| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6386660 | Journal of Marine Systems | 2016 | 44 Pages |
Abstract
By July 2013, the bottom water had again turned anoxic, and DIP and DSi fluxes were even higher than earlier in the study period. These high fluxes are attributed to degradation of sedimentary pools of P and Si that had accumulated during the bottom water oxygenation in 2012. The strong correlation between DIP and DSi fluxes and the similar dynamics of DIP and DSi in the sediment pore water and near bottom water, suggest a similar redox dependency of benthic-pelagic exchange for these nutrients.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Oceanography
Authors
Nils Ekeroth, Mikhail Kononets, Jakob Walve, Sven Blomqvist, Per O.J. Hall,