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The Very Rev. Dr William Buckland DD FRS (12 March 1784 – 14 August 1856) was an English geologist, palaeontologist and Dean of Westminster, who wrote the first full account of a fossil dinosaur, which he named Megalosaurus. His work proving that Kirkdale Cavemarker had been a prehistoric hyaena den, for which he was awarded the Copley Medal, was widely praised as an example of how detailed scientific analysis could be used to understand geohistory by reconstructing events from deep time. He was a pioneer in the use of fossilized feces, for which he coined the term coprolites, to reconstruct ancient ecosystems. Buckland was a proponent of Old Earth creationism, who later became convinced of Louis Agassiz' glaciation theory.

Early life and university

Buckland was born at Axminstermarker in Devonmarker and, as a child, would accompany his father, the Rector of Templeton and Trusham, on his walks where interest in road improvements led to collecting fossil shells, including ammonites, from the Jurassic lias rocks exposed in local quarries.

He was educated at Blundell's Schoolmarker and won a scholarship in 1801, to study for the ministry at Corpus Christi College, Oxfordmarker, also attending the lectures of John Kidd on mineralogy and chemistry, as well as developing an interest in geology and carrying out field research on strata, during vacations. Having taken his BA in 1804, he went on to obtain his MA degree in 1808. He then became a Fellow of Corpus Christi in 1809, was ordained as a priest and continued to make frequent geological excursions, on horseback, to various parts of England, Scotlandmarker, Irelandmarker and Walesmarker. In 1813, he was appointed reader in mineralogy, in succession to John Kidd, giving lively and popular lectures with increasing emphasis on geology and palaeontology. As (unofficial) curator of the Ashmolean Museummarker, he built up collections, touring Europe and coming into contact with scientists including Georges Cuvier.

Rejection of flood geology and Kirkdale Cave

In 1818, Buckland was elected a fellow of the Royal Society. That year he persuaded the Prince Regent to endow an additional Readership, this time in Geology and he became the first holder of the new appointment, delivering his inaugural address on 15 May 1819. This was published in 1820 as Vindiciæ Geologiæ; or the Connexion of Geology with Religion explained, both justifying the new science of geology and reconciling geological evidence with the biblical accounts of creation and Noah's Flood. At a time when others were coming under the opposing influence of James Hutton's theory of uniformitarianism, Buckland developed a new hypothesis that the word "beginning" in Genesis meant an undefined period between the origin of the earth and the creation of its current inhabitants, during which a long series of extinctions and successive creations of new kinds of plants and animals had occurred. Thus, his catastrophism theory incorporated a version of Old Earth creationism or Gap creationism. Buckland believed in a global deluge during the time of Noah but was not a supporter of flood geology as he believed that only a small amount of the strata could have been formed in the single year occupied by the deluge.

From his investigations of fossil bones at Kirkdale Cavemarker, in Yorkshiremarker, he concluded that the cave had actually been inhabited by hyaenas in antediluvian times, and that the fossils were the remains of these hyaenas and the animals they had eaten, rather than being remains of animals that had perished in the Flood and then carried from the tropics by the surging waters, as he and others had at first thought. In 1822 he wrote:

It must already appear probable, from the facts above described, particularly from the comminuted state and apparently gnawed condition of the bones, that the cave in Kirkdale was, during a long succession of years, inhabited as a den of hyaenas, and that they dragged into its recesses the other animal bodies whose remains are found mixed indiscriminately with their own: this conjecture is rendered almost certain by the discovery I made, of many small balls of the solid calcareous excrement of an animal that had fed on bones... It was at first sight recognized by the keeper of the Menagerie at Exter Change, as resembling, in both form and appearance, the faeces of the spotted or cape hyaena, which he stated to be greedy of bones beyond all other beasts in his care.


While criticized by some, Buckland's analysis of Kirkland Cave and other bone caves was widely seen as a model for how careful analysis could be used to reconstruct the earth's past, and the Royal Society awarded Buckland the Copley Medal in 1822 for his paper on Kirkdale Cave. At the presentation the society's president, Humphry Davy, said:
by these inquiries, a distinct epoch has, as it were, been established in the history of the revolutions of our globe: a point fixed from which our researches may be pursued through the immensity of ages, and the records of animate nature, as it were, carried back to the time of the creation.


While Buckland's analysis convinced him that the Bones found in Kirkdale Cave had not been washed into the cave by a global deluge, he still believed it was such a flood that buried them under a layer of fine silt. He developed these ideas into his great scientific work Reliquiæ Diluvianæ, or, Observations on the Organic Remains attesting the Action of a Universal Delugewhich was published in 1823 and became a best seller. However, over the next decade as geology continued to progress Buckland changed his mind, and in his famous Bridgewater Treatise, published in 1836, he acknowledged that the biblical account of Noah's flood could not be confirmed using geological evidence.

Megalosaurus and marriage

He continued to live in Corpus Christi College and, in 1824, he became president of the Geological Society of London. Here he announced the discovery, at Stonesfield, of fossil bones of a giant reptile which he named Megalosaurus (great lizard) and wrote the first full account of what would later be called a dinosaur.

In 1825, Buckland resigned his college fellowship: he planned to take up the living of Stoke Charity in Hampshire but, before he could take up the appointment, he was made a Canon of Christ Churchmarker, a rich reward for academic distinction without serious administrative responsibilities. In December of that year he married Mary Morland of Abingdonmarker, Oxfordshire, an accomplished illustrator and collector of fossils. Their honeymoon was a year touring Europe, with visits to famous geologists and geological sites. She continued to assist him in his work, as well as having nine children, five of whom survived to adulthood. His son Frank Buckland became a well-known practical naturalist, author, and Inspector of Salmon Fisheries. On one occasion, Mary helped him decipher footmarks, found in a slab of sandstone, by covering the kitchen table with paste, while he fetched their pet tortoise and confirmed his intuition, that tortoise footprints matched the fossil marks.

His passion for scientific observation and experiment extended to his home life. Not only was his house filled with specimens – animal as well as mineral, live as well as dead – but he claimed to have eaten his way through the animal kingdom: zoophagy. The most distasteful items were mole and bluebottle; panther, crocodile and mouse were among the other dishes noted by guests. Augustus Hare, a famous English raconteur and contemporary, recalled, “Talk of strange relics led to mention of the heart of a French King preserved at Nuneham in a silver casket. Dr. Buckland, whilst looking at it, exclaimed, ‘I have eaten many strange things, but have never eaten the heart of a king before,’ and, before anyone could hinder him, he had gobbled it up, and the precious relic was lost for ever.” The heart in question is said to have been that of Louis XIV. Buckland was followed in this bizarre hobby by his son Frank.

In 1826 Buckland discovered the Red Lady of Pavilandmarker in Walesmarker, which remains the oldest anatomically modern human found in the United Kingdom. Although he found the skeleton in Paviland Cave in the same strata as the bones of extinct mammals (including mammoth), Buckland shared the view of Georges Cuvier that no humans had coexisted with any extinct animals, and he attributed the skeleton's presence there to a grave having been dug in historical times, possibly by the same people who had constructed some nearby pre-Roman fortifications, into the older layers.

Coprolites and the Lias food chain

The fossil hunter Mary Anning had noticed that stony objects known as "bezoar stones" were often found in the abdominal region of ichthyosaur skeletons found in the Lias formation at Lyme Regismarker. She also noted that if such stones were broken open they often contained fossilized fish bones and scales as well as sometimes bones from small icthyosaurs. These observations by Anning lead Buckland to propose in 1829 that the stones were fossilized feces and coin the name coprolite, which came to be the general name for all fossilized feces, for them. Buckland also concluded that the spiral markings on the fossils indicated that ichthyosaurs had spiral ridges in their intestines similar to those of modern sharks, and that some of these coprolites were black because the ichthyosaur had ingested ink sacs from belemnites. He wrote a vivid description of the liasic food chain based on these observations, which would inspire Henry De la Beche to paint Duria Antiquior, the first pictorial representation of a scene from deep time. After De le Beche had a lithographic print made based on his original watercolour, Buckland kept a supply of the prints on hand to circulate at his lectures. He also discussed other similar objects found in other formations, including the fossilized hyena dung he had found in Kirkdale Cave. He concluded:
In all these various formations our Coprolites form records of warfare, waged by successive generations of inhabitants of our planet on one another: the imperishable phosphate of lime, derived from their digested skeletons, has become embalmed in the substance and foundations of the everlasting hills; and the general law of Nature which bids all to eat and be eaten in their turn, is shown to have been co-extensive with animal existence on our globe; the Carnivora in each period of the world's history fulfilling their destined office, — to check excess in the progress of life, and maintain the balance of creation.
He had been helping and encouraging Roderick Murchison for some years and in 1831 was able to suggest a very good starting point in South Wales for Murchison's researches into the rocks which he later described in great detail in his 'The Silurian System'. In 1832 he presided over the second meeting of the British Association, which was then held at Oxford.

Bridgewater Treatise

He was commissioned to contribute one of the set of eight Bridgewater Treatises, "On the Power, Wisdom and Goodness of God, as manifested in the Creation". This took him almost five years' work and was published in 1836 with the title Geology and Mineralogy considered with reference to Natural Theology. His section was a detailed compendium of his theories of day-age, gap theory and theistic evolution. In response, computing pioneer Charles Babbage produced his "Ninth Bridgewater Treatise".

Following Charles Darwin's return from the Beagle voyage, Buckland discussed with him the Galapagos Land Iguanas and Marine Iguanas. He subsequently recommended Darwin's paper on the role of earthworms in soil formation for publication, praising it as "a new & important theory to explain Phenomena of universal occurrence on the surface of the Earth—in fact a new Geological Power", while rightly rejecting Darwin's suggestion that chalkland could have been formed in a similar way.

Glaciation theory

By this time Buckland was a prominent and influential scientific celebrity and a friend of the Tory prime minister, Sir Robert Peel. In co-operation with Adam Sedgwick and Charles Lyell, he prepared the report leading to establishment of the Geological Survey of Great Britain.

Having become interested in the theory of Louis Agassiz, that polished and striated rocks as well as transported material, had been caused by ancient glaciers, he travelled to Switzerlandmarker, in 1838, to meet Agassiz and see for himself. He was convinced and was reminded of what he had seen in Scotland, Wales and northern England but had previously attributed to the Flood. When Agassiz came to Britain for the Glasgowmarker meeting of the British Association, in 1840, they went on an extended tour of Scotland and found evidence there of former glaciation. In that year Buckland had become president of the Geological Society again and, despite their hostile reaction to his presentation of the theory, he was now satisfied that glaciation had been the origin of much of the surface deposits covering Britain.

In 1845 he was appointed by Sir Robert Peel to the vacant Deanery of Westminster (he succeeded Samuel Wilberforce). Soon after, he was inducted to the living of Islipmarker, near Oxford, a preferment attached to the deanery. As Dean and head of Chapter, Buckland was involved in repair and maintenance of Westminster Abbeymarker and in preaching suitable sermons to the rural population of Islip, while continuing to lecture on geology at Oxford. In 1847, he was appointed a trustee in the British Museummarker and, in 1848, he was awarded the Wollaston Medal, by the Geological Society of London.

Around the end of 1849, he contracted a disease which increasingly invalided him until his death in 1856. Post-mortem examination identified a tubercular infection of the upper cervical vertebrae which had spread to the brain. The plot for his grave had been reserved but, when the gravedigger set to work, it was found that an outcrop of solid Jurassic limestone lay just below ground level and explosives had to be used for excavation. This may have been a last jest by the noted geologist, reminiscent of Richard Whatley’s Elegy intended for Professor Buckland written in 1820:
Where shall we our great Professor inter
That in peace may rest his bones?
If we hew him a rocky sepulchre
He’ll rise and break the stones
And examine each stratum that lies around
For he’s quite in his element underground


See also

  • Earl of Bridgewater for other Bridgewater Treatise
  • The Great Chain of History: William Buckland and the English School of Geology 1814-1849. by Nicolaas Rupke. Oxford University Press. 1983.
  • Dorsum Buckland, a wrinkle ridge on the Moon named after him.
  • Buckland Island (known today as Ani-Jima), in the Bonin Islands (Ogasawara-Jima), named after Professor Buckland by Captain Beechey in 9 June 1827.
  • History of paleontology for more on his contributions to the development of that field.


References



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