HIGHLIGHTS
- who: Mark McClure from the Publisher: University of Arizona have published the Article: Simulated last glacial maximum D14Catm and the deep glacial ocean carbon reservoir, in the Journal: (JOURNAL)
- what: The authors investigate the role of both the sinking of brine and cosmogenic production alongside iron fertilization mechanisms to explain changes in 14Catm during the deglaciation. The same problem arises for the reconstruction located in the deep North Pacific: by extrapolation the authors see that the model is too old compared to this data, and this area is already too old in the modern simulation . . .
If you want to have access to all the content you need to log in!
Thanks :)
If you don't have an account, you can create one here.