bio 111 marine and coastal ecosystems week7

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  • 8/2/2019 Bio 111 Marine and Coastal Ecosystems Week7

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    Marine and Coastal Ecosystems

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    Ocean covers most of the earth's surface

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    amount of O2 in the

    water is strongly affected

    by photosynthesis andcell respiration

    most of the O2 produced

    by photosynthesis in the

    ocean is released to the

    atmosphere

    50% of the world's

    oxygen comes from

    phytoplankton and algae!

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    Water flows in complex currents atdifferent levels of depth

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    the ocean neverrests

    currents move andmix ocean waters

    currents transportheat, nutrients,

    pollutants, andorganisms

    ocean circulationalso affects theearth's climate andtherefore, allhabitats on land

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    Deep water circulation

    the ocean is a three

    dimensional habitat major current maps

    only show circulationat the surface - not

    greater depths surface water is

    partially isolated fromdeeper waters bydifferences in density

    because the densestwater sinks, theocean is stratified(layered)

    warm water floats ina shallow "lens" ontop of cooler water

    sudden changes in

    temperature oversmall depth intervalscalled thermoclines

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    The Great Ocean Conveyor

    after water masses leave

    the surface they sink toa depth determined bydensity

    to sink all the way to the

    bottom of the ocean,surface water mustbecome very dense (coldand salty)

    main places wheresurface waters reach thebottom are in the

    Atlantic Oceans

    after sinking, water

    spreads through theAtlantic to other oceanbasins

    eventually rises to the

    surface again and flowsback to the Atlantic

    this circulation is part ofa global pattern knownas the Great OceanConveyor - mixes theearth's oceans on a

    4,000 year cycle

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    Great Ocean Conveyor

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    Effects of the Great Ocean Conveyor

    small variations in the conveyor circulation canproduce dramatic changes in weather patternsaround the world

    larger changes may even bring on ice ages

    note: keep this in mind for our unit on globalwarming

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    Why are there tides?

    main cause of tides isthe gravity of the moonand sun acting on theocean

    the tidal bulges are

    largest, and thereforethe tidal range isgreatest, when themoon and sun are in

    line and acting together this happens at the

    new and full moons

    when the moon andsun at pulling at rightangles the bulges andtidal range are smallest

    this occurs when the

    moon is in quarter

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    some oceanzones support

    more life thanothers

    the upper,sunlit layers

    are mostproductive

    called thephotic zone

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    Vertical movement of water affectsmarine ecosystems

    nutrients are neededto supportproductivity in thephotic zone

    nutrient rich watersare carried to thesurface nearcontinental margins

    process is calledupwelling

    upwelling zones occurwhere winds blow thesurface water awayfrom the borders ofthe continents

    deeper, nutrient richwater rises to fill inthe gaps

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    Upwelling

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    The world's most productivefisheries are in upwelling zones

    shrimp boats Mississippi

    coast

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    Examples of marine

    ecosystems with highproductivity and biodiversity

    Satellite image of chlorophyll concentration

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    Satellite image of chlorophyll concentration(indicates areas of high productivity)

    high shown ingreen,orange, red

    note: highestphytoplankton

    concentrationin areas ofhighernutrientavailability

    (along coastsand inupwellingzones)

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    Coral reefs

    coral reefs are the

    external skeletonsof tiny marineanimals called

    coral polyps the intricate reef

    structure supportsenormous

    biodiversity

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    Coral structure

    coral polyps

    live brain coral

    brain coral skeleton ofcalcium carbonate

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    microscopiczooxanthellae (algaeliving within the coraltissues) help coralsbuild reefs byproviding extraenergy fromphotosynthesis

    although corals getmost of theirnutrition from thezooxanthellae, theyare also predators

    catch small animalswith their tentacles,in a similar way to

    jellyfish (close

    relatives)

    note: keep the zooxanthellae inmind for our discussion of coralbleaching

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    looking up from below you can see thefishes school above the reef - I included itbecause it's a pretty cool photo and a goodexample of reef productivity

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    Great Barrier Reef 1600 miles long!

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    Estuaries: where rivers meet the sea

    salinity variesdramaticallyfrom place toplace

    most have asandy or softmud bottom

    nutrientscarrieddownriver fromthe land

    Chesapeake Bay aerial view

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    Estuaries are tremendously productiveand home to large numbers of organisms

    wild riceplants in thePatuxent River(tributary to theChesapeakeBay)

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    Salt Marshes

    salt marshes are

    grassy areas thatborder estuaries andextend inland fromthe mudflats

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    Marsh ecosystems

    salt marshes are

    subject to extremechanges in salinity,tides, and temperature

    communities aredominated by a fewhardy grasses andother salt tolerant

    plants

    very high primaryproduction

    marsh plants trap

    and use nutrientswashing off the land(and help preventnutrient pollution)

    contributes to theproductivity of thebordering estuaries

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    Zonation of salt marsh plants

    M f t

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    Mangrove forests mangroves are

    denseforests of

    trees adapted tolive in theintertidal zone

    as with salt marsh

    plants, mangroveshave differenttolerance to saltwater immersionat high tide

    different speciesof mangroves livein zones based onthe level of tidal

    flooding

    mangrove forestsPuerto Ricoaerial view

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    seaweeds, sponges,oysters, and lots ofother types of

    organisms liveattached to the rootsof the red mangrove

    view above water

    view underwater

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    75% of all shelteredtropical shores wereonce fringed with

    mangroves provided protection

    from flooding ofcoastalcommunities,nurseries for fishes,nutrient traps, etc.

    human activitieshave destroyedmuch of theseforests around the

    world

    sprouting mangrovesFlorida Keys

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    Pollution threatens marine resources

    nets and plastic debrisendanger wildlife

    oil pollutionaccumulates from

    hundreds of spills peryear

    toxic pollution enteraquatic ecosystems

    example: mercuryreleased by burningcoal for electricity

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    Pollution threatens marine resources

    excess nutrients

    cause algal blooms nutrients released

    from over-fertilization ofagricultural andresidential lands,food processingwaste, sewage

    treatment, cattleand chicken feedlots etc.

    i i bl

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    marine species are renewable resources,but they can be overexploited

    piles of oyster shells

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    over 70% of allmarine commercial

    fisheries are fullyexploited ordepleted

    modern,

    industrialized fishingoverexploits notonly the targetspecies, but other

    species that are notwanted (bycatch)

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    Aquaculture

    raising marine animalssimilar to farm animals

    applies to both freshwater and marine

    species if use non-polluting

    and sustainablemethods, can take

    pressure offoverexploited marinespecies

    overexploitation - notice thesmaller size of the fish in thetuna market