Photosynthetic fractionation of ¹³C and concentrations of dissolved CO₂ in the central equatorial Pacific during the last 255,000 years

• Main Authors: Jasper, John P, Hayes, J. M., Mix, Alan C., Prahl, Fredrick
• Format: Article in Journal/Newspaper
• Language: English; unknown
• Published: American Geophysical Union
• Subjects: Planktonic foraminifera
• Online Access: https://ir.library.oregonstate.edu/concern/articles/dn39x610d

Carbon isotopically based estimates of CO₂ levels have been generated from a record of the photosynthetic fractionation of ¹³C (≡εp) in a central equatorial Pacific sediment core that spans the last ~255 ka. Contents of ¹³C in phytoplanktonic biomass were determined by analysis of C37 alkadienones. These compounds are exclusive products of Prymnesiophyte algae which at present grow most abundantly at depths of 70-90 m in the central equatorial Pacific. A record of the isotopic composition of dissolved CO₂ was constructed from isotopic analyses of the planktonic foraminifera Neogloboquadrina dutertrei, which calcified at 70-90 m in the same region. Values of εp, derived by comparison of the organic and inorganic δ values, were transformed to yield concentrations of dissolved CO₂ (≡ce) based on a new, site-specific calibration of the relationship between εp and ce. The calibration was based on reassessment of existing εp versus ce data, which support a physiologically based model in which εp is inversely related to ce. Values of P CO₂, the partial pressure of CO₂ that would be in equilibrium with the estimated concentrations of dissolved CO₂, were calculated using Henry’s law and the temperature determined from the alkenone-unsaturation index UK′37. Uncertainties in these values arise mainly from uncertainties about the appropriateness (particularly over time) of the site-specific relationship between εp and 1/ce. These are discussed in detail and it is concluded that the observed record of εp most probably reflects significant variations in ∆p CO₂, the ocean-atmosphere disequilibrium, which appears to have ranged from ~110 μatm during interglacials. Fluxes of CO₂ to the atmosphere would thus have been significantly larger during glacial intervals. If this were characteristic of large areas of the equatorial Pacific, then greater glacial sinks for the equatorially evaded CO₂ must have existed elsewhere. Statistical analysis of air-sea p CO₂ differences and other parameters revealed significant (p<0.01) inverse ...