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Metal accumulation by heterotrophic marine bacterioplankton
Author(s) -
Vogel Catherine,
Fisher Nicholas S.
Publication year - 2010
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2010.55.2.0519
Subject(s) - environmental chemistry , metal , chemistry , ethylenediaminetetraacetic acid , seawater , bioconcentration , heterotroph , oxalate , cadmium , bacteria , inorganic chemistry , chelation , ecology , biology , bioaccumulation , genetics , organic chemistry
Radioisotopes of six metals ( 54 Mn, 55 Fe, 65 Zn, 109 Cd, 137 Cs, and 241 Am) were used to assess the accumulation of these metals by five species of heterotrophic marine bacteria in laboratory cultures exposed to environmentally realistic metal concentrations in natural seawater. Typically, uptake proceeded rapidly for the first 24 h and slowed down over the following 72‐96 h. At steady state, the bioconcentration of metals in cells was Fe > Am ≃ Mn ≃ Cd > Zn > Cs. Concentration factors were 0.6–2.8 × 10 6 for Fe, 0.6–3.5 × 10 4 for Mn and Am, 0.2–4.8 × 10 4 for Cd, 0.5–1.6 × 10 3 for Zn, and 1.9 × 10 2 for Cs. Rinsing with oxalate did not result in significantly lower Fe concentrations, but rinsing the cells with ethylenediaminetetraacetic acid resulted in significantly lower concentration factors for Mn and Am in one species. Interspecific differences in metal uptake were small under the conditions tested and were proportional to surface : volume ratios of the cells. The Q 10 of Zn uptake in two bacterial species examined was about 1, suggesting passive uptake. The Q 10 of Mn uptake was in the range of 1.8–3.6, indicating active uptake and transport into the cells. Given typical bacterial biomass in surface waters, we calculate that < 1% of most metals, but ~ 20% of Fe, should be associated with bacterial cells; they may serve as enriched sources of some metals for those organisms that consume them.