chapter 5 aquatic biomes - sewanhaka high school · 2016-12-12 · 4 marine ecosystems • vertical...
TRANSCRIPT
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Chapter 5
AQUATIC
BIOMES
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OUTLINE
• Marine Ecosystems
Coasts
- Sandy, Rocky, Salt Marsh, Mangrove
Coral Reefs
Open Ocean
Hydrothermal Vents
• Freshwater Ecosystems
- Lakes, Rivers, Wetlands
• Human Disturbance
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MARINE ECOSYSTEMS
• Oceans cover 3/4 of Earth’s surface.
• Photosynthesis is carried out by algae or free
floating plants (phytoplankton). Greatest
amount of photosynthesis near the coast where
nutrients wash in.
• Organisms die and fall to sea floor where the
nutrients are used in deep ocean ecosystems.
• Upwelling currents circulate nutrients from the
ocean floor back to the surface.
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MARINE ECOSYSTEMS
• VERTICAL STRATIFICATION is a key feature.
Light and temperature decrease with depth and deep ocean species often grow slowly.
Cold water holds more oxygen than warm water so productivity is often high in cold oceans such as the North Atlantic.
• Ocean systems classified:
LITTORAL – near/on shore
PELAGIC - water column above the bottom
BENTHIC - bottom
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MARINE ORGANISMS• Aquatic organisms are classified based on how
they move:
PLANKTON – Float and are carried by ocean currents
- Phytoplankton – plants (algae, diatoms)
- Zooplankton – animals (eggs, larvae, jellies)
NEKTON – are able to swim (fish, whales, turtles, etc)
NEUSTON – organisms floating/moving on the surface of the water (man-of-war, water striders)
BENTHOS - live on or in the bottom –dig/crawl (clams, worms, sea stars, etc)
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ZONES OF THE OCEAN
• LITTORAL ZONE
Coastline or shore is
called the. It is
affected by tides.
• NERITIC ZONE away
from shore, where
light can penetrate
bottom (shallow)
• PELAGIC ZONE is
away from the coast
and unaffected by
tides.
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TIDAL ZONES• SUPRATIDAL – above high tide
• INTERTIDAL – between high and low tide
• SUBTIDAL – under the low tide
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SANDY BEACHES / BARRIER ISLANDS
• Narrow islands made of sand that form parallel
to a coastline
• Provide protection from storms, waves, tides
• Since they are made of sand, they should not
be built on, but they are. Oftentimes, storms
destroy the buildings.
examples:
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ROCKY SHORE• Intertidal zone where organisms have
adaptations to withstand exposure to air and
can “stick” to the rocks against wave and
current action. Exhibit vertical zonation.
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TIDE POOLS
• Depressions in a rocky shoreline that are
flooded at high tide but retain some water at
low tide
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ESTUARINE ENVIRONMENTS
• ESTUARY – A bay or semi-enclosed body of
water that forms where rivers and ocean waters
mix.
• Form BRACKISH WATER - diluted salt water
• Estuaries have high productivity and are
protected areas used by many marine organisms
as nurseries and feeding grounds.
ie: salt marsh & mangroves
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SALT MARSH
• SALT MARSHES - coastal wetlands flooded by
tidal waters
• TEMPERATE ESTUARY
• Nutrient rich & biologically diverse.
• 2/3 of marine fish and shellfish rely on estuaries
for spawning and development.
• Threatened by sewage
& agricultural pollutants
from coastal cities
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MANGROVES
• Mangroves are trees that grow in saltwater
along tropical coastlines.
• a TROPICAL ESTUARY
• Help stabilize shoreline – roots prevent erosion
• Nurseries for coral reef organisms
• Mangroves are cut for timber & aquaculture
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CORAL REEFS• Corals are aggregations of coral colonies Their
calcium rich skeletons build up the reef.
Corals have a mutualistic relationship with algae that produce food for the coral animals. Light must penetrate for algal photosynthesis. Therefore, corals live within the photic zone.
Threatened by trash, sewage, urban runoff, industrial waste, introduced pathogens and global warming.
One third of coral reefs have already been destroyed and 60% of the remaining reefs will probably be dead by 2030 ( 2006 UNESCO Conference).
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Global warming causes CORAL BLEACHING in which corals expel their algal partners and then die.
OCEAN ACIDIFICATIONReduces corals ability to create their calcium exoskeletons
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ZONES OF THE OPEN OCEAN
• EPIPELAGIC ZONE
or EUPHOTIC ZONE
or PHOTIC ZONE
• Where enough light
can penetrate – up
to 600 feet – for
photosynthesis to
take place.
• Majority of
biodiversity is here.
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ZONES OF THE OPEN OCEAN
• MESOPELAGIC ZONE
• 200 meters to 1000m
• “Twilight Zone”
• Large predators such as
sharks and squid
• BATHYPELAGIC ZONE
• 1000 to 4000m
• Many organisms create light
– BIOLUMINESCENCE
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ZONES OF THE OPEN OCEAN
• ABYSSAL ZONE
• 4000 – 6000m
• Extreme HYDROSTATIC
PRESSURE
• Many benthic organisms feed
on detritus and dead
organisms that sank to the
bottom
• HADAL ZONE
• Trenches that extend to 11,000+ meters
• Mariana Trench – deepest place on earth.
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HYDROTHERMAL VENT COMMUNITY
This community contains
tube worms, mussels,
etc. supported by
microbes that capture
chemical energy from
thermal vents on the
ocean floor. These
organisms are adapted to
extreme temperatures
(7000 F) and intense
hydrostatic pressure.
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HYDROTHERMAL VENT COMMUNITY
Bacteria (archaea)
convert chemicals such
as hydrogen sulfide and
methane into glucose in a
process called
CHEMOSYNTHESIS.
Mutualistic organisms
such as clams, mussels,
shrimp and tube worms
house the archaea.
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HYDROTHERMAL VENT COMMUNITY
The intense heat dissolves metals and other
inorganic substances from the rock. These form
chimney-like structures called “Smokers” and
metal rich sediments.
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WETLANDS• Land surface is saturated or covered with water
at least part of the year.
SWAMPS - Wetlands with trees.
MARSHES - Wetlands without trees.
BOGS & FENS - Waterlogged soils that tend to accumulate peat. Generally, nutrient poor with low productivity, but many unusual species.
- BOGS are fed by precipitation
- FENS are fed from groundwater
• Water usually shallow enough to allow full sunlight penetration, so the majority of wetlands have high productivity.
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WETLANDS
• Conservation is very important due to rich biodiversity. Wetlands are the breeding grounds for birds and aquatic species. Make up less than 5% of land area, but contain 33% of endangered species. One of the greatest areas of concern for biologists.
• May gradually convert to terrestrial communities through succession
• Trap and filter water, and store runoff.
• About half of all original wetlands in the U.S. have been degraded over the past 250 years.
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Wetlands
Bog
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FRESHWATER ECOSYSTEMS
• LAKES
Freshwater lakes have distinct VERTICAL
ZONES or VERTICAL STRATIFICATION.
- EPILIMNION - warm upper layer
- HYPOLIMNION - cold, deeper layer that
does not mix
- BENTHOS – bottom
- LIMNETIC ZONE - area in water that
light penetrates
- PROFUNDAL ZONE - area in water
below light penetration
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LAYERS OF A LAKE
THERMOCLINE - distinctive temperature
transition zone that separates upper layer and
deeper layer. Layers “overturn” when seasons
change – in summer the top is warmer, in winter
the bottom is warmer – this mixes nutrients
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PLANTS OF A LAKE
EMERGENT PLANTS – rooted on bottom but
leaves and stems extend out of water.
SUBMERGED PLANTS – plants are completely
under water
EMERGENT PLANTS – rooted on bottom with
leaves and flowers on the surface
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ANIMALS OF A LAKE
FISH – stay near center and deep in winter to
avoid freezing.
INSECTS – generally live at the surface or in
detritus. Larvae feed on plants, adults usually fly
REPTILES/AMPHIBIANS – hibernate in mud
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PRODUCTIVITY OF A LAKE
OLIGOTROPHIC lakes
are those bodies of
water that have a
poor nutrient supply
and little/no plant life
MESOTROPHIC lakes
are in between...
EUTROPHIC lakes
have a good nutrient
supply and support
high plant growth.
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HUMAN DISTURBANCE
ACID RAIN – stay near center and deep in
winter to avoid freezing.
SEWAGE, THERMAL POLLUTION
RUNOFF – of fertilizers & detergents can cause
EUTROPHICATION.
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FLOWING WATER – RIVERS / STREAMS
SOURCE – rain,
meting ice, lakes.
FLOODPLAIN –
FERTILE low lying
areas surrounding a
river
DRAINAGE BASIN –
the total land area that
drains into the river
DELTA – collection of
sediments from the
river – generally fertile
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FLOWING WATER – RIVERS / STREAMS
RIPARIAN ZONE – contains water loving plants
and animals adapted to both water and land.
ie: reeds, sedges, cottonwood, willow,
ie: musk rats, otters, turtles, amphibians
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FLOWING WATER – RIVERS / STREAMS
MAJOR RIVER SYSTEMS – Large rivers have
drainage systems that incorporate wide
continental areas.
HUMAN DISTURBANCES include dams,
irrigation, hydroelectric facilities, runoff, and
industrial dumping