Grains that predate the solar system

In recent years, a new source of information about stellar nucleosynthesis and the history of the elements between their ejection from stars and their incorporation into the solar system has become available. This source is the tiny dust grains that condensed from gas ejected from stars at the end of their lives and that survived unaltered to be incorporated into solar system materials. These presolar grains (Fig. 5.1) originated before the solar system formed and were part of the raw materials for the Sun, the planets, and other solar-system objects. They survived the collapse of the Sun s parent molecular cloud and the formation of the accretion disk and were incorporated essentially unchanged into the parent bodies of the chondritic meteorites. They are found in the fine-grained matrix of the least metamorphosed chondrites and in interplanetary dust particles (IDPs), materials that were not processed by high-temperature events in the solar system. 

There are two types of presolar grains. Circumstellar condensates condensed from hot gas ejected from dying stars in the immediate vicinity of their parent stars. They are also sometimes called stardust. Circumstellar condensates give snapshots of the life histories of the stars from which they formed. Although the stars themselves no longer exist, the 

Examples of presolar silicon carbide from the Orgueil meteorite (a, b, c) and hibonite from the Semarkona meteorite (d). These are relatively large for presolar grains. Note the geometric outlines of crystal faces in images (a) and (d). Image (d) is reproduced by permission of the AAS. 

The potential of presolar grains to provide information about nucleosynthesis, stellar evolution, galactic chemical evolution, interstellar processes, and nebular processes is only beginning to be tapped. But as new instrumentation is developed, more and more of the information that they carry will be extracted. 

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