2005 Annual Science Report

University of California, Los Angeles Reporting  |  JUL 2004 – JUN 2005

Geochemical Production of Methane on Mars

Project Summary
4 Institutions
3 Teams
0 Publications
0 Field Sites
Field Sites

Project Progress

Production of Mars methane by fluid-rock interaction in the crust

This work was a collaborative effort, involving J. Lyons, C. Manning, and F. Nimmo (now at UC Santa Cruz), to understand possible sources for the methane recently discovered in the Martian atmosphere. Detection of methane was reported by three different groups (Mumma et al. 2003; Formisano et al. 2004; Krasnopolsky et al. 2004). The observed methane volume fraction varied from 10 ppb (parts per billion) to about 100 ppb methane, with substantial (and surprising) variations with longitude. Given that terrestrial methane is primarily a product of methanogens, it is natural to consider Mars methane to also be biogenic. However, the methane flux implied by 10 ppb methane is only about 107 moles per year, about one-millionth the terrestrial methane flux. Because many abiogenic sources of methane on Earth produce comparable flux levels, we chose to explore abiogenic geochemical sources on Mars.

An obvious possible methane source is serpentinization, in which Fe2+ in olivine is oxidized to Fe3+ during aqueous alteration. The redox couple is balanced by reduction of C in the fluid (e.g., as carbonate) to methane. Another possible methane source, and the one that we focused on, is thermochemical reactions in hydrothermal fluids. Previous work on the shergottite meteorites demonstrated that the oxygen fugacity in the Martian crust is no higher than that of a quartz-fayalite-magnetite (QFM) rock buffer, and may be as low as QFM-4 (in fO2 log units). At these oxygen fugacities magamtic CO2 in a water-dominated hydrothermal fluid will be converted to CH4 at temperatures of about 400 °C and less, assuming thermochemical equilibrium. Phase separation of supercritical water and methane yields methane vapor, which can then diffuse through the crust and reach the atmosphere. We showed that a very small magmatic intrusion (~1 km wide x 10 km long) at a depth of 10 km could easily explain a 10 ppb methane fraction in the Mars atmosphere. This work has been accepted for publication in Geophysical Research Letters. (The thermochemistry and phase diagram calculations in this work were carried out primarily by C. Manning using methods he developed for abiogenic methane production on early Earth. Nimmo provided the geophysical context for the work. Lyons provided the atmospheric context and also initiated the project.)

  • PROJECT INVESTIGATORS:
    James Lyons
    Co-Investigator
    Craig Manning Craig Manning
    Co-Investigator
    Francis Nimmo
    Co-Investigator
  • RELATED OBJECTIVES:
    Objective 2.1
    Mars exploration

    Objective 3.1
    Sources of prebiotic materials and catalysts

    Objective 7.2
    Biosignatures to be sought in nearby planetary systems