| Evolutionary Catastrophes: the Science of Mass Extinction | |||||
| Vincent Courtillot | |||||
| Cambridge Univ Press, 173 pages | |||||
| A review by Peter D. Tillman
Well -- the Chicxulub impact at the KT boundary, 65 million years (my) ago, is indeed well-documented. What's less well-known is that the
Deccan Traps, an enormous outpouring of flood-basalts in what is now western India -- over 2 million cubic km(!) of lava,
along with billions of tons of SO2, CO2, HCl, and
other toxics -- were also in full eruption then. In fact, the famous
KT iridium-signature has recently been identified in Deccan interflow sediments.1 From recent radiometric
dating, it looks like all of the Deccan eruptions occurred within a brief, 0.7 my time-span. The biggest and most
violent eruptions apparently occurred within a few thousand years of the KT boundary; individual flows of several
thousand cubic km of basalt were common.
Compare this to the largest historic 'flood'-basalt eruption: Laki in Iceland produced 12 cu. km of lava in
1783-84. The SO2 and other gases that Laki erupted, destroyed most of the island's crops and forage.
Then 50-80% of the island's livestock, and about one quarter of the Icelandic people, starved to death. Laki lowered global
temperatures by about 1 deg. C (from fine-particle ash and sulfur aerosols).
Extrapolating to a 5,000 cu. km flood-basalt eruption, the average global temperature might decrease by
around 7 deg. C (13 deg. F). The volcanic HCl emissions could destroy most
of the ozone layer,2 dramatically
increasing UV at the surface, and injuring or killing many organisms. The familiar volcanogenic
"toxics" -- F, As, Sb, Hg, Se etc. -- would poison nearby life. And the
volcanic SO2 and HCl would cause severe acid-rain
damage as they were washed out of the atmosphere. Then, repeat this disaster with the next big eruption, over and over
again, a dozen or more times in the next 10,000 years or so. The total 'kill factor' would very likely be greater than
that from the Chicxulub impact, albeit spread out over tens or hundreds of thousands of years. And a more gradual die-off
is a better fit to the known fossil record.
So it turns out that the volcanists and the meteor-strike proponents were both right, at least for the KT
mass-extinction. The combination of the Chicxulub strike with the Deccan mega-eruption turned an 'ordinary'
mass-extinction into the second-worst ever.
And thoroughly muddied the scientific waters while this was being worked out. Once again, reality trumps
fiction -- Nemesis atop Shiva!
But, for the 10 or so "big" mass-extinctions known,3 seven are of the same age as major flood-basalt
eruptions, vs. one or two with major same-age impacts. And those two meteor-strikes coincide with massive
flood-basalt eruptions -- no major mass-extinction appears to be solely impact-caused. So it's fair to say that
flood-basalts are more deadly to Earthly life than meteor-strikes. And a hazard not amenable to any engineering
solution that I know of -- except being ready to move off the planet, when the next new hot-spot head nears
breakout. Which will come, sure as death.4 An unpleasant reminder of our fragility and vulnerability.
Mea culpa: I'd pretty much taken the "KT impact killed off the dinos" theory as proven -- I didn't even bother to
read the last volcanist counter-argument I saw. As Courtillot notes, I'm hardly the only one to do so. Hey, those
guys are the old fuddy-duddies, right? The stamp-collectors, Luis Alvarez called them. Hence this review, a
'heads-up' to others, and an expiation for me.
Evolutionary Catastrophes is clearly written and is (mostly) accessible
to the general reader.5 This is
the latest chapter in the gradualist vs. catastrophist dialogue that is as old as geologic science.
Writing with great good humour, skepticism, and a love for a scientific tale well-told, Courtillot goes a long way
towards redressing the balance in the hottest earth-science argument at the turn of the 21st century. Highly recommended.
2 If the eruption is powerful enough to inject HCl into the stratosphere. Historic basalt eruptions haven't
done so, but we're talking eruptions 500 times larger than any ever seen....
3 Various authors propose from 5 to about 20 "major" mass- extinction events. There seems (to this non-specialist)
to be a rough consensus for the "Big 5":
http://ga-mac.uncc.edu/faculty/haas/geol3190/termpap/wilson,d/index.html
4 Though, sadly, not so predictable. Hot-spot flare-ups appear to be a deep-seated core-cooling mechanism, with an
unknown, but random, trigger. Average time between breakouts seems to be around 30 my, but the events are far from
regularly-spaced. We really don't know very much about what goes on at the Earth's core.
5 Minor caveats: Courtillot goes a bit overboard (IMO) at times in arguing for vulcanism and against impact. Nor
does he pay quite enough attention to the probable multiple causes of major mass-extinctions. Some of the citations are
incomplete, there's no bibliography, and the index is pretty sketchy.
Pete Tillman has been reading SF for better than 40 years now. He reviews SF -- and other books -- for Usenet, "Under the Covers", Infinity-Plus, Dark Planet, and SF Site. He's a mineral exploration geologist based in Arizona. More of his reviews are posted at www.silcom.com/~manatee/reviewer.html#tillman . | |||||
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