Beyond Buckland

DISCOVERING YORKSHIRE’S ANCIENT BEASTS


By Susan Newell

Susan Newell is a doctoral student researching the teaching collections of William Buckland, the first Professor of Geology at Oxford who taught from 1813 to 1849. She reminds us here about Buckland’s role 200 years ago in interpreting the important Pleistocene discoveries being celebrated this year, and the way that Mary Morland, a talented local naturalist, and many others, contributed to making this new knowledge.


This year marks the 200th anniversary of a great advance in our understanding of the geological past… a story which begins in the nineteenth century, with the discovery of a bone-filled cave in Kirkdale, Yorkshire. 

Uncovered by local quarrymen in 1821, the discovery of the Kirkdale cave and its contents of mysterious bone was the source of much intrigue. When news of the discovery reached William Buckland, Professor of Geology at Oxford University, he decided to travel up North to visit the site. However, by the time Buckland arrived at the cave, local collectors had scooped up most of its contents. Nonetheless, he was able to retrieve and examine some of the cave’s remaining material, which led him to an astonishing conclusion — Yorkshire must once have been home to hyaenas, elephants, hippopotamus and rhinoceros, and what was now known as the Kirkdale cave was once a hyaenas’ den.

W. B. Conybeare, lithograph, ‘The Hyaena’s Den at Kirkdale near Kirby Moorside in Yorkshire, discovered A.D. 1821’. Reproduced by kind permission of Christ Church, Oxford.
This light-hearted reconstruction of the hyaenas’ den shows Buckland illuminating the scene, in every sense. It is thought to be the first visual reconstruction of the pre-human past.

Central to Buckland’s theories were some small white balls that he had found amongst the debris in the cave. Buckland sent these balls to William Wollaston, a celebrated chemist based in London, for analysis.  He also asked Wollaston to visit the zoo at Exeter Exchange in London and show the balls to the hyaena’s keeper there.  Together with the results from Wollaston’s chemical analyses, the keeper confirmed Buckland’s hypothesis — the balls were droppings from animals very similar to modern hyaenas. Meanwhile, the anatomist William Clift was able to identify the bones from the Kirkdale cave as belonging to other extinct species related to those found living in tropical countries today. Buckland concluded that the cave must have been a den for ancient hyaenas, who would drag parts of the dead animals they had found (or killed) inside and, after feeding on them, leave piles of bones and droppings behind.

In order to strengthen his theory, Buckland discussed the behaviour of hyaenas in the wild with army officers connected to Britain’s colonial expansion in India. These officers also sent Buckland fresh specimens captured by local people. When a travelling menagerie visited Oxford in 1822, Buckland took the opportunity to experiment; feeding bones to a hyaena and noting that the teeth marks matched those on the fossilised bones from the cave.

Buckland’s findings were something of a shock to his contemporaries. When lecturing, he employed several different methods to try and convince his audiences that his theories were true. This included presenting fossil specimens and bones from living species for comparison, and showing maps, diagrams and drawings. Mary Morland contributed some of these illustrations, including large drawings of living animals, and technical drawings of bones that were later engraved for use in Buckland’s publications. Mary’s Kirkdale drawings seem to have been the first that she produced for William before the couple married in 1825.

Fossil hyaena jaw in the Museum’s collection, possibly the one featured in the engraving alongside it. Engraving is by James Basire after a drawing by Mary Morland. Published in William Buckland’s article in the Royal Society’s journal (1822) on the Kirkdale cave discoveries. [1]

Buckland’s work on the Kirkdale cave was revolutionary, not least because he was the first to make a scientific study of a cache of bones of this type.  Although similar bones from ‘tropical’ species had previously been found in Northern Europe, people thought that they had been washed up by a catastrophic flood, believed by many to be the biblical Noah’s Flood.  Modern analysis has now allowed us to deduce that the bones date to an Interglacial period when Britain was joined to Europe and had a hot climate, about 120,000 years ago.  

Here at the Museum, Buckland’s collections and archives are as much of a treasure trove as the Kirkdale cave. It is through accessing these archives that we can learn about the surprising range of people who contributed to the emergence of new scientific knowledge from the Kirkland cave — quarrymen, collectors, zookeepers, chemists, anatomists, colonial officers in India, workers in India, and artists like Mary Morland. To find out more about the incredible legacy of the Kirkdale Cave, look out for ‘Kirkdale200 – Lost Beasts of the North’, a symposium organised by the Yorkshire Fossil Festival, 12th March 2022.

Mary Morland, watercolour and gouache, lecture illustration of a hippopotamus, signed ‘MM’.
Hippopotamus bones were found at Kirkdale cave in Yorkshire, but as there were no living hippos to be seen in Britain at the time, this drawing would have been a valuable teaching aid.

[1] William Buckland, ‘Account of an Assemblage of Fossil Teeth and Bones of Elephant, Rhinoceros, Hippopotamus, Bear, Tiger, and Hyaena, and Sixteen Other Animals; Discovered in a Cave at Kirkdale, Yorkshire, in the Year 1821: With a Comparative View of Five Similar Caverns in Various Parts of England, and others on the Continent’, Phil. Trans., 2 (1815-30), 165-167.

Snakeflies: Monsters in the Shadows of the Dinosaurs


Header Image: A reconstruction of a delta-estuarine environment in northern Spain during the Cretaceous, habitat of the studied amber snakeflies, by William Potter Herrera.


Post by William Potter Herrera, Undergraduate Student at Portsmouth University


About 105 million years ago, in what is now Cantabria, Spain, rich cycad and conifer forests flourished across a landscape of estuaries and weaving deltas, bordering the then subtropical North Atlantic. While marine crocodiles prowled the waterways and theropod dinosaurs stalked the fern clearings, another ferocious, albeit smaller, predator ruled. Snakeflies, or raphidiopterans, are still around today but their diversity and range is a fraction of what it was during the Mesozoic, the period when the dinosaurs reigned.

Left: Map of the world 105 million years ago, with ancient Cantabria highlighted. Author: William Potter Herrera, based on work from “The Planetary Habitability Laboratory” at UPR Arecibo. Right: An extant snakefly from OUMNH’s pinned collections.

Snakeflies get their name from their long ‘necks’ and ovipositors — the latter being a long, thin tube that females use to deposit eggs into the safety of crevices. Snakeflies are voracious predators, using their compact jaws to devour anything smaller than them. Their unusual necks allow them to pursue prey into tight spaces. No Cretaceous bug would have been safe from these monsters that existed in the shadows of the dinosaurs.

Working in the shadow of the Museum’s very own dinosaur during a bursary project last summer, I got a very real experience of paleontological research. Insects might not be the first thing you think of when considering fossils, but the sheer diversity and beauty of preservation these organisms exhibit in the fossil record made them a delight to work on. Nowhere is this more true than in the remarkable amber of northern Spain. Under the supervision of Dr Ricardo Pérez-de la Fuente, I examined, described and mapped out four specimens of amber which contained insects, our focus being on snakeflies. Through careful comparison with previous work, we discovered a new species of Necroraphidia, meaning “snakefly of the dead”. This genus was previously known from a specimen preserving no more than its characteristic wings, but the new specimen is nearly completely preserved, frozen in amber as if time itself stopped.

Left: William Potter Herrera examines a snakefly preserved in amber. Right: Necroraphidia arcuata, a snakefly species from El Soplao amber (Cantabria, Spain). The arrow points to a fragment of burnt plant matter (extracted from Pérez-de la Fuente et al., 2012. Zookeys 204).

The story of how the snakeflies ended up in the amber is as fascinating as the creatures themselves. Amber begins its life as tree resin — a highly sticky, viscous fluid extruded by conifers in response to trauma. Insects and other small arthropods are frequently trapped in it, either being caught by it as it flows downwards, or simply flying into it. Because larger insects are more likely to free themselves there is a bias in the fossil record towards smaller organisms. In northern Spain, however, the amber is remarkably rich in insects and also tiny fragments of burnt plant matter, indications that the insects might have become entombed during, or in the aftermath of, raging wildfires that drove them into a disoriented frenzy.

It was studying these charred fragments that inspired my dissertation on fossil charcoal — and that was one of just many benefits I gained from this bursary. It cannot be overstated how brilliant the opportunity to dedicate six weeks to study in a Museum was; exploring behind the scenes and talking to world experts in every field. The confidence gained from being entrusted to conduct this research so independently at such an early stage of my career will serve me going forward. The work was not easy but the support I received was brilliant. Even now, months later, as we work together to finalise our manuscript, I am inspired by the dedication and belief that Ricardo and the whole staff at the OUMNH have shown in me.