Marc Kuchner and Sara Seager coined the term "carbon planet" in 2005 and investigated such planets following the suggestion of Katharina Lodders that Jupiter formed from a carbon-rich core. Prior investigations of planets with high carbon to oxygen ratios C/O include Fegley & Cameron 1987. Carbon planets could form if protoplanetary discs are carbon-rich and oxygen-poor. According to planetary science, it would develop differently from Earth, Mars and Venus, planets made up mostly of silicon–oxygen compounds. The theory has gained popularity and is now said by researchers such as Jade Bond to be built on reasonable ideas, specifically that different systems would have different ratios of carbon to oxygen, and that our own solar system's terrestrial planets actually slant toward being "oxygen planets". The unconfirmed extrasolar planet PSR J1719-1438 b, discovered on August 25, 2011, as well as the planet 55 Cancri e, could be such planets.
Such a planet would probably have an iron or steel-rich core like the known terrestrial planets. Surrounding that would be molten silicon carbide and titanium carbide. Above that, a layer of carbon in the form of graphite, possibly with a kilometers-thick substratum of diamond if there is sufficient pressure. During volcanic eruptions, it is possible that diamonds from the interior could come up to the surface, resulting in mountains of diamonds and silicon carbides. The surface would contain frozen or liquid hydrocarbons (e.g. tar and methane) and carbon monoxide. A weather cycle is theoretically possible on carbon planets with an atmosphere provided the average surface temperature is below 77°C.
However, carbon planets will probably be devoid of water, which cannot form since any oxygen delivered by comets or asteroids will react with the massive amounts of carbon on the surface. The atmosphere on a relatively cool carbon planet would consist of carbon dioxide or carbon monoxide with lots of carbon smog darkening the sky 
Carbon planets are predicted to be of similar diameter to silicate and water planets of the same mass, potentially making them difficult to distinguish. The equivalences of geologic features on Earth may also be present, but with different compositions. For instance, the rivers might consist of oils. If the temperature is low enough (below 350 K), then gases may be able to photochemically synthesize into long-chain hydrocarbons, which could rain down onto the surface.
NASA cancelled a mission, called TPF, which was to be an observatory much bigger than Hubble that would have been able to detect such planets. The spectra of carbon planets would lack water, but show the presence of carbonaceous substances, such as carbon monoxide.
Possible planets Edit
The pulsar PSR 1257+12 may possess carbon planets that formed from the disruption of a carbon-producing star. Carbon planets might also be located near the galactic core or globular clusters orbiting the galaxy, where stars have a higher carbon-to-oxygen ratio than the Sun. When old stars die, they spew out large quantities of carbon. As time passes and more and more generations of stars end, the concentration of carbon, and carbon planets, will increase.
In August 2011, Matthew Bailes and his team of experts from Swinburne University of Technology in Australia reported that the millisecond pulsar PSR J1719-1438 may have a binary companion star that has been crushed into a much smaller planet made largely of solid diamond. They deduced that a small companion planet must be orbiting the pulsar and causing a detectable gravitational pull. Further examination revealed that although the planet is relatively small (60,000 km diameter, or five times bigger than the Earth) its mass is slightly more than that of Jupiter. The high density of the planet gave the team a clue to its likely makeup of carbon and oxygen - and suggested the crystalline form of the elements. However, this "planet", is theorized to be the remains of an evaporated white dwarf companion, being only the remnant inner core. According to some definitions of planet, this would not qualify, as it formed as a star.
In October 2012, it was announced that 55 Cancri e showed evidence for being a carbon planet. It has eight times the mass of Earth, and twice the radius. Nikku Madhusudan, the Yale researcher, whose findings are due to be published in the Astrophysical Journal Letters says that the 3,900 °F planet is warmish — and is “covered in graphite and diamond rather than water and granite”. It orbits the star 55 Cancri once every 18 hours.
- ↑ Template:Cite arxiv
- ↑ Lodders, Katharina (2004). Jupiter Formed with More Tar than Ice. The Astrophysical Journal 611 (1).
- ↑ , Bruce, Jr. (April 1987)A vaporization model for iron/silicate fractionation in the Mercury protoplanet. Earth and Planetary Science Letters 82 (3–4): 207–222.
- ↑ (August 2009) The Diversity of Extrasolar Terrestrial Planets. Proceedings of the International Astronomical Union 5 (Symposium S265): 399–402.
- ↑ Musser, George. Earth-Like Planets May Be Made of Carbon. Scientific American. Retrieved 2013-01-03.
- ↑ "Kohlenstoffplaneten", SPACE Magazin April 2014 (page.35, in German)
- ↑ Template:Cite news
- ↑ Seager, Sara (2007). Mass-Radius Relationships for Solid Exoplanets. The Astrophysical Journal 669 (2).
- ↑ Carbon Planets - Space Art and Astronomical Illustrations. Novacelestia.com. Retrieved 2013-01-03.
- ↑ (26 August 2011)Solid diamond planet found. Australian Geographic.
- ↑ Lemonick, Michael (26 August 2011). Scientists Discover a Diamond as Big as a Planet. Time Magazine.
- ↑ Template:Cite news
- ↑ (December 2013)The atomic and molecular content of disks around very low-mass stars and brown dwarfs. The Astrophysical Journal 779 (2): 1–13. Template:Hdl.