Abstract
Biological activity gives rise to a difference in carbon concentration between the ocean surface and the deep waters. This difference is determined by the carbon:nutrient ratio of the sinking organic material and it is crucial in determining the distribution of CO
Original language | English |
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Article number | L14613 |
Number of pages | 4 |
Journal | Geophysical Research Letters |
Volume | 33 |
DOIs | |
Publication status | Published - 2006 |