[sci.bio] Mass Extinction in the Cretaceous

g-rh@cca.UUCP (04/11/87)

	Enquiring minds want to know mechanisms were supposedly involved
in the Cretaceous mass extinction event.  The following is a summary 
drawn from "The Great Dying", previously mentioned on the net.

THE EVENT

	A meteorite hits the Earth.  It may have been an Apollo object
(solid, rocky or metallic, asteroid) or a comet head (big ice ball with
lots of gravel).  Size of the meteorite was on the order of 10 kilometers
diameter.  Mass on the order of a trillion (10^12) metric tons.  Impact
speed 15-40 kilometers per second.  Energy of impact 200 million megatons
of TNT.  Mortality patterns imply that the strike was in the Northern
hemisphere spring, probably in April.  The strike was probably in the
Northern hemisphere.

IMMEDIATE EFFECTS

If it was a water strike about 5000 cubic kilometers of water was 
injected into the atmosphere.  In any case most of the energy of impact
is taken up by the surface (land or ocean bottom).  The impact crater
was about 200 kilometers diameter.  A large amount of extraterrestrial
material was distributed world wide.  About a billion tons of NO molecules
were generated from the impact.  Dust and cloud cover create total 
darkness for about two months.  The ozone layer is wiped out for a
period of 1-10 years.  There are world wide forest fires.

Acid rain (NO molecules rapidly oxidize to form NO2, NO3, and nitrous
and nitric acid in turn) wipes out most of the ocean one celled life.
This is augmented by darkness (for the northern hemispher particularly)
and run off from decaying dead biota in the land masses.  CO2 levels
rise sharply (drastically less plant life) with a green house effect
that brings the average temperature up about 5 degree centigrade.

RECOVERY

The recovery period runs about 50000 years.  Plant life recovers
in about 2000 years.  Rain flushes the acid waters into the ocean
where there are in turn neutralized by lime deposits.  There is
strong selection for plankton species that can thrive in acidic
water.  In the initial recovery period plant life is dominated by
plants which propogate by air born spores (e.g. ferns) with the
flowering plants making a later recovery and resuming their dominance.

Many species die out during the massive mortality of the event itself
and the immediate aftermath.  A substantial number of species that
were typically cretaceous died out in the recovery period.  The
typically tertiary species multiply rapidly and by the end of the
recovery period occupy all of the new niches.

Temperatures drop substantially during the recovery period once the
CO2 surplus is mopped up by recovering plant life.  Extinction of the
remaining cretaceous species occurs because of the heavy environmental
stresses and because of the drastically altered ecology.  The new
tertiary species are descendents of minor species that were better
qualified to survive under the hard times of the event and the early
recovery period.


-- 

Richard Harter, SMDS Inc. [Disclaimers not permitted by company policy.]