1/86
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai | Chat |
|---|
No analytics yet
Send a link to your students to track their progress
biotic factors
living things
abiotic factions
non living factors (air, water, rock, temperatures)
what communities are dominated by biotic factors
organism dense communities
what communities are dominated by abiotic factors
extreme habitations
grass adaptation to sand dunes
thick waxy cuticle → reduce transpiration
stomata in indentations → humid air can remain
leaves roll up in droughts → humid chamber
carb accumulation in root+leaf cells → increase osmotic potential
tree adaptations to mangrove swamps
secretion of excess salt from salt glands in leaves
cable roots grow close to surface for more O2
large buoyant seeds carried by ocean
abiotic variables affecting plant species distribution
temp, water, light, soil pH and salinity, availability of mineral nutrients
abiotic variables affecting animal species distribution
water and temp
transects
investigate tolerance ranges of species
transects examples
line intersect sampling, belt transects, observational transects
sensors
record levels of a parameter
data loggers
conditions required for coral reef formation
depth: less than 50 so light can reach
pH: above 7.8
salinity: 32-42 parts per thousand
clarity for light
temp: 23-29 degrees celsius
biome
all ecosystems of a specific type
ecological niche
every species in an ecosystem fulfills a unique role
species can’t survive unless all niche dimensions are satisfied
what do zones of tolerance determine
habitat
requirements of obligate aerobes
continuous O2
only live in oxic environments
examples of obligate aerobes
all animals and plants
requirements of obligate anerobes
no O2
only live in anoxic environments
examples of obligate anerobes
clostridium tetoni
methanogenic archaea
requirements of facultative anaerobes
use of O2 if available
live in oxic or anoxic environments
examples of facultative anaerobes
e.coli, yeast
modes of nutrition
photosynthesis, holzoic, mixotrophic
what is the energy in sunlight used for
fix CO2, produce sugars/amino acids/other carbon compounts
what uses photosynthesis as a mode of nutrition
plants
eukaryotic algae
some bacteria groups
holozoic nutrition in animals
food is swallowed before digestion
ingestion
digestion
absorption
assimilation (synthesize macromolecules)
egestion (voiding undigested material)
heterotrophic as holozoic nutrition
carbon compounds come from organisms
mixotrophic nutrition in some protists
autotrophs, protists, facultative mixotrophs, obligate mixotrophs
autotrophs
make their own carbon compounds
protists (mixotrophs)
both auto and heterotrophs
falcultative mixotrophs
can’t synthesize the carbon compounds they inject
auto, hetero, or mixotrophs
eg, euglena
obligate mixotrophs
auto and hetero
ecological niche types
fundamental, realized, competative exclusion, saphotropic nutrition
fundamental niches
potential range is defined by tolerance range and adaptations, only if no competition
realized niches
subset of fundamental niche, reductions due to overlaps with the niches of other competitor species
actual extent of potential range, due to competition
competative exclusion
2 species fundamental niches overlaps, if one species outcompetes the other in all parts, the second species is excluded
saprotrophic nutrition
secrete digestive enzymes into dead organic matter, digest externally, and absorb product
includes some fungi and bacteria, aka decomposers
diversity of nutrition in archaea
diverse in every source used for ATP production
phototrophic, chemotrophic, heterotrophic
adaptations for dention and diet of herbivores
large and flat teeth to grind down fibrous plant tissues
adaptations of dention and diet for carnivores
defined canine teeth for tearing meat
adaptations of dention and diet for omnivores
mix of different types
adaptations of herbivors to resistance in plants
ex, insect mouth parts
jaw like for biting off, chewing, and investing leaf pieces (beetles)
tubular for piercing leaves/stems to reach ploem sieve and feed on sap (aphids)
plant adaptations
thorns and other physical structures
toxic secondary compounds in seeds and leaves
some animals have metabolic adaptations for detoxifying these, like milkweed aphids tolerate milkweed toxins
adaptations of predators for finding, catching, killing prey
physical: vampire bats have molars to pierce prey
chemical: black mamba produces paralyzing venom
behavioral: grizzly bears ambush migrating salmon
adaptations of prey for resisting predation
physical: moths resemble broken birch twigs
chemical: caterpillars feed on toxins and display warning stripes
behavioral: blue striped snappers swim in a tight group
adaptations of plants for harvesting light
trees have dominant leading shoot for rapid growth
lianas climb other trees for support to use less xylem
epiphytes grow on trunks to receive higher light intensity, shade out tree leaves
shade tolerant shrubs absorb light reaching forest floor
ecosystems that persisted for a long time
daintree rainforest in northern Australia - 180 million years
requirements for stability in ecosystems
steady supply of energy
nutrient recycling w/o leakages, resulting in nutrients leaving the ecosystem
high genetic diversity in individual species to survive environmental selection pressures
climatic variables remaining within tolerance levels
what species activity has a disproportionate effect on the structure of a community
keystone species
tipping point in ecosystem stability
level of disturbance causing ecosystem to cross ecological threshold
resulting in abrupt change
example of tipping point
amazon rainforest and deforestation as a positive feedback loop
models to investigate the effect of variables on ecosystem stability
small experimental areas set up as ecological experiments
fenced off enclosures
mesocosms
mesocosms
small container w/ transparent sides for sunlight
includes autotrophs, saprotrophs/detrivores to recycle nutrients
changes caused by humans that threaten stability
deforestation, fossil fuels, climate change, forest fires
what does sustainability of resource harvesting depend on
rate of harvesting must be lower than the rate of replacement so no depletion occurs
in ecosystems, what does sustainability rely on
nutrient availability, detoxification of waste products, energy availability
example of resource harvesting
brazil nuts in the amazon rainforest
overfishing cod in north atlantic
factors affecting sustainability of agriculture
soil erosion, leaching nutrients, supply of fertilizers + other inputs, pollution from agro chemicals, carbon footprint
bioaccumulation
concentration increase of a toxin in body tissues during an animal’s life
example of chemical in bioaccumulation
mercury, which is fat soluble
biomagnification
increase in concentration of toxin at each successive trophic level in the food chain
example of biomagnification
DDT (pesticide) in American kestral
eutrophication (nutrient enrichment) of aquatic and marine ecosystems due to leaching
nutrients from fertilizers/manure/urine contain water-soluble nitrates and phosphates
rainfall drains through soil → enters waterways → causes algae blooms that kill other plants → increase decomposition and biochemical O2 demand (BOD)
rewilding as a solution
encourages natural ecosystems to return by stopping human activities, distributing seeds of missing plants, reintroducing apex predators/keystone species, control of invasive species
what does degradation of ecosystems lead to
loss of biodiversity, rapid rates of species extinction, loss of ecosystem services
ways to rewild
carbon sequestration, climate regulation, flood protection, prevention of soil erosion, purification of air and water
what was improved at hinewai reserve in new zealand
town water supply improved, carbon sequestration, public access
what percentage and type of sun radiation is absorbed in atmosphere before reaching earth’s surface
25-30% short form radiation
what percentage of sun radiation reaches surface and is converted into heat
70-75%
what type of radiation in re-emitted
long wave radiation
what percentage of energy is absorbed by greenhouse gasses
70-85%
what temperature would the earth be w/o greenhouse effect
-18 degrees
causes of climate change
carbon dioxide, cellular respiration, combustion of fossil fuels and biomass, methane
all amplified by positive feedback loops
methane
marshes/waterlogged habitats
landfills
extraction of fossil fuels
melting permafrost
increase in absorption of solar radiation
temp rises → arctic sea ice melts → dark oceans absorb more heat →
acceleration rates of decomposition of peat + organic matter
temp rises → permafrost thaws → CO2 and methane released into atmosphere from decomposition →
release of CO2 from deep ocean
increase temperature → gasses bubble from water, solubility decreases → increased CO2 in atmosphere
increase in droughts and forest fires
forest fires → increased dryness + drought bc of increased transpiration rates → increased temp and CO2
example of tipping point
net loss in carbon accumulation in boreal forest → may transition from carbon sink to carbon source
cold temps reduce rate of cellular respiration and decomposition of detritus
photosynthesis captures CO2 in tree biomass
warmer temps/drier winters → droughts → fires
releases CO2 and reduces capacity to store carbon
polar habitat change: landfast ice
landfast ice is attached to shore w/ variability in formation
emperor penguins lose breeding ground and increased distance to food
polar habitat change: sea ice
arctic sea ice is decreasing
walrus pups are in danger of trampling
changes in ocean currents
ocean is stratified, mixing between layers occurs due to wind and current
CC increases stratification and prevents nutrient upwelling
stratified
warmer, less salty water is on top
effect of stratification
decreases ocean’s primary production and energy flow through marine food chains
upslope range shifts of temperate species
tropical montane bird species in new guinea migrate to higher elevation and increase resource competition
poleward shifts of temperate species
northward spread in north America tree species
threats to coral reefs as an example of potential ecosystem collapse
corals need carbonate ions to make calcium carbonate
hydrogen ions react w/ dissolved carbonate ions, reducing concentration → ocean pH has dropped by 30% since late 18th century
corals can’t make skeletons and existing skeletons dissolve → increased temps cause coral bleaching
CC solution
Aforrestation, forest regeneration, restoration of peat-forming wetlands as approaches to carbon sequestration