© James Wheeler Available from www.souvenirpixels.com/photo-blog/campsite-milky-way-view
or https://flic.kr/p/hd2nyz
Life is not easy, but to create
life is even harder. The igniter of life depends on numerous factors. Up till
now, the only place where life is found in the big universe is the Earth. However,
the universe is just too big that this does not make sense at all. Let us start
a journey to the space and explore the planets outside our Earth!
What makes the KEY? – The organic matters
Life starts with organic matters,
which are some chemicals making up every tissue and cell, as well as
controlling the growth of the living things on Earth. Professor Sun Kwok, Dean
of the Faculty of Science in HKU, is famous in explaining the formation of
planetary nebulae as well as the composition of stellar dusts. In his newest
publication in 2015, he has mentioned that over 60 kinds of gas-phase molecules
have been identified in the planetary nebulae and circumstellar envelope of an evolved
star through spectroscopic observation, notably the organic molecules[i].
His article has placed emphasis
on the evidence shown on the pre-solar meteorites that solids can be
transferred from one evolved star to the Sun across the galaxy. These pre-solar
grains may contain diamond, corundum, etc. Such evidence could be linked to the
spectroscopic data of the chemicals in the planetary nebulae as well. These
perhaps indicate that the possibility lives on earth were not solely synthesized
through combining the elements in the atmosphere with the famous Miller-Urey
process, but also of exotic origin. In other words, life could have been
generated from the organic matter delivered from another part of the universe.
An example of meteorite
© PhOtOnQuAnTiQuE Available
from https://flic.kr/p/8T9s8G
Prerequisite of life – a wonderful environment for living, though of
high rareness
Stars could generate organic
matter. However, when it comes to the discussion of sustainable lives, a stable
and habitable environment is necessary. Such environment is rare, but wonderful
for organisms to live forever, while Earth is an excellent but the only known example.
Planets situated in the habitable
zone are able to receive adequate but not too much amount of radiation from
their parent stars to maintain the water in liquid state on their surfaces. Liquid water is crucial for organisms to stay alive.
Functions like regulating body temperature and transferring hemoglobin show the
significant importance of water. Spotting out the habitable zone therefore would
be a giant leap for exploring lives outside the Earth.
Dr. R. Brasser, a Taiwan-based
scientist, has been studying the habitable zone for many years. In his recent
papers published in 2014 and 2015, he has applied the Milankovitch cycles to
the field of research for long term behavior of potential habitable planets[i].
Milankovitch cycles were proposed
by Serbian scientist Milutin Milankovic in 1940s. He suggested that both
orbital eccentricity and obliquity of the Earth changes periodically in 41,000
and 100,000 years respectively[ii].
Planets do not necessarily revolve around a star in circular orbit. It could be
elliptical. The less circular the orbit is, the higher the orbital eccentricity.
Meanwhile, for the obliquity, it has challenged our common sense that the
tilting of the rotational axis of the Earth in fact fluctuates from 21 degrees
to 24 degrees in its cycle.
You can imagine, when you intend
to boil a large bowl of water, someone suddenly moves it away from the stove, the
water could not be heated up as a result, it may even cool down! Same case
occurs if you incline the bowl. Only part of it will be heated. This disturbs
the water convection a lot.
Then, let us turn the eyes to
planetary scale. In fact, it is all the same. Water is an excellent heat
capacitor, any change in ways of receiving energy could affect its internal
activity in the container. Cloud pattern and precipitation style will vary a lot,
making the climate fluctuate from the pleasant one to the harsh one periodically.
© Space.com
Dr. Brasser has investigated one
of the candidates of the habitable planets called HD 40307g located 42 light
years away from usii. First, because of its high orbital eccentricity,
most of the time throughout its orbiting would be away from the habitable zone.
What therefore implies is the incoming solar radiation varies significantly, where
ice age would occur regularly and intensely on this planet. Second, along with its
low obliquity, the climatic mechanism would not allow sufficient heat to
transfer from the equatorial region to the polar region. Polar cap may form
which further worsens the habitability of the planet, not to mention that the
positive feedback mechanism would make the planet looks like a snowball in the
later stage.
In short, you may find that a good
environment is required for organic matter to be converted into a life, but it
is very rare in the big universe. However, the rare chance may have occurred
twice in our amazing solar system.
A potentially habitable place for organisms – Europa, Jupiter’s fourth
largest moon
The 4.2 AU-far Europa-Jupiter system
from our mother Earth is always one of the popular candidates of habitable
planets. One major difference for Europa to be distinguished from other
candidates is, it is just too close to us that only eight-year travelling time
is required under current technology.
Observation of Jupiter and its
moons by a simple telescope
© Tsz-yeung Tang
Europa is the fourth largest moon
of Jupiter. The snowwhite satellite is not only appealing but also famous of
containing a global ocean of water beneath the ice crust. Additionally, through
spectroscopic observation, oxygen is detected on its surface[i].
With these two elements, has the probability of life ever existed there?
Planetary scientist Veronica J.
Bray had led his transnational team to respond to the myth of crustal thickness
by measuring the extent of viscous relaxation during numerous strikes of asteroids[ii].
The work came to disclosure in 2014. Measuring crustal thickness is crucial in
proving the existence of geological activities on Europa.
Older calculation shows that if
Europa has a crustal thickness below 10 km, there will be plate tectonic[iii],
which allows the ejection of the liquid water to the surface to make the
surface warmer and more habitable.
Plate tectonic is doomed as the
most essential mechanism in sustaining the biosphere on earth. Nutrients are
released to supply our need while gases are expelled to keep us warm. The huge
volcanic events also help regulating the climate. This mechanism can only work
when the crust is situated on a fluid (but accurately, in short time scale,
what we see may have no difference to solid for many planets) with certain
flexibility provided. It cannot work neither the crust is too thick nor too
thin. Don’t you see our Earth is just too lucky to have the intermediate one?
© NASA/JPL-Caltech/SETI
Institute
Bray’s work can be explained by
an old-school toy, paper clay. When you drop an object to the wet clay, an
imprint will form. Later, it will solidify and leave a remarkable imprint
behind. Nevertheless, the depth of the imprints depends on the flexibility of
the bottom part of the clay – how watery it is. As mentioned, the mantle part
would behave like fluid while the crust part would behave like solid.
Definitely, there is a gentle and continuous change from crust to mantle,
though, scientists can still pin a more accurate mark on it through years-long
effort.
Example of paper clay with
imprints on it
Say, for 10 km below the surface,
if that region is more ductile and plastic, the greater extent of viscous
relaxation for the crust thus makes the asteroids pressing deeper on the crust
when it bombards the surface, and vice versa. Consequently, the crust should be
defined thinner. The measurement on the extent of viscous relaxation thus could
help defining the crust-mantle boundary.
From the extent of viscous
relaxation, Bray deduces that the crustal thickness of Europa is 7 kmv,
which is lower than the maximum allowed thickness for plate tectonic.
Such discovery helped the
scientists to prove the volcanic origin of the cracks imaged by the Galileo
spacecraft. This study acts as an encouragement for Europa-Jupiter System
Mission (EJSM) to obtain more data in the 2020s[i].
Possibilities on the discovery of microorganisms on the satellite exist
currently. Europa, the pure satellite, would probably be the second proven
habitable place in the solar system very soon.
Being a little organism in the
universe, human still have great dreams towards our enormous universe. They may
just be just too curious on their uniqueness at the time, or they find
themselves too fragile when facing the risk. They need alternatives. And they
need a better environment. In turn, curiosity and crises will keep on driving
us deeper in the universe!
MORE TO
READ
[i] Kwok
S. Organic Compounds in Circumstellar and Interstellar Environments. Springer
Netherlands. 2015 Feburary [accessed:2015 April 25]; http://link.springer.com/article/10.1007%2Fs11084-015-9410-0.
doi: http://dx.doi.org/10.1007/s11084-015-9410-0
[ii]
Brasser R, Ida S, Kokubo E. A dynamical study on the habitability of
terrestrial exoplanets–II The super-Earth HD 40307 g. Monthly Notices of the Royal
Astronomical Society. 2014; 440(4): 3685-3700.
[iii]
Milankovitch M. Canon of the Earth radiation and its application to the ice age
problem [Kanon der Erdebestrahlung und seine Anwendung auf das Eiszeitenproblem].
Royal Serbian Academy [Königlich Serbische Akademie]. 1941.
[iv]
Hall DT, Strobel DF, Feldman PD, McGrath MA, Weaver HA. Detection of an oxygen
atmosphere on Jupiter's moon Europa.Nature.1995[accessed2015April25];373:677-679.
http://www.nature.com/nature/journal/v373/n6516/abs/373677a0.html. doi:
10.1038/373677a0
[v]
Veronica JB, Gareth SC, Joanna VM, Melosh HJ, Paul MS. Hydrocode simulation of
Ganymede and Europa cratering trends – How thick is Europa’s crust?. Icarus.
2014; 231:394-406.
[vi]
McKinnon WB. Convective instability in Europa’s floating ice shell. Geophysical
Research Letter. 1999; 26(7):951–954.
[vii]
EJSM-Laplace home page. European Space Agency. c2012. [accessed 2015 April 25].
http://sci.esa.int/ejsm-laplace/.
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