Concentrations, turnover rates and fluxes of polyamines in coastal waters of the South Atlantic Bight
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  • 作者:Qian Liu ; Xinxin Lu ; Bradley B. Tolar ; Xiaozhen Mou ; James T. Hollibaugh
  • 关键词:Polyamines ; Dissolved organic nitrogen ; Bacterioplankton ; Spermidine ; Spermine ; Putrescine ; DFAA ; South Atlantic Bight
  • 刊名:Biogeochemistry
  • 出版年:2015
  • 出版时间:March 2015
  • 年:2015
  • 卷:123
  • 期:1-2
  • 页码:117-133
  • 全文大小:727 KB
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  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geochemistry
    Biochemistry
    Soil Science and Conservation
    Terrestrial Pollution
  • 出版者:Springer Netherlands
  • ISSN:1573-515X
文摘
Polyamines are short-chain aliphatic compounds containing multiple amine groups. They are important components of the cytosol of eukaryotes and are present at mmol?L? concentrations inside phytoplankton cells, while complex polyamines play a role in biosilica deposition. Concentrations of polyamines measured in seawater are typically in the sub-nmol?L? range, implying rapid and efficient uptake by osmotrophs, likely bacterioplankton. We measured turnover rates of three polyamines (putrescine, spermidine and spermine) using 3H-labeled compounds and determined their concentrations by HPLC to estimate polyamine contributions to dissolved organic matter and bacterioplankton carbon and nitrogen demand. These measurements were made on transects from the inner shelf to the Gulf Stream across the South Atlantic Bight (SAB) during April and October of 2011 and in salt marsh estuaries on the Georgia coast during August of 2011 and April of 2012. We found that turnover rates of polyamines were similar to those of amino acids (arginine and glutamic acid) measured in the same samples; however, fluxes of polyamines into bacterioplankton were much lower than amino acid fluxes as a result of low ambient concentrations. Turnover rates and fluxes of polyamines decreased from near-shore waters to the shelf-break, following the pattern of chlorophyll a concentration. Polyamine uptake accounted for less than 10?% of bacterial N demand and 5?% of bacterial C demand on average, with a large variation among water masses.
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