Did One or Two Impacts Kill the Dinosaurs?
Note: Late post today. I am covering the in-patient service and more time constrained than usual.
By now most people know that the dinosaurs (now clarified as non-avian dinosaurs), along with 85% of species alive at the time, became extinct 65.5 million years ago as a result of a massive meteor impact. This is almost certainly the impact crater at Chicxulub, which dates to the correct time. In addition, examination of fossils and geological layers centers this extinction event at Chicxulub.
This is referred to at the K-T extinction, referring to the end of the Cretaceous and beginning of the Tertiary periods. However, use of the designation “Tertiary” is being phased out, and the K-T extinction is now being referred to as the K-Pg extinction – for Cretaceous-Paleogene.
While the single impact theory is the current consensus, there are two significant if minority competing theories. One is the Deccan Traps flood basalts – a 200 thousand year long event spanning the K-Pg boundary that involved massive volcanic eruptions, which could have causes extinctions through release of dust and sulfuric aerosols into the atmosphere. While not dead, this hypothesis has not fared well under recent evidence and is supported by only a small minority of paleontologists.


Skeptics and parallel rationalist communities spend a lot of time on “inside baseball” — jargon-filled debates about technical matters that seem incomprehensible, dull, or ridiculous to outsiders. These shouldn’t be the main skeptical topics (shouldn’t we be busy solving mysteries and educating the public?) but some discussion on these matters is unavoidable and worthwhile. Many movement-oriented skeptics and organizations have things they hope to accomplish; with goals, there comes discussion of best practices.


