The Apparent Involvement of ANMEs in Mineral Dependent Methane Oxidation, as an Analog for Possible Martian Methanotrophy
| Autor: | Christopher H. House, Emily J. Beal, Victoria J. Orphan |
|---|---|
| Jazyk: | angličtina |
| Rok vydání: | 2011 |
| Předmět: |
Microorganism
Mars chemistry.chemical_element Mineralogy Manganese Article General Biochemistry Genetics and Molecular Biology Methane 03 medical and health sciences chemistry.chemical_compound Martian surface methanotrophy Archaea methane subsurface biosphere Sulfate lcsh:Science Ecology Evolution Behavior and Systematics 030304 developmental biology Martian 0303 health sciences biology 030306 microbiology Paleontology biology.organism_classification chemistry 13. Climate action Space and Planetary Science Environmental chemistry Anaerobic oxidation of methane lcsh:Q |
| Zdroj: | Life; Volume 1; Issue 1; Pages: 19-33 Life : Open Access Journal Life, Vol 1, Iss 1, Pp 19-33 (2011) |
| Popis: | On Earth, marine anaerobic methane oxidation (AOM) can be driven by the microbial reduction of sulfate, iron, and manganese. Here, we have further characterized marine sediment incubations to determine if the mineral dependent methane oxidation involves similar microorganisms to those found for sulfate-dependent methane oxidation. Through FISH and FISH-SIMS analyses using ^(13)C and ^(15)N labeled substrates, we find that the most active cells during manganese dependent AOM are primarily mixed and mixed-cluster aggregates of archaea and bacteria. Overall, our control experiment using sulfate showed two active bacterial clusters, two active shell aggregates, one active mixed aggregate, and an active archaeal sarcina, the last of which appeared to take up methane in the absence of a closely-associated bacterial partner. A single example of a shell aggregate appeared to be active in the manganese incubation, along with three mixed aggregates and an archaeal sarcina. These results suggest that the microorganisms (e.g., ANME-2) found active in the manganese-dependent incubations are likely capable of sulfate-dependent AOM. Similar metabolic flexibility for Martian methanotrophs would mean that the same microbial groups could inhabit a diverse set of Martian mineralogical crustal environments. The recently discovered seasonal Martian plumes of methane outgassing could be coupled to the reduction of abundant surface sulfates and extensive metal oxides, providing a feasible metabolism for present and past Mars. In an optimistic scenario Martian methanotrophy consumes much of the periodic methane released supporting on the order of 10,000 microbial cells per cm2 of Martian surface. Alternatively, most of the methane released each year could be oxidized through an abiotic process requiring biological methane oxidation to be more limited. If under this scenario, 1% of this methane flux were oxidized by biology in surface soils or in subsurface aquifers (prior to release), a total of about 10^(20) microbial cells could be supported through methanotrophy with the cells concentrated in regions of methane release. |
| Databáze: | OpenAIRE |
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