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About three years ago Catherine de Berg and I published a short
article in Nature in which we attempted to explain why the
chemistry of the atmosphere of the Earth is today so completely
different from that of our two neighbor ing planets, Mars and
Venus. Our atmosphere is composed mainly of N2 and O with traces of
A, H0, CO , 0 , etc. , while the atmospheres of both 2 2 2 3 Mars
and Venus are almost entirely made up of CO , Also, the Earth
appears 2 to be the only one ofthe three planets which has oceans
ofliquid water on the surface. Since the presence of liquid water
on Earth is probably an essential requirement for life to have
originated and evolved to its present state, the question of the
apparent absence ofliquid water on Mars and Venus suddenly acquires
significant proportions. In our paper in Nature, and later in a
more detailed discussion of the subject (Planetary Atmospheres, in
Exobiology, edited by C. Ponnamperuma, North Holland Publishing Co.
), we tried to describe why we believe that in the early history of
the solar system all the terrestrial planets lost the atmospheres
of H2 and He which they had acquired from the solar nebula at the
time of their formation. These planets, completely devoid of atmos
pheres, like the Moon today, started accumulating new gases which
were exhumed from the interior by the commencement of volcanic
activity.
I was born in a rich Muslim family in India in 1930 and got Koranic
education at home until the age of nine. Recently I retired from
NASA as a Chief Scientist. How did it happen, it is a long story
full of suspense and adventure and that is what this book is all
about.
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