We know it, theformed about 4.5 billion years ago, from the protoplanetary disk that surrounded our young . The and the dust that composes it gradually accreted to each other, forming larger and larger bodies: first planetesimals, then protoplanets, and finally planets. Not all rocks fuse, as evidenced by the which houses many fragments and small rocks. To trace the exact course of this process, the researchers analyze nearly intact primitive remains of the early solar system, as demonstrated by a study recently published in the journal .
Fossils from the birth of the solar system
Somecame crashing down on Earth only a few thousand years after its formation, and then contains precious traces of our past. “Previous scientific studies have shown that asteroids in the solar system have remained relatively unchanged since their formation billions of years ago”, first author of the study and researcher at ETH Zurich. “So they are an archive, in which the conditions of the early solar system are preserved. »
A. Hunt and his team thus analyzedhaving landed on Earth nearly 4 billion years ago. Specifically, these are samples of 18 of iron, extracted from the metallic cores of asteroids. They then dissolved each sample, with the aim of establishing isotopic abundances for the I’ and the . Indeed, during the first million years of the solar system, these asteroid nuclei were heated by radioactive decay, notably creating a specific isotope of silver from palladium, which then accumulated during cooling. . By measuring its ratio between the other elements, it is possible to know when this cooling started, but also at what it happened. And the results showed, consistent with previous studies, rapid cooling due to numerous collisions: they exposed the hearts of asteroids to the freezing vacuum of space. But what the study brings new is the moment when this cooling occurred.
“Our additional measurements of platinum isotope abundances allowed us to correct silver isotope measurements for distortions caused bycosmic samples in space. So we were able to date the timing of the collisions more accurately than ever before.explains A. Hunt. And to our surprise, all of the asteroid nuclei we examined were exposed almost simultaneously, between 7.8 and 11.7 million years after the formation of the solar system. » Indeed, taking platinum into account has enabled researchers to quantify the influence of which can modify the ratio of silver isotopes: they have thus drastically reduced their uncertainties.
Chaotic beginnings for the solar system
Recall that theis more than 4.5 billion years old: thus, a range between 7.8 and 11.7 million years represents only a short moment in its history. A particularly unstable moment, according to the researchers. “Everything seems to have collapsed at that momentasks A. Hunt. And we wanted to know why. ». Several hypotheses could explain this period: these are who decided. “The theory that best explained this first energetic phase of the solar system indicated that it was mainly caused by the dissipation of the solar nebula”says Maria Schönbächler, co-author of the study and professor of cosmochemistry at ETH Zurich. “This solar nebula is the remnant of gas that was left behind by the cosmic from which was born the . For a few million years it still revolved around the young Sun until it was swept away by the and solar radiationShe adds.
In fact, stars are formed bygravity of a gas cloud called a nebula. But not everything collapses: a part of it remains which gravitates around the recently formed core, which will then become the famous protoplanetary disk. To this disc was particularly dense: but as the Sun lit up, more and more accompanied by write-offs were issued. These winds “blew” a large part of the dust isolated from the disc, making it less and less dense and reducing the drag of the objects that compose it. All the rocky bodies would then have accelerated, and would then have started the famous unstable phase. “Our work illustrates how improvements in laboratory measurement techniques allow us to infer key processes that took place in the early solar system – such as when the solar nebula was likely to disappear. Planets like Earth were still being born at this time. Ultimately, this can help us better understand how our own planets came into existence, but also give us insight into others outside our solar system.concludes Schönbächler.
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