Where I Am Today
My studies at NASA have lead me in several directions. An important part of my
research deals with the origin of stromatolites, which are thin-layered sedimentary
structures that are produced by communities of microorganisms. But I have also been
interested in how some of the tiny microbes that create stromatolites become fossils. We
have actually found tiny microfossils in rocks as far back as 3.5 billion years. Question
is, how do these tiny creatures get preserved and why? By understanding such things we
can learn more about the ancient environment of the early Earth, and also improve our
chances of finding evidence of ancient life in rocks.
I'm still working on these problems. It turns out that on the present Earth,
microorganisms tend to thrive in extreme environments; places that are either too hot,
too cold, or too salty or acidic for larger complex organisms. I have looked at bacterial
life and their fossils in lots of extreme environments. But in trying to better
understand how the earliest communities lived, I have mostly focused on life at high
temperatures, that is, on microbes that live in hot springs found in places like
Yellowstone National Park. I have spent the last five summers in Yellowstone trying to
learn more about how the high-temperature communities survive, interact and become
fossils. This is important for interpreting the fossil record of early life on Earth. We
believe that the last common ancestor of living species on Earth lived at very high
temperatures. We know this because when we compare the DNA in all living things, we can
make a "tree of life" that shows how things are related. Turns out that the most
primitive things, that is, the species that occur near the trunk of the tree, are all
high-temperature bacteria, most of which live in hot springs and geysers. So these are
good places to go to find conditions similar to what prevailed on the early Earth.
But the story doesn't end there. Because hot springs are such good places to fossilize
microorganisms, these environments are also natural places to explore for fossil life on
Mars. So, we have also been looking at images of the surface of Mars for the most likely
spots for ancient hot-spring deposits. If we can find such deposits, we will want to go
there and bring rocks back from those places to look for microfossils. This is in our
present plan for Mars exploration, and has been really given a boost by the recent report
of possible life in the Martian meteorite, ALH84001, which was found in Antarctica.
Although I do not think this rock from Mars has definitive evidence of life, it does have
organic chemicals that were preserved much in the same way we see things preserved in hot
springs on Earth. NASA's Mars Global Surveyor and Mars Pathfinder and Russia's Mars '96
mission are scheduled for three separate launches in November and December 1996. We hope
that with the new information we get back from these missions, we will better know where
to go to bring samples back to Earth that may help us answer the question, "Did life ever
develop on Mars?"
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