Will nitrogen limitation and high CO₂ concentrations impact upon the sinking velocity of phytoplankton?
The biological carbon pump in the ocean plays an important role in controlling atmospheric CO₂ levels. Approximately 1-3% of the yearly 50–60 Pg C of marine primary production settles in the deep ocean, where it is effectively sequestered for centuries to millennia. Central to the strength of the pu...
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| Format: | Thesis |
| Language: | unknown |
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2017
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| Online Access: | https://doi.org/10.4225/03/58b79d337d1d1 https://figshare.com/articles/thesis/Will_nitrogen_limitation_and_high_CO_concentrations_impact_upon_the_sinking_velocity_of_phytoplankton_/4713610 |
| Summary: | The biological carbon pump in the ocean plays an important role in controlling atmospheric CO₂ levels. Approximately 1-3% of the yearly 50–60 Pg C of marine primary production settles in the deep ocean, where it is effectively sequestered for centuries to millennia. Central to the strength of the pump is the sinking velocity of phytoplankton cells and other organic debris. Stokes' Law indicates that the sinking velocity of a spherical cell will depend on its size and density, where larger, heavier cells will sink at a faster rate. Given that growth conditions can result in changes in cell size and macromolecular composition of phytoplankton, it might be expected that such changes could cause alterations in sinking velocity and carbon drawdown via the biological carbon pump. In the future, phytoplankton cells in the open ocean are predicted to be more subject to nutrient limitation due to enhanced stratification reducing the upwelling of nutrients. This will be driven by the warming of surface waters and an increase in the difference between the temperature of the surface and deeper ocean. Therefore the effects of nitrogen limitation on the sinking velocity of Emiliania huxleyi, a coccolithophore responsible for significant phytoplankton blooms and biological drawdown of carbon was examined. Nitrogen limitation caused changes in macromolecular composition, especially lipid content and also alters coccosphere thickness. However, the overall density of the cells remained similar, and, as a consequence, cell size was the major determinant of sinking rate with N-limited cells in exponential phase sinking more slowly than N-replete cells. Cells in stationary phase showed the reverse trend with N-limited cells sinking faster, although not as fast as N-replete cells in exponential phase. N-limited cells produced more transparent exopolymers (TEP), suggesting an increased capacity for aggregation and marine snow formation. Phytoplankton cells are also expected to be to be exposed to higher concentrations of CO₂ in the ... |
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