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Published byEmmeline Johnson Modified over 9 years ago
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BENTHOS Type of Substrate –Hard (Rock) –Soft (Sand or Mud) P
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BENTHOS Degree of Wave Shock –High Energy (Rock) –Low Energy (Sand or Mud) P
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BENTHOS –Intertidal Duration of Exposure –Leads to zonation –Subtidal –Deep-Sea
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15_02a Zonation in a rocky intertidal P
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15_02b S PERIWINKLES
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15_02g S BARNACLES
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15_02i S ANEMONE
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15_04 S
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15_05b S SEA URCHINS
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15_06 S ALGAE
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Zonation partly dependent on exposure, but also partly dependent on competition P
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East side of the Galveston jetties - notice light green band of algae AND dark green of a different algae S
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P
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15_08 S SAND BEACH ZONATION less obvious, but still there
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15_09a-e S CLAM BURROWING
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15_12a S Nematode Head (x804)
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15_12b S Amphipod (crustacean)
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15_12c S Polychaet (segmented worm)
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LIVING STRATEGIES Attached Free Living Burrowing P
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15_14a S Kelp (attached)
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15_18b S Sponge (attached)
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15_15a S Spiny Lobster (free living)
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15_16 S Oyster Drill (free living)
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S Polychaete (burrowing)
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SIZE Macrobenthos - large organisms (lobster) –High biomass, Low productivity Meiobenthos - medium-sized (clam) –Low biomass, High productivity Microbenthos - small-sized (round worms) –Low biomass, High productivity P
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15_15a S Macrobenthos
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Meiobenthos
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15_12a S Microbenthos
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CORAL REEFS serve as important habitats in the tropical oceans are populated by about 25% of all fish species are presently in a severe state of decline world-wide from ocean warming, sedimentation and exploitation P
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15_17 P Speciation radiates from Indo-Pacific
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15_19 S Zonation of Coral Reefs
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P Coral Polyps
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S Coral Reef Fishes
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S
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S Coral Atoll
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ENERGY TRANSPORT TO DEEP-SEA ORGANISMS Small sinking particles Overlapping ladders of migration Transport from land Large sinking particles P
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15_22 P Schematic Food Pathways
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15_Ctl S Baited Camera - 9600 meters
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15_Ctr S
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15_Ccl S
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15_Ccr S
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15_Cbl S
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15_Cbr S
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S
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15_01 P DEEP-SEA BIOMASS ONLY ABOUT 1% OF BIOMASS IN SHALLOW WATER - WHY?
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