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Biomes/Aquatic Biology
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Salma Abouelella
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Cards (49)
Earths
climate has the most significant influences on distribution of
organisms
Four major components of climate:
temperature
, precipitation,
sunlight
and wind
Macroclimate: the climate of a
large geographic
area, such as a
continent
or region, over a long period
The two main components of macroclimate are
solar energy
and
earths movement
in space
Solar energy
: the way light strikes the earth causes different temps depending on
latitudes
Earths movement has to do with the titled
axis
that gives us different day lengths,
solar radiation
and temp
Other factosrs that influence macroclimate can be
ocean currents
and
mountains
Mircoclimate
: climate of
localized
small area, such as a valley or a pond.
Global Climate change
: large scale changes in the earths climate causes by either human activity or natural disasters
Potential outcomes of global climate change: alteration of
ocean currents
,
shrinking
range of plants, habitat losses, and shifting biomes
Biome:
major life zone
characterized by a distinct
climate
, physical envrinment and vegetation.
Climate determines
location
of
terrestrial biomes
Ecotone
:
transition
of one type of habitat/ecosystem to another
Terrestrial biomes names are determined by the dominant
plant
type and the
climate
of the region.
Terrestrial
biomes have
vertical
layering of vergitation
Aquatic Biomes
are characterized by
physical environment
There are
two
major categories:
freshwater
and marine
Freshwater: closely linked to
soil
and biotic components of surrounding environment and is influenced by patterns/speed of
water
flow
Marine
: largest marine biomes, covers
75
% of earths surface
Zonation:
Physical
and
chemical layers
Two types of zonation:
vertical
and
horizontal
Vertical Zonation
: light absorption
decreases
with depth
Five zones in vertical zonation: photic zone,
hphotic zone
,
abyssal zone
, pelagic zone, and benthic zone
Photic zone: enough
light
for
photosynthesis
, highest primary production
Hphotic:
no light
and only
consumers
Abyssal zone
: deepest part of ocean (marine) and
no light
pelagic zone: all
water
Benthic
Zone: The bottom of the ocean, where the
sediment
is the most dense.
Benthos
: communities of detrivovers
Thermoclines
: layers of
water
with significantly different temperatures
Spring turnover
: surface area heats and ice melts, water becomes warmer, oxygen is at the bottom, and nutrients to the top
Fall turnover: air temps
drops
, water becomes
cooler
, oxygen
moves
to bottom and spreads nutrient through lake
Horizontal
Zonation are different across marine and
lakes
Horizontal Zonation in marine three zones: intertidal zone,
neurotic zone
, and
oceanic zone
Intertidal
zone: periodically exposed and submerged by tides
Neritic
zone: from low tide to edge of
continental
shelf
Oceanic
zone: open
water
Horizontal zonation in lakes:
littoral
zone and
limnetic
zone
Littoral zone
: shallow, well lit waters close to shore, plants are primary producers
Limnetic zone: father from shore and too deep for rooted plants
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