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Updated: Feb 5, 2026

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Modified Most Probable Number Assay to Quantify Salmonella in Raw and Ready-to-Cook Chicken Products
Published on: January 31, 2025
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Can Rates of Ocean Primary Production and Biological Carbon Export Be Related Through Their Probability
B B Cael1,2, Kelsey Bisson3, Christopher L Follett1
1Massachusetts Institute of Technology Cambridge MA USA.
Summary
This study presents a theory interpreting phytoplankton primary production and carbon export fluxes using probability distributions. Findings show these fluxes follow lognormal distributions, revealing a statistical scaling relationship between them.
Area of Science:
- Biogeochemistry
- Oceanography
- Ecology
Background:
- Phytoplankton primary production (p) and biological carbon export (f) are key ocean processes.
- These fluxes are mechanistically linked but measured on different scales and exhibit variability.
- Understanding their relationship is crucial for marine ecosystem and carbon cycle research.
Purpose of the Study:
- To develop a theoretical framework for interpreting biogeochemical fluxes (p and f) using probability distributions.
- To test the hypothesis that collections of p and f measurements exhibit a quantitative relationship.
- To explore the utility of a distributional approach for analyzing these oceanographic fluxes.
Main Methods:
- Utilized compilations of phytoplankton primary production (p) and biological carbon export (f) measurements.
- Applied a null model hypothesizing lognormal distributions for large-scale p and f.
- Inferred statistical scaling relationships and derived linear relationships between the log-moments of their distributions.
Main Results:
- Compilations of p and f measurements are consistent with lognormal distribution hypotheses.
- Subsets of p measurements (by biome, basin, depth, season) are also well-described by lognormals.
- A statistical scaling relationship between p and f was inferred, with consistent estimates for its slope and intercept.
Conclusions:
- The distributional approach provides a valuable framework for interpreting biogeochemical fluxes.
- The distribution of f measurements aligns with predictions derived from the moments of the p distribution.
- This approach offers potential for further development and application in marine science.
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