linking global climate change to oceanic ecosystem functioning ocean...
TRANSCRIPT
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Linking Global Climate Change to Oceanic Ecosystem Functioning
Ocean Acidification
Uta Passow
Marine Science Institute UC Santa Barbara
Understanding Ocean Acidification: WorkshopChannel Islands National Marine Sanctuary, 10/2010
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The Problem:Fossil Fuel EmissionResulting Increase in CO2
Discussion:What if peopled do not believe this?The basics: plants and animals and oil
www.globalwarmingart.com
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http://carboncycle.aos.wisc.edu/index.php?page=global-carbon-cycle
Global C-Cycle
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Fate of Anthropogenic CO2 Emissions (2000-2008)
Le Quéré et al. 2009, Nature Geoscience; Canadell et al. 2007, PNAS, updated
1.4 PgC y-1
+7.7 PgC y-1
3.0 PgC y-1
29%
4.1 PgC y-1
45%
26%2.3 PgC y-1
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What can we do?• Reduce your CO2 foot print
• Reduce gasoline / energy usage• Use CO2 neutral energy• plant trees
• Lobby for Reduction of CO2 foot print• Public transportation• Development of “alternative technology”
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2000 2050
390
Measurements from ice coresdirect Measurements
2010: 387 ppmV
Atmospheric CO2 concentration
Redrawn after www.globalwarmingart.com
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We can already measure the anthropogenic CO2 in the ocean in the upper 1000 m.
Feely 2004
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Ocean acidification
Doney, Scientific American 2006
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Dissolved Inorganic Carbon in Seawater
DIC = CO2 +HCO3- + CO3
2-
pHAs pH decreases• DIC increases• Composition of DIC shifts (Impact cells as it matters what type of ion they have available)
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As atm. CO2 increases•DIC in seawater increases• pH decreases• Saturation state for calcium carbonate decreases
Feely, Doney, Oceanography 22, 2009
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A shift of 1 pH unit e.g. 8.2 to 7.2 is a factor of 10 difference in H+ Ions
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How does the ocean work – in 3 slides!&
Biological Impacts of Ocean Acidification – Lots of Examples!
Not much question that ocean acidification is happening!The question is how the marine ecosystems react to this.
• Stress• Acclimatization• Adaptation
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Phytoplankton
Diatoms:
Coccolithophores
Dinoflagellates
Phaeocystis
Cyanobacteria
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http://rohlenscience.pbworks.com/Energy%20Notes
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How does the ocean work?
Burd & Passow, unpubl.
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Eelgrass
Primary production increases
Photosynthesis increases!
Not for all organisms!
MEPS 2007
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Phytoplankton
Species composition shifts!
Feng et al MEPS 2009
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Calcification
Calcite Aragonite Mg-CalciteCoccolithophorids Pteropods Coraline AlgaeForaminifera Corals cold water Coralssome Bivalves most MollusksSpongesEcinoderms
SHELLED ORGANISMS and crystal structure of CaCO3
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Aragonite saturationHorizon
MODERNPAST
Calcite Saturation Horizon
SaturationHorizonsare shallowing
Oceanography 22, 2009
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Waters that are naturally acidic
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Coccolithophorids
Calcification decreasesAt least in many organisms
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Phytoplankton
Coccolithophores
CaCO3-plates
May use organic nitrogen or phosphorus.
Blooms visible from space
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N-Fixation
Nitrogen fixation: Biological process by which nitrogen (N2) is converted into ammonia. This process is essential for life (amino acids, proteins) contain N.
Some bacteria, especially cyano-bacteria can fix nitrogen. Some plants have a symbionticrelationship with such bacteria (lupines, peanuts).
Cyanobacteria common in surface ocean.
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Hutchins, Oceanography 22, 2009
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N-fixation by Trichodesmium sp.
Oceanography 22, 2009
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N-Fixation:Percent increase in N-fixation of 7 different strains of Trichodesmiumspp. under at future (750 ppmV) vs. current CO2 levels.Calculted increase in global N-fixation, minimum (red) or maximum (blue). Green atm. pCO2
Oceanography 22, 2009
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Oyster
Lifecycle
Calcification/ Reproduction
3 weeks planktonic
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Precipitation of oyster shell after settlement (benthic)
970 ppmVVs 380
Shell precipitated
16% less
Size @ settelment
7% less
Size after 4-5 days
42% less
Exp 1
After Hettinger ASLO 2010
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Larvae 380 970 380 970juvenile 380 970 970 380
Hypothesis
ResultsCarry -over
H L H L * (35%)
* Even if then put in normal environment 40 days later still 28% smaller: larvae effect persists After Hettinger ASLO 2010
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Calcification, Reproduction: decrease with higher CO2, Photosynthesis, N fixation increase, or remain constant Oceanography 22, 2009
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DIC-drawdown (ΔDIC)
pH decrease
Net community carbon consumption(photosynthesis, C:N, TEP)
Loss of OC = ΔDIC-(Δ POC+ Δ DOC)
Past Future
OA will lead to an increase in sedimentation
Budget in the “black box”
Carbon flux: CO2 perturbation in mesocosms
The Future Riebesell, Nature 2007
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http://oceanservice.noaa.gov/education/kits/corals/coral01_intro.htmlhttp://animals.nationalgeographic.com/animals/invertebrates/coral.html
Coral polyps are tiny, soft-bodied organisms related to sea anemones and jellyfish. At their base is a hard, protective limestone skeleton called a calicle, which forms the structure of coral reefs. Reefs begin when a polyp attaches itself to a rock on the sea floor, then divides, or buds, into thousands of clones. The polyp calicles connect to one another, creating a colony that acts as a single organism. As colonies grow over hundreds and thousands of years, they join with other colonies and become reefs. Some of the coral reefs on the planet today began growing over 50 million years ago.
Corals
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Almost all corals are colonial organisms. This means that they are composed of hundreds to hundreds of thousands of individual animals, called polyps. Each polyp has a stomach that opens at only one end. This opening, called the mouth, is surrounded by a circle of tentacles.
Corals
Corals live in tropical waters throughout the world, generally close to the surface where the sun's rays can reach the algae.
While corals get most of their nutrients from the byproducts of the algae's photosynthesis, they also have barbed, venomous tentacles they can stick out, usually at night, to grab zooplankton and even small fish.
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Most reef-building corals contain photosynthetic algae, called zooxanthellae, that live in their tissues.
The corals and algae have a mutualisticrelationship. The coral provides
a protected environment compounds for photosynthesis
The algae produceoxygenhelp to remove wastesglucose, glycerol, amino acids,
The relationship between the algae and coral polyp facilitates a tight recycling of nutrients in nutrient-poor tropical waters.
Corals
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Zooxanthellae cells provide corals with pigmentation. On the left is a healthy stony coral. On the right is a stony coral that has lost its zooxanthellae cells and bleached.
http://www.osdpd.noaa.gov/ml/ocean/cb/hotspots.htmlMap with hot spots
Zooxanthellae are responsible for the unique and beautiful colors of many stony corals.
Corals: Bleaching, a temperature effect
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Corals
Cohen, Oceanography 22, 2009
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Cohen
Ambient 780-1200 ppmV pCO2
3 x NO3
7 x NO3
Enough food can compensate stress by high CO2, as proton pumping costs energyInternal pH is different from external (Ω internal: 3.7 if external 0.2
or internal 3 if external 20)
% ambient calcification
80%
25%
Interaction of several processes
Corals
Oceanography 22, 2009
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Kleypas, Oceanography 22, 2009
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Coral reef: many calcifying organisms
Oceanography 22, 2009
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Corals
Kleypas, Oceanography 22, 2009
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Oceanography 22, 2009
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No skeleton, polyps healthy. Survived Permian extinction?
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Oceanography 22, 2009
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Fossil fuel
Ocean uptake
http://carboncycle.aos.wisc.edu/index.php?page=carbon-budget-tool
Land use
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Ocean acidification at the organism level tends to lead to• increase in photosynthesis – but temperature effects
change this• increase in N-fixation – but iron availability important• decrease in calcification – some species survive without shell• decreased reproduction: benthic calcifiers (larvae vulnerable)
Variability is highgenetic variationmany interdependent processes
Biological Reactions to OA
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pCO2
today
370
Year 2100
~750 µatm
irradiance
pH ~8.1 ~7.8
mixing
• Growth conditions- [CO2]aq / pH / Ω …
- light regimes
- nutrient availability
nutrientinput
Temperature & Stratification
- Temperature increase
Overall photosynthesis decrease observed. That could be a real problem as phytoplankton make up almost 50% of global photosynthesis.
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Questions?
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THANK YOU!