Orgueil (meteorite)

Orgueil (meteorite)
Orgueil
no image
Type Chondrite
Class Carbonaceous chondrite
Group CI1
Country France
Region Midi-Pyrénées
Coordinates 43°53′N 1°23′E / 43.883°N 1.383°E / 43.883; 1.383Coordinates: 43°53′N 1°23′E / 43.883°N 1.383°E / 43.883; 1.383[1]
Observed fall Yes
Fall date May 14, 1864
TKW 14 kg
Original painting of an individual fragment from the Orgueil meteorite
Original painting of an individual fragment from the Orgueil meteorite

Orgueil is a scientifically important carbonaceous chondrite meteorite that fell in southwestern France in 1864.

Contents

History

It fell on May 14, 1864, a few minutes after 8 pm, near Orgueil in southern France. About 20 stones fell over an area of several square miles. A specimen of the meteorite was analyzed that same year by François Stanislaus Clöez, professor of chemistry at the Musée d'Histoire Naturelle, who focused on the organic matter found in this meteorite. He wrote that it contained carbon, hydrogen, and oxygen, and its composition was very similar to peat from the Somme valley or to the lignite of Ringkohl near Kassel. An intense scientific discussion ensued, continuing into the 1870s, as to whether the organic matter might have a biological origin.[2]

Composition and classification

Orgueil is one of five known meteorites belonging to the CI chondrite group (see meteorites classification), this being the largest (14 kg). This group is remarkable for having a composition that is essentially identical to that of the sun, excluding gaseous elements like hydrogen and helium.

Because of its extraordinarily primitive composition and relatively large mass, Orgueil is one of the most-studied meteorites. One notable discovery in Orgueil was a high concentration of isotopically anomalous xenon called "xenon-HL". The carrier of this gas is extremely fine-grained diamond dust that is older than the solar system itself, known as presolar grains.

In 1962, Nagy et al. announced the discovery of 'organised elements' embedded in the Orgueil meteorite that were purportedly biological structures of extraterrestrial origin. These elements were subsequently shown to be either pollen (including that of ragwort) and fungal spores (Fitch & Anders, 1963) that had contaminated the sample, or crystals of the mineral olivine.

The hoax

In 1965, a fragment of the Orgueil meteorite, kept in a sealed glass jar in Montauban since its discovery, was found to have a seed capsule embedded in it, whilst the original glassy layer on the outside remained apparently undisturbed. Despite great initial excitement, the seed capsule was shown to be that of a European rush, glued into the fragment and camouflaged using coal dust. The outer "fusion layer" was in fact glue. Whilst the perpetrator is unknown, it is thought that the hoax was aimed at influencing 19th century debate on spontaneous generation by demonstrating the transformation of inorganic to biological matter.

Claim of fossils

Richard B. Hoover of NASA has claimed that the Orgueil meteorite contains fossils, some of which are similar to known terrestrial species.[3] Hoover has previously claimed the existence of fossils in the Murchison meteorite. However, NASA has formally distanced itself from Hoover's claims and his lack of expert peer-reviews.[4]

References

  1. ^ Meteoritical Bulletin Database: Orgueil
  2. ^ Burke, John G. (1986). Cosmic Debris: Meteorites in History. Berkeley and Los Angeles, California: University of California Press. pp. 168–169. ISBN 0-520-05651-5. 
  3. ^ Hoover, Richard B. (2011). "Fossils of Cyanobacteria in CI1 Carbonaceous Meteorites: Implications to Life on Comets, Europa, and Enceladus". Journal of Cosmology 13. http://journalofcosmology.com/Life100.html. Retrieved 2011-03-05. 
  4. ^ "NASA shoots down alien fossil claims". ABC News. 7 March 2011. http://www.abc.net.au/news/stories/2011/03/08/3157645.htm. Retrieved 2011-03-07. 
  • Nagy B, Claus G, Hennessy DJ (1962) Organic Particles Embedded in Minerals in Orgueil and Ivuna Carbonaceous Chondrites. Nature 193 (4821) p. 1129
  • Fitch FW, Anders E (1963) Organized Element - Possible Identification in Orgueil Meteorite. Science 140 (357) p. 1097
  • Gilmour I, Wright I, Wright J 'Origins of Earth and Life', The Open University, 1997, ISBN 0-7492-8182-0

External links


Wikimedia Foundation. 2010.

Игры ⚽ Нужно решить контрольную?

Look at other dictionaries:

  • Orgueil meteorite — ▪ astronomy        meteorite that fell on the village of Orgueil, near Toulouse, France, in May 1864 and that is often used to infer the relative proportions of elements in the solar system (cosmic abundances). It is classified as a carbonaceous… …   Universalium

  • Météorite d'Orgueil — Caractéristiques Type Chondrite carbonée Groupe CI1 …   Wikipédia en Français

  • Orgueil — Orgueil …   Wikipedia

  • Orgueil (tarn-et-garonne) —  Pour l’article homonyme, voir Orgueil.  Orgueil …   Wikipédia en Français

  • Meteorite — Météorite Pour les articles homonymes, voir Météorite (homonymie). Météorite de Willamette. Une météorite est un corps matériel extraterrestre …   Wikipédia en Français

  • Orgueil (Tarn-et-Garonne) —  Pour l’article homonyme, voir Orgueil.  43° 54′ 19″ N 1° 24′ 43″ E …   Wikipédia en Français

  • Meteorite — This article is about debris from space that survives impact with the ground. For other uses of Meteor and Meteors , see Meteor (disambiguation). For popular applications, see Falling star. For the fictional superhero in the Marvel Comics… …   Wikipedia

  • Météorite — Pour les articles homonymes, voir Météorite (homonymie). Météorite de Willamette. Une météorite est un corps solide (rocheux et/ou ferreux) du milieu …   Wikipédia en Français

  • Meteorite fall — Witnessed Bolide Meteorite falls, also called observed falls, are those meteorites that were witnessed by people or automated devices as they moved through the atmosphere or hit the Earth, and were subsequently collected. All other meteorites are …   Wikipedia

  • Allende meteorite — Meteorite Name= Allende Image caption= Allende fragment Image width= 180px Type= Chondrite Class= Carbonaceous chondrite Group= CV3 Structural classification= Composition= 23.85% total iron Shock= S1 Weathering= Country= Mexico Region= Pueblito… …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”