It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
A conspicuous biomorphic ovoid structure has been discovered in the Nakhla martian meteorite, made of nanocrystalline iron-rich saponitic clay and amorphous material. The ovoid is indigenous to Nakhla and occurs within a late-formed amorphous mesostasis region of rhyolitic composition that is interstitial to two clinopyroxene grains with Al-rich rims, and contains acicular apatite crystals, olivine, sulfides, Ti-rich magnetite, and a new mineral of the rhoenite group. To infer the origin of the ovoid, a large set of analytical tools was employed, including scanning electron microscopy and backscattered electron imaging, wavelength-dispersive X-ray analysis, X-ray mapping, Raman spectroscopy, time-of-flight secondary ion mass spectrometry analysis, high-resolution transmission electron microscope imaging, and atomic force microscope topographic mapping. The concentric wall of the ovoid surrounds an originally hollow volume and exhibits internal layering of contrasting nanotextures but uniform chemical composition, and likely inherited its overall shape from a preexisting vesicle in the mesostasis glass. A final fibrous layer of Fe-rich phases blankets the interior surfaces of the ovoid wall structure. There is evidence that the parent rock of Nakhla has undergone a shock event from a nearby bolide impact that melted the rims of pyroxene and the interstitial matter and initiated an igneous hydrothermal system of rapidly cooling fluids, which were progressively mixed with fluids from the melted permafrost. Sharp temperature gradients were responsible for the crystallization of Al-rich clinopyroxene rims, rhoenite, acicular apatites, and the quenching of the mesostasis glass and the vesicle. During the formation of the ovoid structure, episodic fluid infiltration events resulted in the precipitation of saponite rinds around the vesicle walls, altered pyrrhotite to marcasite, and then isolated the ovoid wall structure from the rest of the system by depositing a layer of iron oxides/hydroxides. Carbonates, halite, and sulfates were deposited last within interstitial spaces and along fractures. Among three plausible competing hypotheses here, this particular abiotic scenario is considered to be the most reasonable explanation for the formation of the ovoid structure in Nakhla, and although compelling evidence for a biotic origin is lacking, it is evident that the martian subsurface contains niche environments where life could develop.
. We are getting closer.
of subsurface Niche environments where life could develop
Nakhla is a famous martian meteorite fallen in Egypt in 1911. It was the first meteorite reported from Egypt, the first one to suggest signs of aqueous processes on Mars, and the prototype for Nakhlite type of meteorites.
originally posted by: Aleister
a reply to: BGTM90
Would be interested in hearing from Jim Oberg, JadeStar, and others who have 'connections' within the space community on this. To me it looks like just a squished up rock, but then the spice is in the squish.
originally posted by: nOraKat
a reply to: BGTM90
They already determined this rock had fossilized life and bacteria.
ALH84001
news.bbc.co.uk...
The only contention is whether it was contamination from Earth.
I don't see how that is possible, being that it is fossilized and deep inside the rock.
In the article, “A Conspicuous Clay Ovoid in Nakhla: Evidence for Subsurface Hydrothermal Alteration on Mars with Implications for Astrobiology,” Elias Chatzitheodoridis, National Technical University of Athens, Greece, and Sarah Haigh and Ian Lyon, the University of Manchester, UK, describe the use of tools including electron microscopy, x-ray, and spectroscopy to analyze the ovoid structure. While the authors do not believe the formation of this structure involved biological materials, that is a possible hypothesis, and they note that evidence exists supporting the presence of niche environments in the Martian subsurface that could support life. - See more at: www.astrobio.net...
originally posted by: BGTM90
a reply to: JadeStar
JadeStar what are your thought on the Viking lander test that used radio-carbon to test for life? Where the results flawed? experiment it self flawed? Do you know of any scientific papers that disprove the experiment I can look at? I know that this is not proof of life as I stated in the op I just thought it was neat find worth looking at.
originally posted by: nOraKat
a reply to: BGTM90
They already determined this rock had fossilized life and bacteria.
ALH84001
news.bbc.co.uk...
The only contention is whether it was contamination from Earth.
I don't see how that is possible, being that it is fossilized and deep inside the rock.
A few years later, Swindle tried to do the poll again but couldn’t get enough respondents to form a representative sample. He thinks most people had made up their mind that ALH84001 did not carry biosignatures from Mars. But that doesn’t mean that sifting through the meteorite hasn’t been worth it. - See more at: www.astrobio.net...
originally posted by: nOraKat
a reply to: Baddogma
Yes, chemical tests in the 70's did confirm life.
It only takes a few 'official' scientist not to agree to put anything into contention.
Washington Post
"All the criticisms of our original paper got widely distributed, but when we did the work to prove the critics were wrong, it hardly made a ripple,"
originally posted by: DexterRiley
a reply to: nOraKat
That reminded me of an interview with NASA's David McKay at a 2010 Astrobiology conference. With respect to his team's 1996 work on the ALH84001 meteorite, and discovery of microbial fossils:
Washington Post
"All the criticisms of our original paper got widely distributed, but when we did the work to prove the critics were wrong, it hardly made a ripple,"
That seems to be the standard operating procedure these days:
1. Make a bold claim.
2. Endure harsh criticism.
3. Answer those criticisms.
4. Be ignored...
Dex
It’s improbable that Martian microbes deposited magnetite grains directly in the rock, so Thomas-Keprta and her colleagues have to argue that the magnetite formed outside of the rock and washed in. They also have to assume that Mars had a much stronger magnetic field in the past so that building an intracellular magnetic compass would be an advantage. - See more at: www.astrobio.net...
Except they did not do what they claimed. They did not really rebut the criticism. They attempted to rebut ONE criticism. Their new evidence is the magnetite is too pure to be natural. As far as no one caring, my link earlier directly addressed this. The reason no one is really caring is this ...
Very pure magnetite not found on Earth .. Therefore Mars can't either. It's a logical fallacy.
The researchers used six physical properties they refer to as the Magnetite Assay for Biogenicity (MAB) to compare all the magnetic material found in the ancient meteorite — using the MAB as a biosignature. A biosignature is a physical and/or chemical marker of life that does not occur through random processes or human intervention.
"No non-biologic magnetite population, whether produced by nature or in the laboratory, has ever met the MAB criteria," said Kathie Thomas-Keprta, an astrobiologist at NASA’s Johnson Space Center (JSC) in Houston and the lead researcher on the study. "This means that one-quarter of the magnetite crystals embedded in the carbonates in Martian meteorite ALH84001 require the intervention of biology to explain their presence."
- See more at: www.astrobio.net...
It’s improbable that Martian microbes deposited magnetite grains directly in the rock, so Thomas-Keprta and her colleagues have to argue that the magnetite formed outside of the rock and washed in...
They also have to assume that Mars had a much stronger magnetic field in the past so that building an intracellular magnetic compass would be an advantage.
The fact that Mars Global Surveyor data suggest that early Mars had a magnetic field is consistent with a reason why Mars would have magnetotactic bacteria. "Our best working hypothesis is that early Mars supported the evolution of bacteria that share several traits with magnetotactic bacteria on Earth, most notably the MV-1 group," said Simon Clemett, a coauthor of the paper at Johnson. - See more at: www.astrobio.net...
Treiman and others argue that the magnetite could be explained more easily with some sort of shock event that heated the carbonate enough to allow magnetite grains to form. Thomas-Keprta says these abiotic models are fatally flawed. The problem is in the cooling time. If the rock cools too fast, the magnetite ends up full of impurities. Too slow and the surrounding carbonate becomes too uniform.
- See more at: www.astrobio.net...