Oceanography: Primary Production – Flashcards
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Respiration
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This process produced Carbon Dioxide
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what sinks to the ocean floor
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The difference between Photosynthesis and Respiration is what?
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Plankton
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Small organisms that drift with the ocean currents
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Phytoplankton
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Small cells (often single cells, but sometimes chains or colonies of many cells) that contain chlorophyll and drift with ocean currents
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Photosynthesis
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uses water and carbon dioxide (gas) and the energy of sun light to form glucose and oxygen.
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sunlight and essential plant nutrients
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the magnitude of primary production depends on these two things
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Net Primary Production (NPP)
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the difference between the amount of CO2 consumed by photosynthesis and the amount of CO2 produced by respiration.
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Net Primary Production (NPP)
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the Net Gain or Net Loss of carbon within the cell
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Diatoms
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Phytoplankton that require Silica
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Flagellates
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Phytoplankton that are motile so they are able to avoid sinking in calm waters
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Photosythetic Bacteria
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Phytoplankton that is able to grow at very low nutrient concentrations
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light limited
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At low light levels, phytoplankton are
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light saturated
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At optimal light levels, phytoplankton are
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photoinhibted
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At very high light levels, phytoplankton are
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compensation depth
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The depth at which the ambient light intensity is equal to the compensation light intensity is called the
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phytoplankton cells do not have sufficient light to photosynthesize fast enough to meet their basal metabolic needs and so cell respiration exceeds photosynthesis and this then leads to negative values of net primary production
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What happens below the compensation light level?
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Oxygen
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Primary Production makes...
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Primary Production
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Consumes Carbon Dioxide Gas and forms particulate organic carbon that can sink into the deep ocean
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Nutrient transportation is related to surface area and smaller cells have a larger surface area to volume ratio than larger cells
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Why can smaller cells grow better at lower nutrient concentrations?
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Nitrogen Phosphorous Silica (for diatoms) Iron
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The 4 Phytoplankton Nutrients of Interest to Oceanographers
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mixing across the thermocline/pcynocline
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The the main mechanism for getting deep nutrients into the surface (sunlit) layer of the ocean is
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thermocline
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acts to hold phytoplankton near the sunlit surface ocean
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thermocline
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a significant barrier to upward mixing of nutrient rich deep water. The stronger the thermal stratification the strong the inhibition of nutrient mixing
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It is the number one Iron Limited Region
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The Southern Ocean is important because
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Subtropical Gyre Regions Equatorial Pacific and Atlantic Regions Coastal Regions
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Three Spatial Patterns Due to Physical Biological Interactions
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Low Primary Production (on a per meter square basis) and Very Little Seasonal Variation
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Subtropical Gyres exhibit....and.....
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Tidal mixings
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brings nutrients to the surface year-round.
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Coastal Upwelling
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seasonally superimposes additional nutrients
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cells spend an increasing proportion of the day below the compensation depth in the dark
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The average light level that phytoplankton experience over the course of a day becomes dimmer as mixing depth increases because...
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they have spent too much of the day below the compensation depth losing carbon
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When cells mix below to the Critical Depth
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1. Deep Winter Mixing. 2. Strong Springtime Stratification
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Large Seasonal Increase in Primary Production Occurs in the North Atlantic Due To:
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46%
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What percent of Ocean NPP is Global NPP
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50 Gt of Carbon per year
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How much Carbon does the ocean produce per year?
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71% because of the vast area that these take up. This is surprising because they have relatively low intensities of Primary Production
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The Open Ocean (Trade Winds, Westerly Wind and Polar regions) contributes how much of the total NPP of the ocean and why? why is this surprising?
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