Our golden Sun
Working one night in 1859, chemists Robert Bunsen and Gustav Kirchhoff saw a fire raging in the town of Mannheim, Germany, about 10 miles (16 km) from their Heidelberg University laboratory. They rolled their newly improved spectroscope (a device they invented that breaks light into its component wavelengths, which allows chemical elements to be identified) to the window and quickly detected the elements barium and strontium within the bright glow given off by the flames. Bunsen wrote that the “same mode of analysis must be applicable to the atmospheres of the Sun and the bright stars.” The second half of the 19th century saw an explosion of discoveries using this powerful tool.
During the total solar eclipse on August 18, 1868, several astronomers using spectroscopy detected a new element — and, it turned out, the universe’s second most abundant one — in the Sun: helium. Carbon, nitrogen, iron, and all the heavier elements of the periodic table — including gold — were eventually identified in a gaseous state in the Sun’s atmosphere.
In the late 18th and early 19th centuries, rock and mineral collecting became the science of geology. Men and women such as Charles Lyell, James Hutton, and the great fossil collector Mary Anning, discoverer of the first Ichthyosaurus skeleton, clearly demonstrated that Earth was far older than the 6,000 years suggested by many contemporary theologians. Lyell and Hutton said Earth must be millions or even billions of years old. If this was true, what could keep the Sun and stars shining for such an incredibly long time?
German physicist Julius Robert Mayer strongly favored the meteoric theory of solar heat. He had calculated that, lacking an external source of energy, the Sun could shine for only 5,000 years. In 1848, he suggested the Sun was fueled by billions of meteorites raining down on it, which provided its energy. This material also, supposedly, would have brought heavy elements to our star.