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?