We humans have always been fascinated by our origins. The question, 'How did life begin?' has concentrated scientific minds long before the concept of 'scientist' had been established. The conventional scenario has early microbial life teeming in the Earth's warm shallow waters. The abyssal depths were thought too cold, too energy poor and too inhospitable to nurture life. Even when the first hydrothermal vents were discovered, they were thought to be exceptions to a rule. Now a USC geomicrobiologist has discovered there are thousands of times more bacteria living happily on the seafloor than in the overhead water. So, 'If these deep underwater basalt plains are bulging with microbes, what do they live off?' I hear you ask. It seems the microbes live off the very rocks forming the Earth's crust itself. Chemical reaction with the basalt seam (all 60,000 km of it) generates sufficient energy to overcome their carbon poor environment. It may even be that life first fired up in the calm, stable deep water before migrating towards the light. Now wouldn't that be an ironic reversal of a popular scientific theory!

Thriller writers around the globe were looking smug and saying, 'I told you so.' as news of the discovery of a new ultra-small species of bacteria (Chryseobacterium greenlandensis) that survived despite being frozen in a Greenland glacier for 120,000 years hit the news wires. These bacteria are so small they easily slide through standard microbiological filters. It is one of only 10 to have been found to date in glaciers and polar ice.
http://www.usc.edu/uscnews/stories/15317.html http://live.psu.edu/story/31052 Image: 1. Microbial life ecosystem, Nicolle Rager-Fuller/National Science Foundation, 2. Scientists work with a 6m ice core section in Greenland, Mark Twickler, University of New Hampshire/National Oceanic and Atmospheric Administration Paleoclimatology Program/department of Commerce, 3. Cutting core samples for analysis, Todd Sowers, Penn State University.