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Two microbes team up to munch methane.


Vast stores of methane gas lie buried beneath the seafloor, yet little escapes from the sediments into the ocean and the atmosphere above. Geochemists have long suspected that methane-munching microbes gobble the gas before it can seep upward out of the ooze. But scientists had been at a loss to explain how a microorganism microorganism /mi·cro·or·gan·ism/ (-or´gah-nizm) a microscopic organism; those of medical interest include bacteria, fungi, and protozoa.  could consume methane where oxygen is in short supply, as it is in the sediments.

As it turns out, not one microbe microbe /mi·crobe/ (mi´krob) a microorganism, especially a pathogenic one such as a bacterium, protozoan, or fungus.micro´bialmicro´bic

mi·crobe
n.
 but two probably work as a tag team to feed off the methane. A group of researchers studying methane-bearing sediments collected off the coast of Oregon has discovered aggregates of two fundamentally different microorganisms, which appear to be collaborating to consume the gas. Led by Antje Boetius, a microbiologist at the Max Planck Institute for Marine Microbiology The Max Planck Institute for Marine Microbiology is located in Bremen, Germany. It was founded in 1992 and moved into new buildings at the campus of the University of Bremen in 1996. It is one of 80 institute in the Max Planck Society (Max Planck Gesellschaft).  in Bremen, Germany, the scientists report their findings in the Oct. 5 NATURE.

Most methane in Earth's atmosphere is produced in low-oxygen environments by a class of single-celled microbes known as archaea archaea: see Archaebacteria.
archaea

A group of prokaryotes whose members differ from bacteria, the most prominent prokaryotes, in certain physical, physiological, and genetic features. The archaea may be aquatic or terrestrial microorganisms.
. However, in the presence of bacteria that use sulfate sulfate, chemical compound containing the sulfate (SO4) radical. Sulfates are salts or esters of sulfuric acid, H2SO4, formed by replacing one or both of the hydrogens with a metal (e.g., sodium) or a radical (e.g., ammonium or ethyl).  ions rather than oxygen to fuel their metabolism, some species of archaea can consume methane rather than produce it.

Boetius' team found cell aggregates that typically had a core of about 100 methane-consuming archaea. This dense sphere of cells was fully or partially surrounded by a shell of about 200 sulfate-consuming bacteria. These cellular consortia measured on average, 3.2 micrometers across.

The highest concentration of the cellular clusters--more than 30 million per cubic centimeter--occurred within the top 5 cm of sediment. There, the concentration of sulfate ions from the ocean water and the rate at which the sulfate ions are consumed were also highest.

Edward F. DeLong, a microbiologist at the Monterey Bay Aquarium Research Institute The Monterey Bay Aquarium Research Institute (MBARI) is a not-for-profit oceanographic research center in Moss Landing, California affiliated with the Monterey Bay Aquarium. It was founded in 1987 by David Packard of Hewlett-Packard fame.  in Moss Landing, Calif., says it's likely that the bacteria in the outer shell use the sulfate ions in the shallow sediments to help them metabolize me·tab·o·lize
v.
1. To subject to metabolism.

2. To produce by metabolism.

3. To undergo change by metabolism.



metabolize

to subject to or be transformed by metabolism.
 the organic compounds produced by the methane-consuming archaea.

DeLong says the tight clustering of the two microorganisms is "a solid piece of evidence" that the groups of cells have formed an intimate partnership enabling them to feed off the methane.
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Title Annotation:ocean bottom
Author:Perkins, S.
Publication:Science News
Article Type:Brief Article
Date:Oct 7, 2000
Words:357
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