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Published byWade Hampton Modified over 9 years ago
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What are larvae? How biology affects larval transport How physics affect larval transport Upwelling and larval transport in the California Current
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Holoplankton: Plankton that are free-swimming for their entire life cycle.
Goals: Eat, avoid being eaten, reproduce Meroplankton: A planktonic life stage (“larvae”) of organisms that are strong swimmers or live on the bottom as adults. Microscopic, ~0.1 to ~5 mm Goals: Develop, avoid being eaten, find habitat
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Example of life cycle for species with larvae
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Most larvae bear little resemblance to adults
Sea star Phoronid worm Octopus Snail
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Most seafood species have larvae
Mussel Crab Lobster Tuna Dinner Adults Larvae
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Most fouling organisms have larvae
Barnacle life cycle Feeding Non-feeding (Oceanographers are always looking for better ways to keep barnacle larvae from settling on their boats and instruments!)
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What makes larval ecology so important
What makes larval ecology so important? ~70% of benthic invertebrates have planktonic larvae Population dynamics Ecologically important (population limited by supply) Edible species (valuable +$) Fouling organisms and invasive species (costly -$) Biogeography -- geographic distributions range expansions Conservation -- Identify “source” and “sink” populations design of marine reserves
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Larval Transport: Horizontal movement of larvae from one point to another
Larval Dispersal: Spread of larvae from spawning sites to wherever they die or settle Settlement: When a larva metamorphoses and adopts a benthic lifestyle Recruitment: Defined by when we first observe the “new recruit” in the population
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What influences larval transport?
Biological Processes Development Mode Pelagic Larval Duration Response to Environment Larval Behavior Physical Processes Currents, turbulence Upwelling
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Two potential development modes
Planktotrophic larvae Feed on other plankton, usually phytoplankton Female produces many small embryos with a long pelagic larval duration (PLD). Lecithotrophic larvae Do not feed on other plankton. Instead they consume yolk that is added to the embryo. Female produces fewer, larger embryos with shorter PLD.
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Sea slug (Alderia willowi) switches seasonally from plantotrophic to lecithotrophic larvae
Planktotrophic eggs Adult Lecithotrophic eggs P. J. Krug
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Feeding larvae tend to be in the plankton longer and disperse farther than non-feeding larvae
This is about half the earth’s diameter! This is about half a mile! Shanks et al. 2003
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An extreme example -- this Pacific snail can remain in the larval stage for 4.5 years!
If average current speed is 20 cm/s, this thing can travel 28,000 km, or 2/3 the distance around Earth, before settling! Strathmann and Strathmann 2007
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Comparable odds ratios
1 in 176,000,000 1 in 3,000,000 1 in 20,000 1 in 10 Comparable odds ratios Average number of eggs produced per female per season Brooders Lecitho- trophic Plankto- trophic Thorson 1950
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Development rate depends on temperature
25.2 oC 17.5 oC Scheltema 1967
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For feeding larvae, development rate also depends on temperature & food availability
10 days 20 days Barnacle development rate Development is fraction of progress towards becoming a cyprid Pfeiffer-Hoyt & McManus 2005
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Behavior affects distance and direction of transport
SINK SWIM SWIM SINK
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Particle Reynolds Number
Inertia: an object in motion tends to stay in motion (tendency for gliding) Viscosity: “stickiness” of a fluid, like friction (inhibits gliding) Reynolds number: ratio of inertial forces to viscous forces
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Particle Reynolds Number Rep
If Rep>1, Inertia dominates. If Rep<1, viscosity dominates. Plankton with Rep1 feel like they’re swimming in molasses.
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Swimming velocity scales with body size
Most Invertebrate Larvae u 1 mm/s to 1 cm/s Fish Larvae u 1 to 20 cm/s From Huntley & Zhou 2004
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Reynolds number scales with body size
Most larvae are <0.1 cm long and have Rep<1. Some exceptions include large crustacean larvae, fish larvae At Rep<1, Net velocity = flow + behavior Inertia Viscosity Mann & Lazier, after Okubo 1987
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Horizontal advection x = (Ucurrent + Uswim) t [distance] = [distance/time] x [time] Ucurrent 1 to 100 cm/s Uswim 0.01 to 1 cm/s **Currents dominate horizontal advection Vertical advection z = (Wcurrent + Wswim/sink) t [distance] = [distance/time] x [time] Typical Wcurrent 1 to 10 cm/s, but average = 0 Typical Wswim/sink 0.01 to 1 cm/s **Behavior dominates vertical advection Diffusion (Random motion due to turbulent mixing)
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Larval Transport: Focus in on California Current, Oregon upwelling zone
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Upwelling in California Current has big effect on dispersal of rocky shore species
Mussels and barnacles form patches in intertidal zones and stay attached to rock after settlement.
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Note the direction arrows
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WA OR Point Conception CA Halpin et al. 2004
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Primary production in California Current is strongly dependent on upwelling
Temperature Chlorophyll MBARI data from August (peak upwelling season)
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Separation of coastal jet can be seen in Chl A map
WA OR S. Calif. Point Conception CA San Diego
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2. Central California Coast
1 2 1. Oregon Coast 2. Central California Coast -Weak, intermittent upwelling -Strong, steady upwelling -High invertebrate recruitment -Low invertebrate recruitment
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Barnacle Mussel California Oregon California Oregon 2 years of
recruitment data California Oregon California Oregon Connolly et al. 2001
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Central California example - barnacle data
Counted barnacle larvae # to 1984 #63, to 1984 Roughgarden et al. 1988
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Upwelling transports larvae offshore
Roughgarden et al. 1988
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Central California example - barnacle recruitment peaks during relaxation events
Farrell et al. 1991
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Oregon region: -Seasonal upwelling, weak/intermittent in summer -coastal jet remains near coast -upwelling increases production -upwelling doesn’t prevent larvae from getting to shore -upwelling positively affects recruitment of feeding larvae California region: -continuous upwelling, strong in summer -upwelling pushes coastal jet and larvae offshore -nearshore production may be lower -relaxation events are important for recruitment
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