Abstract: Core top confirmation of the carbonate ion effect in multiple species of planktic foraminifera and a reassessment of the upper water column equatorial Pacific δ<sup>13</sup>C<sub>FORAM </sub>records. (2017 AGU Fall Meeting)

Core top confirmation of the carbonate ion effect in multiple species of planktic foraminifera and a reassessment of the upper water column equatorial Pacific δ¹³C_FORAMrecords.

Jennifer S Fehrenbacher, Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States and Howard J Spero, University California Davis, Davis, CA, United States

Back to: Climate, Carbon Cycle, and Biogeochemical Reconstructions from the Eastern Tropical Pacific I

Core top confirmation of the carbonate ion effect in multiple species of planktic foraminifera and a reassessment of the upper water column equatorial Pacific δ13CFORAM records.

Core top confirmation of the carbonate ion effect in multiple species of planktic foraminifera and a reassessment of the upper water column equatorial Pacific δ¹³C_FORAMrecords.