Chapter 3 The Origin of Earth and the Solar System

Karla Panchuk

Figure 3.2.1 Periodic table showing the origin of elements in the Solar System, based on data by Jennifer Johnson at Ohio State University. The percentages of each element’s origin are represented by squares (out of a hundred). Elements above Plutonium are not included.

There are 92 naturally occurring elements in the universe (Figure 3.2.1), though hydrogen and helium are estimated to make up roughly 74% and 24% of all matter in the universe respectively (Figure 3.2.2 left). Most of this hydrogen and helium was produced within a few hundred seconds after the Big Bang. However, if we were to take an inventory of the elements that make up Earth, we would find that 99% of Earth’s mass comes from only eight elements: iron, oxygen, silicon, magnesium, nickel, calcium, aluminum, and sulfur (Figure 3.2.2 right); with the bulk of the Earth made up of just 4 elements (iron, oxygen, silicon, magnesium). Hydrogen and helium don’t even make the top eight on Earth. We know that the Big Bang produced hydrogen, helium, and lithium during what is called Big Bang nucleosynthesis, but where did the rest of the heavier elements come from and why does the elemental make up of Earth look so much different than that of the universe?

Figure 3.2.2 Elemental abundance of the 8 most common elements in the Milky Way Galaxy (left) and Earth (right).

The answer is that the other elements were made by stars. Sometimes stars are said to “burn” their fuel, but burning is not at all what is going on within stars. The burning that happens when wood in a campfire is turned to ash and smoke is a chemical reaction—heat causes the atoms that were in the wood and in the surrounding atmosphere to exchange partners. Atoms group in different ways, but the atoms themselves do not change. What stars do is change the atoms. The heat and pressure within stars cause smaller atoms to smash together and fuse into new, larger atoms. For example, when hydrogen atoms smash together and fuse, helium is formed (Figure 3.2.3). Large amounts of energy are released when some atoms fuse and that energy is what causes stars to shine.

It takes larger stars to make elements as heavy as iron and nickel (Figure 3.2.1). Our Sun is an average star; after it uses up its hydrogen fuel to make helium, and then some  of that helium is fused to make small amounts of beryllium, carbon, nitrogen, oxygen, and fluorine, it will be at the end of its life. It will stop making atoms

Figure 3.2.3 Nuclear Fusion. In a nuclear fusion reaction, lighter nuclei combine to produce a heavier nucleus. As shown, fusion of 3H and 2H to give 4He and a neutron releases an enormous amount of energy.

and will cool down and bloat until its middle reaches the orbit of Mars. In contrast, large stars end their lives in spectacular fashion, exploding as supernovae and casting off newly formed atoms—including the elements heavier than iron—into space. It took many generations of stars creating heavier elements and casting them into space before heavier elements were abundant enough to form planets like Earth.

Until recently, astronomers have only been able to see stars that already contain heavier elements in small amounts, but not the first-generation stars that started out before any of the heavier elements were produced. That changed in June of 2015 when it was announced that a distant galaxy called CR7 had been found that contained stars made only of hydrogen and helium. The galaxy is so far away that it shows us a view of the universe from only 800 million years after the big bang.[1]

 

 

 

Media Attributions


  1. Read more about the discovery of CR7 here: "Astronomers spot first-generation stars, made from big bang," (http://bit.ly/CR7galaxy)

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Dynamic Earth Through the Lens of Yellowstone Copyright © 2019 by Steven Earle is licensed under a Creative Commons Attribution 4.0 International License, except where otherwise noted.

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