Image_3_Phytoplankton Growth and Productivity in the Western North Atlantic: Observations of Regional Variability From the NAAMES Field Campaigns.JPEG

• Main Authors: James Fox, Michael J. Behrenfeld, Nils Haëntjens, Alison Chase, Sasha J. Kramer, Emmanuel Boss, Lee Karp-Boss, Nerissa L. Fisher, W. Bryce Penta, Toby K. Westberry, Kimberly H. Halsey
• Format: Still Image
• Language: unknown
• Published: 2021
• Subjects: Oceanography; Marine Biology; Marine Geoscience; Biological Oceanography; Chemical Oceanography; Physical Oceanography; Marine Engineering; phytoplankton; NPP; carbon; photoacclimation; modeling; optics; North Atlantic; Subarctic
• Online Access: https://doi.org/10.3389/fmars.2020.00024.s003; https://figshare.com/articles/figure/Image_3_Phytoplankton_Growth_and_Productivity_in_the_Western_North_Atlantic_Observations_of_Regional_Variability_From_the_NAAMES_Field_Campaigns_JPEG/14046899

The ability to quantify spatio-temporal variability in phytoplankton growth and productivity is essential to improving our understanding of global carbon dynamics and trophic energy flow. Satellite-based observations offered the first opportunity to estimate depth-integrated net primary production (NPP) at a global scale, but early modeling approaches could not effectively address variability in algal physiology, particularly the effects of photoacclimation on changes in cellular chlorophyll. Here, a previously developed photoacclimation model was used to derive depth-resolved estimates of phytoplankton division rate (μ) and NPP. The new approach predicts NPP values that closely match discrete measurements of 14 C-based NPP and effectively captured both spatial and temporal variability observed during the four field campaigns of the North Atlantic Aerosols and Marine Ecosystems Study (NAAMES). We observed favorable growth conditions for phytoplankton throughout the annual cycle in the subtropical western North Atlantic. As a result, high rates of μ are sustained year-round resulting in a strong coupling between growth and loss processes and a more moderate spring bloom compared to the high-latitude subarctic region. Considerable light limitation was observed in the subarctic province during the winter, which resulted in divergent growth dynamics, stronger decoupling from grazing pressure and a taxonomically distinct phytoplankton community. This study demonstrates how detailed knowledge of phytoplankton division rate furthers our understanding of global carbon cycling by providing insight into the resulting influence on phytoplankton taxonomy and the loss processes that dictate the fate of fixed carbon.