Hydromechanical Model Shows that Pockmarks in the Chatham Rise-Bounty Trough May Have Released Significant Volumes of Geologic CO<sub>2</sub> During the Last Glacial Termination

Magno, Katrina

Hydromechanical Model Shows that Pockmarks in the Chatham Rise-Bounty Trough May Have Released Significant Volumes of Geologic CO₂ During the Last Glacial Termination

Katrina Magno, Stanford University, Department of Geophysics, Stanford, United States, Ludovic Räss, ETH Zurich, Zurich, Switzerland, Lowell D Stott, University of Southern California, Los Angeles, CA, United States and Jenny Suckale, Stanford University, Department of Geophysics, Stanford, CA, United States

Hydromechanical Model Shows that Pockmarks in the Chatham Rise-Bounty Trough May Have Released Significant Volumes of Geologic CO2 During the Last Glacial Termination

Hydromechanical Model Shows that Pockmarks in the Chatham Rise-Bounty Trough May Have Released Significant Volumes of Geologic CO₂ During the Last Glacial Termination