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5. Summary and Conclusions
The martian meteorite Y000593 contains two distinctive
sets of features associated with the martian-derived iddingsite.
The tunnel and microtunnel structures are typically
found in olivine along the margins of mineralogically complex
iddingsite veins. These microtunnels contain areas of
enhanced carbon abundance that, in some cases, are not associated
with common carbonate cations and therefore are
interpreted as carbonaceous material, perhaps similar to
kerogen. The second set of features consists of nanometer- to
micrometer-sized spherules sandwiched between layers of
indigenous iddingsite and distinct from carbonate and the
underlying silicate layer. Similar spherules have also been
described in Nakhla (Gibson et al., 2001). EDS spectra of the
Y000593 spherules show that they are significantly enriched
in carbon compared to the nearby surrounding iddingsite
layers. A striking observation is that these two sets of features
in Y000593, recovered from Antarctica after about
*50-thousand-year residence time, are similar to features
found in Nakhla, an observed fall collected shortly after
landing. We cannot exclude the possibility that the carbonrich
regions in both sets of features may be the product of
abiotic mechanisms; however, textural and compositional
similarities to features in terrestrial samples, which have
been interpreted as biogenic, imply the intriguing possibility
that the martian features were formed by biotic activity.
MysterX
It's actually somewhat annoying to those of us who already knew years ago, back in the 90s.
We cannot exclude the possibility that the carbonrich
regions in both sets of features may be the product of
abiotic mechanisms; however, textural and compositional
similarities to features in terrestrial samples, which have
been interpreted as biogenic, imply the intriguing possibility
that the martian features were formed by biotic activity.
JimOberg
This paper has just been cleared for publication, and an old, old friend of mine is one of the authors.
Aleister
Nice. So the conclusion is "maybe life, maybe other processes", which is a very good indicator of possible past life on Mars (at least as percentage points go).
gortex
Doesn't sound unequivocal to me .