<?xml version="1.0" encoding='utf-8'?>
<!DOCTYPE wml PUBLIC "-//WAPFORUM//DTD WML 1.1//EN" "http://www.wapforum.org/DTD/wml_1.1.xml">
<wml>
<card id="card1" title="Prebiotic atmosphere - Page 24 - Wikipedia">
<p>
<a accesskey="1" href="page.php?w=Prebiotic_atmosphere&amp;p=23">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Prebiotic_atmosphere&amp;p=25">3.Next</a>
</p>
<p>it was not nearly as abundant in the prebiotic atmosphere. This is favorable for the origin of life, as O<sub>2</sub> would oxidize organic compounds needed in the origin of life. The prebiotic atmosphere O<sub>2</sub> abundance can be theoretically calculated with models of atmospheric chemistry. The primary source of O<sub>2</sub> in these models is the breakdown and subsequent chemical reactions of other oxygen containing compounds. <a href="page.php?w=Photodissociation">Incoming solar photons</a> or <a href="page.php?w=lightning">lightning</a></p><p>
<a accesskey="1" href="page.php?w=Prebiotic_atmosphere&amp;p=23">1.Previous</a><br />
<a accesskey="3" href="page.php?w=Prebiotic_atmosphere&amp;p=25">3.Next</a>
</p>

<do type="prev" label="Search">
        <go href="search.wml"/>
</do>

</card>
</wml>
