Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 11, 1599-1611, 2014
http://www.biogeosciences.net/11/1599/2014/
doi:10.5194/bg-11-1599-2014
© Author(s) 2014. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
26 Mar 2014
Phosphate supply explains variation in nucleic acid allocation but not C : P stoichiometry in the western North Atlantic
A. E. Zimmerman1,3, A. C. Martiny1,2, M. W. Lomas4, and S. D. Allison1,2 1Department of Ecology and Evolutionary Biology, University of California Irvine, Irvine, CA 92697-2525, USA
2Department of Earth System Science, University of California Irvine, Irvine, CA 92697-3100, USA
3Monterey Bay Aquarium Research Institute, Moss Landing, CA 95039, USA
4Bigelow Laboratory for Ocean Sciences, East Boothbay, ME 04544, USA
Abstract. Marine microbial communities mediate many biogeochemical transformations in the ocean. Consequently, processes such as primary production and carbon (C) export are linked to nutrient regeneration and are influenced by the resource demand and elemental composition of marine microbial biomass. Laboratory studies have demonstrated that differential partitioning of element resources to various cellular components can directly influence overall cellular elemental ratios, especially with respect to growth machinery (i.e., ribosomal RNA) and phosphorus (P) allocation. To investigate whether allocation to RNA is related to biomass P content and overall C : P biomass composition in the open ocean, we characterized patterns of P allocation and C : P elemental ratios along an environmental gradient of phosphate supply in the North Atlantic subtropical gyre (NASG) from 35.67° N, 64.17° W to 22.676° N, 65.526° W. Because the NASG is characterized as a P-stressed ecosystem, we hypothesized that biochemical allocation would reflect sensitivity to bioavailable phosphate, such that greater phosphate supply would result in increased allocation toward P-rich RNA for growth. We predicted these changes in allocation would also result in lower C : P ratios with increased phosphate supply. However, bulk C : P ratios were decoupled from allocation to nucleic acids and did not appear to vary systematically across a phosphate supply gradient of 2.2–14.7 μmol m−2 d−1. Overall, we found that C : P ratios ranged from 188 to 306 along the transect, and RNA represented only 6–12% of total particulate P, whereas DNA represented 11–19%. We did find that allocation to RNA was positively correlated with phosphate supply rate, suggesting a consistent physiological response in biochemical allocation to resource supply within the whole community. These results suggest that community composition and/or nonnucleic acid P pools may influence ecosystem-scale variation in C : P stoichiometry more than nucleic acid allocation or P supply in diverse marine microbial communities.

Citation: Zimmerman, A. E., Martiny, A. C., Lomas, M. W., and Allison, S. D.: Phosphate supply explains variation in nucleic acid allocation but not C : P stoichiometry in the western North Atlantic, Biogeosciences, 11, 1599-1611, doi:10.5194/bg-11-1599-2014, 2014.
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