We’re so used to thinking of our Sun as a solitary object that having two Suns in the sky inspires the imagination of artist and writer alike. But what about whole clusters of stars? Evidence is mounting that the Sun was actually born in such a cluster. That’s quite a jump from the era, not so long ago, when astronomers assumed stars like ours formed without companions, but cosmochemists like the wonderfully named Martin Bizzarro (University of Copenhagen) think they have the data to prove it.

So here’s the new notion: Most single stars like the Sun evolve in multiple systems, clusters of stars that also contain massive stars that burn their hydrogen and explode while the cluster is still producing young stars. If this is the case, then we should expect the early history of the surviving younger stars to be affected by the nearby fireworks. Bizzarro’s team studied short-lived isotopes like aluminum-26 (26Al) and iron-60 (60Fe) as found in meteorites to see whether stellar debris from such explosions left its mark.

The trick, as discussed in a fine summary by G. Jeffrey Taylor in Planetary Science Research Discoveries, is that these short-lived isotopes no longer exist in most meteorites, their half lives ranging from 0.1 to 100 million years. But they have left decay products including 60Ni (from the decay of 60Fe and 26Mg (from the decay of 26Al). Taylor’s article goes through the process of isotope measurement to determine the ratio of decay products to common isotopes.

This, in fact, is where Bizzarro’s work will receive the most scrutiny, since not all such studies agree. But working with terrestrial samples, Martian meteorites, chondritic meteorites and differentiated meteorites — from asteroids that melted at an early stage of protoplanetary development — the team comes up with its result. One thing stands out: The lack of 60Fe in the differentiated meteorites, which represent the oldest planetesimals to form in the Solar System. Let Taylor summarize:

Formation of the Sun might have involved the formation and rapid life span (only 4 million years) of a massive star, 30 times more massive than the Sun. Astronomical observations indicate that such stars pass through a stage in which they lose mass–up to an Earth mass per day!– rapidly by blowing it into space at a couple of thousand kilometers per hour. These stellar winds contain 26Al, but 60Fe is still ensconced in the interior. At some point the star blows up, sending the products of nuclear fusion into interstellar space, including 60Fe. Note the sequence here: 26Al leaves with the strong stellar winds, which possibly triggered the collapse of a cloud of gas and dust to form a new star, our Sun. There is good evidence that 26Al was uniformly distributed throughout the Solar System… The 60Fe comes about a million years later when the star explodes, but also after many planetesimals differentiated. They did not contain any 60Fe, but had their full complement of 26Al. In fact, they had enough 26Al to heat up internally and melt.

Was the exploding star that left its mark on these meteorites a Wolf-Rayet star? Such stars blow off heavier elements on their way to eventual supernova explosion. It’s an interesting hypothesis that it was just such a star that helped give birth to our Sun and its accompanying system. What should emerge next is a series of further analyses of such meteorites to pin down the data on 60Fe deficiency. These investigations are nowhere near conclusion, but we are at least developing a working theory on stellar formation that may depict our Sun’s earliest era.

The paper is Bizzarro et al., “Evidence for a later supernova injection of 60Fe into the protoplanetary disk,” Science, Vol. 316 (2007), pp. 1178-1181 (abstract). The Taylor article, called “The Sun’s Crowded Delivery Room,” is from the July 6, 2007 issue of Planetary Science Research Discoveries, available online.