A Global Catastrophe Caused End Cretaceous Extinction

Study of Antarctic Fossils Provides Evidence for Rapid Extinction

The demise of the non-avian dinosaurs, their flying reptile cousins, many marine vertebrates and a whole host of other flora and fauna some 66 million years ago has been well documented.  However, debate still rages over the cause or the causes of this mass extinction event at the Cretaceous-Palaeogene (K-Pg) boundary.  Was this extinction sudden and dramatic, caused by a catastrophic event such as an extraterrestrial impact or was it a gradual decline with many genera becoming extinct but over a longer period of time, perhaps as a result of global climate change?

A new study published recently in the journal “Nature Communications” suggests that the extinctions were rapid.  Analysis of sediment from Seymour Island in the Antarctic Peninsula indicates that there was a rapid and severe decline in marine fauna, this study supports the hypothesis that rather than a slow, gradual decline the K-Pg boundary represents a very rapid mass extinction event.

A Dramatic Reduction in the Number and Variety of Fossils

Antarctic fossil study supports theory of rapid end Cretaceous extinction.

The white strip represents the Cretaceous-Palaeogene boundary.

Picture Credit: Leeds University

Working on the remote Seymour Island in Antarctica, scientists from Leeds University along with researchers from the British Antarctic Survey, mapped and explored a series of highly fossiliferous marine sediments that date from approximately 69 million years ago through to around 65 million years ago.  James Witts, a PhD student in the School of Earth and Environment (Leeds University), lead author of the scientific paper, was instrumental in identifying the various fauna that the 6,000 fossils represented.  It was then a case of ensuring that the fossils were documented in the correct stratigraphic sequence and from this, the researchers were able to conclude that there was a sudden reduction in the number of species living in Antarctic waters some 66 million years ago.  Around two thirds of the species disappear from the fossil record, at a time that coincides with the dinosaur extinction (K-Pg boundary).

In the picture above the K-Pg boundary is represented by the white paper strip.  There is a band of rocks in which no fossils can be found and in younger sediments deposited later, only a handful of different species are represented

Student James commented:

“Our research essentially shows that one day everything was fine, the Antarctic had a thriving and diverse marine community and the next, it wasn’t.  Clearly, a very sudden and catastrophic event had occurred on Earth.  This is the strongest evidence from fossils that the main driver of this extinction event was the after-effects of a huge asteroid impact, rather than a slower decline caused by natural changes to the climate or by severe volcanism stressing global environments.”

A Rich and Diverse Maastrichtian Marine Ecosystem

This study is the first to conclude that the mass extinction that marked the end of the dinosaurs, pterosaurs and many other forms of life, was a truly global event and that it was just as sudden in high latitudes as it was in lower latitudes.  In short, the polar ecosystems were hammered too.

The fossils from the Late Maastrichtian strata that pre-date the extinction event indicate a rich and highly diverse marine food web populated by a huge array of molluscs such as gastropods, bivalves and cephalopods.  In turn, there were large numbers of different types of fish, the fish shared the shallow sea with a variety of marine reptiles including Mosasaurs.  Numerous soft bodied organisms such as sea slugs, anemones, starfish and jelly fish would also have been present but their remains are not frequently preserved as fossils.  One of the more peculiar molluscs known from the Upper Cretaceous rocks of Seymour Island is the giant ammonite Diplomoceras.  This invertebrate, related to modern day cuttlefish and squid had a shell that uncoiled to a large extent.  It resembled a two-metre long paper clip.  Although Diplomoceras fossils are found in rocks older than 66 million years, just like the rest of the ammonites, its fossils are absent in rocks laid down in the Palaeogene Epoch.

An Illustration of the Bizarre Ammonite Diplomoceras

Diplomoceras (ammonite) illustration.

The bizarre Late Cretaceous ammonite Diplomoceras.

Picture Credit: James McKay

Although the majority of ammonites had coiled shells, a number of families evolved in the Early Cretaceous with shells that were uncoiled to varying degrees.  In 2012, Everything Dinosaur wrote an article detailing research undertaken by scientists from the Natural History Museum of Vienna that provided an explanation for this adaptation.

To read more: Unravelling the Mystery of the Unravelling Ammonite

A Rich and Diverse Marine Fauna – Prior to the Extinction Event

Seymour Island Late Cretaceous fossils.

A rich and diverse marine fauna preserved in the strata of Seymour Island.

Picture Credit: Leeds University

Everything Dinosaur acknowledges the help of Leeds University in the compilation of this article.  This blog post has also been constructed with reference to the academic paper: “Macrofossil evidence for a rapid and severe Cretaceous–Paleogene (K–Pg) mass extinction in Antarctica”, published in the journal Nature Communications in May 2016.

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