The Simons Collaboration on Computational Biogeochemical Modeling of Marine Ecosystems (CBIOMES) seeks to develop and apply quantitative models of the structure and function of marine microbial communities at seasonal and basin scales.
CBIOMES Marine Ecosystem Currencies Reconciliation Workshop
Dates: October 5 – 8, 2026
Venue: MIT Endicott House, Dedham, MA
Latest News

October 2026 CBIOMES e-meeting Ziyue (Patrick) Zheng (UCSC)
Incorporating Biological Knowledge into Autogating for Flow Cytometry Analysis. Please note access to this page is restricted to CBIOMES associates. (more…)

October 2026 CBIOMES e-meeting Ben Grodner (UW)
Eukaryotic phytoplankton in the North Pacific Transition Zone invest in high-affinity siderophore uptake genes to manage iron demand. Please note access to this page is restricted to CBIOMES associates. (more…)

CBIOMES Welcomes Trisha Dawn
CBIOMES is pleased to welcome Trisha Dawn to the team as a postdoc in Justin Hyun's group at the University of California, Santa Cruz. (more…)
Latest Publications
Ashley N. Bulseco, Wenzhuo Yang, Julie A. Huber, Joseph J. Vallino (2026), Growth characteristics of natural microbial populations are skewed toward bacteria with low specific growth rates, Microbiology Spectrum, doi: 10.1128/spectrum.02193-26
Davor Mance, Diana Mance, Žarko Kovač, Shubha Sathyendranath, Anja Kovač (2026), The production-function structure of marine primary-production models: Marginal products, elasticities, and light–nutrient trade-offs, Journal of Marine Systems, doi: 10.1016/j.jmarsys.2026.104275
Sing-how Tuo, Ying-Yu Hu, Andrew J. Irwin, Michael J. Follows, Zoe V. Finkel (2026), Phosphate modulates elemental and macromolecular composition of unicellular nitrogen-fixing cyanobacteria, Limnology and Oceanography, doi: 10.1002/lno.70475
Alexandra E. Jones-Kellett, Jesse C. McNichol, Yubin Raut, Jed A. Fuhrman, and Michael J. Follows (2026), The dynamic mesoscale sink and source niches for eukaryotic phytoplankton in a subtropical gyre, PNAS, doi: 10.1073/pnas.2608700123?af=R


