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Can the ocean run out of oxygen? - Kate Slabosky

  • 0:08 - 0:13
    For most of the year, the Gulf of Mexico
    is teeming with marine life,
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    from tiny crustaceans
    to massive baleen whales.
  • 0:18 - 0:21
    But every summer, disaster strikes.
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    Around May,
    animals begin to flee the area.
  • 0:25 - 0:30
    And soon, creatures that can’t swim
    or can’t swim fast enough
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    begin to suffocate and die off
    in massive numbers.
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    From late spring to early autumn,
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    thousands of square kilometers
    along the coast become a marine dead zone—
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    unable to support
    most forms of aquatic life.
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    This strange annual curse isn’t unique;
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    dead zones like this one
    have formed all over the world.
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    But to explore what’s creating
    these lethal conditions,
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    we first need to understand
    how a healthy marine ecosystem functions.
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    In any body of water that receives
    sufficient sunlight,
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    plant-like organisms such as algae
    and cyanobacteria thrive.
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    Clouds of algae streak the surface
    of deep waters,
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    and in shallower regions, large seaweeds
    and seagrass cover the ground.
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    Not only do these organisms form
    the foundation of local food chains,
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    their photosynthesis provides the oxygen
    necessary for aquatic animals to survive.
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    Besides sunlight and C02,
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    algae growth also depends on nutrients
    like phosphorus and nitrogen.
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    While such resources
    are typically in short supply,
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    sometimes the surrounding watershed can
    flood coastal waters with these nutrients.
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    For example, a large rainstorm
    might wash nutrient-rich sediment
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    from a forest into a lake.
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    These additional resources lead
    to a massive increase in algae growth
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    known as eutrophication.
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    But rather than providing
    more food and oxygen,
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    this surge of growth
    has deadly consequences.
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    As more algae grows on the surface,
    it blocks sunlight to the plants below.
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    These light-deprived plants
    die off and decompose
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    in a process which uses up the water’s
    already depleted oxygen supply.
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    Over time, this can reduce
    the oxygen content
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    to less than 2 milligrams
    of oxygen per liter,
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    creating an uninhabitable dead zone.
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    There are rare bodies of water
    that rely on natural eutrophication.
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    Regions like the Bay of Bengal
    are full of bottom-dwelling marine life
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    that has adapted
    to low-oxygen conditions.
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    But human activity has made eutrophication
    a regular and widespread occurrence.
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    Nutrient-rich waste from our sewage
    systems and industrial processes
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    often end up in lakes, estuaries
    and coastal waters.
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    And the Gulf of Mexico is one
    of the largest dumping zones on earth
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    for one particular pollutant: fertilizer.
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    American agriculture relies
    heavily on
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    nitrogen and phosphate-based fertilizers.
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    31 states, including America’s
    top agricultural producers,
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    are connected
    to the Mississippi River Basin,
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    and all of their runoff
    drains into the Gulf of Mexico.
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    Farmers apply most of this fertilizer
    during the spring planting season,
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    so the nutrient flood
    occurs shortly after.
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    In the Gulf,
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    decomposing algae sinks into the band
    of cold saltwater near the seafloor.
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    Since these dense lower waters don’t mix
    with the warmer freshwater above,
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    it can take four months
    for tropical storms
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    to fully circulate oxygenated water
    back into the gulf.
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    This dead zone currently costs
    U.S. seafood and tourism industries
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    as much as $82 million a year,
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    and that cost will only increase
    as the dead zone gets bigger.
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    On average the gulf dead zone
    is roughly 15,000 square kilometers,
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    but in 2019 it grew
    to over 22,000 square kilometers—
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    approximately the size of New Jersey.
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    Human activity is similarly responsible
    for growing dead zones around the world.
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    So what can be done?
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    In the short term, countries can set
    tighter regulations on industrial run-off,
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    and ban the dumping of untreated
    sewage into ocean waters.
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    On farms, we can plant buffer zones
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    composed of trees and shrubs
    to absorb runoff.
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    However, long term solutions will require
    radical changes to the way we grow food.
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    Farmers are currently incentivized
    to use techniques
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    that reduce the health of the soil
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    and rely heavily
    on nitrogen-rich fertilizers.
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    But there would be less need
    for these chemicals
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    if we restore the soil’s natural nutrients
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    by planting diverse crops that manage
    soil erosion and fertility.
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    Hopefully we can make
    these fundamental changes soon.
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    Because if we don’t,
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    the future of our marine ecosystems
    may be dead in the water.
Title:
Can the ocean run out of oxygen? - Kate Slabosky
Speaker:
Kate Slabosky
Description:

View full lesson: https://ed.ted.com/lessons/can-the-ocean-run-out-of-oxygen-kate-slabosky

For most of the year, the Gulf of Mexico is teeming with marine life, from tiny crustaceans to massive whales. But every summer, disaster strikes. Around May, animals begin to flee the area. And soon, creatures that can't swim or can't swim fast enough begin to suffocate and die off in massive numbers. What's going on? Kate Slabosky dives into the lethal conditions that create dead zones.

Lesson by Kate Slabosky, directed Mette Ilene Holmriis.

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Video Language:
English
Team:
closed TED
Project:
TED-Ed
Duration:
06:00
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