Michaelsarsia elegans
Coccolithophores, a globally ubiquitous type of phytoplankton, play an essential role in the cycling of carbon between the ocean and atmosphere. New research from Bigelow Laboratory for Ocean Sciences shows that these vital microbes can survive in low-light conditions by taking up dissolved organic forms of carbon, forcing researchers to reconsider the processes that drive carbon cycling in the ocean.
As part of a parallel process called the alkalinity pump, coccolithophores also convert bicarbonate molecules in surface water into calcium carbonate — essentially limestone — that forms their protective coccoliths. Again, when they die and sink, all that dense inorganic carbon is ballasted to the seafloor. Some of it then dissolves back into bicarbonate, thus ‘pumping’ alkalinity from the surface to depth.
This is the third and final paper published as part of a three-year National Science Foundation-funded project. The overall effort was inspired by a decades-old dissertation by William Blankley, a graduate student at Scripps Institution of Oceanography, Balch’s alma mater. In the 1960s, Blankley was able to grow coccolithophores in the dark for 60 days feeding them glycerol, one of the organic compounds used in the present study. Unfortunately, he died before his research could be published.
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