Coral Growth in Response to Increased Atmospheric CO 2 Jim Billingsley Biology 881 University of...
-
Upload
warren-lester -
Category
Documents
-
view
213 -
download
0
Transcript of Coral Growth in Response to Increased Atmospheric CO 2 Jim Billingsley Biology 881 University of...
Coral Growth in Response to Increased Atmospheric CO2
Jim Billingsley
Biology 881
University of Nebraska, Kearney
Introduction
• Overview
• Coral Structure
• Seawater Chemistry
• Affects of CO2 on Seawater
• Conclusions
Overview
– CO2 emissions
– Physiology of marine organisms.CO2
CO32-
Overview
Photosynthesis and calcification problems
• Sealevel rise
• Faster growing algae
• Boring organisms and storm damage
Trends in Atmospheric CO2
Mauna Loa, Hawaii and Law Dome, Antarctica
(Etheridge et al, 1998); (Keeling and Whorf, 2001)
Vostok, Antarctica Ice Core Atmospheric CO2 Record
(Petit, et al, 1999)
100
200
300
400
0100000200000300000
Years before present
CO
2, p
pm
100
200
300
400
1000 1200 1400 1600 1800 2000
Year
Ice coreKeeling
Global Emission of CO2
0
50
100
150
200
250
300
1700 1750 1800 1850 1900 1950 2000 2050
Year
Gt
C
280
300
320
340
360
380
CO
2, p
pm
EmissionsCO2
(Marland, Boden and Andres 2001)
Coral Structure
• Polyps• Colony• Nematocysts
Coral Structure
• Animal• Calcium carbonate
skeleton• Symbiotic plant
Zooxanthellae
• Dinoflaggellate
• Photosynthetic
• Pigments
Seawater Chemistry
H2O + CO2 (aq) H2CO3 HCO3- + H+
Dissolution of calcium carbonate
• Temperature, pressure and partial pressure of carbon dioxide
• CaCO3 + H20 + CO2 Ca2+ + 2HCO3-
• Higher pressures and cooler temperatures
• Corrosive
CO2 Emissions and Calcification in the Oceans
• Rising atmospheric CO2
• Carbonate equilibrium • Decrease in alkalinity
• Reduces the CaCO3 saturation
• Harder for coral reefs to grow
1880
Present
Future – Double CO2
Calculated changes seawater carbonate chemistry(assuming S=35, TA=3.5 meq/L)
1
2
3
4
5
1800 1850 1900 1950 2000 2050 2100 2150
Year
War
ag
5
10
15
20
CO
2 aq
, mm
ol k
g-1
-0.011 y-1
Warag
CO2 aq
Observations at the Hawaii Ocean Times Series Station
3
4
5
1990 1992 1994 1996 1998 2000
Year
War
ag
slope = -0.022±0.08 (95% CI) y-1
Chemical treatments
nweeks
pCO2
matm
HCO3-
mmol kg-1
CO32-
mmol kg-1
pH sws
29 22529
154670
31028 8.230.04
47 37155
169676 22625 8.050.06
43 74199
195445 14918 7.810.06
Effect of CO2 on community calcification
y = 62373.77x-1.24
R2 = 0.61
0
40
80
120
0 200 400 600 800
pCO2, matm
Cal
cifi
cati
on
mm
ol C
aCO
3 m
-2 d
-1
Coral Response
(Marubini et al., 2001)
200 matm
700 matm
Porites compressa
Effect of a doubling in CO2 (350-700) on calcification, (% decrease)
Calcareous macroalgaeAmphiroa foliacea -36 Borowitzka, 1981Porolithon gardineri -16 Agegian, 1985Corallina pilulifera -44 Gao et al., 1993
CoralsStylophora pistillata -3 Gattuso et al., 1998Porites porites -16 Marubini & Thake, 1999Porites compressa -27 Marubini et al., 2001Acropora sp. -37 Schneider & Erez, 2000Porites/Montipora -50 Langdon &
Atkinson, in prep.
CoccolithophoridsEmiliania huxleyi -10 Riebesell et al.,
2000
Gephyrocapsa oceanica -29 “ “
Natural pop. (N. Pac.) -38 “ “
Emiliania huxleyi -17 Zondervan et al., 2001
Gephyrocapsa oceanica –29 “ “
CommunityBiosphere 2 -40 Langdon et al., 2000
Monaco mesocosm -21 Leclercq et al., 2000
Bahama Bank -30 Broecker & Takahashi, 1966
Future pH Changes• Burn all known stocks of fossil fuels
– Atmospheric CO2 would exceed 1,900 parts per million around the year 2300
• pH reduction at the ocean surface– Calcium carbonate skeletons
• Unabated CO2 emissions – Changes in ocean pH
Conclusions
CO2 Calcification
• for 200 to 280 matm pCO2 Calcif. 34%
• for 350 to 700 matm pCO2 Calcif. 58%
Conclusions
• Saturation state (W) controls calcification
• Consequences of reduced calcification
– Space and light
– Sealevel rise
– Erosion and damage
• Decomposition of Calcium Carbonate
Literature Cited• Barker, S., Higgins, J.A., and Elderfield, H. 2003. The future of the carbon cycle: review,calcification response,
ballast and feedback on atmospheric CO2. Philosophical Transaction of the Royal Society, 361, 1977–1999.
• Caldeira, K. and Wickett, M.E. 2003 Oceanography: anthropogenic carbon and ocean pH. Nature, 425, 365.
• Etheridge, D.M., ,Steele, L.P., R.L. Langenfelds, Francey, R.J., Barnola, J.M., and Morgan, V.I.. 1998. Historical CO2
records from the Law Dome DE08, DE08-2, and DSS ice cores. In Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.
• Gattuso, J.-P., Allemand, D., and Frankigoulle, M. 1999. Photosynthesis and Calcification at Cellular, Organismal and Community Levels in Coral Reefs: A Review on Interactions and Control by Carbonate Chemistry. American Zoological Society, 39, 160-183.
• Gerin, F. & Edmunds, B. 2001. Mechanisms of interaction between macroalgae and scleractinians on a coral reef in Jamaica. Journal of Experimental Marine Biology and Ecology, 261, 159–172.
Literature Cited
• Keeling, C.D. and Whorf, T.P. 2005. Atmospheric CO2 records from sites in the SIO air sampling network. In Trends:
A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.
• Langdon, C. 2001. Overview of experimental evidence for effects of CO2 on calcification of reef builders. Proceedings of the 9th International Coral Reef Symposium, Oct 23.27, 2000, Bali Indonesia.
• Marland, G., Boden, T.A., and Andres, R.J. 2006. Global, Regional, and National Fossil Fuel CO2 Emissions. In
Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.
• Marubini, H., Barnett, C., Langdon, M., and Atkinson, M.J. 2001. Dependence of calcification on light and carbonate ion concentration for the hermatypic coralPorites compressa. Marine Ecology Progress Series, 220, 153–162.
• Marubini, F., Ferrier-Pages, C., and Cuif, J.-P. 2003. Suppression of skeletal growth in scleractinian corals by decreasing ambient carbonate-ion concentration: a cross-family comparison. Proceedings of the Royal Society of London B, 270, 179–184.
• Petit, R., Jouzel, J., and Raynaud, D. 1999. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399, 429-436.