Biomes/Canadian Ecosystems Flashcards
Biomes
area classified based on dominant plant species, communities and climates
usually caterogized based on abiotic and biotic elemts
Precipitationa dn temp will deine biomes
Climate Lattitude
lattitude- locations distance from equator in degrees
Variation associated with solar radition - temp and precipiation patterns
Variation in climate lattiude is associated with differences in the intensity of solar raditaion, wind patterns and associated pecitpation patterns at diff lattitudes
Variation in climate in terestrial systems can be found over altityde and is infleucned by the oceans
- Air pressure decreases with altitude, causing air to expand and become cooler
- water has high heat capcty which allows nearby systems to not heat or cool as easily
Rain Shadow Effect
Mountain ranges create this effect
Produces extremes in precipitation on eitehr side of a mountain range
Warm, humid air from oceans moves eastward toward mountains, as air rises over mountain it cools, lowering it dew point (ability to carry water) and it rains, and by the time it reaches the otehr side its lost all water and is now dry - desert
Lattitude
Variation associated withs olar radiatiion - temp and precipitation patterns
Other things associated with precipitation and temp = altitude and how far inland
Lattitudinal (north or south of equator)
toporgophic
Physical features of an area
Tundra
- Treeless land - located above the treeline
- Uplands
- Treeless mountain○ Very cold temperatures, below freezing for most of the year, with seasonal temperature variation
Very little precipitation but lots of sun
○ Dry desert like conditions with little seasonal variability in rainfall
○ Further north, direr it gets, descending side of the polar cell - air has already dropped most of its water
○ Day length - sunlight - is also seasonally variable - less in winter○ Impact on primaryproducers: permafrost - soil is frozen, short growing season, soil is nutreint poor therefore low productivty§ Active layer - the top layer of soil that thaws in the summer - where biological activty occurs □ Solifuction - thawed upper layer of soil when wet flows downslope to form terraces - damages root systems of plants and fills in animal burrows § Deep permafrost layer - slow biological acivty, impedes water flow and root development □ Polygon landform - frost pushes stones up and out to form a patteerned surface of frost hummocks, frost boilds, stripes, and polugons § Polar grassland with up to 100% plant cover and wet to moist soil Polar desert: less than 250 mm of pecipitaion, dry soil, les sthan 5% plant cover
○ Adaptions to a cold, dry, windy envirnment with limited food resources
○ Fur - thick layers like the musk ox
Reduced surface area: volume - overall body shape, appendages
○ Herbivores - consumes plants and lichen
○ Carnivorous - consume terrestrial and aquatic animals
○ Camouflage - small animals have coats that change colour during the summer and winter to better hide from predators
- Hibernation/Dormancy - reduce metabolism whne food is scarce
○ Migrate - most animals inhabit the tundra temporaily
Active Layer
The top layer of soil that thaws in the summer
Specialist
Animals that are adpated to a specific set of environmental conditions
Alpine
- Alpine tundra is a cold, windy, high elevation biome that cannot support tree growth
- Treeline - elavtion/latitude beyond which trees cant grow
- Transition zone - smaller sparsely growing trees
- Timberline - elevation/latitude below which trees form a forest with a closed canopy○ Cold, windy and dry like the artic tundra
○ Most preciptation falls as snow but the high winds redistribute it
§ Snowfileds accumulate on the lee side of mountains while ridgelines tend to be snow free
○ Local climate varies with lattude, altitude and proximity to an ocean§ Growing season 45-90 days § High winds cause soil erosion § High winds and solar radiation cause high evaporation of water Tehrefore low productivty
○ Species diveristy is relatively higher than found in artic tundra
○ Very isolated systems due to elevation
○ Highly varied microhabits due to abiotic conditions associated with topography
○ High rate of endemism (speciies found only in one place)
Alpine ecosystems cover 3.5% of global land area and host 4% of all flowering plant species○ Cold, cry, windy habitat with limted food availability or standing water
○ Similar adaptions to cold found in artic tundra animals
Aditional adpations to living in mountainous terain- split, rough hooves to climb rocky ledges
Endemnism
Species only found in one place
Boreal Forest (Taiga)
- Key definidng feature is coniferous trees
- Boreal region is arguably the largest terestrial biome on earth, coeing 14% of earths land area
- Taiga - mongolaim - land of the little sticks
- Boreal - latin - denotes the god of north wind
- Largest biome in Canada - 60% of land area and 75% of forests○ Cold temps with marked seasonal fluctations
§ Avg -20 in the winter and 18 in the summer
○ Low precipiation - most falls as rain during summer
§ 38-50cm
§ Precipatyoon is greater than evapration which allows wetlands
○ Continental climate - wide rang of temps, low humidity, low preciptation
§ Coldest winter temps may be lower than those in tundra§ Short growth season - 50-150 days with long periods of sunlight § Permafrost § Soil is nutreint poor, shallow and acidic; often waterlogged in summer § Low productivty High standing biomass
○ Comprised of relatvely young, evenly aged stands of trees due to consistent cycle of natrual disturbances
○ Fire:
§ Often caused by lighting - lots of flamable dried needles in the floor
§ Recycles nutrients back into soil
§ Adpations - resin sealed cones (jack pine) vehetaive growth (aspen)
○ Insect Outbreaks:
§ Spruce budrwom
§ Typically feed on current year growth of needles
§ Outbreaks occuring for a millenia - not sure what causes and duration is variable○ Disturbances create species diveristy over time: opens space for pioneer and other early succesional plant species and provides new habitat for consumers
○ Fire:
§ Provides dead logs as habitat and food for decomposers and their predators
§ Dead trees provide nesting sites for birds and snmall mammals
○ Insect outbreaks:
§ At least three species of warblers have distrbutions that overlap with spruce budworm outbreaks, which provide a major food source
○ Adaptions to lviing in a cold heaviliy wooded seasonal climate:
§ Fur - thick layers like in wood bison
§ Herbivores - broad diet, cosnume lichen, conifers - ex. Spruce grouse
§ Camouflage - small mammals have coats that change colour during the summer and winter to better hunt/hide from predators - ex. Ermine
§ Snowshoes - ability to move on snow - ex. Canada lynx
§ Hibernation/dormancy - reduce metabolism when food is scarce - ex. Wood frog
Migrate - some animals inhabit the higher latitudes temporarily - ex. Dark eyed junco
Oceans
The largest areas of marine waters, loosely defined by continental boundaries but are all interconnected
5 oceans: Pacific, Atlantic, Arctic, Indian and Southern
Marginal Seas
Divisions of the oceans, often bounded by islands or peninusulas
Affetced by regional climate patterns (precipitation and evaporation)
More river input, less exchange with open oceans
Neritic and Oceanic Province
Neritic - open water over continental shelves (near shore)
Oceanic - open water over deeper ocean basisn
The Deep - Physical properties
- ocean system change as you go deeper
Clines – changes over depth
Pycnocline is density and pressure – deepr in ocean, more weight pressed on you – have to be adapted to this pressure
Thermocline is temperature – deeper is colder
Salinity – changes as you go down
Oxygen highest at the top - depeleted as you go down – organisms use it for cellular respiration at too
Oxugen minimum zone – levels will climb as you go further – as you go deeper, number of organusms using oxygen there is lower
Oxygen Minimal Zone
persistent layers in the water column that have low oxygen concentration due to biological, chemical, and physical processes
Deep Sea Floor
Some animals venture between the deep sea and shallower areas
Most of sea bottom is covered with sediments, skeletones of organisms (whale fall) and debris
Pressure is great, ranging from 300-600atm on the abyssal floor and 1000atm in trenches
Little dissolved o2
Pressure in teh deep:
- Lower metabolic rates
- Lowered growth rates
- Lowered reprodutive rates
- Longer life spans
- Gigantism
- these trends because they need to conserve energy
Tidal zones
Spray/splash zone
Upper intertidal zone
Middle intertidal zone
Lower intertidal zone
Subtidal zone
Animals must adapt to ever changing conditions with both submerged and exposed (to the atompherpe) and adaptations
Surface Currents
Ocean surface currents are driven mainly by wind
Currents are created by a trasnfer of momentom from wind to water
Stable wind pattersn - like the trades or westerlies - mainatin large, slow moving oceanic currents
Westerlies
Wind from the west to the east
30 and 60 degrees in lattitude
Easterlies - Eastely trade winds
Winds at the equator
Moving east to west
Coriolis effect
Deflection of air as a result of the area around the equator moving faster than the area aroind the poles
(earth is a globe fatter at the equator and the earth spins to the right)
Things in the northern hemisphere deflect to the right
Things in the eastern hemisphere deflect to the left
ex. in the northern hemisphere, when air goes into the hurricane, air is deflected to the right which moves the hruicane counterclockwise. but in the southernhemisphere the air is being deflected to the left so hurricane moves clockwise
Surface currents
Trade winds are the stable east to west blowing winders that occcur between the 30n and 30s lattitudes
Hadley cells: high temp rises, and falls at 30 degrees in latitude
30 degrees is high pressure zone –Air then moves back to equator
Equator is low pressure zone
Air moves back to equator from high pressure
The air deflect to the right
From souther hemisphere, the air will deflect to the left
Eevrything ends up going left creating the easterlies tradewinds
At 60 dgerees more low pressure system
Air goes from high to kiw pressure so it goes to the left at north and to the right at southern creating westerlies
Boundary Currents
Created by currents being obstructed by land masses