Ancient lava bubbles show old Earth’s air filled with greenhouse gases
Tiny bubbles that formed inside volcanic rock 2.7 billion years ago are providing insight into the conditions on primordial Earth.
Scientists say an analysis of gas bubbles trapped in ancient basalt rock that formed from ancient lava flows in western Australia showed the planet back then possessed a much thinner atmosphere, with air pressure half of what it is today.
That finding contradicts a long-held notion that Earth then had a thicker atmosphere to compensate for a fainter sun, with sunlight about 15% dimmer. The sun is slowly brightening over time, part of a star’s natural evolution.
Earth formed about 4.5 billion years ago. The planet 2.7 billion years ago was very different to what it is today.
In addition to the fainter sun, the air lacked oxygen, the moon was closer so tides were stronger, Earth spun more quickly so days were shorter and the only life forms were single-cell microbes, said study leader Sanjoy Som, chief executive of Seattle-based Blue Marble Space, a nonprofit organisation focusing on space science research, education and public outreach.
The findings demonstrate that “a planetary environment completely different to modern Earth can sustain life on its surface”, said Som, who worked on the study while at the University of Washington and is now based at Nasa’s Ames Research Centre in California.
“Life doesn’t need conditions like modern Earth to survive and thrive.
This is important in our quest for habitable environments in extra-solar planets,” Som added.
The scientists used scanning technology to analyse the size and distribution of bubbles in the ancient lava rock found along the shores of Australia’s Beasley River that solidified at sea level.
Lava flows cool rapidly from top and bottom, with bubbles trapped at the bottom being smaller than those at the top. The size difference in these bubbles provided a record of the atmospheric pressure pushing down on the molten rock as it cooled, the researchers said.
The findings suggest Earth’s atmosphere was rich in greenhouse gases.
“This study doesn’t yield direct knowledge about the air composition,” Som said. “Nonetheless, because most of the air pressure is nitrogen, and you needed greenhouse gases to compensate for a faint sun, methane — a powerful greenhouse gas — was a likely important constituent, as well as water vapour, another powerful greenhouse gas.”