2.3a Ocean Productivity

00:06:31
https://www.youtube.com/watch?v=0UOXo7jN6ps

Ringkasan

TLDRThe video explores ocean productivity, detailing how photosynthetic productivity varies by location, particularly in tropical and temperate regions. It explains the thermocline's impact on nutrient availability, leading to low productivity in the tropics despite ample sunlight. In temperate zones, seasonal changes create spikes in phytoplankton and zooplankton populations. The video also discusses energy transfer through trophic levels, highlighting the significant loss of energy at each step, and concludes with a comparison of food chains and food webs, emphasizing the complexity of oceanic feeding relationships.

Takeaways

  • 🌊 Ocean productivity varies by region.
  • ☀️ Tropics have low productivity due to nutrient depletion.
  • 🌱 Temperate regions see seasonal spikes in productivity.
  • 🔄 Energy transfer between trophic levels is inefficient.
  • 🐟 Only 10% of energy is passed to the next level.
  • 🔗 Food chains are simple, while food webs are complex.
  • 📉 Humans are at the top of the energy pyramid with minimal energy access.
  • 🌊 Nutrient-rich waters are often blocked from the surface.
  • 📈 Spring and fall are key seasons for productivity in temperate zones.
  • 🔄 Feeding relationships are intricate in marine ecosystems.

Garis waktu

  • 00:00:00 - 00:06:31

    The video discusses ocean productivity, focusing on photosynthetic productivity influenced by location. In the tropics, warm, nutrient-depleted surface water limits productivity despite ample sunlight, as nutrients are trapped below a thermocline. In temperate regions, productivity spikes in spring and fall due to nutrient buildup and sunlight availability, leading to phytoplankton and zooplankton population fluctuations. The cycle continues with winter nutrient buildup and summer balance. The video also explains energy transfer in feeding relationships, illustrating a trophic pyramid where only a fraction of energy is passed between levels, culminating in humans at the apex with minimal energy retention. Lastly, it contrasts food chains and webs, emphasizing the complexity of oceanic feeding relationships beyond simple linear paths.

Peta Pikiran

Video Tanya Jawab

  • What is ocean productivity?

    Ocean productivity refers to the rate at which photosynthetic organisms, like phytoplankton, produce organic compounds in the ocean.

  • Why is productivity low in the tropics?

    Productivity is low in the tropics due to warm, nutrient-depleted surface waters that prevent nutrient-rich waters from rising to the surface.

  • What seasonal patterns affect productivity in temperate regions?

    In temperate regions, productivity spikes in spring and fall due to nutrient buildup and sunlight availability.

  • How does energy transfer between trophic levels?

    Energy transfer between trophic levels is inefficient, with only about 10% of energy passing from one level to the next.

  • What is the difference between a food chain and a food web?

    A food chain shows a simple linear path of energy transfer, while a food web illustrates the complex interconnections between various organisms in an ecosystem.

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Teks
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Gulir Otomatis:
  • 00:00:00
    Aloha welcome to our video on ocean
  • 00:00:02
    productivity in here we'll list the
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    factors that influence a region's
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    photosynthetic productivity but also
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    will describe Oceanic feeding
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    relationships
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    okay so let's look at productivity by
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    location and when you're in productivity
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    here we're talking photosynthetic
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    productivity the first place we're gonna
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    go is here to the tropics and in the
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    tropics what we notice is we have this
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    warm nutrient depleted surface water
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    there's this thermocline that we talked
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    about this temperature gradient and then
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    we have this cool nutrient-rich water
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    below now notice we have this nutrient
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    rich water down here but it's blocked by
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    this thermal climb from getting up to
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    the surface so we don't get a lot of
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    productivity in the tropics because the
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    nutrients are already been depleted so
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    even though there's a lot of Sun and we
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    would expect to have a lot of
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    photosynthesis there's not those
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    nutrients that that phytoplankton needs
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    for photosynthesis to occur so we don't
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    see a lot of it happening there now if
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    we go up to the temperate ocean regions
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    and this is gonna be just outside of the
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    tropics and up north a little ways what
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    we notice is we have a couple spikes in
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    productivity we're gonna have one here
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    in the spring and then we'll have one
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    here in the fall the one in the spring
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    occurs because as winter comes and
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    there's less sunlight in the temperate
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    regions the nutrients are gonna be
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    allowed to build up a little bit because
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    there's less sunshine and we can see
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    there less sunshine here that's gonna
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    cause photosynthesis to go down and if
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    there's no photosynthesis going down and
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    there's no phytoplankton zooplankton
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    have nothing to eat so there's not a lot
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    of biological activity in the winter
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    time but what we do see is as charging
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    in the water at these nutrients as the
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    Sun comes back in the springtime we
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    notice a spike in phytoplankton which is
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    gonna rise up here and then we followed
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    by a spike in this so plankton will peak
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    out here and what happens is is the
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    nutrients start to deplete so that
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    causes the phytoplankton to drop down
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    the nutrients are down here and then we
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    have this zou planktonic curve that
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    catches up and that's what we see over
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    the summer time so in the spring we see
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    an awful lot of productivity in the
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    summer time everything kind of balances
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    out from that one and then in the fall
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    we see a little bit of nutrient rise
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    we're gonna see a little spike in the
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    phytoplankton it's gonna cause a little
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    bump in the soul plankton and then
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    basically the whole level would crash
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    except as the sunlight comes down to a
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    certain point that's where we see the
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    crash of photosynthesis that's gonna
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    cause the crash of those animals that
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    are feeding on those and we start seeing
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    this winter buildup of nutrients again
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    so that's how that cycle is going to
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    continue
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    now we're looking at these feeding
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    relationships one of the interesting
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    things to notice is and you should
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    remember this from biology class that
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    remember that not all the energy is able
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    to transfer from one trophic level to
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    the other remember trophic is just
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    energy levels so here we're gonna build
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    our little pyramid here and we're gonna
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    make our pyramid gonna be five layers
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    okay so we have three four and five so
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    our first trophic layers that takes the
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    energy from the Sun so here we have a
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    half a million units of energy from the
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    Sun coming through and only about 10,000
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    that units is going to be converted to
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    energy by this first one which is going
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    to be our phytoplankton so through
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    photosynthesis we're only trapping about
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    10,000 units of radiant energy so here
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    our trophic level 1 is where we're gonna
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    find our phytoplankton ok and this is
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    what's taking energy from the Sun now
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    our phytoplankton is then gonna be fed
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    on by Zoll plankton and we're going to
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    see a transfer of about a thousand units
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    and remember it's about 10 percents
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    gonna transfer over so our trophic level
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    2 is going to be made up of zooplankton
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    okay and these feed on the phytoplankton
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    from there we're going to see a hundred
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    units transfer up to level 3 and that'll
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    be our third trophic level and this is
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    just gonna be let's call it just a small
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    fish ok and that'll take us up to our
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    next trophic level where we have 10% and
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    again going through so that's only 10
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    units are going to transfer to that one
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    and here we'll have our big fish and
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    then finally we get to the apex of our
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    pyramid and here we're going to use us
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    will use humans and notice only one
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    energy so we're seeing half a million
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    units of energy receive
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    only ten thousand of it gets converted
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    into this energy pyramid through
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    phytoplankton and every step we take
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    we're gonna lose 10% of that tempura
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    snotty percent is gonna go into living
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    and reproduction and things are there
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    only ten percent gets moved on so for a
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    half a million units of energy we as
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    humans are only going to be able to get
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    about one unit so you can see how it
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    depletes as we go through
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    ok the last topic we wanted to talk
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    about our food chains and webs and again
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    this is a review from biology class but
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    notice that we're going to start off
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    with our photosynthetic organisms down
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    here and our photosynthetic organisms
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    will then be consumed by a primary
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    producer so we'll take the nice simple
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    one will use a copepod right here and
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    then our copepod is gonna be fed on by a
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    secondary consumer and that would be our
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    North Sea herring so a food chain shows
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    us a very simple path of energy by
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    consumption of what's going on so we
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    start off with our photosynthetic
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    organisms our producers and then we have
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    our consumers moving up in the ocean it
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    doesn't work that way at all in the
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    ocean these photosynthetic organisms are
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    going to be fed on by some so Plankton's
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    they're gonna be fed on by some
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    tunicates some mollusk larvae some
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    assyrians those in turn are gonna be fed
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    on by other organisms like amphipods and
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    then up to the North Sea hearing which
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    is gonna be our apex predator in this
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    example so you can see a food chain is
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    going to be a straight shot from one
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    organism to another and it's chain looks
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    like that and then when we link all of
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    these together we end up with a food web
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    that looks something like this one here
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    ok so that's it for this video as always
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    good luck on your quiz and we will see
  • 00:06:28
    you in the next video
Tags
  • ocean productivity
  • photosynthesis
  • trophic levels
  • food chains
  • food webs
  • nutrient availability
  • phytoplankton
  • zooplankton
  • energy transfer
  • marine ecosystems