Fig. 7: Time series of phytoplankton-specific C:P ratios calculated from the trait-based model approach of Tanioka et al.38. | Nature Communications

Fig. 7: Time series of phytoplankton-specific C:P ratios calculated from the trait-based model approach of Tanioka et al.38.

From: Adaptive carbon export response to warming in the Sargasso Sea

Fig. 7: Time series of phytoplankton-specific C:P ratios calculated from the trait-based model approach of Tanioka et al.38.The alternative text for this image may have been generated using AI.

Model phytoplankton C:P in the surface 100 m is computed as a function of growth rate and POC:Chl-a ratio derived from MODIS-Aqua combined with a map of temperature-dependent nutrient limitation.

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