Evidence for substantial accumulation rate variability in Antarctica during the Holocene, through synchronization of CO2 in the Taylor Dome, Dome C and DML ice cores

• Main Authors: Monnin, Eric, Steig, Eric J., Siegenthaler, Urs, Kawamura, Kenji, Schwander, Jakob, Stauffer, Bernhard, Stocker, Thomas F., Morse, David L., Barnola, Jean-Marc, Bellier, Blandine, Raynaud, Dominique, Fischer, Hubertus
• Format: Text
• Language: unknown
• Published: Elsevier 2004
• Subjects: 530 Physics; Dronning Maud Land; Taylor Dome; Antarc*; Antarctica; DML; ice core
• Online Access: https://dx.doi.org/10.48350/158542; https://boris.unibe.ch/158542/

High resolution records of atmospheric CO2 concentration during the Holocene are obtained from the Dome Concordia and Dronning Maud Land (Antarctica) ice cores. These records confirm that the CO2 concentration varied between 260 and 280 ppmv in the Holocene as measured in the Taylor Dome ice core. H...