The major nutrients nitrate and phosphate have one of the strongest correlations in the sea, with a slope similar to the average nitrogen to phosphorus content of plankton biomass (16:1). Why this global relationship exists, despite the wide range of nitrogen to phosphorus ratios at the organism level, is unknown. Here, an ocean circulation model and observed nutrient distributions have been used to show that the covariation of dissolved nitrate and phosphate is maintained by ocean circulation.
- Thomas S. Weber
- Curtis Deutsch