Resource allocation by the marine cyanobacterium Synechococcus WH8102 in response to different nutrient supply ratios
Resource allocation by the marine cyanobacterium Synechococcus WH8102 in response to different nutrient supply ratios
Date
2015-05
Authors
Mouginot, Céline
Zimmerman, Amy E.
Bonachela, Juan A.
Fredricks, Helen F.
Allison, Steven D.
Van Mooy, Benjamin A. S.
Martiny, Adam C.
Zimmerman, Amy E.
Bonachela, Juan A.
Fredricks, Helen F.
Allison, Steven D.
Van Mooy, Benjamin A. S.
Martiny, Adam C.
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Abstract
Differences in relative availability of nitrate vs. phosphate may contribute to regional
variations in plankton elemental stoichiometry. As a representative of the globally
abundant marine Synechococcus, strain WH8102 was grown in 16 chemostats up to 52
days at a fixed growth rate with nitrogen-phosphorus ratios (N:Psupply) of 1 to 50. Initially,
the phosphate and nitrate concentrations in the vessel decreased when the respective
nutrient was limiting. Cell growth generally stabilized, although several chemostats had
apparent oscillations in biomass. We observed extensive plasticity in the elemental
content and ratios. N:Pcell matched the supply values between N:Psupply 5 and 20. The
C:Pcell followed a similar trend. In contrast, the mean C:Ncell was 6.8 and did not vary as
a function of supply ratios. We also observed that induction of alkaline phosphatase, the
fraction of P allocated to nucleic acids, and the lipid
sulfoquinovosyldiacylglycerol:phosphatidyglycerol ratio inversely correlated with P
availability. Our results suggest that this extensive plasticity in the elemental content and
ratios depends both on the external nutrient availability as well as past growth history.
Thus, our study provides a quantitative understanding of the regulation of the elemental
stoichiometry of an abundant ocean phytoplankton lineage.
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Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here by permission of Association for the Sciences of Limnology and Oceanography for personal use, not for redistribution. The definitive version was published in Limnology and Oceanography 60 (2015): 1634–1641, doi:10.1002/lno.10123.