Professor of Chemistry
Phytoplankton in the sunlit surface of the ocean photosynthesise to generate half of our atmosphere’s oxygen and become edible energy for life in the ocean.
These microorganisms have been called “beacons of climate change”; phytoplankton are not farmed, fished or part of any human commercial activity, so any shift in their abundance or diversity is a direct signal of environmental pressures such as ocean acidification, rising temperatures, and deoxygenation.
The European Union’s Marine Strategy Framework Directive (MSFD) requires monitoring of plankton indicators. However, numerous different methods of monitoring and the high-cost of equipment has limited our ability to make regional-scale observations and none can yet monitor the ability to generate calcium carbonate.
The Oxford Martin Programme on Monitoring Ocean Ecosystems aims to develop and undertake preliminary field-testing on a prototype for a low-cost sensor technology to continuously count and monitor oceanic phytoplankton and the calcium carbonate shells that they produce as part of their lifecycle.
This sensor technology could be transformative in our understanding of the future global ocean carbon cycle and ecosystem status. Establishing a baseline of phytoplankton productivity and diversity could provide vital information for identifying environmental pressures, as well as providing an early warning system on developments like algal blooms, which can be harmful to fisheries and conservation efforts.
A novel fluoro-electrochemical technique for classifying diverse marine nanophytoplankton
Rapid Opto-electrochemical Differentiation of Marine Phytoplankton
Quantifying the Extent of Calcification of a Coccolithophore Using a Coulter Counter
Calcium Carbonate Dissolution from the Laboratory to the Ocean: Kinetics and Mechanism
Single Calcite Particle Dissolution Kinetics: Revealing the Influence of Mass Transport
Single-entity coccolithophore electrochemistry shows size is no guide to the degree of calcification
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