Can the world survive the daisy-tramplers?

Can the world survive the daisy-tramplers?

Image by NASA (Public Domain)

Originally published 30 March 1992

What a win­ter! The snow shov­el nev­er came out of the shed until after St. Pad­dy’s Day. A few swipes with a broom was almost all it took to keep the dri­ve­way and walks clear.

Is this the much bal­ly­hooed green­house effect? Is the plan­et warm­ing up because we are pump­ing too much car­bon diox­ide into the atmos­phere? Are more snow­less win­ters to be expected?

Don’t throw your snow shov­el away just yet.

First, vari­a­tions from the norm will occur even in the absence of green­house warm­ing. Sec­ond, even if the plan­et is get­ting warmer no one knows for cer­tain what the long-range effects will be. Some cli­ma­tol­o­gists say we’ll have less snow because of warmer tem­per­a­tures on land; oth­ers say we’ll have more snow because more water vapor will be evap­o­rat­ed from warmer seas.

All of these sce­nar­ios for cli­mate change are based upon com­put­er sim­u­la­tions of the huge­ly com­pli­cat­ed envi­ron­ment — so huge­ly com­pli­cat­ed, in fact, that it is dif­fi­cult to have much con­fi­dence in any­thing the com­put­ers pre­dict for our future.

The one thing most cli­ma­tol­o­gists have in com­mon is pre­dic­tion of dis­as­ter. Some say the ice­caps will melt and flood low-lying coasts. Oth­ers say the ice caps will grow and leave coastal cities high and dry. Some say fer­tile parts of the earth will become drought-strick­en dust bowls. Oth­ers pre­dict fer­tile lands will become water-logged with rain.

We can take our pick of disasters.

One sci­en­tist who is rather less pes­simistic that the rest is James Love­lock, the orig­i­na­tor of the so-called Gaia Hypoth­e­sis (Gaia was the Greek god­dess of the Earth). This states that the bios­phere — the sys­tem of all liv­ing things, some­times called sim­ply “Gaia” — active­ly keeps the glob­al envi­ron­ment com­fort­able for life. In oth­er words, life is capa­ble of main­tain­ing its envi­ron­ment in an approx­i­mate­ly con­stant state.

Love­lock illus­trates his idea with a com­put­er sim­u­la­tion called Daisy­world. Daisy­world is an imag­i­nary plan­et with only two com­pet­ing species of life, white daisies and dark daisies. Like all organ­isms, the daisies have an ide­al range of tem­per­a­tures at which they will thrive. If too hot, they wilt. If too cold, they fail to blossom.

The tem­per­a­ture of Daisy­world, as with Earth, depends upon how much heat is received from its sun and how much is radi­at­ed back into space. If the tem­per­a­ture of the plan­et ris­es above the com­fort­able range for some rea­son, the white daisies do mar­gin­al­ly bet­ter because they reflect sun­light and keep their imme­di­ate envi­ron­ment cool. The dark daisies do less well. There­fore, the sur­face of the plan­et becomes whiter, more sun­light is reflect back to space, and the tem­per­a­ture cools.

If the tem­per­a­ture falls below the opti­mum range, the dark daisies, which absorb more heat from the sun, thrive at the expense of white daisies. The sur­face of the plan­et becomes dark­er, more sun­light is absorbed, and the tem­per­a­ture rises.

Thus, life on Daisy­world acts as a kind of ther­mo­stat, main­tain­ing the tem­per­a­ture of the plan­et approx­i­mate­ly constant.

Love­lock believes that life on Earth does the same thing. He imag­ines the bios­phere exist­ing in a kind of sym­bi­ot­ic rela­tion­ship with the oceans and atmos­phere — con­nect­ed to the envi­ron­ment by a vast sys­tem of feed­back loops. For exam­ple, if the lev­el of car­bon diox­ide in the atmos­phere increas­es, then life responds in such a way as to reduce the lev­el of that gas. Accord­ing to Love­lock, for almost 4 bil­lion years, as life evolved, it has main­tained the phys­i­cal and chem­i­cal con­di­tions of the oceans and atmos­phere at com­fort­able lev­els — even repair­ing the envi­ron­ment after such cat­a­stroph­ic dis­rup­tions as major mete­orite impacts.

Many sci­en­tists find Love­lock­’s views unac­cept­able, or mean­ing­less. Dar­win­ian biol­o­gists argue that there is no con­ceiv­able mech­a­nism of nat­ur­al selec­tion that would cause such a self-reg­u­lat­ing sys­tem to evolve. Oth­ers accuse Love­lock of per­son­i­fy­ing a pure­ly phys­i­cal sys­tem, endow­ing Gaia with pur­pose and fore­thought. Gaia is a fig­ment of his imag­i­na­tion, they say, more akin to reli­gion than science.

For myself, I rather like the notion of Gaia, and have no trou­ble imag­in­ing a bio-phys­i­cal sys­tem that responds in the way that Love­lock pro­pos­es. And, if Love­lock is right, you and I may be liv­ing in a kind of Daisy­world that has the capac­i­ty to restore devi­a­tions from the norm — and per­haps even frus­trate or delay cat­a­stroph­ic glob­al warming.

The big ques­tion is: Are human inter­ven­tions in the envi­ron­ment occur­ring faster than Gaia’s abil­i­ty to bring things back into bal­ance? Feed­back loops that worked over bil­lions of years may fal­ter and fail in the face of mas­sive envi­ron­men­tal changes caused by reck­less appli­ca­tions of tech­nol­o­gy. Even if the bios­phere is capa­ble of repair­ing envi­ron­men­tal dam­age, it can pre­sum­ably do so only on a time scale that will be of lit­tle con­so­la­tion to present gen­er­a­tions of humans.

For the time being, at least, we should keep our ears open to the crit­ics of Gaia and prophets of doom. Daisy­world may indeed be a love­ly metaphor for Earth. But Daisy­world might not be able to main­tain itself so pleas­ant­ly con­stant if we add to that hypo­thet­i­cal plan­et a third species with a capac­i­ty for tech­nol­o­gy — and an unchecked propen­si­ty to tram­ple daisies.


In the three decades since this essay was first writ­ten, obser­va­tion­al evi­dence for cat­a­stroph­ic cli­mate change has sig­nif­i­cant­ly increased, and sci­en­tif­ic sup­port for the Gaia hypoth­e­sis has reced­ed. ‑Ed.

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