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Murchison meteorite


Murchison meteorite

A Murchison meteorite specimen at the National Museum of Natural History (Washington)
Type Chondrite
Class Carbonaceous chondrite
Group CM2
Composition 22.13% total iron, 12% water
Shock stage S1-2
Country Australia
Region Victoria
Coordinates [1]
Observed fall Yes
Fall date 28 September 1969
TKW 100 kg

Pair of grains from the Murchison meteorite

The Murchison meteorite is named after organic compounds.


  • History 1
  • Classification and composition 2
  • Organic compounds 3
    • Nucleobases 3.1
  • See also 4
  • References 5
  • External links 6


On 28 September 1969 at about 10:58 local time, near the town of Murchison, Victoria, in Australia, a bright fireball was observed to separate into three fragments before disappearing,[1] leaving a cloud of smoke. About 30 seconds later, a tremor was heard. Many fragments were found over an area larger than 13 km², with individual mass up to 7 kg; one, weighing 680 g, broke through a roof and fell in hay.[1] The total collected mass exceeds 100 kg.

Classification and composition

The meteorite belongs to the CM group of carbonaceous chondrites (see meteorite classification). Like most CM chondrites, Murchison is petrologic type 2, which means that it experienced extensive alteration by water-rich fluids on its parent body[2] before falling to Earth. CM chondrites, together with the CI group, are rich in carbon and are among the most chemically primitive meteorites.[3] Like other CM chondrites, Murchison contains abundant CAIs. Over 15 amino acids (some of the basic components of life) have been rapidly identified in the meteorite,[4] and more later. All the amino acids found in the Murchison meteorite have been synthesized in laboratory experiments by the action of electric discharge on a mixture of methane, nitrogen, and water with traces of ammonia.[4]

Organic compounds

Fragment of the Murchison meteorite (at right) and isolated individual particles (shown in the test tube).

Murchison contains common amino acids such as glycine, alanine and glutamic acid as well as unusual ones like isovaline and pseudoleucine.[5] A complex mixture of alkanes was isolated as well, similar to that found in the Miller–Urey experiment. Serine and threonine, usually considered to be earthly contaminants, were conspicuously absent in the samples. A specific family of amino acids called diamino acids was identified in the Murchison meteorite as well.[6]

The initial report stated that the amino acids were polyols by 2001.[12]

Compound class[13] Concentration (ppm)
Amino acids 17-60
Aliphatic hydrocarbons >35
Aromatic hydrocarbons 3319
Fullerenes >100
Carboxylic acids >300
Hydrocarboxylic acids 15
Purines and pyrimidines 1.3
Alcohols 11
Sulphonic acids 68
Phosphonic acids 2

Although the meteorite contained a mixture of left-handed and right-handed amino acids, most amino acids used by living organisms are left-handed in chirality, and most sugars used are right-handed. A team of chemists in Sweden demonstrated in 2005 that this homochirality could have been triggered or catalyzed, by the action of a left-handed amino acid such as proline.[14]

Several lines of evidence indicate that the interior portions of well-preserved fragments from Murchison are pristine. A 2010 study using high resolution analytical tools including

 This article incorporates public domain material from websites or documents of the National Aeronautics and Space Administration.

  • Rosenthal, Anne M. (12 February 2003). "Murchison's Amino Acids: Tainted Evidence?". Astrobiology Magazine. 
  • Matson, John (15 February 2010). "Meteorite That Fell in 1969 Still Revealing Secrets of the Early Solar System". Scientific American. 

External links

  1. ^ a b c MurchisonMeteoritical Bulletin Database:
  2. ^ Airieau, S. A.; Farquhar, J.; Thiemens, M. H.; Leshin, L. A.; Bao, H.; Young, E. (2005). "Planetesimal sulfate and aqueous alteration in CM and CI carbonaceous chondrites". Geochimica et Cosmochimica Acta 69 (16): 4167–4172.  
  3. ^ "Planetary Science Research Discoveries: Glossary". 
  4. ^ a b Wolman, Yecheskel; Haverland, William J.; Miller, Stanley L. (April 1972). "Nonprotein Amino Acids from Spark Discharges and Their Comparison with the Murchison Meteorite Amino Acids" (PDF). Proc. Nat. Acad. Sci. USA 69 (4): 809–811.  
  5. ^ Kvenvolden, Keith A.; Lawless, James; Pering, Katherine; Peterson, Etta; Flores, Jose; Ponnamperuma, Cyril; Kaplan, Isaac R.; Moore, Carleton (1970). "Evidence for extraterrestrial amino-acids and hydrocarbons in the Murchison meteorite".  
  6. ^ Meierhenrich, Uwe J.; Hendrik Bredehöft, Jan; Jessberger, Elmar K.; Thiemann, Wolfram H.-P. (2004). "Identification of diamino acids in the Murchison meteorite".  
  7. ^ Engel, Michael H.; Nagy, Bartholomew (29 April 1982). "Distribution and enantiomeric composition of amino acids in the Murchison meteorite".  
  8. ^ Bada, Jeffrey L.; Cronin, John R.; Ho, Ming-Shan; Kvenvolden, Keith A.; Lawless, James G.; Miller, Stanley L.; Oro, J.; Steinberg, Spencer (10 February 1983). "On the reported optical activity of amino acids in the Murchison meteorite".  
  9. ^ Cronin, John R.; Pizzarello, S. (1997). "Enantiomeric excesses in meteoritic amino acids". Science 275 (5302): 951–955.  
  10. ^ Engel, Michael H.; Macko, S. A. (1 September 1997). "Isotopic evidence for extraterrestrial non-racemic amino acids in the Murchison meteorite".  
  11. ^ Pizzarello, Sandra; Cronin, JR (1998). "Alanine enantiomers in the Murchison meteorite". Nature 394 (6690): 236.  
  12. ^ Cooper, George; Kimmich, Novelle; Belisle, Warren; Sarinana, Josh; Brabham, Katrina; Garrel, Laurence (20 December 2001). "Carbonaceous meteorites as a source of sugar-related organic compounds for the early Earth".  
  13. ^ Machalek, Pavel (17 February 2007). "Organic Molecules in Comets and Meteorites and Life on Earth" (PDF). Department of Physics and Astronomy (Johns Hopkins University). Retrieved 2008-10-07. 
  14. ^ Córdova, Armando; Engqvist, Magnus; Ibrahem, Ismail; Casas, Jesús; Sundén, Henrik (2005). "Plausible origins of homochirality in the amino acid catalyzed neogenesis of carbohydrates".  
  15. ^ Walton, Doreen (15 February 2010). "Space rock contains organic molecular feast". BBC News. Retrieved 2010-02-15. 
  16. ^ Schmitt-Kopplin, Philippe; Gabelica, Zelimir; Gougeon, Régis D.; Fekete, Agnes; Kanawati, Basem; Harir, Mourad; Gebefuegi, Istvan; Eckel, Gerhard; Hertkorn, Norbert (16 February 2010). "High molecular diversity of extraterrestrial organic matter in Murchison meteorite revealed 40 years after its fall" (PDF).  
  17. ^ Matson, John (15 February 2010). "Meteorite That Fell in 1969 Still Revealing Secrets of the Early Solar System". Scientific American. Retrieved 2010-02-15. 
  18. ^ Martins, Zita; Botta, Oliver; Fogel, Marilyn L.; Sephton, Mark A.; Glavin, Daniel P.; Watson, Jonathan S.; Dworkin, Jason P.; Schwartz, Alan W.; Ehrenfreund, Pascale (20 March 2008). "Extraterrestrial nucleobases in the Murchison meteorite" (PDF). Earth and Planetary Science Letters.  


See also

Measured life's origin.[18]



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