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Journal Article

Elemental composition of natural populations of key microbial groups in A tlantic waters

Carolina Grob; Martin Ostrowski; Ross J. Holland; Mikal Heldal; Svein Norland; Egil S. Erichsen; Claudia Blindauer; Adrian P. Martin; Mikhail V. Zubkov; David J. Scanlan
Environmental Microbiology · Vol. 15, Issue 11 · pp. 3054-3064 · 2013

Abstract

Summary Intracellular carbon ( C ), nitrogen ( N ) and phosphorus ( P ) content of marine phytoplankton and bacterioplankton can vary according to cell requirements or physiological acclimation to growth under nutrient limited conditions. Although such variation in macronutrient content is well known for cultured organisms, there is a dearth of data from natural populations that reside under a range of environmental conditions. Here, we compare C , N and P content of S ynechococcus , P rochlorococcus , low nucleic acid ( LNA ) content bacterioplankton and small plastidic protists inhabiting surface waters of the North and South subtropical gyres and the E quatorial R egion of the A tlantic O cean. While intracellular C : N ratios ranged between 3.5 and 6, i.e. below the R edfield ratio of 6.6, all the C : P and N : P ratios were up to 10 times higher than the corresponding R edfield ratio of 106 and 16, respectively, reaching and in some cases exceeding maximum values reported in the literature. Similar C : P or N : P ratios in areas with different concentrations of inorganic phosphorus suggests that this is not just a response to the prevailing environmental conditions but an indication of the extremely low P content of these oceanic microbes.

Bibliographic Information

JournalEnvironmental Microbiology
PublisherWiley
Publication Date2013-11-01
Publication Year2013
Volume15
Issue11
Pages3054-3064
Document TypeJournal Article
Print ISSN1462-2912
eISSN1462-2920
DOI10.1111/1462-2920.12145
SubjectMicrobial Ecology

Access Information

NARA Access Coverage1999-01-01~Current
Journal Homepagehttps://onlinelibrary.wiley.com/loi/14622920
Publisher PageOpen Publisher Page
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