @ which producers convert solar energy into chemical energy as biomass (rate of solar to chemical energy)gross primary productivity (GPP)
rate @ which energy made by producers is available for use by consumers (rate energy is created for consumers) **carrying capacitynet primary productivity (NPP)
based on function and complexity (1.biosphere. 2.ecosystem, 3.community, 4.population, 5.organism)organizing matter
terrestrial and aquaticbiosphere division
distinct species and climates, large terrestrial regions characterized by similar climate, soil, plants, and animalsbiomes
average temperature and precipitationclimate
made up of interacting ecosystemsbiosphere
nonliving componentsabiotic
living componentsbiotic
zones of transition between 2 adjacent habitatstransition zones
flow of matter and energy between zonscycling
any chemical element or compound an organism must have to live, grow, and reproducenutrient
goods humans use directly (ex. food, lumber, medical plants)provisions
natural processes necessary to maintain other ecosystem servicessupport services
steps of converting something from one form to anotherprocess
control, adjust, manageregulate
dependent on diversity (insurance of continuance of ecosystem services)resilience
aesthetic beautycultural services
crucial for maintaining community, determine structure and function of ecosystemskeystone species
absence, presence, or abundance tells about environmental conditionsindicator species
native to area, help protect biodiversity by protecting habitatendemic species
deliberate or accidental introduction, harmful to environmentexotic/invasive species
range of physical and chemical environment a species can exist inspecies tolerance
evolution through natural selectionadaptation
through process of natural selection (allopatric and sympatric)speciation
geographic and reproductive isolationallopatric speciation
mutation or behavioural change (less common)sympatric speciation
low level species disappearance, change in local conditionsbackground extinction
catastrophic and widespreadmass extinction
higher than background but limitedmass depletion
things species do to survive that contribute to reproductive success (subject to natural selection)behavioural adaptation
change (removal of biomass), occurs over space and time **anthropogenic (human) or natural (environment)disturbance
ecosystems experiencing intermediate levels of disturbance are more diverse than those with high or low levels of disturbance (necessary to maintain species diversity)intermediate disturbance hypothesis
high competition and dominance (lowers diversity within a system)rare disturbance
weedy species - high growth rate, tend to dominate (lowers species diversity)frequent disturbance
rate @ which an ecosystem returns to its original state after a disturbance/change in flow of energy and matter cyclingresilience
fast to return to original statehigh resilience
slow to return to original statelow resilience
how disturbance is responded to (dependent on structure, function, and functional/structural redundancy)stability
species diversity, population sizes, physical/geographical factors, species interactionsstructure
rate of matter cycling and energy flowfunction
many species perform same structure and function within an ecosystemfunctional and structural redundancy
change in species composition in area, diversity, trophic structure, matter cycling, and energy flowsuccession
all biota are wiped out (complete loss)primary succession
biota and sediments remain, has starting point/has soilsecondary succession
human intervention to assist in successionrestoration
local area's short-term conditions such as temperature and precipitation (short term conditions, predict patterns)weather
long-term conditions, average precipitation and temperatureclimate
regulates climate and distributes nutrientsocean currents (water circulation)
drive surface currentsprevailing winds
driven by thermohaline circulation (temperature and salinity differences)great ocean conveyor belt
atmosphere closest to earth's surfacetroposphere
regulates global climatenatural greenhouse effect
features of earth's surfacetopography
effect on local climate as a result of human interferenceurban heat island effect
distinct texture and composition that differs with soil typessoil horizons
top layer, organic nutrients that fall on earth's surfaceO horizon
already has organic material beginning to breakdown (typically from O horizon)A horizon
organic material already beginning to be broken downhumus
organic material broken down even more, has rock and parent material (greater composition of parent vs organic material)B horizon
parent material (bedrock soil has been built in)C horizon
relatively large O layer, well developed A horizon (seasons input organic material)deciduous forest soil
most productive in NPP, not much A horizon (high rainfall leaches nutrients out of soil, lack of seasons)tropical rain forest soil
limited O/A horizons (hard for vegetation to grow, harsh/extreme conditions, vegetation does not drop/shed any part to retain nutrients and h2o)desert soil
lots of organic inputgrassland soil
bedrock is much larger, less O/A than deciduous (evergreens: needles are hard to breakdown, needles: high acidity, slower rate of decomposition)coniferous forest soil
evaporation exceeds precipitation (little precipitation and vegetation)desert biomes
wind and limited vegetation, topography changes quite frequently due to lack of vegetation holding it in placetropical desert
more rain therefore more vegetation (vegetation is drought-resistant physiologically/structurally)temperate desert
precipitation often as snow, cold temperatures limit vegetationpolar desert
shed parts or die, leave behind dormant long-lived seeds/eggsexpire (adaptation)
move to less stressful location, change timing of activityevade (adaptation)
lack of h2o = store, conserve, tolerateendure (adaptation)
requires some precipitation, endures seasonal drought and withstands fire, grazing by large herbivoresgrassland biomes
warm year round w/ distinct wet/dry seasons, scattered vegetation w/ herds of hoofed grazers and browserstropical (savanna) grasslands
cold winters and hot summers with moderate rainfall, dominated by drought-tolerant and fire-adapted grasses, ideal for growing cropstemperate grasslands
bitterly cold with frigid winds, mostly covered in snow/ice, vegetation is scarcepolar (arctic tundra) grasslands
coastal regions that border deserts, desirable area to live in but high chance of forest fireschaparral (temperate shrubland)
undisturbed, moderate to high precipitation to support trees, vegetation is variedforest biomes
equatorial, little temperature variation, rain almost dailytropical rainforest
how needs are met for food, shelter, and reproductionstratified niches
seasonal moderate temperatures with evenly spread abundant precipitation, warm summers and cold winters, mature community of few tree species, diverse ground level vegetationtemperate deciduous forests
long dry cold winters and moderate to warm summers, dominated by few cone-bearing trees, low diversityevergreen coniferous forest (boreal)
found in temperate coastal areas, fog and rainfall common, huge cone-bearing evergreen trees, mosses, and fernscoastal coniferous forest (temperate rainforest)
dramatic changes in altitude, climate, soil, and vegetation over short distance, regulates earth's climate and hydrologic cyclemountain biomes
l --> g (h2o-->vapor)evaporation
plants absorb h2o through roots, give off h2o vapor through pores in leavestranspiration
g --> l (more dense-->less dense)condensation
h2o falls from skyprecipitation
h2o from top of soil surface into soilinfiltration
h2o moves through soilpercolation
involves elevationrunoff