Middle-late Pleistocene deep water circulation in the southwest subtropical Pacific
The modern δ13CDIC distribution in southwest subtropical Pacific deep waters is consistent with a regional mixing regime between water masses of open Pacific Ocean and Tasman Sea origin. This mixing regime is reconstructed across the middle-late Pleistoc
|Collections||ANU Research Publications|
|01_Russon_Middle-late_Pleistocene_deep_2009.pdf||757.97 kB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.