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Nemesis (hypothetical star)

Hypothetical star orbiting the Sun, supposedly responsible for extinction events

  • 7 min read
  • 4 chapters

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Through Sun, Light-year and Extinction event

More recent theories suggest that other forces, like close passage of other stars, or the angular effect of the galactic gravity plane working against the outer solar orbital plane (Shiva hypothesis), may be the cause of orbital perturbations of some outer Solar System objects. In 2010, researchers found evidence in the fossil record confirming the extinction event periodicity originally identified in 1984, but at a higher confidence level and over a time period nearly twice as long. However, in 2011, researchers analyzed the ages of known craters on Earth's surface and found strong evidence against periodic impacts, concluding that the earlier findings based on small samples were statistical artifacts. The Infrared Astronomical Satellite (IRAS) failed to discover Nemesis in the 1980s. The 2MASS astronomical survey, which ran from 1997 to 2001, failed to detect an additional star or brown dwarf in the Solar System.

Using newer and more powerful infrared telescope technology able to detect brown dwarfs with temperatures as low as 150 K, out to a distance of 10 light-years from the Sun, the Wide-field Infrared Survey Explorer (WISE survey) has not detected Nemesis. In 2011, David Morrison, a senior scientist at NASA known for his work in risk assessment of near Earth objects, has written that there is no confidence in the existence of an object like Nemesis, since it should have been detected in infrared sky surveys.

Claimed periodicity of mass extinctions

In 1977, Alfred G. Fischer and Michael A. Arthur first suggested a periodicity in life proliferation in pelagic environments, basing on fossil record. They do believe that this was driven by a terrestrial mechanism led by climate and oceanic circulation, without proposing an extraterrial cause.

In 1984, paleontologists David Raup and Jack Sepkoski published a paper claiming that they had identified a statistical periodicity in extinction rates over the last 250 million years using various forms of time series analysis. They focused on the extinction intensity of fossil families of marine vertebrates, invertebrates, and protozoans, identifying 12 extinction events over the time period in question. The average time interval between extinction events was determined as 26 million years. At the time, two of the identified extinction events (Cretaceous–Paleogene and Eocene–Oligocene) could be shown to coincide with large impact events. Although Raup and Sepkoski could not identify the cause of their supposed periodicity, they suggested a possible non-terrestrial connection. The challenge to propose a mechanism was quickly addressed by several teams of astronomers.

In 2010, Melott & Bambach re-examined the fossil data, including the now-improved dating, and using a second independent database in addition to that Raup & Sepkoski had used. They found evidence for a signal showing an excess extinction rate with a 27-million-year periodicity, now going back 500 million years, and at a much higher statistical significance than in the older work.

At any rate, the periodicity of extinction events is still debated in the paleontological community. For example, some recent works claimed that the periodicity is not statistically relevant.

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