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Introduction: Carbon Cycle
• Carbon isotopes have been very heavily utilized to study various aspects of the earth’s carbon cycle. • Extremely diverse applications -Global, regional and local scales -Ocean, atmosphere, terrestrial environments -Current, historic, geologic time scales • Mainly CO2 cycle, but CH4 cycle also important.
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Earth’s Carbon Cycle
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Size and d13C of Earth’s Carbon Reservoirs
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d13C in the Carbonate Rock Record
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Equilibrium Fractionation effects for DIC (CO2aq, HCO3- and CO3=)
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d13C of Fossil Fuels Consumed Globally
Natural gas ~ –44 ‰ Oil ~ –27 ‰ Coal ~ –24 ‰
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d13C of Atmospheric CO2
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d13C vs CO2 Concentration in Air
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Current Atmospheric CO2 Budget
R. Feely (PMEL)
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Decadal Change in the DIC and d13C in the surface waters of the subtropical N. Pacific
C.D. Keeling et al, in GLOBAL BIOGEOCHEMICAL CYCLES, VOL. 18, GB4006, 2004.
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S d13C of plants
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Seasonal Atmospheric CO2 and d13C
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d13C of Seasonal Atmospheric CO2 Changes
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Photosynthetic Pathways for C3 and C4 Plants
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Photosynthetic Pathway for C3 Plants
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Photosynthetic Pathway for C4 Plants
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Fractionation Factors during Photosynthesis
α = Klight/Kheavy Sensitivity of αnet to pCO2int
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Two Step Photosynthesis Model in a Leaf
CO2 CO2aq CO2ext CO2int C6H12O6 Inside Leaf Air
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Sensitivity of d13C of C4 plants to pCO2int/pCO2ext
d13Cplant=d13CCO2ext – a – (b4+b3*f – a)*pCO2int/pCO2ext
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Altitude Effects on d13C of plants
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Within Tree d13C Variations
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Recycling of CO2 in the Forest
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Plant d13C Fractionation Effect (predicted by ecosystem model)
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