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Biological Productivity in the Ocean
Part I
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Overview Productivity is related to photosynthesis, which is affected by sunlight and nutrients. Productivity is globally and seasonally variable. Feeding relationships are represented by food chains and food webs. Oceans are being overfished.
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Primary Productivity Primary productivity = storage of energy in organic matter that comes from a non-organic source like the sun (not from other plants or animals) Photosynthesis uses solar radiation. Chemosynthesis uses chemical reactions. 99.9% of the ocean’s biomass relies directly or indirectly on photosynthesis for food.
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Energy to Food: Photosynthesis
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Cyanobacteria
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Cyanobacteria Diatoms
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Cyanobacteria Dinoflagellates Diatoms
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Seagrass Dinoflagellates Diatoms
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Seagrass Dinoflagellates Kelp
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Seagrass Mangroves Kelp
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Photosynthesis vs. Respiration
Photosynthesis: Creates food & releases O2, daylight only Respiration: Burns food, releases CO2, day and night
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Measurement of Primary Productivity
Directly – capture plankton in plankton nets Measure radioactive carbon in seawater Monitor ocean color with satellites Green pigment chlorophyll SeaWiFS
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Ocean Chlorophyll – SeaWiFS Satellite
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Factors Affecting Primary Productivity
Nutrient availability Nitrate, phosphorous, iron, silica Most from river runoff Productivity high along continental margins Redfield ratio – C:N:P proportions usually 106:16:1 for most phytoplankton
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Factors Affecting Primary Productivity
Solar radiation Uppermost surface seawater and shallow seafloor Compensation depth – net photosynthesis becomes zero (O2 produced = CO2 produced) Euphotic zone—from surface to about meters (330 feet)
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Light Transmission in Ocean Water
Blue wavelengths penetrate deepest Longer wavelengths (red, orange) absorbed first
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Transmission of Light in Seawater
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Color in the Ocean Color of ocean ranges from deep blue to yellow- green Factors Turbidity from runoff Photosynthetic pigments (chlorophyll) Eutrophic (high CHL) Oligotrophic (low CHL) Secchi Disk – measures water transparency
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Upwelling and Nutrient Supply
Cooler, deeper seawater is nutrient-rich. Areas of coastal upwelling are sites of high productivity.
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Types of Photosynthetic Marine Organisms
Anthophyta Seed-bearing plants Macroscopic (large) algae Microscopic (tiny) algae Photosynthetic bacteria
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Anthophyta Only in shallow coastal waters
Primarily grasses and mangroves Eelgrass
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Surfgrass
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Young Mangroves
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Young Lemon Shark in mangrove roots
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Upside-down Jelly in Mangrove roots
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Anthophyta Mangrove seed pods
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Mangrove Swamps in Florida Keys
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Macroscopic Algae “Seaweeds” Brown algae Green algae Red algae
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Macroscopic Algae Southern Sea Palm Elk Kelp
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Giant Kelp
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Giant Kelp Attach to rocks with holdfasts Unlike roots
• Do not absorb nutrients • Do not take in water • Sole function is to hold plant in place
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Giant Kelp & Urchin Predators
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Microscopic Algae Produce food for 99% of marine animals
Most are planktonic (“free-floating”) Diatoms – tests (shells) made of silica Coccolithophores – plates of calcium carbonate Dinoflagellates – tail-like flagella
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Microscopic Algae Diatoms silica-shelled organisms
dominant in colder water diatomaceous ooze
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Microscopic Algae Coccolithophores carbonate-shelled organisms
dominant in warmer waters
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Microscopic Algae Coccolithophores carbonate-shelled organisms
dominant in warmer waters
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Microscopic Algae Dinoflagellates Two whip-like flagella
for propulsion
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Microscopic Algae Dinoflagellates “Red tides” Toxic algal blooms
Phosphorescence But most not harmful Lingulodinium polyedrum
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Microscopic Algae Dinoflagellates Lingulodinium polyedrum,
San Diego County
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Microscopic Algae Dinoflagellates Zooanthellae
photosynthesize inside corals and provide nutrients: Symbiotic relationship
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Photosynthetic Bacteria
Cyanobacteria Extremely small May be responsible for half of total photosynthetic biomass in oceans Very important: bring new nitrogen into marine ecosystems
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Photosynthetic Bacteria
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