source: Phys.org

Since 1934, the Redfield ratio—the recurring ratio of 106:16:1 of carbon to nitrogen to phosphorus (C:N:P) in phytoplankton and the pathways by which these elements are circulated throughout all parts of the Earth—has been a cornerstone of oceanography. While differences in C:N:P ratios exist and have been observed across ocean biomes, to date there has not been an established way to quantify or predict that variation. However, a new study from a University of Rhode Island professor could help to fill in the blanks for scientists studying and trying to understand these variances. Read Full Article Here