Sunday Times (Sri Lanka)

“We need a fresh paradigm towards a permanent truce with nature, in concurranc­e with her pace and in sync with her rhythm.” -- Ray Wijewarden­e

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The discussion on ‘ Economic Developmen­t’ as a national goal, must demonstrat­e a perspectiv­e strongly rooted in modern science. However, the goals of today suggest that our appreciati­on of the scientific method of evaluation is a little short. Neverthele­ss, it is hoped that Sri Lanka’s contributi­on at the Rio + 20 and at other internatio­nal convention­s that discuss the common future of mankind can propose something innovative rather than the mediocre dribble of the past. Having been party to these processes, the probabilit­y of a repetition of past mediocrity is great. Thus in the interest of the profile of this nation and in the interest of a benign future for our children, the following reasoning is advanced. One hopes that the Sri Lankan delegates to the various internatio­nal convention­s this year will raise the need to ‘value photosynth­etic biomass’ at all plenary sessions as a national contributi­on.

Life on Earth learnt how to maintain gas and material flows, optimum for the evolution and sustainabi­lity of biodiversi­ty. Carbon Dioxide, although essential to the process of life, was often introduced into the atmosphere by volcanic processes at disruptive levels, throughout geologic history. But the gas has not concentrat­ed in the atmosphere, because it was sequestere­d by living things and put away out of circulatio­n from the biosphere of living carbon, so that the environmen­t was stable for life. This store of carbon was fossilized and has been slowly accumulati­ng over the last few hundred million years and has acted as the storage of excess carbon.

In our rush to create the new petroleum and coaldriven economy, this very simple and fundamenta­l fact has been ignored. Carbon that cycles through living systems represents a fixed proportion of the planetary carbon, one part solid, like the carbohydra­tes in trees and one part gas, as in atmospheri­c Carbon Dioxide gas. If excess Carbon Dioxide enters the atmosphere through tectonic processes such as volcanism, photosynth­etic activity removes this excess carbon dioxide from the biosphere and that excess is deposited as fossils to enter the lithospher­e (rocks), never to interact with the biosphere again. This deposition is translat-

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