the effects of ocean acidification on the physiology of dominant antarctic algal species

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    The Effects of Ocean

    Acidification on the Physiologyof Dominant Antarctic Algal

    SpeciesAmelia SnowDr. Oscar Schofield and Dr. Grace Saba

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    The CO2 Problem

    Since 1800s 40% increase Preindustrial= 280 ppm Current= 385ppm 0.5% increase per year

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    Carbonate chemistry controls pH of seawater atmCO2 = CO32- andpH Decrease by 0.12 pH units and 28% increase in ocean acidity

    CO2 projected to double by 2100

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    Warming in the West AntarcticPeninsula

    Fastest warming location on Earth (winter)Increase of 6oC in past 50 years (>5x the global average)

    Increase in ocean heat content87% of laciers in retreat

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    Changes in West AntarcticPeninsula Phytoplankton

    Changes in climate=changes in phytoplanktonWarming =chl a by 12%Shift from large to small cells

    Montes-Hugo et al. 2009

    1970s-1980s

    1995-2005

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    Phytoplankton Ocean Acidification

    Tortell etal. 2008

    Few studies in Ross Sea, AntarcticaCO2= relative growth rate and primary productivity

    Low CO2-small pennate diatoms

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    Diatoms v. Cryptophytes

    http://tolweb.org

    http://www.jgi.doe.gov http://www.biol.tsukuba.ac.jp

    Fragilariopsis cylindrus Chaetoceros atlanticus Geminigera cyrophila

    15-270 mSingle-celledChain-formingCell wall made of silicaResponsible for 20% of globalphotosynthesis

    Responsible for most carbon sequestrationMost trophic carbon transfer

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    Objectives and Hypothesis

    Objectives:Compare cell growth and photosynthetic performance of threespecies of dominant Antarctic algae

    Cryptophyte-Geminigera cryophila Pennate diatom-Fragilariopsis cylindrus Chain-forming diatom-Chaetoceros atlanticus

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    Objectives and Hypothesis

    Objectives:Compare cell growth and photosynthetic performance of threespecies of dominant Antarctic algae

    Cryptophyte-Geminigera cryophila Pennate diatom-Fragilariopsis cylindrus Chain-forming diatom-Chaetoceros atlanticus

    Hypothesis:pH will decrease as CO2 increases

    Diatom abundance and photosynthetic efficiency will increase asCO2 increasesCryptophyte abundance and photosynthetic efficiency will decreaseas CO2 increases

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    SignificancePhytoplankton are

    link between lowerand higher trophiclevels in food web

    Drastic changes in

    phytoplankton resultin extreme changesin higher trophiclevels

    Ultimately couldaffect carbon cycle

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    Experimental DesignCO2 bubbling setup

    27 1L bottles 3 replicates of each species

    3 treatments180 ppm385 ppm

    750 ppmDilution 180 ppm 385 ppm 750 ppm

    Geminigera cryophila

    Fragilariopsiscylindrus

    Chaetoceros atlanticus

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    Experimental DesignMeasurements

    pH (pH probe)Cell count (coulter counter)fv/fm (FIRe)

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    Results-pH

    pH

    Geminigera cryophila Fragilariopsis cylindrus Chaetoceros atlanticus

    G h C G

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    Growth Curve-Geminigeracryophila

    Cells/mL

    Time (Days)

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    Growth Curves-Fragilariopsis cylindrus

    Cells/mL

    Time (Days)

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    Growth Curves -Chaetoceros atlanticus

    Cells/mL

    Time (Days)

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    Results-Growth Rates

    k

    180 385 750

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    Results-Photosynthetic Efficiency

    fv/fm

    180 750385

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    Conclusions Geminigerabest under ambient conditions and

    did not survive 750 ppm

    Fragilariopsis does not vary between pCO2

    Chaetoceros more successful under higher CO2 Community structure unknown future

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    Further Investigation

    1000 ppm

    Fe Limitation

    Low vs. High Light Time

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    Acknowledgements Dr. Oscar Schofield

    Dr. Grace Saba

    Emily Pirl

    Dr. Josh Kohut

    Dr. Scott Glenn Dr. John Reinfelder

    George H. Cook Honors Program

    Rutgers Coastal Ocean Observation Lab

    Institute of Marine and Coastal Sciences

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    Questions?