El antiguo evento de extinción masiva puede no ser tan extraño después de todo

El antiguo evento de extinción masiva puede no ser tan extraño después de todo

Contrariamente a la creencia de que la extinción masiva del Ordovícico Superior (LOME), que ocurrió hace 443 millones de años y acabó con aproximadamente el 85% de todas las especies, fue causada principalmente por una edad de hielo de corta duración, un nuevo estudio sugiere que el calentamiento también jugó un papel importante.

El evento de extinción masiva del Ordovícico superior (LOME) se ha considerado durante mucho tiempo extraño en comparación con otros eventos de extinción masiva en la historia de la Tierra. A diferencia de casi todas las demás fases importantes de extinción conocidas a partir del registro fósil, parece haber sido provocada por una edad de hielo. Sin embargo, un nuevo estudio muestra que la LOME probablemente estuvo gobernada por mecanismos como los que se ven en la mayoría de los otros eventos, incluido el calentamiento global.

Los libros de texto escritos en los últimos 50 años le dirán que hace 443 millones de años, más del 85% de todos[{» attribute=»»>species disappeared towards the end of the Ordovician Period because of a short-lived ice age in what is known as the oldest and probably second most severe mass extinction event in all of Earth’s history. However, a new study just published in Trends in Ecology and Evolution by researchers of the universities of Copenhagen, Ghent, and California-Berkeley questions this long-standing view because – as the study points out – the massive loss of biodiversity started millions of years earlier than hitherto believed during a warming phase that preceded the well-known glacially associated extinction pulses.

The LOME has long been a bit of a conundrum. Strangely two mass extinction pulses seem associated with the waxing and waning of major ice sheets. This is unique as all other extinction events of similar scale later in the fossil record appear to be associated with global warming – a scenario which is also like that observed during the current biodiversity loss. The new study points out that new, temporally better-resolved fossil biodiversity data through the LOME-event show the extinctions to occur in at least three pules during an up to nine million yearlong interval. This fundamentally changes the Late Ordovician extinction scenario and thus likely also the drivers behind it.


Did volcanoes instigate the Ordovician biodiversity loss?

Within the Earth Sciences community, many hypotheses circulate as to what drove the event. These disagreements are also reflected within the author group of the paper. However, the authors do agree that the classic hypothesis now is outdated and in need of revision. One revised scenario, for instance, suggests the LOME to be associated with some of the largest volcanic eruptions ever recorded in Earth’s history. All evidence points to a much more complex climate history at play during the LOME than previously recognized. And, that extinction triggers could well have been global warming induced by greenhouse gas overloading through volcanic outgassing, as well as deoxygenation of the oceans. Whereas some of this had already been explored for the classic ice age interval, this has not been studied in any detail during this new first wave of the LOME extinctions.

Analogs to the Anthropocene?

Today anthropogenic activities have led to a major loss of biodiversity through first and foremost CO2 overloading of the atmosphere, causing global warming and acidification of global oceans, and habitat loss through overexploitation of natural resources.

The current biodiversity loss occurs at concerning speeds, likely far outpacing most major extinction events known from the fossil record. So, although perhaps still not at the scale of past mass extinctions, the current rates of extinctions are certainly alarming. The new study highlights these differences in extinction rates, arguing that the LOME exhibits some of the same extinction drivers as seen today albeit naturally induced and thus apparently operating at slower temporal scales than the current human-induced biodiversity crisis. However, fossil biodiversity data through extinction events becomes increasingly better temporally resolved and with that, some concerning new evidence is emerging.

Are we currently facing a prolonged biodiversity crisis?

The better-resolved data shows that even though these naturally induced extinctions known from the fossil record may be nested in prolonged million-year phases of biodiversity decline, they are punctuated by sudden, catastrophic extinction pulses of just a few millennia in duration. This new evidence from the fossil record may be an indication that once biodiversity loss accelerates, ecosystems fall out of balance, causing much greater and irreversible disruption. This has a concerning resemblance to what is seen during the past few centuries – not least if this means that we are facing a prolonged, irreversible loss of biodiversity similar to what has occurred previously in Earth’s history.

Reference: “Was the Late Ordovician mass extinction truly exceptional?” by Christian M.Ø. Rasmussen, Thijs R.A. Vandenbroucke, David Nogues-Bravo and Seth Finnegan, 12 May 2023, Trends in Ecology and Evolution.
DOI: 10.1016/j.tree.2023.04.009

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