AEM
Home Help [Feedback] [For Subscribers] [Archive] [Search] [Contents]
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrowReprints and Permissions
Right arrow Copyright Information
Right arrow Books from ASM Press
Right arrow MicrobeWorld
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by King, G. M.
Right arrow Articles by Lovley, D. R.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by King, G. M.
Right arrow Articles by Lovley, D. R.
Agricola
Right arrow Articles by King, G. M.
Right arrow Articles by Lovley, D. R.

 Previous Article  |  Next Article 

Appl Environ Microbiol. 1983 June; 45(6): 1848-1853
Copyright © 1983, American Society for Microbiology. All Rights Reserved.

Metabolism of Acetate, Methanol, and Methylated Amines in Intertidal Sediments of Lowes Cove, Maine {dagger}

Gary M. King, M. J. Klug and D. R. Lovley

1 I. C. Darling Center, University of Maine, Walpole, Maine 04573; W. K. Kellogg Biological Station, Michigan State University, Hickory Corners, Michigan 490602; and Department of Anaerobic Microbiology, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 240613

ABSTRACT

The fates and the rates of metabolism of acetate, trimethylamine, methylamine, and methanol were examined to determine the significance of these compounds as in situ methane precursors in surface sediments of an intertidal zone in Maine. Concentrations of these potential methane precursors were generally <3 µM, with the exception of sediments containing fragments of the seaweed Ascophyllum nodosum, in which acetate was 96 µM. [2-14C]acetate turnover in all samples was rapid (turnover time <2 h), with 14CO2 as the primary product. [14C]trimethylamine and methylamine turnover times were slower (>8 h) and were characterized by formation of both 14CH4 and 14CO2. Ratios of 14CH4/14CO2 from [14C]trimethylamine and methylamine in uninhibited sediments indicated that a significant fraction of these substrates were catabolized via a non-methanogenic process. Data from inhibition experiments involving sodium molybdate and 2-bromoethanesulfonic acid supported this interpretation. [14C]methanol was oxidized relatively slowly compared with the other substrates and was catabolized mainly to 14CO2. Results from experiments with molybdate and 2-bromoethanesulfonic acid suggested that methanol was oxidized primarily through sulfate reduction. In Lowes Cove sediments, trimethylamine accounted for 35.1 to 61.1% of total methane production.


FOOTNOTES

{dagger} Contribution no. 163 of the Darling Center, 83-01 of the Maine Benthic Research Group, 500 of the Kellogg Biological Station, and 10,730 of the Michigan Agricultural Experiment Station.


Appl Environ Microbiol. 1983 June; 45(6): 1848-1853
Copyright © 1983, American Society for Microbiology. All Rights Reserved.




This article has been cited by other articles:




Home Help [Feedback] [For Subscribers] [Archive] [Search] [Contents]
J. Bacteriol. Microbiol. Mol. Biol. Rev. Eukaryot. Cell All ASM Journals

Copyright © 1983 by the American Society for Microbiology. All rights reserved.