Ancient minerals that could have existed when life began on Earth revealed
Washington: A new analysis of Hadean mineralogy challenges the assumption that the mineral species found on Earth today are much the same as they were during Earth`s first 550 million years-the Hadean Eon-when life emerged.
Carnegie`s Robert Hazen compiled a list of every plausible mineral species on the Hadean Earth and concludes that no more than 420 different minerals-about 8 percent of the nearly 5,000 species found on Earth today-would have been present at or near Earth`s surface.
"This is a consequence of the limited ways that minerals might have formed prior to 4 billion years ago," Hazen said.
"Most of the 420 minerals of the Hadean Eon formed from magma-molten rock that slowly crystallized at or near Earth`s surface-as well as the alteration of those minerals when exposed to hot water," he said.
By contrast, thousands of mineral species known today are the direct result of growth by living organisms, such as shells and bones, as well as life`s chemical byproducts, such as oxygen from photosynthesis.
In addition, hundreds of other minerals that incorporate relatively rare elements such as lithium, beryllium, and molybdenum appear to have taken a billion years or more to first appear because it is difficult to concentrate these elements sufficiently to form new minerals. So those slow-forming minerals are also excluded from the time of life`s origins.
"Fortunately for most origin-of-life models, the most commonly invoked minerals were present on early Earth," Hazen said.
For example, clay minerals-sometimes theorized by chemists to trigger interesting reactions-were certainly available.
Sulfide minerals, including reactive iron and nickel varieties, were also widely available to catalyze organic reactions.
However, borate and molybdate minerals, which are relatively rare even today, are unlikely to have occurred on the Hadean Earth and call into question origin models that rely on those mineral groups.
The study is published in American Journal of Science.
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