William Buckland
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William Buckland DD, FRS (12 March 1784 – 14 August 1856) was an English theologian, geologist and palaeontologist.
His work in the early 1820s proved that Kirkdale Cave in North Yorkshire had been a prehistoric hyena den, for which he was awarded the Copley Medal. It was praised as an example of how scientific analysis could reconstruct events in the distant past. He pioneered the use of fossilised faeces in reconstructing ecosystems, coining the term coprolites. Buckland also wrote the first full account of a fossil dinosaur, which he named Megalosaurus in 1824.
Buckland followed the Gap Theory in interpreting the biblical account of Genesis as two widely separated episodes of creation. It had emerged as a way to reconcile the scriptural account with discoveries in geology suggesting the earth was very old. Early in his career Buckland believed he had found evidence of the biblical flood, but later saw that the glaciation theory of Louis Agassiz gave a better explanation, and played a significant role in promoting it.
Buckland served as Dean of Westminster from 1845 until his death 1856.
Early life
Buckland was born at Axminster in Devon<ref name=EB>Chisholm, 1911</ref> 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 Early Jurassic Lias rocks exposed in local quarries.
He was educated first at Blundell's School, Tiverton, Devon, and then at Winchester College, from where he won a scholarship to Corpus Christi College, Oxford, matriculating in 1801 and graduating BA in 1805.<ref>Template:Alox2</ref> He also attended lectures of John Kidd on mineralogy and chemistry, developed an interest in geology, and carried out field research on strata during his vacations.<ref name=EB/> He went on to obtain his MA degree in 1808, became a Fellow of Corpus Christi in 1809, and was ordained as a priest. He continued to make frequent geological excursions, on horseback, to various parts of England, Scotland, Ireland and Wales.
In 1813, Buckland was appointed Reader in mineralogy, in succession to John Kidd, giving lively and popular lectures with increasing emphasis on geology and palaeontology. As an unofficial curator of the Ashmolean Museum, he built up collections, touring Europe and coming into contact with scholars including Georges Cuvier.
Career, work and discoveries
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.<ref>Template:Cite web</ref>
From his investigations of fossil bones at Kirkdale Cave, in Yorkshire, 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 recognised by the keeper of the Menagerie at Exeter 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.<ref>Template:Cite journal</ref>
While criticised 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.<ref name="Rudwick2005">Rudwick, Martin Bursting The Limits of Time: The Reconstruction of Geohistory in the Age of Revolution (2005) pp. 622–638, 631</ref> 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.<ref name="Rudwick2005"/>
While Buckland's analysis convinced him that the bones found in Kirkdale Cave had not been washed into the cave by a global flood, he still believed the thin layer of mud that covered the remains of the hyaena den had been deposited in the subsequent 'Universal Deluge'.<ref name="Rudwick2005"/> He developed these ideas into his great scientific work Reliquiæ Diluvianæ, or, Observations on the Organic Remains attesting the Action of a Universal Deluge<ref>Reliquiæ Diluvianæ, or, Observations on the Organic Remains attesting the Action of a Universal Deluge</ref> which was published in 1823 and became a best seller. However, over the next decade as geology continued to progress Buckland changed his mind. 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.<ref>Template:Cite book</ref> By 1840 he was very actively promoting the view that what had been interpreted as evidence of the 'Universal Deluge' two decades earlier, and subsequently of deep submergence by a new generation of geologists such as Charles Lyell, was in fact evidence of a major glaciation.
Megalosaurus

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 was elected a Foreign Honorary Member of the American Academy of Arts and Sciences.<ref name=AAAS>Template:Cite web</ref> That year he 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 Church, a rich reward for academic distinction without serious administrative responsibilities.
Marriage
In December 1825 he married Mary Morland of Abingdon, 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 daughter, author Elizabeth Oke Buckland Gordon, wrote a biography of her father that included appendices of positions held by Buckland, his membership in professional societies, and an index of his publications.
The Red Lady of Paviland
On 18 January 1823 Buckland walked into Paviland Cave in south Wales, where he discovered a skeleton which he named the Red Lady of Paviland,<ref>A Field Guide to the English Clergy Butler-Gallie, F. p. 94: London, Oneworld Publications, 2018 Template:ISBN</ref> as he at first supposed it to be the remains of a local prostitute.<ref>Sommer, Marianne Bones and ochre: the curious afterlife of the Red Lady of Paviland (2007) p. 1</ref> Although Buckland 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.<ref>Rudwick, Martin Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform (2008) pp. 77–79</ref>
Carbon-data tests have since dated the skeleton, now known to be male as from circa 33,000 years before present (BP).<ref>Template:Cite journal</ref> It is the oldest anatomically modern human found in the United Kingdom.
Coprolites and the Liassic food chain

The fossil hunter Mary Anning 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 Regis. She also noted that if such stones were broken open they often contained fossilised fish bones and scales, and sometimes bones from small ichthyosaurs. These observations by Anning led Buckland to propose in 1829 that the stones were fossilised faeces. He coined the name coprolite for them; the name came to be the general name for all fossilised faeces.
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 Liassic 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 the distant past.<ref>Rudwick, Martin Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform pp. 154–155.</ref> 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.<ref>Gordon, Mrs [Elizabeth Oke] The life and correspondence of William Buckland, D.D., F.R.S. (1894) pp. 116–118</ref> He also discussed other similar objects found in other formations, including the fossilised 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.<ref>Rudwick, Martin Worlds Before Adam: The Reconstruction of Geohistory in the Age of Reform p. 155.</ref>
Buckland had been helping and encouraging Roderick Murchison for some years, and in 1831 was able to suggest a good starting point in South Wales for Murchison's researches into the rocks beneath the secondary strata associated with the age of reptiles. Murchison would later name these older strata, characterised by marine invertebrate fossils, as Silurian, after a tribe that had lived in that area centuries earlier.<ref>Template:Harvnb</ref> In 1832 Buckland presided over the second meeting of the British Association, which was then held at Oxford.
Bridgewater Treatise

Buckland was commissioned to contribute one of the set of eight Bridgewater TreatisesTemplate:Broken anchor, "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.<ref>Retrieved 2 August 2018.</ref> His volume included a detailed compendium of his theories of day-age, gap theory and a form of progressive creationism where faunal succession revealed by the fossil record was explained by a series of successive divine creations that prepared the earth for humans.<ref>Template:Harvnb</ref> In the introduction he expressed the argument from design by asserting that the families and phyla of biology were "clusters of contrivance":
The myriads of petrified Remains which are disclosed by the researches of Geology all tend to prove that our Planet has been occupied in times preceding the Creation of the Human Race, by extinct species of Animals and Vegetables, made up, like living Organic Bodies, of 'Clusters of Contrivances,' which demonstrate the exercise of stupendous Intelligence and Power. They further show that these extinct forms of Organic Life were so closely allied, by Unity in the principles of their construction, to Classes, Orders, and Families, which make up the existing Animal and Vegetable Kingdoms, that they not only afford an argument of surpassing force, against the doctrines of the Atheist and Polytheist; but supply a chain of connected evidence, amounting to demonstration, of the continuous Being, and of many of the highest Attributes of the One Living and True God.
Following Charles Darwin's return from the Beagle voyage, Buckland discussed with him the Galapagos land iguanas and Marine iguanas.<ref name=Letter359>Template:Cite web</ref> 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.<ref name=Letter404>Template:Cite web</ref>
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 the 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 Switzerland, 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 Glasgow 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<ref>Daily Telegraph Issue no 50,404 dated 10 June 2017 p33 > "The Abbey dean who ate the heart of a king"</ref> (he succeeded Samuel Wilberforce). Soon after, he was inducted to the living of Islip, near Oxford, a preferment attached to the deanery. As Dean and head of Chapter, Buckland was involved in repair and maintenance of Westminster Abbey 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 Museum and, in 1848, he was awarded the Wollaston Medal by the Geological Society of London.
Illness and death
Around the end of 1850, William Buckland contracted a disorder of the neck and brain, and died of it in 1856.<ref name="Art1933">Template:Cite book</ref> Frank Buckland reported that an autopsy showed "the portion of the base of the skull upon which the brain rested, together with the two upper vertebrae of the neck, to be in an advanced state of caries, or decay. The irritation...was quite sufficient cause to give rise to all symptoms." Frank Buckland attributed the cause of death of both his parents to a severe accident years earlier.<ref>Template:Cite book</ref>
The plot for William's 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 Whately's Elegy intended for Professor Buckland written in 1820:
Known eccentricities
Buckland preferred to do his field palaeontology and geological work wearing an academic gown.<ref name=ODNB>Template:Harvnb</ref> His lectures were notable for their dramatic delivery.<ref name="oumBuckland">Template:Cite web</ref> When he lectured indoors he would bring his presentations to life by imitating the movements of the dinosaurs under discussion.<ref>Burke, Peter (18 April 2013). A Social History of Knowledge II: From the Encyclopaedia to Wikipedia: 2 (Kindle Location 2276). Wiley. Kindle Edition.</ref> Buckland's passion for scientific observation and experiment extended to his home, where he had a table inlaid with dinosaur coprolites. The original table top is exhibited at the Lyme Regis Museum.<ref>"William Buckland's Coprolite Table" Lyme Regis Museum Template:Webarchive</ref><ref name="bp news">Harry Hogger "19th century table created out of fossil poo recreated for descendants of original owner" Bridport News" 30 July 2013</ref>
Not only was William Buckland's home filled with specimens – animal as well as mineral, live as well as dead<ref name=":2" /> – but he claimed to have eaten his way through the animal kingdom. Reportedly according to an anecdote recounted by Augustus Hare, the most distasteful animals Buckland consumed were in his opinion mole and bluebottle fly.<ref name=":0">Template:Cite book</ref> Ostrich,<ref>Template:Cite book</ref> hedgehogs, mice, frogs and snails, were among other animals reportedly served to guests.<ref name=":1">Template:Cite book</ref><ref name=":2">Template:Cite news</ref> Buckland was followed in this hobby by his son Frank.<ref name=":1" /><ref name=":2" />
One story recounted by Peter Lund Simmonds in 1859 reports that Buckland served soup to his guests before claiming that it was an alligator that he had dissected earlier that day, to the guests significant discomfort. When asked if he had really served an alligator, he reportedly responded "as good a calf's head as ever wore a coronet".<ref>Template:Cite book</ref>
According to one story, Buckland consumed, perhaps unintentionally, a portion of the mummified heart of the French King Louis XIV during a dinner at Nuneham House,<ref>Template:Cite web</ref> though the veracity of this particular story has been questioned.<ref>Template:Cite web</ref><ref>Template:Cite book</ref> The Louis XIV heart story goes back at least as far as an 1863 book by Nathaniel Hawthorne.<ref>Template:Cite book</ref>
Charles Darwin criticised Buckland for his behaviour in his autobiography, saying that "Buckland, who though very good-humoured and good-natured, seemed to me a vulgar and almost coarse man. He was incited more by a craving for notoriety, which sometimes made him act like a buffoon, than by a love of science."<ref>Template:Cite journal</ref>
Legacy
Dorsum Buckland, a wrinkle ridge on the Moon, is named after him. Buckland Island (known today as Ani-Jima), in the Bonin Islands (Ogasawara-Jima), was named after him by Captain Beechey on 9 June 1827. In 1846, William Buckland was rector of St. Nicholas in Islip and is commemorated on a plaque in the south aisle of the church and the "East Window" was dedicated to the memory of Buckland and his wife in 1861.<ref>Template:Cite book</ref> A plaque is dedicated to him near his summer home by the Old Rectory, The Walk, Islip (10 August 2008). There is also a bust by Henry Weekes in the south aisle at Westminster Abbey.<ref>'The Abbey Scientists' Hall, A.R. p53: London; Roger & Robert Nicholson; 1966</ref>
In 1972, botanist Heikki Roivainen circumscribed Bucklandiella, a genus of moss in the family Grimmiaceae, which was named in his honour.<ref>Template:Cite book</ref> Buckland Peaks in New Zealand's Paparoa Range was named after him.<ref>Template:Cite book</ref>
The Iñupiat village of Buckland (Template:Langx) in Alaska's Northwest Arctic Borough takes its English name from William Buckland, being named by Royal Navy officer Frederick William Beechey in 1826.
See also
Notes
References
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Further reading
External links
Template:Commons category Template:Wikiquote
- Buckland at the Oxford University Museum of Natural History Template:Webarchive
- Buckland's blue plaque in Islip
- William Buckland in Retrospect
- The Life and Correspondence of William Buckland... By his daughter, Mrs. Gordon Template:Webarchive, (London : J. Murray, 1894) – digital facsimile available from Linda Hall Library
- William Buckland (1823) Reliquiæ Diluvianæ Template:Webarchive (English) – digital facsimile available from Linda Hall Library. A number of high-resolution images of the maps and other illustrations from this book are available hereTemplate:Dead link.
Template:Natural history Template:GLS Presidents Template:Copley Medallists 1801-1850 Template:Deans of Westminster
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