Extraterrestrial Dust Found in the Antarctic

A new family of extraterrestrial particles has been identified for the first time in Central Antarctica.

Discovered by researchers from the Center for Nuclear Spectrometry and Mass Spectrometry (CSNSM), attached to the Institut national de physique nucléaire et de physique des particules, the micrometeorites, which are remarkably well preserved, are made up of organic matter containing small assemblages of minerals from the coldest and most remote regions of the Solar System.

The team discovered two micrometeorites in ultra-clean snow near the French-Italian camp, “Concordia,” established in 1955 to 1970 and located in the central region of the Antarctic continent, one of the most remote places in the world.

The larger object is 85% carbon -the essential ingredient for the organic chemistry needed for life, and the smaller one is 48% carbon. Both contain higher-than-expected amounts of deuterium, a rare form of hydrogen, in a concentration 30 times higher than is usually found mixed with hydrogen on Earth – all elements common in interstellar clouds of dust in deep space, far more ancient than the Sun.

When the team used a microscope to examine the dust particles, says the study, they also found tiny crystals which could only have been “condensed or processed at close distances from the young sun.”

Comets are made up of a mixture of icy materials and dust. Occasionally, some of them enter the inner Solar System. When they pass near the Sun, the rise in temperature causes massive sublimation of the icy materials, leading to an ejection of a mixture of gases and cometary grains into interplanetary space. Some dust grains may cross Earth’s orbit as they drift towards the Sun, where most of them finish their journey. It is probably some of these cometary grains that the CSNS scientists discovered in Antarctica.

Until now, only the US Stardust space mission had enabled international teams to carry out mineralogical and geochemical analysis of cometary grains. The micrometeorites discovered at Concordia show numerous similarities to the samples from the Stardust mission.

For the first time, they allow scientists to study extremely well preserved assemblages of minerals and organic material that were present beyond Jupiter’s current orbit at the time when the Sun and the planets were being formed. Their chemical and isotopic composition should make it possible to comprehend the physical and chemical processes at work inside the disk of gas and dust that surrounded the early Sun 4.5 billion years ago.

via CNRS

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