One of the most well known debates in science is that over what
caused the extinction of the dinosaurs. During the extinction
about 65 million years ago, dinosaurs weren't the only creatures
to perish: scientists estimate that over 70% of all life on earth
came to an end. This widespread loss of diversity is referred
to as the K-T event, or Cretaceous-Tertiary Mass Extinction, so
named because of its place on the geologic time scale at the very
end of the Cretaceous
period.
Explanations for the extinction were for many years provided
by two competing theories: that the global effects of either increased
volcanism or the effects of a large object (asteroid or comet)
impact created conditions too harsh for most life on earth. Chicxulub
crater, first detected by offshore oil exploration conducted by
Petroleos Mexicanos in the 1970s was not immediately identified
as a crater, due in part to its burial beneath a kilometer of
Cenozoic limestones.
It wasn't until the early 1990s that it was recognized as the
site of a massive impact, at least 180 km (112 miles) wide, 65
million years ago. Estimates put the size of the asteroid or comet
at 10 to 20 km (6.2 to 12.4 miles) in width. Its impact would
have created huge tsunamis, earthquakes, and winds; it would also
have released gases and debris into the atmosphere, thereby darkening
the sky, lowering temperatures and creating acid rain. The temporal
correlation combined with strong geochemical evidence, lends great
weight to the impact theory as the cause of the K-T event.