Astrobiology: Life in the Universe

Astrobiology Science and Technology for Exploring Planets (ASTEP)


  1. Seminar Detail

    Methane<br />
greenhouses and anti-greenhouses on the early Earth

    Methane
    greenhouses and anti-greenhouses on the early Earth


    Presenter: Jim Kasting

    October 14, 2003 12:00 AM Pacific

    Methane was probably much more abundant in the low-O2
    Archean/early Paleoproterozoic atmosphere, prior to 2.3 Ga, than it is
    today. CH4 concentrations of 1000 ppm or more are predicted once
    methanogenic bacteria had evolved. Greenhouse warming from this CH4 could
    have been a major factor in offsetting reduced solar luminosity at that
    time. However, if CH4 became more abundant than CO2, it would have
    polymerized to form hydrocarbon smog in the stratosphere. This, in turn,
    would have created an anti-greenhouse effect that cooled the surface. The
    rise of O2 at 2.3 Ga wiped out most of this methane and may have triggered
    the very deep (possibly global) Paleoproterozoic glaciations.

    Participation Instructions

    http://nai.arc.nasa.gov/seminars/instructions.cfm

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