This is an interesting bit of thinking, particularly since plenty of rocks are micaceous or containing blebs of mica. I have already posted on the likely importance of solid crystalline acids in the creation of life. Mica provides the sort of handy ‘wave’ guides that may make it practical.
At least by now looking at rocks, we may be looking at a real molecule assembling environment.
We as yet do not know how to produce a primordial cell let alone one able to replicate. However this is all a good start at producing a natural cell test tube to produce precursors.
We still have long way to go with this but at least the goal is pretty clear.
We can already say that if a replicating cell can be formed in the conditions we have already defined then life is a certainty in a just about every planet with conditions comparable to the worst ours can throw at us. It may be undeveloped and it may be mostly dormant, but it will exist and waiting for propitious conditions.
Peeking Between The Sheets For Life's Origin
Biomolecules (gray structures) between sheets of mica (green lines) in a primitive ocean. Credit: Helen Greenwood Hansma, University of California , Santa Barbara
by Staff Writers
That age-old question, "where did life on Earth start?" may have a new answer, thanks to a hypothesis that says life originated between sheets of mica that were layered like the pages in a book.
The so-called "life between the sheets" mica hypothesis was developed by Helen Hansma of the University of California , Santa Barbara
This hypothesis was originally introduced by Hansma at the 2007 annual meeting of the American Society for Cell Biology, and is now fully described by Hansma in the September 7, 2010 issue of Journal of Theoretical Biology.
According to the "life between the sheets" mica hypothesis, structured compartments that commonly form between layers of mica--a common mineral that cleaves into smooth sheets--may have sheltered molecules that were the progenitors to cells.
Provided with the right physical and chemical environment in the structured compartments to survive and evolve, the molecules eventually reorganized into cells, while still sheltered between mica sheets.
Mica chunks embedded in rocks could have provided the right physical and chemical environment for pre-life molecules and developing cells because mica compartments could have held, protected and sheltered molecules, and thereby promoted their survival.
Also, mica could have provided enough isolation for molecules to evolve without being disturbed and still allow molecules to migrate towards one another and eventually bond together to form large organic molecules. And mica compartments may have provided something akin to a template for the production of a life form composed of compartments, which are now known as cells.
Mica sheets are held together by potassium. If high levels of potassium were donated by mica sheets to developing cells, the high levels of potassium found in mica sheets could account for the high levels of potassium currently found in human cells.
Mica chunks embedded in rocks that were sitting in an early ocean would have received an endless supply of energy from waves, the sun, and the occasional sloshing of water into the spaces between the mica sheets. This energy could have pushed the mica sheets into up-and-down motions that could have pushed together molecules sitting between mica sheets, thereby enabling them to bond together.
Because mica surfaces are hospitable to living cells and to all the major classes of large biological molecules, including proteins, nucleic acids, carbohydrates and fats, the "between the sheets" mica hypothesis is consistent with other well-known hypotheses that propose that life originated as RNA, fatty vesicles or primitive metabolisms.
Hansma says a "mica world" might have sheltered all the ancient metabolic and fat-vesicle and RNA "worlds."
Hansma also says that mica would provide a better substrate for developing cells than other minerals that have been considered for that role. Why? Because most other minerals would probably have tended to intermittently become either too wet or too dry to support life.
By contrast, the spaces between mica sheets would probably have undergone more limited wet/dry cycles that would support life without reaching killing extremes.
In addition, many clays that have been considered as potential surfaces for life's origins respond to exposure to water by swelling. By contrast, mica resists swelling and would therefore provide a relatively stable environment for developing cells and biological molecules, even when it did get wet.
Hansma sums up her hypothesis by observing that "mica would provide enough structure and shelter for molecules to evolve but also accommodate the dynamic, ever-changing nature of life."
What's more, Hansma says that "mica is old." Some micas are estimated to be over 4 billion years old. And micas such as biotite have been found in regions containing evidence of the earliest life-forms, which are believed to have existed about 3.8 million years ago.
Hansma's passion for mica evolved gradually--starting when she began conducting pioneering, NSF-funded research in former husband Paul K. Hansma's AFM lab to develop techniques for imaging DNA and other biological molecules in the atomic force microscope (AFM)--a high-resolution imaging technique that allows researchers to observe and manipulate molecular and atomic level features.
Says Helen Hansma, "Mica sheets are atomically flat, so we can see DNA molecules on the mica surface without having to cover the DNA with something that makes it look bigger and easier to see. Sometimes we can even see DNA molecules swimming on the surface of mica, under water, in the AFM. Mica sheets are so thin (one nanometer) that there are a million of them in a millimeter-thick piece of mica."
Hansma's "life between the sheets" hypothesis first struck her a few years ago, after she and family members had collected some mica from a Connecticut
"It occurred to me that this might be a good place for the origins of life--sheltered within these stacks of sheets that can move up and down in response to flowing water, which could have provided the mechanicalenergy for making and breaking chemical bonds," says Hansma.
Hansma says that recent advancements in imaging techniques, including the AFM, made possible her recent research, leading to her "between mica sheets" hypothesis. She adds that direct support for her hypothesis might be obtained from additional studies involving mica sheets in an AFM, being subjected its push-and-pull forces while sitting in liquids resembling an early ocean.
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