Protein content and protein synthesis rates of planktonic marine bacteria
- 1 January 1989
- journal article
- research article
- Published by Inter-Research Science Center in Marine Ecology Progress Series
- Vol. 51 (3) , 201-213
- https://doi.org/10.3354/meps051201
Abstract
Bacterial carbon production is an important parameter in understanding the flows of carbon and energy in aquatic ecosystems, but has been difficult to measure. Present methods are based on measuring the rate of cell production, and thus require a knowledge of cellular carbon content of the growing bacteria to convert cell production into carbon production. We have examined the possibility that protein synthesis rate of pelagic bacteria might serve as the basis for directly estimating bacterial carbon production. We measured bacterial protein content and protein production of pelagic bacteria. Bacterial protein content was measured as amino acids by high performance liquid chromatography of cell hydrolysates of bacterial assemblages of mean diameters from 0.026 to 0.4 .mu.m. Cellular protein:volume (w/v) in the largest bacteria was 15.2 % (similar to cultued Escherichia coli) but increased with decreasing cell size to 46.5 % in 0.026 .mu.m bacteria. Protein per bacterium was correlated with cell volume by the power function y = 88.6x0.59 (r2 = 0.67; p < 0.01; n = 25). An inventory of major bacterial macromolecular pools revealed that cell protein:dry weight and cell protein:carbon were essentially constant (63% and 54 %, respectively) for the entire cell size range although cell protein:volume increased with decreasing cell size. Thus, the smaller cells in the size range were rich in carbon and dry weight and poor in water compared with larger cells. We established the experimental conditions for estimating protein synthesis on the basis of 3H leucine incorporation by bacteria, and determined the necessary parameters (including the intracellular isotope dilution by HPLC) for converting 3H leucine incorporation into protein synthesis rate. In samples from Scripps Institution of Oceanography pier the intracellular isotope dilution was only 2-fold. In a field study in Southern California Bight bacterial protein production and 3H-thymidine incorporation method yielded comparable rates of bacterial production. Bacterial protein production method was an order of magnitude more sensitive and yielded bacterial carbon production directly without the need to know the cell size of the part of the assemblage in growth state.This publication has 18 references indexed in Scilit:
- High methane emissions from thermokarst lakes in subarctic peatlandsLimnology and Oceanography, 2016
- Periplasmic gel: new concept resulting from the reinvestigation of bacterial cell envelope ultrastructure by new methodsJournal of Bacteriology, 1984
- Bacterioplankton growth in seawater: I. Growth kinetics and cellular characteristics in seawater culturesMarine Ecology Progress Series, 1984
- The Ecological Role of Water-Column Microbes in the SeaMarine Ecology Progress Series, 1983
- Thymidine incorporation as a measure of heterotrophic bacterioplankton production in marine surface waters: Evaluation and field resultsMarine Biology, 1982
- Assimilatory Sulfur Metabolism in Marine Microorganisms: Considerations for the Application of Sulfate Incorporation into Protein as a Measurement of Natural Population Protein SynthesisApplied and Environmental Microbiology, 1982
- Bacterioplankton Secondary Production Estimates for Coastal Waters of British Columbia, Antarctica, and CaliforniaApplied and Environmental Microbiology, 1980
- High performance liquid chromatographic determination of subpicomole amounts of amino acids by precolumn fluorescence derivatization with o-phthaldialdehydeAnalytical Chemistry, 1979
- Use of nuclepore filters for counting bacteria by fluorescence microscopyApplied and Environmental Microbiology, 1977
- Determination of bacterial number and biomass in the marine environmentApplied and Environmental Microbiology, 1977