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Marine Biology Study of living organisms in the ocean LIFE = ? –Ability to capture, store, and transmit energy –Ability to reproduce –Ability to adapt to their environment –NASA: A self-sustained chemical system capable of Darwinian evolution
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Evolution Explains the unity and diversity of life Charles Darwin and Alfred Wallace Definition? –Change Mechanism = natural selection –reproduction, mutation/variation, selection
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Diversity of Life
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Likely between 6- 12 million species total Likely about 1 million marine species 2000 new marine species discovered each year
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Land is more variable- leads to more species Oceans more stable Ex: temperature
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Classifying marine organisms Pelagic (in water) –Plankton (drifters) –Nekton (swimmers) Benthic (along the bottom)
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Life Cycle of a Squid
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Divisions of the Marine Environment
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Living in the Ocean: Advantage= Water everywhere makes up large % of living organisms supportive
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Living in the Ocean: Disadvantage= Hard to move Streamlining in larger organisms
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Living in the Ocean: Advantage= Hard to move Appendages to slow sinking in plankton
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Common Problem: Surface Area to Volume Ratios
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Primary Producers aka autotrophs Organisms that can capture solar energy and convert it to chemical energy by building organic compounds Photosynthesis
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Fig. 12-2, p. 238
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Primary Producers Others use chemosynthesis –Much less common –Use the oxidation of inorganic compounds as energy source, –ex: bacteria use hydrogen sulfide at hydrothermal vents
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Cellular Respiration Opposite of photosynthesis Breakdown of food All organisms
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Figure 13.1
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Consumers aka heterotrophs Must consume (eat) other organisms
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Consumers Primary consumers –Eat producers Secondary Consumers –Eat primary consumers These all are Trophic Levels
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Food webs Complex representation of who eats who
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Primary Productivity Refers to how active the producers are grams of Carbon bound into organic material per square meter per year (gC/m 2 /y)
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Figure 13.18
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Only 10% of “food” gets transferred to the next trophic level
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Figure 13.19
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Ocean’s Primary Producers Algae – in Kingdom Protista –Have chlorophyll but no vessels to conduct fluids –Unicellular = phytoplankton – pelagic –Multicellular = seaweed – benthic Plants –Angiosperms = flowering plants
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The Pelagic Zone Pelagic organisms are suspended in the water –Plankton = drifters Phytoplankton= unicellular photosynthetic algae Zooplankton = “animal” plankton –Nekton = swimmers
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Phytoplankton 95% of ocean’s primary productivity Mostly Single-celled organisms Diatoms & Dinoflagellates
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Diatoms Dominant (>5600 species) Silica shell – two valves Produce large portion of O 2 in ocean and atmosphere
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Dinoflagellates Mostly autotrophs Most are free living (except zooxanthellae) Two whip-like flagella “Red tides” or HABs (Harmful Algal Blooms)
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Phytoplankton Distribution Depends on: –light availability –nutrient concentration Varies with: –Depth, Proximity to land, Location on the earth
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Phytoplankton Distribution Compensation Depth –Where rate of photosynthesis = rate of respiration –Below this phytoplankton will die
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Phytoplankton Distribution Higher near coast –Runoff –upwelling
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Figure 13.6
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Phytoplankton Distribution Varies across the globe – How?
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Phytoplankton Distribution Tropics –Low –Nutrients trapped below thermocline
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Phytoplankton Distribution Poles –Mostly Low (except for summer peak) –Insufficient light
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Phytoplankton Distribution Temperate Regions –Highest overall –sufficient light & nutrients –Spring Peak Increasing sunlight –Fall Peak Increasing mixing of nutrients
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Zooplankton Animal plankton – many different types Heterotrophic – primary consumers Based on the phytoplankon abundance graph…how would you expect zooplankton abundance to vary?
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Figure 13.11a: Arctic Ecosystem
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Figure 13.13a: Temperate Ecosystem
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Zooplankton Major types – –Radiolarians –Foraminifers –Copepods –Krill
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Zooplankton Holoplankton –Spend their entire life in plankton Major types – –Radiolarians –Foraminifers –Copepods –Krill –Jellyfish (cnidarians) and comb jellies (ctenophores)
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Figure 14.3: Radiolarians Single- celled; Hard shell made of silica
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Figure 14.4: Foraminifers Single-celled; shell made from calcium carbonate
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Copepods Small crustaceans (<1 mm) Very abundant
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Figure 14.5: Copepod diversity
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Fig. 13-9, p. 265 Krill – Important in Antarctic Ecosystem
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Fig. 13-10c, p. 266
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Zooplankton Meroplankton –Only found in plankton for part of their life cycle –Larvae of benthic adults & fish
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Meroplankton
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