JOURNEY TO THE END OF THE EARTH
Tishani Doshi
Questions and Answers
1. ‘The world’s geological history is trapped in
Antarctica: How is the study of this region useful to us?
Ans: The world’s geological history is trapped in
Antarctica. In the past, around 650 million years ago, India and Antarctica
were part of a supercontinent named Gondwana. The climate was favourable for
the huge variety of flora and fauna to thrive. Later several land masses
drifted away from it to form some of the continents that exist today. A cold
circumpolar current was created. It made Antarctica frigid. All these events of
history are embedded in the age old carbon records of Antarctica.
2. What are Geoff Green’s reasons for including
high school students in the Students on Ice expedition?
Ans: Students on Ice is a programme that aims at taking high school
students to the ends of the world and providing them with inspiring educational
opportunities which will help them foster a new
understanding for our planet. It’s been in operation for six years. This
programme is headed by Canadian Geoff Green.
Geoff thinks that taking students to Antarctica is more fruitful than
carting celebrities and rich. He wants to give the future generation of
policy-makers a life-changing experience at an age when they’re ready to
absorb, learn, and act. He wants to give them a first-hand experience of ice
shelves melting and collapsing which may offer them a clue to the stark future
of life on earth.
3. ‘Take care of the small things and the big
things will take care of themselves.’ What is the relevance of this statement
in the context of the Antarctic?
Ans: Antarctica has a special ecosystem which gives a
big scope to study the delicate nature of our environment. The author
exemplifies this through very small single celled plants called phytoplankton
which feed and sustain the entire southern ocean’s food chain. These
phytoplanktons absorb carbon and synthesise various organic compounds through
photosynthesis. These micro-organisms can survive only in low degree of
temperature. But, depletion of ozone layer and rise of global warming are
giving alarming treats to the very existence of these organisms. Extinction of
phytoplanktons will have far reaching consequences in our ecosystem.
So, human beings are expected to take care of all
living beings including the tiny forms of flora and fauna to prevent the
depletion of ozone layer by reducing carbon emissions. If we take care of small
things big things will automatically fall into place
3. Why is Antarctica the place to go to, to
understand the Earth’s present, past and future?
Ans: For those
who study and examine the Earth’s present, past and future, Antarctica is the
ideal place to go.
To visit Antarctica is to be a part
of the earth’s past history. We come to know that about 650 million years ago
there was a giant super-continent in the south. It was called Gondwana. India
and Antarctica were parts of the same landmass-Gondwana. Things were quite
different then. Human had not arrived on the earth. The climate of Antarctica
was much warmer. Dinosaurs became extinct. The age of mammals started. The
landmass was forced in to be separated into countries as they exist today. Geological
history is trapped inside the ice layers in Antarctica.
Present unfurls in front of our eyes
when we see glaciers melting and ice-caps falling. We can relate them to the
results of global warming.
Antarctica also warns us for the
future. It tells us how little changes in the environment can have big
repercussions. Phytoplanktons nourish and sustain the entire Southern Ocean’s
food chain. Further depletion in the ozone layer would affect the lives of all
the marine animals and birds of the region and the global carbon cycle. It
could also lead to the end of the world. In this way it suggests future
possibilities about our planet.
There is no place in the Earth
except Antarctica where we can find the records of present, past and future.
Thus, Antarctica is the perfect place to go to, to understand the earth’s
present, past and the future.
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