The first chemical elements appeared during the Big Bang, about 13.8 billion years ago. During the first three minutes, temperature and density conditions allowed the formation of light nuclei:
Hydrogen (\(^1H\)): 75% of baryonic matter
Deuterium (\(^2H\)): traces
Helium-4 (\(^4He\)): 25% of baryonic matter
Lithium-7 (\(^7Li\)): 10-9 of hydrogen abundance
These proportions, predicted by primordial nucleosynthesis theory, were confirmed by observations of the cosmic microwave background by the COBE (1989-1993) and Planck (2009-2013) satellites.
Stellar Nucleosynthesis: Alchemy of the Stars
Stars are the main sites for producing elements heavier than lithium. This process, called stellar nucleosynthesis, was theorized by Fred Hoyle (1915-2001), William Fowler (1911-1995), Geoffrey Burbidge (1925-2010) and Margaret Burbidge (1919-2020) in their foundational 1957 paper.
In the cores of stars, nuclear fusion reactions gradually transform light elements into heavier ones:
Proton-proton chain (solar-type stars): 4 \(^1H\) → \(^4He\) + energy
CNO cycle (more massive stars): catalyzed by carbon, nitrogen and oxygen
Duration: A few hundred to thousand years (e.g.: 600 years for a 20 M☉ star).
Key products: \(^{20}Ne\), \(^{24}Mg\), \(^{28}Si\), \(^{32}S\), and traces of \(^{26}Al\) (radioactive).
Supernovae: Factories of Heavy Elements
Elements heavier than iron (atomic number 26) can only be synthesized under extreme conditions:
r process: in core-collapse supernovae (e.g.: SN 1987A)
s process: in AGB stars (e.g.: stars like Aldebaran)
Explosive fusion: during the core collapse of a supernova (e.g.: formation of gold and platinum)
A typical supernova like SN 1054 can disperse several solar masses of newly formed elements into interstellar space, enriching the medium for future generations of stars and planets.
Observational Evidence: Spectroscopy and Meteorites
Spectral analysis of starlight reveals the presence of chemical elements through their characteristic absorption lines. For example:
Hydrogen lines (Balmer series) at 410, 434, 486 and 656 nm
Ionized calcium lines (H and K) at 393 and 397 nm
Neutral iron lines around 500 nm
Carbonaceous meteorites, like the Murchison meteorite, contain presolar grains whose isotopic composition reveals their specific stellar origin.
Main processes of chemical element formation and their locations
Understanding these processes has major implications:
Origin of elements essential to life (C, N, O, P, S)
Formation of terrestrial planets and their composition
Dating of cosmic events via radioactive isotopes (e.g.: \(^{26}Al\) for dating young stars)
Understanding the chemical evolution of the galaxy (increasing metallicity)
As Carl Sagan (1934-1996) pointed out: "We are all star stuff," reminding us that the atoms making up our bodies were forged in the hearts of stars billions of years ago.