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Published byPoppy Wilkins Modified over 9 years ago
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Marine Food Chains/Webs Energy from primary production is transferred up the trophic chain Each step is inefficient (~90% energy is lost) Shorter chains are more efficient at producing apex predators
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Bottom Up Control on the Marine Food Webs Primary Secondary Production Phytoplankton h CO 2 O2O2 PlantsNUTS Food Web
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Marine Food Chains/Webs Energy from primary production is transferred up the trophic chain Each step is inefficient (~90% energy is lost) Shorter chains are more efficient at producing apex predators
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Primary Production by Biome Ryther (1969) Science
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Primary Production by Biome Ryther (1969) Science
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Marine Food Chains/Webs Open ocean = 90% area & most of the NPP but little fish production Coastal ocean = 9.9% area & 20% of the global NPP but ½ of the fish production Upwelling systems = 0.1% area & little NPP but ½ fish production
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CalCoFI Zooplankton Sampling
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Dudley Chelton [OSU] CalCoFI Zooplankton
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Seasonal Zooplankton Zoo Winds
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Seasonal Zooplankton Zoo Winds
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CalCoFI Zooplankton Highest in the tongue of CA Current
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The Upwelling Conveyor Belt Highest NUTS High NUTSLow NUTS High ChlLow ChlLower Chl High ZooLow ZooLower Zoo Sinking POM
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CalCoFI Zooplankton Corresponds to low salinity waters from north
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CalCoFI Zooplankton Highest in the tongue of CA Current
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The Upwelling Conveyor Belt Highest NUTS High NUTSLow NUTS High ChlLow ChlLower Chl High ZooLow ZooLower Zoo Sinking POM
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CalCoFI Zooplankton Hi Zoo ’ s = Low Temp ENSO connection All in pre-1977
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CalCoFI Zooplankton 70% Decline in 1970 ’ s
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The 1977 Regime Shift McGowan et al, 1998: Climate-Ocean Variability and Ecosystem Response in the Northeast Pacific, Science
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Cool vs. Warm Water Species T. Spinifera = cool water N. Simplex = warm
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Cool water species – gone during ENSO
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Zooplankton in CA Current Zooplankton follow climatic changes both ENSO and PDO are seen Long term zoo distribution consistent with upwelling conveyor & advection from N Pac Evidence of species switching is also observed
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