ArticleComputational and structural biotechnology journal2021
Modeled temperature dependencies of macromolecular allocation and elemental stoichiometry in phytoplankton.
Article in Computational and structural biotechnology journal, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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Who cites it
9 citing papers in PubMed.
- Article
- Nitrogen deposition reveals global patterns in plant and animal stoichiometry.Nature communications · 2025Article
- Metabolic biochemical models of NmSystems · 2025Article
- The effect of temperature on phytoplankton physiology: a mesocosm and modeling study.Microbiology spectrum · 2025Article
- Warm-Loving Species Perform Well Under Limiting Resources: Trait Combinations for Future Climate.Global change biology · 2025Article
- Diel variation of plankton in the highly impacted freshwater zone of Hooghly estuary in relation to ecological alteration.Environmental monitoring and assessment · 2024Article
- Saturating growth rate against phosphorus concentration explained by macromolecular allocation.mSystems · 2023Article
- Modeling the elemental stoichiometry and silicon accumulation in diatoms.Current research in microbial sciences · 2022Article
- Saturating relationship between phytoplankton growth rate and nutrient concentration explained by macromolecular allocation.Current research in microbial sciences · 2022Article
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2 authors.
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Abstract
Warming oceans may affect how phytoplankton allocate nutrients to essential cellular processes. Despite the potential impact of such processes on future biogeochemical cycles, questions remain about how temperature affects macromolecular allocation and elemental stoichiometry within phytoplankton cells. Here, we present a macromolecular model of phytoplankton and the effect of increasing temperature on the intracellular allocation of nutrients at a constant growth rate. When temperature increases under nitrogen (N) and phosphorus (P) co-limitation, the model shows less investment in phosphorus-rich RNA molecules relative to nitrogen-rich proteins, leading to a more severe decrease in cellular P:C than N:C causing increased cellular N:P values. Under P limitation, the model shows a similar pattern, but when excess P is available under N limitation, we predict lowered N:P due to the effect of luxury uptake of P. We reflected our model result on the surface ocean showing similar latitudinal patterns in N:P and P:C to observation and other model predictions, suggesting a considerable impact of temperature on constraining the elemental stoichiometry in the ocean.
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