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Meteorite may carry organic Martian cargo.


Meteorite meteorite, meteor that survives the intense heat of atmospheric friction and reaches the earth's surface. Because of the destructive effects of this friction, only the very largest meteors become meteorites.  may carry organic Martian cargo

Amidst major ifs, a trio of space scientists reports that a meteorite discovered 10 years ago in Antartica may have come from Mars bearing a smidgen of the kind of carbon-containing material thought necessary for the emergence of life. Though falling short of proving the presence of such organic material on Mars, the new evidence resurrects that possibility, which experiments during the 1976 Viking mission to Mars had all but killed.

"We want to draw attention to a very interesting meteorite with strange, unusual and unexpected things in it," says Ian P. Wright, leader of the research team at the Open University in Milton Keynes, England. In their analysis of a 5-milligram sample of the roughly 8-kilogram, football-sized meteorite designated EETA EETA Electronic Engineering Times - Asia  79001 -- which many scientists suspect originated on Mars -- the researchers found two distinct reservoirs of carbon-containing material. One consists of the mineral calcium carbonate calcium carbonate, CaCO3, white chemical compound that is the most common nonsiliceous mineral. It occurs in two crystal forms: calcite, which is hexagonal, and aragonite, which is rhombohedral.  and the other appears to contain still-unspecified organic (nonmineral) compounds.

The researchers discovered the two pools of carbon by measuring the ratio of stable carbon isotopes -- carbon-13 to carbon-12 -- in the meteorite sample as combustion liberated these elements. Various natural processes, such as mineralization Mineralization
The process by which the body uses minerals to build bone structure.

Mentioned in: Rickets

mineralization,
n the bioprecipitation of an inorganic substance.
 or metabolism, produce carbon-containing products with somewhat characteristic isotope ratios. Heating the meteorite sample in stepwise stepwise

incremental; additional information is added at each step.


stepwise multiple regression
used when a large number of possible explanatory variables are available and there is difficulty interpreting the partial regression
 fashion burns off the mineral and organic carbon components at different times, yielding carbon dioxide carbon dioxide, chemical compound, CO2, a colorless, odorless, tasteless gas that is about one and one-half times as dense as air under ordinary conditions of temperature and pressure.  for isotope analysis, Wright says.

Using a mass spectrometer, he and his co-workers found that most of the carbon in the meteorite sample came off between the temperatures of 450[deg.]C and 700[deg.]C and that this fraction was enriched in the heavier carbon-13 isotope. Wright reads this as a sign that the heat decomposed de·com·pose  
v. de·com·posed, de·com·pos·ing, de·com·pos·es

v.tr.
1. To separate into components or basic elements.

2. To cause to rot.

v.intr.
1.
 carbon-containing minerals, or carbonates. The mass spectrometer also detected carbon coming from a smaller sample component that burned at lower temperatures and that was depleted de·plete  
tr.v. de·plet·ed, de·plet·ing, de·pletes
To decrease the fullness of; use up or empty out.



[Latin d
 in carbon-13. "This was from the combustion of organic materials," the researchers claim in the July 20 NATURE.

"The work has demonstrated that there is an organic component there," comments space scientist James L. Gooding of NASA's Johnson Space Center in Houston. But, he says, the big question remains: Did the organic carbon come from Mars?

Although Wright says "the evidence is stacked solidly for a Martian origin" of EETA 79001 and a handful of other meteorites Meteorites
See also astronomy.

aerolithology

the science of aerolites, whether meteoric stones or meteorites. Also called aerolitics.

astrolithology

the study of meteorites. Also called meteoritics.
 of Mars-like composition (SN: 10/18/86, p.246), some doubt will linger in the absence of independent confirming evidence from, say, a Mars rock-collecting trip.

Even granting the Martian origin of such meteorites -- as many scientists do -- the organic matter Wright detected still could derive from whatever cosmic cue ball -- a comet, for example -- jolted the Martian surface and sent EETA 79001 on its way to Earth. Geochemist John F. Kerridge of the University of California, Los Angeles UCLA comprises the College of Letters and Science (the primary undergraduate college), seven professional schools, and five professional Health Science schools. Since 2001, UCLA has enrolled over 33,000 total students, and that number is steadily rising. , leans against this interpretation, noting that the sample's carbon ratios don't seem to reflect a cometary source. Instead, he says, they could indicate contamination with organic carbon from Earth.

Wright argues that the meticulous handling of EETA 79001 "militates against a wholly terrestrial origin" of the organic matter. As for the Viking Lander's failure to detect organic carbon on Mars, Wright notes that it examined only surface material and not samples liek EETA 79001, which presumably pre·sum·a·ble  
adj.
That can be presumed or taken for granted; reasonable as a supposition: presumable causes of the disaster.
 represent deeper Martian crust.

"There is a remote chance that we're looking at some [extraterrestrial] fossil life form," Wright Cautiously told SCIENCE NEWS.

Kerridge think's it's too early to reconsider the life-on-Mars issue. "The implications [of the British study] really are quite considerable, particularly in light of the Viking data," he says. "But I'd like some other line of evidence to support this before saying there really is organic matter on Mars."
COPYRIGHT 1989 Science Service, Inc.
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 1989, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Article Details
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Author:Amato, I.
Publication:Science News
Date:Jul 22, 1989
Words:612
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