Do We Owe Everything to Volcanoes?


	Do We Owe Everything to Volcanoes?

CrazyRedHead

9-4-2007 10:12 PM

690 views

tags:

science, biology, voncanoes, geology

1 Comment |

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9-5-2007 12:05 AM

The REAL Napster

...so in short, Volcanoes are the incubators of life on this third rock from the Sun. Interesting clip.

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<div style="margin: 12px 0px; font-family: arial; color: #333333; background: #ffffff; border: solid 4px #e5e5e5; width: 100%; clear: left;"><div class="CM_CTB_Content_Wrap" style="margin: 0px; padding: 0px;background-color: #ffffff;"><div style="border-bottom: solid 1px #dcdcdc; white-space: nowrap; margin-bottom: 8px; background-color: #eeeeee ;background-image: url(http://clipmarks.com/images/source-bg.gif); background-repeat: repeat-x; height: 24px; line-height: 24px; vertical-align: middle; padding-bottom: 4px; color: #666666; font-size: 10px;" ><a href="http://clipmarks.com/clip-to-blog/" title="see clips that are hot right now"><img src="http://content.clipmarks.com/blog_embed/6dcd2d38-154e-4500-8a26-570cced3aa2c/70E6B3A2-4D72-4EFA-8C0E-9AFB1F346A2A/" alt="" width="19" height="19" border="0" style="vertical-align: middle; margin: 0px 4px; display: inline; border: none; float:none;" /></a>clipped from <a title="http://news.nationalgeographic.com/news/bigphotos/8254847.html" href="http://news.nationalgeographic.com/news/bigphotos/8254847.html" style="font-size: 11px;">news.nationalgeographic.com</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/bigphotos/8254847.html"><div align="center"><img src="http://content8.clipmarks.com/blog_cache/news.nationalgeographic.com/img/28102CA3-732D-4133-A59E-67A8F5D4E87B" alt="" /></div></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/bigphotos/8254847.html"><MAJOR_CUTLINE _moz-userdefined="">A rise in oxygen levels around 2.5 billion years ago may have occurred after a massive tectonic shift forced many submerged volcanoes above water, a new study says.</MAJOR_CUTLINE></blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/bigphotos/8254847.html"><P>These above-ground volcanoes, such as the Piton de La Fournaise volcano on the island of La Réunion (above, erupting in April 2007) stopped spewing oxygen-destroying chemicals into the air—allowing vital ingredients for complex life to build up. </P></blockquote><div style="border-bottom: solid 1px #dcdcdc; white-space: nowrap; margin-bottom: 8px; background-color: #eeeeee ;background-image: url(http://clipmarks.com/images/source-bg.gif); background-repeat: repeat-x; height: 24px; line-height: 24px; vertical-align: middle; padding-bottom: 4px; color: #666666; font-size: 10px;" ><a href="http://clipmarks.com/clip-to-blog/" title="see clips that are hot right now"><img src="http://content9.clipmarks.com/images/clip-icon.gif" alt="" width="19" height="19" border="0" style="vertical-align: middle; margin: 0px 4px; display: inline; border: none; float:none;" /></a>clipped from <a title="http://news.nationalgeographic.com/news/2007/08/070829-volcano-life.html" href="http://news.nationalgeographic.com/news/2007/08/070829-volcano-life.html" style="font-size: 11px;">news.nationalgeographic.com</a></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/2007/08/070829-volcano-life.html">
At that time, Earth's early atmosphere wasn't fit to breathe. Filled with nitrogen, carbon dioxide, and sulfurous fumes, the air would have left humans gasping.</blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/2007/08/070829-volcano-life.html">
These noxious fumes held a clamp on evolution: Complex life didn't really get going until the planet's skies began to fill with oxygen, allowing more efficient methods of extracting energy from nutrients.</blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/2007/08/070829-volcano-life.html">
Submerged volcanoes spew a different set of gases than those that erupt into the air. </blockquote><div style="height: 2px; font-size: 2px; background: #dcdcdc; border-bottom: solid 1px #f5f5f5; margin: 2px 4px;"></div><blockquote style="text-align: left; padding: 0px 8px; margin: 4px 0px 8px 0px; background: transparent; border: none;" cite="http://news.nationalgeographic.com/news/2007/08/070829-volcano-life.html">
Magma from aerial volcanoes, on the other hand, stays hot and releases gases like carbon dioxide</blockquote></div><div style="margin: 0px 6px 6px 4px;"><table style="font-size: 11px;border-spacing: 0px;padding: 0px;" cellpadding="0" cellspacing="0" width="100%"><tr><td style="background:transparent;border-width:0px;padding:0px;">&nbsp;</td><td align="right" style="background:transparent;border-width:0px;padding:0px;width:107px" width="107"><a href="http://clipmarks.com/share/70E6B3A2-4D72-4EFA-8C0E-9AFB1F346A2A/blog/" title="blog or email this clip"><img src="http://content6.clipmarks.com/images/c2b-foot.png" border="0" alt="blog it" width="107" height="17" style="border-width:0px;padding:0px;margin:0px;" /></a></td></tr></table></div></div>

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