School of Earth, Environmental, & Marine Sciences Faculty Publications
Document Type
Article
Publication Date
7-23-2026
Abstract
Global biogeochemical models are powerful tools used to interpret observations and empirical data, create hypotheses, and make predictions. Many of these models, however, represent marine microbes as static stoichiometric reactions that convert nutrients into biomass. To better constrain the biological processes that control nutrient cycling in the global ocean, we extend the Cell Flux Model of Phytoplankton to explore the impact of dissolved iron concentration on the allocation of macromolecules and elemental ratios within phytoplankton cells. This model is supported by data obtained from a range of incubation experiments conducted with phytoplankton of varying species and size categories. Model output is applied globally to highlights the effects of iron and light availability and physiological adaptation on the distribution of open ocean and neritic phytoplankton taxa. This research aims to elucidate the role of phytoplankton physiology within biogeochemical cycles, allowing for better characterization of marine microbial distribution and elemental makeup for interpretive and predictive models.
Recommended Citation
Bernish, Margaret, Meng Gao, Jongsun Kim, Benoit Pasquier, and Keisuke Inomura. "Using a cell flux model to investigate phytoplankton growth and macromolecular allocation under iron limitation." Frontiers in Earth Science 14 (2026): 1839921. https://doi.org/10.3389/feart.2026.1839921
Creative Commons License

This work is licensed under a Creative Commons Attribution 4.0 International License.
Publication Title
Frontiers in Earth Science
DOI
10.3389/feart.2026.1839921

Comments
© 2026 Bernish, Gao, Kim, Pasquier and Inomura.
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