[meteorite-list] Ultracarbonaceous micrometeorites
From: Whitney Riner <majesticmeteorites_at_meteoritecentral.com>
Date: Tue, 11 May 2010 12:39:56 -0400 Message-ID: <AANLkTin9sxU0z8Cy96bhBVpIH_cTpR1SVzlPz7EJgozJ_at_mail.gmail.com> A new study of (likely) cometary dust is published in Science: http://tinyurl.com/39w6wyt http://tinyurl.com/33dcy97 According to the scientists, the ultracarbonaceous micrometeorites, which are about 0.1 millimetre (mm) in size and contain between 50% to 80% carbonaceous material, are unique because no other laboratory has meteorites of this kind in its collection. Thanks to the results of this exciting research, further investigations have been initiated involving the CSNSM, the University of Lille 1, the Ecole Normale Sup?rieure, Paris, and the French Natural History Museum. In their analyses, the CSNSM team used an ion microprobe to show that the micrometeorites' hydrogen isotopic composition has a very high deuterium/hydrogen (D/H) ratio. 'Primitive interplanetary dust is expected to contain the earliest solar system components, including minerals and organic matter,' the authors write. 'We have recovered, from central Antarctic snow, ultracarbonaceous micrometeorites whose organic matter contains extreme deuterium excesses (10 to 30 times terrestrial values), extending over hundreds of square micrometres.' The results showed that the particles most likely stem from comets, which are relatively small bodies in the Solar System. Comets' nuclei are collections of ice, dust and tiny rocky particles. As comets draw closer to the Sun, rising temperatures trigger the massive sublimation of the icy materials. This results in an ejection of a mixture of gases and cometary grains into interplanetary space. Some dust grains may cross Earth's orbit as they move towards the Sun, and the researchers speculate that it may be some of these cometary grains that they found in central Antarctica. In their paper, the authors note that so far, only the US Stardust space mission has provided researchers worldwide with the opportunity to perform mineralogical and geochemical analyses of cometary grains. The specks of dust discovered at Concordia are similar to samples obtained from the Stardust mission. 'The masses of the particles range from a few tenths of a microgram to a few micrograms, exceeding by more than an order of magnitude those of the dust fragments from comet 81P/Wild 2 returned by the Stardust mission,' the authors write. Received on Tue 11 May 2010 12:39:56 PM PDT |
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