TOP 10 EXTINCTION EVENTS
My Top 10 Geological Time Periods leads me naturally to my Top 10 Extinction Events – the latter being identified by the former
It always intrigues me how the evolution of life on Earth consistently seems to be dragging itself up by its bootstraps, or to mix metaphors, consistently a process of two steps forward and one step back. The steps back are of course extinction events.
These recurring extinction events are so striking as to make me ponder how complex life survived at all, particularly as the evolution of complex life is compressed into the last 10% or so of the planet’s history. If the history of the Earth was scaled to a single year, complex life only emerges in the last couple of months or so of the year (with the dinosaurs in about mid-December and us a few minutes or so before midnight on 31 December).
Sure, simple or microbial life emerged relatively early in the planet’s history, pretty much when the planet had cooled enough for it, but complex life really only took off in the Cambrian Period 541 to 485 million years ago although it had preceded that period. Thereafter however complex life seems to have been regularly hammered with extinction events in the periods after that – hence making one ponder how it survived at all. I suppose once life reached a certain threshold of diverse and complex life, it was a matter of bouncing back – particularly if you have millions of years to do it.
“An extinction event (also known as a mass extinction or biotic crisis) is a widespread and rapid decrease in the biodiversity on Earth. Such an event is identified by a sharp fall in the diversity and abundance of multicellular organisms.”
When it comes to extinction events, the focus of attention is on the so-called Big Five, followed by a proposed sixth such event – so no prizes guessing as to six entries in my top ten. The Big Five originate from “a landmark paper published in 1982”, in which “Jack Sepkoski and David M. Raup identified five particular geological intervals with excessive diversity loss”.
So here are my Top 10 Extinction Events, as a shallow dip top ten.
(1) CRETACEOUS–PALEOGENE / K-PG
(66 MILLION YEARS AGO – 75% OF SPECIES)
This is the big one – not the deadliest but the most dramatic and famous of all extinction events, the one that killed the dinosaurs, brought about by the impact of a 10-20 km wide asteroid at Chicxulub in Mexico. Formerly known as the K-T or Cretaceous-Tertiary extinction event from the previous name for the Paleogene Period – I still prefer it as catchier.
(2) PERMIAN-TRIASSIC
(252 MILLION YEARS AGO – 90-95% SPECIES)
This is the real big one – the biggest as in deadliest extinction event in Earth’s history, as indicated by its colloquial name of the Great Dying – estimated to have wiped out 90-95% of all marine species, although land species (which included amphibians and reptiles) may have been luckier. Volcanic eruptions in Siberia are hypothesized as the primary cause, with widespread climate change including ocean acidification and acid rain. Alas, poor trilobites!
(3) ORDOVICIAN-SILURIAN
(444 MILLION YEARS AGO – 85% SPECIES)
Once I got the most famous extinction event out of the way, I’m ranking the Big Five by order of deadliness in terms of extinction rates. Life had crawled or swam its way up with the Great Ordovician Biodiversity Event – perhaps even with the first arthropods on land – only for the planet to punch it in the guts again, with this extinction event of climate change and glaciation.
(4) TRIASSIC-JURASSIC
(200-201 MILLION YEARS AGO – 80% OF SPECIES)
Well, the dinosaurs can’t complain too much since although they were around beforehand, they got their big break from this extinction event – from climate change (probably volcanic in origin).
(5) DEVONIAN
(360-375 MILLION YEARS AGO – 75% OF SPECIES)
The least deadly of the Big Five extinction events, from global cooling. The Devonian has been dubbed the Age of Fishes, although amphibians were getting started on land, so the saying that there’s more fish in the sea was much less so after this event. It also took aim at the trilobites but they made it through, only to be snagged by the Permian.
(6) HOLOCENE
(PRESENT – ? OF SPECIES)
Yes – it’s our present epoch with its ongoing Holocene extinction, the ranked as the sixth big extinction event to add to the Big Five, because of – ahem – us. Hence the proposed Anthropocene Epoch for us screwing the planet.
(7) GREAT OXIDATION EVENT
(SIDERIAN – RHYACIAN PERIODS 2.60-2.46 BILLION YEARS AGO
“The “Big Five” of the Phanerozoic Eon were anciently preceded by the presumed far more extensive mass extinction of microbial life during the Great Oxidation Event (also known as the Oxygen Catastrophe) early in the Proterozoic Eon”. It’s strange to think of more oxygen in the atmosphere – from microbial life that had evolved photosynthesis – as toxic to the life that preceded it even at much lower levels than our own atmosphere but there you are.
As extinction events are measured by the fossil record of complex life, that precludes identifying extinction events prior to the Phanerozoic Era, as by its nature simple or microbial life tends not to leave a fossil record.
(8) END EDIACARAN
(539 MILLION YEARS AGO)
“At the end of the Ediacaran and just before the Cambrian Explosion, yet another Proterozoic extinction event (of unknown magnitude) is speculated to have ushered in the Phanerozoic” – that is, our own eon of diverse complex life.
(9) CAMBRIAN & CAMBRIAN-ORDOVICIAN
(513-509, 501-497 & 486 MILLION YEARS AGO)
“Several events in the Cambrian and early Ordovician meet or exceed the “Big Five” in proportional severity.”
There’s the End-Botomian extinctions in the Cambrian 513 to 509 million years ago, the Dresabachian extinction event in the Late or Upper Cambrian 501-497 million years ago, and the Cambrian-Ordovician extinction event 485 million years ago – that last imploding the Cambrian Explosion back a bit and gunning for the trilobites, although they made it through.
(10) LATE PLEISTOCENE
(129,000 – 11,700 YEARS AGO)
Not quite up there with the big extinction events but notable none the less for the extinction of the majority of megafauna, again probably due to, ahem, us. The Late Pleistocene also saw the extinction of all other human species but our own – as well as the spread of modern humans beyond Africa, including to the Americas and Australasia, mapping closely to megafauna extinction.










