Carbon dioxide (CO₂) from the atmosphere is fixed into organic carbon
by phytoplankton in the sunlit surface ocean. This organic carbon fuels
marine food webs, but a portion of it is exported to the deep ocean,
where it can remain isolated from the atmosphere for centuries to
millennia. This vertical export of organic carbon is one of the primary
ways the ocean buffers rising atmospheric CO₂ from human activity.
My research explores questions such as:
To investigate these questions, I collaborate with a broad range of ocean scientists, integrating biogeochemical, bio-optical, remote sensing, and experimental data to gain a holistic understanding of ocean microbial dynamics.