shallow roots, big leaves, lots of rain
pitcher plants-eat animals
epiphytes-grow on other plants (e.g. orchids)
air roots
specialized animals
tropical dry forest——
deciduous forest: warm, but variable rain (e.g. monsoon)
autumn leaves-loss to protect plant, changes in photosynthesis
waxy leaves (e.g. pine needles) if over winter plants
estivation: hibernation
migration: birds (why birds and not other animals?)
savanna——
very dry, few trees, seasonal grasses, fires
porous soils (like Kona), often coffee locations (s. america)
waxy leaves, deep roots
desert——
under 25 cm (250 mm) of water per year (10 inches)
dry dry dry, so dramatic temp variations (opposite of ocean biomes)
few plants, low nutrient levels in soil
nocturnal animals (e.g. rats, snakes)
succulents: store water (e.g. cacti)
large, shallow roots, also taproots (160 ft. deep)
temperate rain forest——
not too warm, not too cold, just right
rainy, warm, mossy, foresty (e.g. washington, oregon, BC)
coniferous-have pine cones, conifers: oily needles (don’t freeze)
lumber
temperate forest——
eastern US: oak etc. seasonal loss of leaves
hibernating animals
temperate (mild) grassland——
prairie, steppe (russia)
moderate rain, but not enough for trees. grass only.
grass grows from below, so can be eaten by cattle and still live
roots capture moisture, hold soil together (kikuyu grass)
chaparral——
California, mediterranean (middle of the earth, contrast with chinese translation of the word “china”: middle earth kingdom)
dry, seasonal rain, drought (like now)
Boreal (north) forest———
taiga
acidic soils (from conifers/pine needles as competition)
very cold
conifer shape sheds snow, preserves branches (christmas trees)
when ground freezes, no water for roots, all water stored as sap in trees (oily compound, very sticky, makes retsina in Greece)
tundra——
russia, alaska, canada
very cold-study the climatograph (-220 °C!) right….
permafrost-permanently frozen ground, so only shallow roots
polar ice—
not really a biome, but stuff lives there (aquatic mammals, fish, very small rocks, churches, mud, but no ducks)
Notothenioids-antifreeze fish
blubbery mammals
mountains—
another non-biome, but look at this!
how cool is that?
aquatic ecosystems—
salinity, depth, standing or flowing water
salt water = 30-50 ppt (parts per thousand)
ppt, ppm, ppb
fresh water = 0.5 ppt
in between 0.5-30 ppt = brackish (anchialine ponds in Kona)
study the fishies in the pictures
DEPTH!!!!
determines amount of light, tf. photosynthesis
photic zone=light
aphotic=no light
benthic=really no light, never, ever ever. don’t even think about it.
aquatic mammals must surface for air
fishies don’t-gills
DO dissolved oxygen (very important) depends on plants (so depth) and temp (cooler water can hold more O2)
warm water has low O2 generally.
best place to fish: cool water after a waterfall (why?)
flowing water: rivers
standing water: ponds
lakes can become inland seas
littoral=shore, limentic=away from shore benthic=botttom
wetlands:
marshes, swamps, bogs and fens
marshes marshes marshes!-tall grasses
swamps-some trees
bogs-acidic, poor decomposition, floating stuff
fens-spring underneath, less acidic, better nutrients
bogs decay slowly-ancient cheese story, peat moss
rivers-oxbow lake and meander
source, tributary (continuity concept), mouth (delta)
slope exponential as distance from source
deposition rates (rapids vs. plains)
silt carrying capacity, turbidity
estuaries-like deltas
tidal estuary: hudson river: deeper than the body it serves
oceans——
200 ft. of salt if all oceans evaporated
oceans were red (iron) then ppt out (iron range in WI, MI)
salinity, wind and temperature determine flow
upwelling (recall Peruvian fisherpersons)
also downwelling
photic zones-
intertidal zone-makes sense, between tides
neritic zone-close to shore, less than 200 ft. deep (not in Hawaii, we have no continental shelf-boo hoo)
open ocean (pelagic) zone
kelp forests-e.g. california coast
coral reefs-away from fresh water, coastal, photic
open ocean-scary stuff
Comments