Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic

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. Laborat...

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Published in:Biogeosciences
Main Authors: Zimmerman, AE, Martiny, AC, Lomas, MW, Allison, SD
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 2014
Subjects:
Online Access:http://www.escholarship.org/uc/item/8mw6x3gp
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spelling ftcdlib:qt8mw6x3gp 2023-05-15T17:32:08+02:00 Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic Zimmerman, AE Martiny, AC Lomas, MW Allison, SD 1599 - 1611 2014-03-26 application/pdf http://www.escholarship.org/uc/item/8mw6x3gp english eng eScholarship, University of California qt8mw6x3gp http://www.escholarship.org/uc/item/8mw6x3gp Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Zimmerman, AE; Martiny, AC; Lomas, MW; & Allison, SD. (2014). Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic. Biogeosciences, 11(6), 1599 - 1611. doi:10.5194/bg-11-1599-2014. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/8mw6x3gp article 2014 ftcdlib https://doi.org/10.5194/bg-11-1599-2014 2018-12-14T23:51:56Z 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 μ4mol 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. ©Author(s) 2014. Article in Journal/Newspaper North Atlantic University of California: eScholarship Biogeosciences 11 6 1599 1611
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language English
description 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 μ4mol 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. ©Author(s) 2014.
format Article in Journal/Newspaper
author Zimmerman, AE
Martiny, AC
Lomas, MW
Allison, SD
spellingShingle Zimmerman, AE
Martiny, AC
Lomas, MW
Allison, SD
Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic
author_facet Zimmerman, AE
Martiny, AC
Lomas, MW
Allison, SD
author_sort Zimmerman, AE
title Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic
title_short Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic
title_full Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic
title_fullStr Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic
title_full_unstemmed Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic
title_sort phosphate supply explains variation in nucleic acid allocation but not c: p stoichiometry in the western north atlantic
publisher eScholarship, University of California
publishDate 2014
url http://www.escholarship.org/uc/item/8mw6x3gp
op_coverage 1599 - 1611
genre North Atlantic
genre_facet North Atlantic
op_source Zimmerman, AE; Martiny, AC; Lomas, MW; & Allison, SD. (2014). Phosphate supply explains variation in nucleic acid allocation but not C: P stoichiometry in the western North Atlantic. Biogeosciences, 11(6), 1599 - 1611. doi:10.5194/bg-11-1599-2014. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/8mw6x3gp
op_relation qt8mw6x3gp
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op_rights Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/bg-11-1599-2014
container_title Biogeosciences
container_volume 11
container_issue 6
container_start_page 1599
op_container_end_page 1611
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